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External Data Spec

EURO-CORDEX Data

External Data Spec Published 04 Feb 2014
1 min read
EURO-CORDEX data: Climate change projections for Europe based on an ensemble of regional climate model simulations provided by the EURO-CORDEX initiative
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EURO-CORDEX
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https://www.euro-cordex.net/060378/index.php.en
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The dataset URL is not available. Please contact the organisation for further clarification.

Related content

Produced figures

Figure Observed annual mean temperature change from 1960 to 2019 (left panel) and projected 21st century change under different emissions scenarios (right panels) in Europe RCP, representative concentration pathway. Left panel: boxes outlined in black indicate areas with at least three stