name | description | link |
Antarctic | Applicable within region south of 66°33´ South. | |
Arctic | Applicable within region north of 66°33´ North. | |
Atlantic Iberic Biscay Irish area | Applicable within maritime region of ocean waters off western Europe | |
Atlantic Ocean | Applicable within maritime region of the Atlantic Ocean | |
Baltic Sea | Applicable within Baltic Sea region | |
Black Sea | Applicable within Black Sea region | |
Continental | Applicable over specified continent. | |
Disaster affected areas | Applicable within specified impact region | |
Disaster risk hotspots | Applicable within specified region of risk | |
EEA33 | Applicable within the 33 EEA member nations | |
EEA38 | ???? | |
EEA39 | Applicable within the 33 EEA member nations and 6 cooperating countries | |
EU member states | Applicable within EU member borders | |
EU27 | Applicable within the 27 EU nations excluding the UK | |
Europe | Applicable within Europe | |
Global | Applicable globally. | |
Global Land | Applicable globally for all solid surfaces | |
Global (outside Europe) | Applicable globally, outside Europe | |
Local | Applicable within the specified sub-national district | |
Marine | ||
Marine / Land | ||
Mediterranean Sea | Applicable within Mediterranean Sea region | |
National | Applicable within the specified country | |
North Atlantic, North West shelf | Applicable within maritime region of the northwest Atlantic Ocean | |
Regional | Applicable within the specified region | |
N/A | Not Applicable | |
Other |
name | description |
Accuracy | The accuracy of the data set is not meeting the requirements |
Availability | The availability of the data set is restricted due to technical or access condition reasons |
Costs | The cost of the data set or service is not sustainable |
Coverage | The coverage of the data set is partial |
Data policy | Access and use condition are too restrictive |
Format | The available format is not exploitable |
Metadata | Missing or incomplete metadata |
Resolution | The spatial resolution is not sufficient |
Support | The access to the data set is not technically supported by the data provider |
Timeliness | The period in between the data collection and data access is too large |
Update Frequency | The data set frequency of updating is lower than the required one |
N/A | Not applicable |
TBD | To be defined |
name | description | link |
Fully | The data set is fully compliant with the requirements | |
Partially | The data does not fully match the requirements | |
None | The data does not match the requirements | |
N/A | Not applicable | |
TBD | To be defined |
acronym | name | service | entrusted entities |
MWR | Micro-Wave Radiometer | Copernicus Space Component |
|
SRAL | Synthetic Aperture Radar Altimeter | Copernicus Space Component |
|
OLCI | Ocean and Land Colour Instrument | Copernicus Space Component |
|
SLSTR | Sea and Land Surface Temperature Radiometer | Copernicus Space Component |
|
SLSTR/OLCI | Sea and Land Surface Temperature Radiometer/Ocean and Land Colour Instrument | Copernicus Space Component |
|
CCC | Climate Change | Copernicus Climate Change Service |
|
EWC | Early Warning | Copernicus Emergency Management Service |
|
BSC | Border Surveillance | Copernicus Security Service |
|
MSC | Maritime Surveillance | Copernicus Security Service |
|
AMC | Atmosphere Monitoring | Copernicus Atmosphere Monitoring Service |
|
MMC | Marine Environment Monitoring | Copernicus Marine Service |
|
TROPOMI | TROPOspheric Monitoring Instrument | Copernicus Space Component |
|
Sentinel-5 | Sentinel-5p | Copernicus Space Component |
|
Se-3-Ocean | Sentinel-3-Ocean | Copernicus Space Component |
|
Sen-3-Land | Sentinel-3-Land | Copernicus Space Component |
|
Priority Area Monitoring | Copernicus Land Monitoring Service |
|
|
Land Cover and Land Use Mapping | Copernicus Land Monitoring Service |
|
|
Bio-geophysical Parameters | Copernicus Land Monitoring Service |
|
|
Satellite Data | Copernicus Land Monitoring Service |
|
|
Reference and Validation Data | Copernicus Land Monitoring Service |
|
|
Ground Motion Monitoring | Copernicus Land Monitoring Service |
|
|
SESA | Support to EU External and Security Actions | Copernicus Security Service |
|
EM | Exposure Mapping | Copernicus Emergency Management Service |
|
RM | On demand Rapid Mapping | Copernicus Emergency Management Service |
|
RR | On demand Risk and Recovery | Copernicus Emergency Management Service |
|
acronym | name | description | website | created_at | updated_at |
CAMS | Copernicus Atmosphere Monitoring Service | The Copernicus Atmosphere Monitoring Service (CAMS) provides continuous data and information on atmospheric composition. The service describes the current situation, forecasts the situation a few days ahead, and analyses consistently retrospective data records for recent years. | http://atmosphere.copernicus.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
CEMS | Copernicus Emergency Management Service | The Copernicus emergency management service (CEMS) provides all actors involved in the management of natural disasters, man-made emergency situations, and humanitarian crises with timely and accurate geo-spatial information derived from satellite remote sensing and completed by available in situ or open data sources. The Copernicus EMS consists of a mapping component and of an early warning component. | http://emergency.copernicus.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
CLMS | Copernicus Land Monitoring Service | The Copernicus land monitoring service (CLMS) provides geographical information on land cover and on variables related, for instance, to the vegetation state or the water cycle. It supports applications in a variety of domains such as spatial planning, forest management, water management, agriculture and food security, etc. The service became operational in 2012 and it consists of three main components: A global component; A Pan-European component; and A local component. | http://land.copernicus.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
CMEMS | Copernicus Marine Service | The Copernicus Marine Service (or Copernicus Marine Environment Monitoring Service) is the marine component of the Copernicus Programme of the European Union. It provides free, regular and systematic authoritative information on the state of the Blue (physical), White (sea ice) and Green (biogeochemical) ocean, on a global and regional scale. The observations and forecasts produced by the service support all marine applications. | http://marine.copernicus.eu/ | Nov. 6, 2017, 11:30 a.m. | Nov. 25, 2022, 12:04 p.m. |
C3S | Copernicus Climate Change Service | The Copernicus Climate Change service (C3S) responds to environmental and societal challenges associated with human-induced climate changes. The service will give access to information for monitoring and predicting climate change and will, therefore, help to support adaptation and mitigation. It benefits from a sustained network of in situ and satellite-based observations, re-analysis of the Earth climate and modelling scenarios, based on a variety of climate projections. The service will provide access to several climate indicators (e.g. temperature increase, sea level rise, ice sheet melting, warming up of the ocean) and climate indices (e.g. based on records of temperature, precipitation, drought event) for both the identified climate drivers and the expected climate impacts. | http://climate.copernicus.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
CSS | Copernicus Security Service | The Copernicus service for Security (CSS) applications aims to support European Union policies by providing information in response to Europe’s security challenges. It improves crisis prevention, preparedness and response in three key areas: Border surveillance; Maritime surveillance; and Support to EU External Action. | http://www.copernicus.eu/main/security | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
CSC | Copernicus Space Component | N/A | N/A | July 12, 2019, 2:24 p.m. | Feb. 24, 2021, 1:27 p.m. |
name | description | link |
Desirable | Availability of data could improve the product. Data are included for redundancy purposes | |
Essential | Product specifications will not be met if essential data are unavailable. | |
Optional | ||
Useful | Additional in situ data not directly linked to product generation, validation or calibration are considered as useful. | |
N/A | Not applicable | |
TBD | To be defined |
flag | code | name |
AF | Afghanistan | |
AFR | Africa | |
AX | ÅLand Islands | |
AL | Albania | |
DZ | Algeria | |
AS | American Samoa | |
AD | Andorra | |
AO | Angola | |
AI | Anguilla | |
AQ | Antarctica | |
AG | Antigua And Barbuda | |
AR | Argentina | |
AM | Armenia | |
AW | Aruba | |
AU | Australia | |
AT | Austria | |
AZ | Azerbaijan | |
BS | Bahamas | |
BH | Bahrain | |
BD | Bangladesh | |
BB | Barbados | |
BY | Belarus | |
BE | Belgium | |
BZ | Belize | |
BJ | Benin | |
BM | Bermuda | |
BT | Bhutan | |
BO | Bolivia, Plurinational State Of | |
BA | Bosnia And Herzegovina | |
BW | Botswana | |
BV | Bouvet Island | |
BR | Brazil | |
IO | British Indian Ocean Territory | |
BN | Brunei Darussalam | |
BG | Bulgaria | |
BF | Burkina Faso | |
BI | Burundi | |
KH | Cambodia | |
CM | Cameroon | |
CA | Canada | |
CV | Cape Verde | |
CAB | Caribbean | |
KY | Cayman Islands | |
CF | Central African Republic | |
TD | Chad | |
CL | Chile | |
CN | China | |
CX | Christmas Island | |
CC | Cocos (Keeling) Islands | |
CO | Colombia | |
KM | Comoros | |
CG | Congo | |
CD | Congo, The Democratic Republic Of The | |
CK | Cook Islands | |
CR | Costa Rica | |
CI | Côte d'Ivoire | |
HR | Croatia | |
CU | Cuba | |
CY | Cyprus | |
CZ | Czech Republic | |
DK | Denmark | |
DJ | Djibouti | |
DM | Dominica | |
DO | Dominican Republic | |
EC | Ecuador | |
EG | Egypt | |
SV | El Salvador | |
GQ | Equatorial Guinea | |
ER | Eritrea | |
EE | Estonia | |
ET | Ethiopia | |
EU | European | |
FK | Falkland Islands (Malvinas) | |
FO | Faroe Islands | |
FJ | Fiji | |
FI | Finland | |
FR | France | |
GF | French Guiana | |
PF | French Polynesia | |
TF | French Southern Territories | |
GA | Gabon | |
GM | Gambia | |
GE | Georgia | |
DE | Germany | |
GH | Ghana | |
GI | Gibraltar | |
GR | Greece | |
GL | Greenland | |
GD | Grenada | |
GP | Guadeloupe | |
GU | Guam | |
GT | Guatemala | |
GG | Guernsey | |
GN | Guinea | |
GW | Guinea-Bissau | |
GY | Guyana | |
HT | Haiti | |
HM | Heard Island And Mcdonald Islands | |
VA | Holy See (Vatican City State) | |
HN | Honduras | |
HK | Hong Kong | |
HU | Hungary | |
IS | Iceland | |
IN | India | |
ID | Indonesia | |
INT | International | |
IR | Iran, Islamic Republic Of | |
IQ | Iraq | |
IE | Ireland | |
IM | Isle Of Man | |
IL | Israel | |
IT | Italy | |
JM | Jamaica | |
JP | Japan | |
JE | Jersey | |
JO | Jordan | |
KZ | Kazakhstan | |
KE | Kenya | |
KI | Kiribati | |
KP | Korea, Democratic People'S Republic Of | |
KR | Korea, Republic Of | |
KW | Kuwait | |
KG | Kyrgyzstan | |
LA | Lao People'S Democratic Republic | |
LV | Latvia | |
LB | Lebanon | |
LS | Lesotho | |
LR | Liberia | |
LY | Libya | |
LI | Liechtenstein | |
LT | Lithuania | |
LU | Luxembourg | |
MO | Macao | |
MG | Madagascar | |
MW | Malawi | |
MY | Malaysia | |
MV | Maldives | |
ML | Mali | |
MT | Malta | |
MH | Marshall Islands | |
MQ | Martinique | |
MR | Mauritania | |
MU | Mauritius | |
YT | Mayotte | |
MX | Mexico | |
FM | Micronesia, Federated States Of | |
MD | Moldova, Republic Of | |
MC | Monaco | |
MN | Mongolia | |
ME | Montenegro | |
MS | Montserrat | |
MA | Morocco | |
MZ | Mozambique | |
XX | Multiple Countries /Not a specific country | |
MM | Myanmar | |
N/A | N/A | |
NA | Namibia | |
NR | Nauru | |
NP | Nepal | |
NL | Netherlands | |
NC | New Caledonia | |
NZ | New Zealand | |
NI | Nicaragua | |
NE | Niger | |
NG | Nigeria | |
NU | Niue | |
NF | Norfolk Island | |
MP | Northern Mariana Islands | |
MK | North Macedonia | |
NO | Norway | |
OM | Oman | |
OTH | Other | |
PK | Pakistan | |
PW | Palau | |
PS | Palestinian Territory, Occupied | |
PA | Panama | |
PG | Papua New Guinea | |
PY | Paraguay | |
PE | Peru | |
PH | Philippines | |
PN | Pitcairn | |
PL | Poland | |
PT | Portugal | |
PR | Puerto Rico | |
QA | Qatar | |
XK | Republic of Kosovo | |
RE | Réunion | |
RO | Romania | |
RU | Russian Federation | |
RW | Rwanda | |
BL | Saint Barthélemy | |
SH | Saint Helena, Ascension And Tristan Da Cunha | |
KN | Saint Kitts And Nevis | |
LC | Saint Lucia | |
PM | Saint Pierre And Miquelon | |
VC | Saint Vincent And The Grenadines | |
WS | Samoa | |
SM | San Marino | |
ST | Sao Tome And Principe | |
SA | Saudi Arabia | |
SN | Senegal | |
RS | Serbia | |
SC | Seychelles | |
SL | Sierra Leone | |
SG | Singapore | |
SK | Slovakia | |
SI | Slovenia | |
SB | Solomon Islands | |
SO | Somalia | |
ZA | South Africa | |
GS | South Georgia And The South Sandwich Islands | |
ES | Spain | |
LK | Sri Lanka | |
SD | Sudan | |
SR | Suriname | |
SJ | Svalbard And Jan Mayen | |
SZ | Swaziland | |
SE | Sweden | |
CH | Switzerland | |
SY | Syrian Arab Republic | |
TW | Taiwan, Province Of China | |
TJ | Tajikistan | |
TZ | Tanzania, United Republic Of | |
TH | Thailand | |
TL | Timor-Leste | |
TG | Togo | |
TK | Tokelau | |
TO | Tonga | |
TT | Trinidad And Tobago | |
TN | Tunisia | |
TR | Turkey | |
TM | Turkmenistan | |
TC | Turks And Caicos Islands | |
TV | Tuvalu | |
UG | Uganda | |
UA | Ukraine | |
AE | United Arab Emirates | |
GB | United Kingdom | |
US | United States | |
UM | United States Minor Outlying Islands | |
UY | Uruguay | |
UZ | Uzbekistan | |
VU | Vanuatu | |
VE | Venezuela, Bolivarian Republic Of | |
VN | Viet Nam | |
VG | Virgin Islands, British | |
VI | Virgin Islands, U.S. | |
WF | Wallis And Futuna | |
EH | Western Sahara | |
YE | Yemen | |
ZM | Zambia | |
ZW | Zimbabwe |
name | description | link |
ASCII | A generic Ascii file | |
Binary | A generic binary file | |
Excel file | An Excel spreadsheet | |
Grid | The grid is a native Esri raster dataset storage format | |
INSPIRE format | ||
Multiple | ||
NetCDF | NetCDF | |
Raster dataset | A raster is a set of cells arranged in rows and columns and is a commonly used dataset in GIS | |
Vector dataset | A coordinate-based data model that represents geographic features as points, lines, and polygons | |
N/A | Not Applicable | |
TBD | To be defined |
name | description | link |
Freely accessible | Data set and information accessible without any fee but than can be subject to re-dissemination policy | |
Full and Open | Data set and information accessible without any fee and supported by redistribution policy | |
Members state/provider data policy | ||
Payment Required | Data set and information accessible only under payment | |
Restricted | Sensitive data set and information accessible only to a restricted gruop of user and/or with restriction in the redistribution | |
N/A | Not Applicable | |
TBD | To be defined |
name | description |
Data Provider | Individual institution, organization or commercial entity that is the originator or the final distributor of the in-situ data. A Data Provider can be part of a wider Data Provider Network. |
Data Provider Network | A network, a group or an association of institutions, organizations or commercial entities supporting the collection, organization and distribution of in situ data. |
Edmo code | Identifier code in the European Directory of Marine Organisations (https://edmo.seadatanet.org/) |
name | description |
Originator | Who is in charge of the creation, updating and maintenance of the data. |
Distributor | Who is responsible for the distribution/supply of the data. The distributor should provide information about the data owner. |
name | description | link |
Analysis | Information obtained by the analysys of remote sensed or collected data set | |
Copernicus Service Product | Data sets with significant in-situ contributions, produced by a Copernicus Service and used by other Copernicus Services for production or validation. | |
Composite | Aggregation of disparate or separate data set or information | |
Forecast | Data set or information calculated in advance | |
Geospatial data | Numerically represent a physical object, events or other features identified by a geographic coordinate system (latitude, longitude). | |
Image | The representation of a portion of the Earth produced by an optical or electronic device. Common examples include remotely scanned data, satellite images, aerial photographs and drone images. An image is stored as a raster dataset of binary or integer values. | |
Map | A bi/three-dimension representation, on a flat surface, of the features of, or a portion of, the Earth | |
Observation | Data or information obtained by surface-based and airborne in-situ instruments, as well as by surface-based remote sensing. | |
Re-analysis | Information obtained by a subsequent analysys of remote sensed or collected data set | |
N/A | Not Applicable | |
TBD | To be defined |
name | description | link |
Firm | Result of impact studies of actual data used in actual applications of numerical or conceptual models. | |
Reasonable | Not firm, but based on a strong heritage of experiments with similar data. | |
Speculative | Generic interest expressed; requirement figures not provided; experimentation envisaged | |
Tentative | Positive impact expected but not yet validated due to lack of suitable data and/or models. | |
N/A | Not applicable | |
TBD | To be determined |
name | description | link |
Client Service | An application that communicates with a remote central server | |
Delayed mode | Delayed mode | |
Download Service | ||
Database or data repository | The data is accessed through a database extraction or data repository (e.g., a folder). | |
INSPIRE Service | ||
NRT Service | Near Real Time Service that enable the access to data set and information in a period between the real time measure and the release after the data processing | |
OGC Service | The Open Geospatial Consortium recognised services | |
Offline | Absence of services to access data swet and information | |
View Service | ||
View and Download Service | Access through web browser interface that enable the view or the download of data set and information | |
N/A | Not applicable | |
TBD | To be determined |
acronym | name | website | created_at | updated_at |
EEA | European Environment Agency | https://www.eea.europa.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
ECMWF | European Centre for Medium-Range Weather Forecasts | https://www.ecmwf.int/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
MOi | Mercator Ocean International | https://www.mercator-ocean.fr/en/ | Nov. 6, 2017, 11:30 a.m. | Nov. 25, 2022, 12:09 p.m. |
EMSA | European Maritime Safety Agency | http://www.emsa.europa.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
FRONTEX | European Border and Coast Guard Agency | http://frontex.europa.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
SATCEN | European Union Satellite Centre | https://www.satcen.europa.eu/ | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
JRC | Joint Research Centre | https://ec.europa.eu/jrc/en | Nov. 6, 2017, 11:30 a.m. | Jan. 30, 2020, 3:33 p.m. |
ESA | European Space Agency | https://www.esa.int/ESA | July 12, 2019, 2:28 p.m. | Jan. 30, 2020, 3:33 p.m. |
EUMETSAT | European Organisation for the Exploitation of Meteorological Satellites | https://www.eumetsat.int/website/home/index.html | July 12, 2019, 2:28 p.m. | Jan. 30, 2020, 3:33 p.m. |
EUMETSAT | European Organisation for the Exploitation of Meteorological Satellites | https://www.eumetsat.int/ | March 28, 2022, 12:58 p.m. | March 28, 2022, 12:58 p.m. |
domain | component | parameter | description | link |
Atmosphere | Surface | Precipitation | Precipitation, either liquid or solid, is the most important climate variable directly affecting humans. Through either its duration, intensity and frequency or its lack of occurrence, it influences the supply of water, causes risks to life and livelihoods when associated with floods, landslides and droughts, and affects infrastructure planning, leisure activities and more. Precipitation is closely related to cloud properties, a number of terrestrial ECVs and to ocean-surface salinity. It is indicative of the release of latent heat within the energy cycle, as well as being at the heart of the hydrological cycle. | Link |
Atmosphere | Surface | Pressure | The humidity of air near the surface of the Earth affects the comfort and health of humans, livestock and wildlife, the swarming behaviour of insects and the occurrence of plant disease. The humidity near the surface affects evaporation and the strength of the hydrological and energy cycles. Evaporation from the surface of the earth is the source of water in the atmosphere and so is responsible for important feedbacks in the climate system due to clouds and radiation. | Link |
Atmosphere | Surface | Surface radiation budget | The Surface Radiation Budget is a fundamental component of the surface energy budget that is crucial to nearly all aspects of climate, and needs to be monitored systematically. | Link |
Atmosphere | Surface | Temperature | Surface air temperature has profound and widespread impacts on both natural systems and on human lives and activities. It affects health, agriculture, energy demand and much more. Extremes of surface air temperature, both heat waves and extreme cold periods, are particular important for human health. Surface air temperature provides a key indicator of climate change, contributing to the “global surface temperature record”. A goal of limiting changes in global surface temperature provides the measure for the Paris climate agreement. | Link |
Atmosphere | Surface | Water vapour | The humidity of air near the surface of the Earth affects the comfort and health of humans, livestock and wildlife, the swarming behaviour of insects and the occurrence of plant disease. The humidity near the surface affects evaporation and the strength of the hydrological and energy cycles. Evaporation from the surface of the earth is the source of water in the atmosphere and so is responsible for important feedbacks in the climate system due to clouds and radiation. | Link |
Atmosphere | Surface | Wind speed and direction | Surface winds drive the exchange of momentum between the atmosphere and ocean, producing ocean waves and provides a key forcing of the ocean circulation responsible for the global transport of important amounts of heat and carbon. Extreme winds have huge social and economic impacts, most obviously during hurricanes and tropical cyclones, leading to loss of human life, damage to ecosystems, the destruction of infrastructure and loss of shipping. | Link |
Atmosphere | Upper-air | Earth radiation budget | The Earth Radiation Budget (at the top of the atmosphere) describes the overall balance between the incoming energy from the sun and the outgoing thermal (longwave) and reflected (shortwave) energy from the earth. It can only be measured from space. The radiation balance at the top of the atmosphere is the basic radiative forcing of the climate system. Measuring its variability in space and time over the globe provides insight into the overall response of the system to this forcing. | Link |
Atmosphere | Upper-air | Lightning | Lightning is one of the most dramatic weather phenomena, causing many fatalities as well as substantial loss and damage for example by forest fires, damage to electrical infrastructure and other sectors every year all over the world. On top, even more damage is caused by the storms which generate lightning. This direct link to convection makes lightning also a potentially valuable indicator to track and understand trends in storminess, particularly under climate variability and change. In addition, lightning itself impacts the global climate by producing nitrogen oxides (NOX), a strong greenhouse gas. | Link |
Atmosphere | Upper-air | Temperature | Temperature is one of the fundamental state variables for understanding and predicting the behaviour of the atmosphere. It is basic to the energy budget of the climate system as a whole through the temperature dependence of the long-wave radiation of energy from the atmosphere to space. Upper-air observations are of key importance for detecting and attributing climate change in the troposphere and stratosphere because the warming of the troposphere and the cooling of the stratosphere are unique fingerprints of anthropogenic GHG. They are needed for the development and evaluation of climate models, and for the initialization of medium term and seasonal forecasts. | Link |
Atmosphere | Upper-air | Water vapour | Water vapour is the predominant gaseous source of infrared opacity in the atmosphere, accounting for about 60% of the natural greenhouse effect for clear skies. Water vapour condenses to produce clouds, changing radiative properties and releasing latent heat that drives or modifies atmospheric circulation systems. Water vapour in the lower stratosphere, though present only in small amounts, is radiatively significant. Consequently, there is potential for additional climate change feedbacks through perturbations of the processes that control the amount of water vapour in the stratosphere, such as the Brewer-Dobson circulation that strongly influences tropical tropopause temperatures and the amount of CH4 oxidized in the stratosphere. | Link |
Atmosphere | Upper-air | Wind speed and direction | Wind is one of the fundamental state variables for understanding and predicting the behaviour of the atmosphere. It is basic to the working of the climate system through transport of heat, moisture and trace constituents. Measurements of wind are vital for initializing and verifying climate projections and for detecting, understanding and attributing variability and change in the climate system. | Link |
Atmosphere | Upper-air | Clouds | The variable properties of clouds determines the clouds profound effects on radiation and precipitation. They are influenced by and in turn influence the motion of the atmosphere on many scales. They are affected by the presence of aerosols, and modify atmospheric composition in several ways, including the depletion of ozone when they form in the polar stratosphere. | Link |
Atmosphere | Atmospheric Composition | Aerosols | Atmospheric aerosols are minor constituents of the atmosphere by mass, but a critical component in terms of impacts on the climate and especially climate changes. Aerosols influence the global radiation balance by directly scattering solar radiation and indirectly through influencing cloud reflectivity, cloud cover and cloud lifetime. | Link |
Atmosphere | Atmospheric Composition | Carbon dioxide, methane and other greenhouse gases | The atmospheric abundance of carbon dioxide (CO2), the dominant human-produced greenhouse gas, has increased by about 50% since pre-industrial times due to the proliferation of fossil fuel combustion. Methane (CH4) is also a strong greenhouse gas; its atmospheric abundance has more than doubled since the pre-industrial era because of human activities. Other significant greenhouse gases include nitrous oxide (N2O), chlorofluorocarbons (CFCs), hydrochlorofluorocarbons (HCFCs), hydrofluorocarbons (HFCs), perfluorocarbons (PFCs) and sulphur hexafluoride (SF6). | Link |
Atmosphere | Atmospheric Composition | Ozone | Ozone (O3) is a naturally occurring trace gas in the stratosphere that inhibits harmful UV radiation from reaching Earth’s surface. Ozone in the troposphere is a pollutant, harmful to all living things. Ozone is strongly linked to climate by its influence on Earth’s radiation budget. The amount of ozone in the global stratosphere began to decrease in 1980 due to catalytic reactions with chlorine and bromine from man-made CFCs and other halocarbons. Severe, seasonal depletions over Antarctica (“ozone hole”) have occurred annually since 1985. Thanks to the Montreal Protocol, an international treaty enacted to curtail the production and consumption of ozone-depleting substances, stratospheric ozone levels are expected to return to pre-depletion values. | Link |
Atmosphere | Atmospheric Composition | Precursors for aerosols and ozone | Precursor species lead to the production of aerosols and ozone. Precursors include nitrogen dioxide (NO2), sulphur dioxide (SO2), carbon monoxide (CO) and formaldehyde (HCHO). Aerosols and ozone in the near-surface atmosphere can directly harm human health and produce detrimental environmental impacts (e.g., crop damage, acid rain). Reductions in near-surface aerosols and ozone have been observed in specific regions where the emissions of some precursors are regulated. | Link |
Land | Hydrosphere | Groundwater | It is estimated that groundwater accounts for about 30% of the world’s total freshwater resources, and it is by far the largest available reservoir of liquid freshwater. Groundwater counts in average for one third of the freshwater consumed by humans, but at some parts of the world, this percentage can reach up to 100%. Climate change affects groundwater recharge rates through changes in precipitation and evapotranspiration. However, attributing observed groundwater change to climate change is difficult because of the influence of land-use change and groundwater abstraction. The extent to which groundwater recharge and storage has already been affected by climate change is widely unknown. Climate change can also affect groundwater through saltwater intrusion in coastal aquifers as sea level rises. | Link |
Land | Hydrosphere | Lakes | Information on changes in lake level and area is required on a monthly basis for climate assessment purposes. Approximately 95% of the volume of water held globally in approximately 4 000 000 lakes is contained in the world’s 80 largest lakes. | Link |
Land | Hydrosphere | River discharge | River-discharge measurements have essential direct applications for water management and related services, including flood protection. They are needed in the longer term to help identify and adapt to some of the most significant potential effects of climate change. The flow of freshwater from rivers into the oceans also needs to be monitored because it reduces ocean salinity, and changes in flow may thereby influence the thermohaline circulation. | Link |
Land | Hydrosphere | Terrestrial water storage | TWS is the total amount of water stored in all continental storage compartments (ice caps, glaciers, snow cover, soil moisture, groundwater, surface water bodies, water in biomass). The change of TWS over time balances the budget of the water fluxes precipitation, evapotranspiration and runoff, i.e., it closes the continental water balance. TWS changes thus represent the net effect of climate variability and climate change as well as of anthropogenic impacts on the water cycle. | Link |
Land | Cryosphere | Glaciers | Glacier changes provide independent and reliable evidence of climate change. Past, current and future glacier changes impact global sea level, the regional water cycle, and may increase local hazard risks. | Link |
Land | Cryosphere | Ice sheets and ice shelves | The understanding of the timescale of ice sheet response to climate change has changed dramatically over the last decade. Rapid changes in ice-sheet mass have surely contributed to abrupt changes in climate and sea level in the past. | Link |
Land | Cryosphere | Permafrost | The properties of frozen ground react sensitively to climate and environmental changes in high-latitude and high-altitude regions. This includes the temperature distribution in the permafrost layer and the depth of the overlying active layer where seasonal freezing and thawing occur. Changes in these quantities have important impacts on terrain stability, coastal erosion, surface and subsurface water, the carbon cycle and vegetation development. | Link |
Land | Cryosphere | Snow | Snow refers to forms of ice crystals that precipitate from the atmosphere (usually from clouds) and undergo changes on the Earth's surface. Snow cover on the ground plays a significant role in the climate system due to its high albedo, heat insulation and contribution to soil moisture and runoff, thus an important variable in monitoring climate change. | Link |
Land | Biosphere | Above-ground biomass | Vegetation biomass is a crucial ecological variable for understanding the evolution and potential future changes of the climate system. Photosynthesis withdraws CO2 from the atmosphere and stores carbon in vegetation in an amount comparable to that of atmospheric carbon. Vegetation systems have the potential either to sequester more carbon in the future or to contribute as an even larger source. Depending on the quantity of biomass, vegetation cover can have a direct influence on local, regional and even global climate, particularly on air temperature and water vapour. | Link |
Land | Biosphere | Albedo | The land surface albedo is the ratio of the radiant flux reflected from Earth’s surface to the incident flux. It is a key forcing parameter controlling the partitioning of radiative energy between the atmospheric and surface. In the case of vegetation, a reference surface is typically defined at or near the top of the canopy and must be specified explicitly. Surface albedo depends on natural variations, highly variable in space and time as a result of terrestrial properties changes, and with illumination conditions and human activities and is a sensitive indicator of environmental vulnerability. | Link |
Land | Biosphere | Evaporation from land | Terrestrial evaporation is an important process in the global water cycle. It acts like an air conditioner for the surface, as it absorbs radiation (latent heat) that otherwise would be used to warm up the atmosphere (sensible heat). At the same time, water vapour acts as a greenhouse gas by trapping radiation in the lower atmosphere. Evaporation acts as a climate change diagnostic, being very sensitive to changes in atmospheric composition and the Earth's radiation balance. Moreover, it plays a crucial role in dampening the intensification of drought and heatwave events, it is a pivotal variable for agriculture that determines the needs for irrigation, and it constrains human water management. | Link |
Land | Biosphere | Fire | Fires have impacts on several identified radiative forcing agents. While they can be a natural part of many ecosystems, they have a strong human control, particularly in Tropical ecosystems. Fires contribute to the build-up of CO2 through deforestation and forest degradation, emissions from peatland fires, and alterations of fire regimes(more frequent, larger or more severe fires). They also emit CH4, and are a major source of aerosols, CO and oxides of nitrogen, thus affecting local and regional air quality. Estimates of greenhouse gas emissions due to fires are essential for realistic modelling of climate and its critical component, the global carbon cycle. Fires caused deliberately for land clearance (agriculture and ranching) or accidentally (lightning strikes and human error) are a major factor in land-cover variability and change, and hence affect fluxes of energy and water to the atmosphere. | Link |
Land | Biosphere | Fraction of absorbed photosynthetically active radiation (FAPAR) | Solar radiation in the spectral range 400–700 nm, known as photosynthetically active radiation (PAR), provides the energy required by terrestrial vegetation to produce organic materials from mineral components. The part of this PAR that is effectively absorbed by plants is called FAPAR. FAPAR is related to, but different from, Leaf Area Index, which describes the amount of leaf material in the canopy. FAPAR plays a critical role in assessing the primary productivity of canopies, the associated fixation of atmospheric CO2 and the energy balance of the surface. Monitoring FAPAR provides information on the amount and health cycle of vegetation. | Link |
Land | Biosphere | Land cover | Land cover is the observed (bio)-physical cover on the Earth’s surface. It influences climate by modifying water and energy exchanges with the atmosphere and by changing greenhouse gas and aerosol sources and sinks. Land-cover conditions are inherently dynamic (i.e. seasonality) and distributions are linked to regional climatic conditions, so changes in cover can be due to climate change on a regional scale as well as directly due to human activities. | Link |
Land | Biosphere | Land surface temperature | The Land Surface Temperature (LST) is the skin temperature of ground. It is mainly a product of albedo, the vegetation cover and the soil moisture. From a climate perspective, LST is important for evaluating land surface and land-atmosphere exchange processes, constraining surface energy budgets and model parameters, and providing observations of surface temperature change both globally and in key regions. | Link |
Land | Biosphere | Leaf area index | The Leaf Area Index (LAI) of a plant canopy or ecosystem, defined as one half of the total green leaf area per unit horizontal ground surface area, measures the area of leaf material present in the specified environment. On sloping surfaces, the leaf area should be projected to the underlying ground along the normal to the slope. This dimensionless variable varies between 0 and values of about 10 or so, depending on local conditions. It partly controls important mass and energy exchange processes, such as radiation and rain interception, as well as photosynthesis and respiration, which couple vegetation to the climate system. Hence, LAI appears as a key variable in many models describing vegetation–atmosphere interactions, particularly with respect to the carbon and water cycles. | Link |
Land | Biosphere | Soil carbon | Carbon in soils occurs in organic and inorganic forms. The inorganic carbon is derived from weathered bedrock, is relatively inert and constitutes little to the carbon cycle. Soil organic carbon is derived from plant and other decaying matter and is a significant part of the carbon cycle. About 10% of the atmospheric carbon cycles through soils each year. Soil organic carbon represents the largest terrestrial carbon pool, amounting to about two to three times the net size of the biomass pools. Carbon sinks may be explained by changes in above-ground biomass on seasonal to decadal timescales, but soil organic carbon stocks become significant on longer timescales, and can be a significant source at all timescales after disturbances. | Link |
Land | Biosphere | Soil moisture | Soil moisture is an important variable in land–atmosphere feedbacks at both weather and climate timescales. It plays a major role in partitioning the incoming radiation flux onto the land into fluxes of latent and sensible heat from the land to the atmosphere, and in separating precipitation into runoff, subsurface flow, and infiltration. Soil moisture is intimately involved in the feedback between climate and vegetation, as both local climate and vegetation influence soil moisture through evapotranspiration, while soil moisture is a determinant of the type and condition of vegetation in a region. Changes in soil moisture can accordingly have substantial impacts on agricultural productivity, forestry and ecosystem health. | Link |
Land | Anthroposphere | Anthropogenic greenhouse gas fluxes | Global anthropogenic emissions of Greenhouse gases (CO2, CH4, N2O and F-gases) continue to be emitted at an annual rate that is not yet significantly decreasing. The global warming potential of each of the greenhouse gases and their long residence time in the atmosphere are causing increased surface temperature and climate change. The scientific community illustrated with inverse models and data assimilation how consistent the reported inventories and the atmospheric observations are, which is taken up also in few national inventory reports (e.g. UK, Switzerland, Australia). | Link |
Land | Anthroposphere | Anthropogenic water use | Data on water extractions by sector and available renewable freshwater provide key information on the availability of freshwater and the amount of water stress in a country. Climate Change is projected to reduce renewable surface-water and groundwater resources significantly in most dry subtropical regions. In contrast, water resources are projected to increase at high latitudes. Climate change is also projected to reduce raw water quality, posing risks to drinking water quality, even with conventional treatment. The availability of freshwater plays a crucial role in food production and food security. | Link |
Ocean | Physical | Ocean surface heat flux | Surface heat flux is exchange of heat, per unit area, crossing the surface between the ocean and the atmosphere. It consists of the turbulent and the radiative components. These fluxes are major contributors to the energy and moisture budgets, and are largely responsible for thermodynamic coupling the ocean and atmosphere at global and regional scales, and variability of these fluxes is in part related to large-scale variability in weather and climate patterns. | Link |
Ocean | Physical | Sea ice | Sea ice variability is a key indicator of climate variability and change in the polar regions. The primary parameters that define the state of sea ice include: concentration, area and extent, ice type, motion, deformation, age, thickness, and volume. The presence of sea ice strongly modifies surface waves and air-sea exchanges of heat, momentum, moisture and gases. Sea ice has a significant impact on the Earth’s albedo and hence changes in Sea Ice impact the global energy budget. The properties of many water masses of the global ocean and strongly influenced determined freezing and melting processes in sea ice regions. | Link |
Ocean | Physical | Sea level | Sea Level is one of the primary indicators of global climate change. Change in the global mean sea level provides a measure of the net change in ocean mass due to melting of glaciers and ice sheets, and net change in ocean volume due to thermal expansion. Sea level observations characterize inter-seasonal variability such as ENSO. On the regional scales, changes in sea level can be far larger than the globally averaged value due to changes in temperature, salinity and circulation. Along many continental margins vertical land displacement associated with crustal adjustments to past and current land ice melt also cause regional variations in apparent sea level independent of the ocean. Coastal sea level change is a major driver of societal impacts. | Link |
Ocean | Physical | Sea state | Sea State is the characterization of wave and swell, typically in terms of height, wavelength, period, and directional wave energy flux. Waves generated by ocean surface stress evolve from wind waves to swell through nonlinear dynamical processes.. Wave characteristics are modified by bathymetry when the depth of the water is comparable to the wavelength, and by surface currents. Sea state is most well known for its impacts on marine safety, marine transport and damage to structures. It is also a substantial modifier of air-sea exchanges of momentum, moisture and CO2. Waves also impact beach erosion, storm-related water damage (wave set-up contributes to storm surge), surface albedo, and transport of larva. Waves can also modify the growth or decay of sea ice. | Link |
Ocean | Physical | Sea surface currents | The surface ocean general circulation is responsible for significant surface transport of heat, salt, passive tracers and ocean pollutants. On basin scales, surface currents and their variations are a major player in climate to weather fluctuations. The boundary currents on each side of the ocean basins transport significant amounts of heat, salt and passive tracers. Western Boundary Currents in particular transport heat and properties polwards, moderating climate. Convergences/divergences, spiralling eddies, and filaments all contribute to vertical motions and mass exchange. Surface currents impact the steepness of surface waves, and are thus important for generating accurate marine sea state forecasts. | Link |
Ocean | Physical | Sea surface salinity | Sea surface salinity observations contribute to monitoring the global water cycle (evaporation, precipitation and glacier and river runoff). On large scales, surface salinity can be used to infer long-term changes of the global hydrological cycle. Surface salinity, together with surface temperature, is indicative of the surface expression of ocean frontal features and eddies. | Link |
Ocean | Physical | Sea surface stress | Ocean surface stress (OSS) is the two-dimensional vector drag at the bottom of the atmosphere and the dynamical forcing at the top of the ocean. OSS influences the air-sea exchange of energy, water and gases. OSS is important for determining the large scale momentum forcing of the ocean, and consequent ocean circulation including ocean upwelling regions. Accurate knowledge of stress magnitudes is also essential for reliable computations of air-sea heat fluxes as well as air-sea gas exchanges and mass fluxes. | Link |
Ocean | Physical | Sea surface temperature | Sea Surface temperature (SST) is a vital component of the climate system as it exerts a major influence on the exchanges of energy, momentum and gases between the ocean and atmosphere. SST largely controls the atmospheric response to the ocean at both weather and climate time scales. Daily variations in SST can exceed 3 degrees Celsius and could alter the surface energy budget by more than 10 Wm-2 over the tropics and subtropics. Therefore, the SST and horizontal gradients in SST are also important for coupling with the atmosphere for sub-seasonal to seasonal prediction timescales. The spatial patterns of SST reveal the structure of the underlying ocean dynamics, such as, ocean fronts, eddies, coastal upwelling and exchanges between the coastal shelf and open ocean. | Link |
Ocean | Physical | Subsurface currents | Observations of subsurface ocean velocity contribute to estimates of ocean transports of mass, heat, freshwater, and other properties on local, to regional and basin to global scales. They are essential in resolving the wind and buoyancy driven ocean circulation, and the complex vertical velocity structure, for example, in the major ocean boundary currents, tides, equatorial currents, wave propagations, ocean eddies. Vertical velocity profile information can be used to estimate the order of ocean mixing using fine-scale parameterizations of turbulent dissipation by internal wave breaking. Velocity estimates can be combined in data assimilation models to provide gridded global estimates of ocean circulation at varying temporal and spatial scales. | Link |
Ocean | Physical | Subsurface salinity | The global subsurface salinity observing system is vital for closure of the global hydrological cycle, estimates of oceanic evaporation and precipitation, and halosteric component of sea level change. Subsurface salinity are required to calculate in situ density and ocean freshwater transports, respectively, and coincident subsurface observations of salinity, temperature and pressure provide an estimate of the ocean geostrophic velocity. In addition, subsurface salinity is used to derive large-scale gridded climate products including ocean velocity, mixed-layer depth, density stratification, sea level and indirect subsurface ocean mixing used in many weather and climate applications. | Link |
Ocean | Physical | Subsurface temperature | Subsurface temperature is a fundamental variable that is required to monitor variability and change in the physical environment of the ocean, energy flows, climate patterns and sea level. Many other physical variables are derived from subsurface temperature along with subsurface salinity, including subsurface density, geostrophic circulation, heat transport and steric sea level. Heat uptake by the global ocean accounts for more than 90% of the excess heat trapped in the Earth system in the past few decades. This ocean heat uptake helps to mitigate surface warming but, in turn, increases the global ocean volume through thermal expansion, and thus results in global-mean sea-level rise, accounting for about one third of the increase observed over the past few decades. | Link |
Ocean | Biogeochemical | Inorganic carbon | The ocean is a major component of the global carbon cycle, absorbing enormous quantities of carbon in natural cycles driven by the ocean circulation, biogeochemistry and biology. Since seawater has very high capacity for absorbing carbon, the ocean has an inhibitory effect on the atmospheric accumulation of carbon dioxide and related greenhouse effect. The net ocean carbon uptake depends significantly on chemical and biological activity, and therefore it varies due to changing oceanic conditions and ecosystem composition. The chemical pathways of the inorganic carbon in the ocean mean that this uptake causes a decline in ocean pH, also known as ocean acidification. | Link |
Ocean | Biogeochemical | Nitrous oxide | Nitrous oxide (N2O) is an important climate-relevant trace gas in the Earth’s atmosphere. In the troposphere it acts as a strong greenhouse gas and in the stratosphere it acts as an ozone depleting substance because it is the precursor of ozone depleting nitric oxide radicals. The ocean - including its coastal areas such as continental shelves, estuaries and upwelling areas - contribute about 30% to the atmospheric N2O budget. | Link |
Ocean | Biogeochemical | Nutrients | Nutrients are essential for ocean life. Nutrient data provide important biogeochemical information, and provide essential links between physical climate variability and ecosystem variability. They can provide additional information on ocean mixing and climate related phenomena such as changes in primary and export production (nutrient transports regulate new production which is correlated with export production), eutrophication and shifts in phytoplankton community composition. Therefore it is necessary to develop accurate observations of trends in dissolved nutrients in both upper- and deep-ocean waters. | Link |
Ocean | Biogeochemical | Ocean colour | Ocean colour is the radiance emanating from the ocean normalized by the irradiance illuminating the ocean. Products derived from ocean colour remote sensing (OCRS) contain information on the ocean albedo and information on the constituents of the seawater, in particular, phytoplankton pigments such as chlorophyll-a. OCRS products are used to assess ocean ecosystem health and productivity, and the role of the oceans in the global carbon cycle, to manage living marine resources, and to quantify the impacts of climate variability and change. | Link |
Ocean | Biogeochemical | Oxygen | Oxygen (O2) is essential for nearly all multicellular life. Subsurface oxygen concentrations reflect a balance between supply through circulation and ventilation and consumption by respiratory processes. Changes in either of these processes is susceptible to lead to changes in O2 distribution. A global ocean O2 observing network will act as a sensitive early warning system for trends that climate change is causing. Ocean deoxygenation (decline in O2 concentration) is under way in part because of ocean warming and increased stratification, but also because of increased nutrient loads in the coastal ocean. Deoxygenation has been largely under the radar to most people including policy advisers and decision makers. Yet it is deoxygenation that will have profound implications not just for ecosystems but also for communities and economies that depend on a healthy ocean. | Link |
Ocean | Biogeochemical | Transient tracers | Oxygen (O2) is essential for nearly all multicellular life. Subsurface oxygen concentrations reflect a balance between supply through circulation and ventilation and consumption by respiratory processes. Changes in either of these processes is susceptible to lead to changes in O2 distribution. A global ocean O2 observing network will act as a sensitive early warning system for trends that climate change is causing. Ocean deoxygenation (decline in O2 concentration) is under way in part because of ocean warming and increased stratification, but also because of increased nutrient loads in the coastal ocean. Deoxygenation has been largely under the radar to most people including policy advisers and decision makers. Yet it is deoxygenation that will have profound implications not just for ecosystems but also for communities and economies that depend on a healthy ocean. | Link |
Ocean | Biological/ecosystems | Marine habitats | Marine coastal regions are amongst the most productive systems of the planet, yet they are undergoing rapid transformations in response to intensifying human activities and global change. Regime shifts, abrupt transitions between alternative states, are increasingly observed in a wide range of coastal systems, including coral reefs, macroalgal forests, seagrasses and mangroves. These non-linear responses to deteriorating environmental conditions often result in considerable loss of ecosystem functions and services. | Link |
Ocean | Biological/ecosystems | Plankton | Plankton are at the base of the marine food web and generally not fished by humans. Changes in the plankton will have impacts on the rest of the marine ecosystem including on the carbon cycle, living marine resources used by humans and threatened marine species including apex predators. Climate variability significantly impacts plankton in the ocean, both the microflora (phytoplankton) and the microfauna (zooplankton), over both short and long timescales. | Link |
name | annex | description | link |
Addresses | Annex I | Location of properties based on address identifiers, usually by road name, house number, postal code | |
Administrative units | Annex I | Units of administration, dividing areas where Member States have and/or exercise jurisdictional rights, for local, regional and national governance, separated by administrative boundaries | |
Cadastral parcels | Annex I | Areas defined by cadastral registers or equivalent | |
Coordinate reference systems | Annex I | Systems for uniquely referencing spatial information in space as a set of coordinates (x,y,z) and/or latitude and longitude and height, based on a geodetic horizontal and vertical datum | |
Geographical grid systems | Annex I | Harmonised multi-resolution grid with a common point of origin and standardised location and size of grid cells | |
Geographical names | Annex I | Names of areas, regions, localities, cities, suburbs, towns or settlements, or any geographical or topographical feature of public or historical interest | |
Hydrography | Annex I | Hydrographic elements, including marine areas and all other water bodies and items related to them, including river basins and sub-basins. Where appropriate, according to the definitions set out in Directive 2000/60/EC of the European Parliament and of the Council of 23 October 2000 establishing a framework for Community action in the field of water policy, and in the form of networks | |
Protected sites | Annex I | Area designated or managed within a framework of international, Community and Member States' legislation to achieve specific conservation objectives | |
Transport networks | Annex I | Road, rail, air and water transport networks and related infrastructure. Includes links between different networks. Also includes the trans-European transport network as defined in Decision 1692/96/EC of the European Parliament and of the Council of 23 July 1996 on Community guidelines for the development of the trans-European transport network and future revisions of that decision | |
Elevation | Annex II | Digital elevation models for land, ice and ocean surfaces. Includes terrestrial elevation, bathymetry and shoreline | |
Geology | Annex II | Geology characterised according to composition and structure. Includes bedrock, aquifers and geomorphology | |
Land cover | Annex II | Physical and biological cover of the earth's surface including artificial surfaces, agricultural areas, forests, (semi-)natural areas, wetlands, water bodies | |
Orthoimagery | Annex II | Geo-referenced image data of the Earth's surface, from either satellite or airborne sensors | |
Agricultural and aquaculture facilities | Annex III | Farming equipment and production facilities (including irrigation systems, greenhouses and stables) | |
Area management/restriction/regulation zones & reporting units | Annex III | Areas managed, regulated or used for reporting at international, European, national, regional and local levels. Includes dumping sites, restricted areas around drinking water sources, nitrate-vulnerable zones, regulated fairways at sea or large inland waters, areas for the dumping of waste, noise restriction zones, prospecting and mining permit areas, river basin districts, relevant reporting units and coastal zone management areas | |
Atmospheric conditions | Annex III | Physical conditions in the atmosphere. Includes spatial data based on measurements, on models or on a combination thereof and includes measurement locations | |
Bio-geographical regions | Annex III | Areas of relatively homogeneous ecological conditions with common characteristics | |
Buildings | Annex III | Geographical location of buildings | |
Energy resources | Annex III | Energy resources including hydrocarbons, hydropower, bio-energy, solar, wind, etc., where relevant including depth/height information on the extent of the resource | |
Environmental monitoring facilities | Annex III | Location and operation of environmental monitoring facilities includes observation and measurement of emissions, of the state of environmental media and of other ecosystem parameters (biodiversity, ecological conditions of vegetation, etc.) by or on behalf of public authorities | |
Habitats and biotopes | Annex III | Geographical areas characterised by specific ecological conditions, processes, structure, and (life support) functions that physically support the organisms that live there. Includes terrestrial and aquatic areas distinguished by geographical, abiotic and biotic features, whether entirely natural or semi-natural | |
Human health and safety | Annex III | Geographical distribution of dominance of pathologies (allergies, cancers, respiratory diseases, etc.), information indicating the effect on health ( biomarkers, decline of fertility, epidemics) or well-being of humans (fatigue, stress, etc.) linked directly (air pollution, chemicals, depletion of the ozone layer, noise, etc.) or indirectly (food, genetically modified organisms, etc.) to the quality of the environment | |
Land use | Annex III | Territory characterised according to its current and future planned functional dimension or socio–economic purpose (e.g. residential, industrial, commercial, agricultural, forestry, recreational) | |
Meteorological geographical features | Annex III | Weather conditions and their measurements; precipitation, temperature, evapotranspiration, wind speed and direction | |
Mineral resources | Annex III | Mineral resources including metal ores, industrial minerals, etc., where relevant including depth/height information on the extent of the resource | |
Natural risk zones | Annex III | Vulnerable areas characterised according to natural hazards (all atmospheric, hydrologic, seismic, volcanic and wildfire phenomena that, because of their location, severity, and frequency, have the potential to seriously affect society), e.g. floods, landslides and subsidence, avalanches, forest fires, earthquakes, volcanic eruptions | |
Oceanographic geographical features | Annex III | Physical conditions of oceans (currents, salinity, wave heights, etc.) | |
Population distribution and demography | Annex III | Geographical distribution of people, including population characteristics and activity levels, aggregated by grid, region, administrative unit or other analytical unit | |
Production and industrial facilities | Annex III | Industrial production sites, including installations covered by Directive 96/61/EC of 24 September 1996 concerning integrated pollution prevention and control and water abstraction facilities, mining, storage sites | |
Sea regions | Annex III | Physical conditions of seas and saline water bodies divided into regions and sub-regions with common characteristics | |
Soil | Annex III | Soils and subsoil characterised according to depth, texture, structure and content of particles and organic material, stoniness, erosion, where appropriate mean slope and anticipated water storage capacity | |
Species distribution | Annex III | Geographical distribution of occurrence of animal and plant species aggregated by grid, region, administrative unit or other analytical unit | |
Statistical units | Annex III | Units for dissemination or use of statistical information | |
Utility and governmental services | Annex III | Includes utility facilities such as sewage, waste management, energy supply and water supply, administrative and social governmental services such as public administrations, civil protection sites, schools and hospitals | |
N/A | Not applicable | ||
TBD | To be determined |
name | description |
Threshold | The “threshold” or “minimum requirement“ is the value that has to be met to ensure that data are useful. Below this minimum, the benefit derived does not compensate for the additional cost involved in using the observation. Threshold requirements for any given observing system cannot be stated in an absolute sense; assumptions have to be made concerning which other observing systems are likely to be available. |
Breakthrough | Within the range between threshold and goal requirements, the observations become progressively more useful. The “breakthrough” is an intermediate level between “threshold” and “goal“ which, if achieved, would result in a significant improvement for the targeted application. |
Goal | The “goal” or “maximum requirement“ is the value above which further improvement of the observation would not cause any significant improvement in performance for the application in question. The cost of improving the observations beyond the goal would not be matched by a corresponding benefit. The goals are likely to evolve as applications progress and develop a capacity to make use of better observations. |
name | description |
AMC Antropogenic Emissions | CAMS products concerning antropogenic emissions |
AMC Atmospheric Composition NRT Analysis and Forecast | CAMS products concerning global atmospheric composition analysis and forecast |
AMC Atmospheric Composition Reanalysis | CAMS products concerning global atmospheric composition reanalysis |
AMC Climate Forcings | CAMS products concerning climate forcings |
AMC European Air Quality NRT Analysis and Forecast | CAMS products concerning European air quality analysis and forecast |
AMC European Air Quality Reanalysis | CAMS products concerning European air quality reanalysis |
AMC European Interim Air Quality Reanalysis | CAMS products concerning European interim air quality reanalysis |
AMC Fire Emissions | CAMS products concerning fire emissions |
AMC Greenhouse Gas Fluxe Inversions | CAMS products concerning greenhouse gas flux inversions |
AMC Policy Support | CAMS products concerning policy support |
AMC Solar Radiation | CAMS products concerning solar radiation |
CCC climate monitoring | C3S reanalysis products for the monthly climate bulletin |
AMC Ship Emissions | |
CSS Border Surveillance | CSS Border Surveillance products |
CSS Maritime Surveillance | CSS Maritime Surveillance products |
CSS Support to External Action | CSS Support to External Action products |
EMC Exposure | EMS Exposure Mapping products |
EMC Mapping | EMS Rapid Mapping products |
EMC Risk and Recovery | EMS Risk and Recovery mapping products |
EU-GM | Pan-EU Land Ground Motion products |
EWC Forecasts | Early Warning - forecast products |
EWC Hydrological conditions | Early Warning - information about the hydrological conditions |
EWC Meterological conditions | Early Warning - information about the meteorological conditions |
GLC Cryosphere | Global Land products containing information about the cryosphere |
GLC Energy | Global Land products containing information about energy |
GLC Hot Spots | GLC Hot Spots products provide detailed land information on specific areas of interest (Protected Areas and Key Landscapes for Conservation). |
GLC Vegetation | Global Land products containing information about vegetation |
GLC Water | Global Land products containing information about water |
LLC Coastal Zones | This LC/LU product maps from the European baseline a 10 km landwards buffer. The justification for monitoring LC/LU dynamics in coastal zones is in the need to coordinate an economic growth that maintains a resilient state of the coastal environment, safeguarding coastal protection and the basis for human wellbeing. |
LLC Natura 2000 | Local Land products containing information about Natura 2000 zones |
LLC Riparian Zones | Local Land products containing information about riparian zones |
LLC Urban Atlas | Local Land Urban Atlas products |
MMC NRT Observations | CMEMS NRT observations |
MMC NRT/REP Observations | CMEMS NRT observations and reprocessing observations |
MMC REP Observations | CMEMS re-processing observations |
MMC Biogeochemical and Biological RAN | CMEMS reanalysis products on the biological state of the oceans |
MMC Biogeochemical NRT/RAN | CMEMS NRT and reanalysis products on the biological state of the oceans |
MMC Biogeochemical and Biological analysis/forecast | CMEMS NRT products on the biological state of the oceans |
MMC Physical NRT/RAN | CMEMS NRT and reanalysis products on the physical state of the oceans |
MMC Physical RAN | CMEMS reanalysis products on the physical state of the oceans |
MMC Physical analysis/forecast | CMEMS NRT products on the physical state of the oceans |
MMC Wave RAN | CMEMS reanalysis products containing information about sea surface waves |
MMC Wave NRT/RAN | CMEMS NRT and reanalysis products containing information about sea surface waves |
MMC Wave analysis/forecast | CMEMS NRT products containing information about sea surface waves |
PLC Biophysical Parameters | The systematic monitoring of biophysical parameters consists of a set of bio-geophysical products on the status and evolution of the land surface. These high spatial resolution products are used to monitor dynamics of the vegetation, the water cycle, energy budget and terrestrial cryosphere variables. The products are continuously produced at an European extent. |
PLC Corine Land Cover | Pan-European Land Corine Land Cover products |
PLC High Resolution Layers | Pan-European Land high resoultion layers |
PLC Image Mosaics | Image mosaics products |
PLC Reference Data | Pan-European Land reference data |
Sentinel-3-OLCI | |
Sentinel-3-Synergy | |
Sentinel-3 | |
Sentinel-3-SLSTR | |
Sentinel-3-Altimetry | |
Sentinel-5p | |
Sentinel-5p-TROPOMI | |
Wildfire monitoring | Wildfire monitoring |
N/A | Not applicable |
TBD | To be defined |
name | description | link |
Commercial | Private entities that collect in situ data for commercial use or collect them in operations linked to their commercial activities. | |
Institutional | National or governmental bodies collecting in situ data in the framework of environmental monitoring activities to answer to legal (National or European) requirements. | |
Public | Public-funded institution collecting in situ data for public utility. | |
Research | Public or private, Research or scientific institution collecting data for research and innovation purposes based on short term research funds. | |
N/A | Not applicable | |
TBD | To be defined |
name | description | link |
Calibration and validation | Utilised to calibrate and validate imagery, other measurements or products | |
Product generation | Used to underpin specific products | |
Supporting exploitation | Supporting the exploitation of products, but not essential | |
N/A | Not applicable | |
TBD | To be determined |
name | description |
Administrative boundaries | It includes all the official administrative boundaries from the continental up to the district ones. |
Aerial Ortho-imagery | The aerial ortho-imagery are all the remote sensed imageries not acquired by the satellite (i.e. acquired from aircraft or UAV or drone etc). |
Atmosphere | Atmosphere |
Cryosphere | It includes snow, sea ice, lake and river ice, icebergs, glaciers, permafrost and seasonally frozen ground. |
Digital Elevation Model | The digital elevation model (DEM) is a digital model or 3D representation of the terrain's surface. If it represents the bare ground surface without any objects like plants and buildings it is defined Digital Terrain Model (DTM). |
Hydrology | Measurement (or science of) the amount and flow of water in the environment, and its properties. Includes products of river flow, lake volume, water quality, etc. |
Hydrography | The mapping of the rivers and the coast and ocean, i.e. static spatial data. Includes products of map of rivers, streams, and catchments. |
Industry and Utilities | It includes mainly industries facilities and power station. |
Land cover / Land use | Land cover refers to the observed (bio)physical cover on the earth's surface mapping homogeneous landscape patterns. It typically includes artificial surface (urban areas, industrial areas etc), agricultural areas, forest / natural and semi natural areas, wetlands and water bodies with different levels of detail. Additionally, this group includes land use referring to the purpose the land serves, such as recreation, wildlife habitat, or agricultural production, characterized by the arrangements, activities and inputs humans undertake in a certain land cover type to produce, change or maintain it. |
Land parcel (LPIS) data | Land parcel data (i.e. cadastral data) provide geographically referenced information about the rights, interests, and value of property. Land Parcel Identification System data contain alphanumeric data sets, Vector and raster. |
Large scale population information | Ir refers to information on the population in terms of number of people, age, education and so on. |
Maritime elements | It includes all types of objects related to the open sea (vessel, nautical charts, etc). |
Meteorology | It includes all types of meteorological data (atmospheric parameters, precipitations, wind and wave parameters, etc). |
Natural risk zones | Vulnerable areas characterised according to natural hazards (all atmospheric, hydrologic, seismic, volcanic and wildfire phenomena that, because of their location, severity and frequency, have the potential to seriously affect society), e.g. floods, landslides and subsidence, avalanches, forest fires, earthquakes, volcanic eruptions’ |
Ocean | It includes all types of data related to the ocean (sea ice, surface/subsurface temperature and salinity, etc.) and its composition (Clorophyll, Oxygen, etc). |
Physiography | It includes information on elevation such as contour lines, cliffs and heights above sea level. |
Settlements | Includes all typologies of settlements from the big city to the rural hamlet, but also taking into account temporary and informal settlements like slums or refugee camps |
Terrestrial | Includes data related to physical properties of the earth and vegetation such as soil moisture, surface temperature, and surface reflectance properties. |
Toponyms | geographical name (toponym of a feature on the Earth) - proper noun applied to a real world entity (INSPIRE 2010) |
Transportation network | The transportation network is a basic layer that displays the network which permits any type of vehicular movements (i.e. roads, railways, airports/airfileds, harbours, etc) |
Other | Additional geospatial information that fall under the In Situ data umbrella (e.g. GCP, GNSS, etc.) |
TBD | To be determined |
name | description | link |
Automatic | Automatic quality check | |
Manual | Manual quality check | |
Semiautomatic | Semiautomatic quality check | |
N/A | Not applicable | |
TBD | To be determined |
name | description |
Draft | This is the state that the object has on its creation. In this state the object and its relations are editable. The owner or one of their teammates can mark as ready the object. |
Ready for validation | In this state the object and its relations cannot be edited. A user different from the owner or their teammates can either mark as valid the object and end the workflow or request changes if that user considers that there is missing information. |
Changes requested | In this state the object and its relations cannot be edited. The owner or one of their teammates can get the object back to the draft state. When an object’s state is changed into “changes requested”, the user requesting the changes can fill a feedback field in which they inform the owner of the object about the changes that should be made. The owner receives an e-mail that their object has requests for changes, the user that made those requests and what changes the user requested (from the feedback field). The users in the application can see this feedback when the object is in state “Changes requested” or “Draft” on the detail page of the object. |
Valid | In this state the object and its relations cannot be edited. The workflow has ended and the object cannot be modified anymore. The object can be placed back in the “Draft” state if the users agree that more changes should be made to it. |
name | description | link |
Demonstrational | Products that are provided to users without any commitment on the quality or availability of the service. Considered to be useful to be disseminated in order to enabling users to test the product and to provide feedback. | Link |
In development | Products that are in development and not yet available to users. | Link |
Pre-operational | Products with documented limitations that are able to satisfy the majority of applicable requirements | Link |
Operational | Products with documented non-relevant limitations that largely satisfy the applicable requirements. | Link |
Discontinued | Products that have been previously (pre-) operationally provided to users but are not (pre-) operational anymore and are considered not useful for further dissemination. | Link |
N/A | Not Applicable | |
TBD | To Be Defined |
name | description | link |
<5 min | ||
< 1 hr | refers to the time expectation for the accessibility of data | |
1 hour | refers to the time expectation for the accessibility of data | |
3 hours | refers to the time expectation for the accessibility of data | |
6 hours | refers to the time expectation for the accessibility of data | |
12 hours | refers to the time expectation for the accessibility of data | |
1 day | refers to the time expectation for the accessibility of data | |
2 days | refers to the time expectation for the accessibility of data | |
3 days | refers to the time expectation for the accessibility of data | |
1 week | refers to the time expectation for the accessibility of data | |
1 month | refers to the time expectation for the accessibility of data | |
6 months | refers to the time expectation for the accessibility of data | |
Latest version available | Not reliant on current data | |
N/A | Not applicable | |
TBD | To be determined |
name | description | link |
<5 min | refer to the time expectation of data update | |
5 min | refer to the time expectation of data update | |
15 min | refer to the time expectation of data update | |
30 min | refer to the time expectation of data update | |
<1 hr | refer to the time expectation of data update | |
Hourly | refer to the time expectation of data update | |
Four times a day | refer to the time expectation of data update | |
2 Hours | refer to the time expectation of data update | |
Twice a day | refer to the time expectation of data update | |
Daily | refer to the time expectation of data update | |
1-5 days | refer to the time expectation of data update | |
Weekly | refer to the time expectation of data update | |
Monthly | refer to the time expectation of data update | |
10-16 days | refer to the time expectation of data update | |
Yearly | refer to the time expectation of data update | |
Continuous | Very near real-time data essential | |
Irregular | Infrequent updates | |
Historical | A historical dataset that is not being updated | |
Periodic Update | Update done when necessary, not on regular basis | |
Single Acquisition | Not reliant on current data | |
N/A | Not applicable | |
TBD | To be determined |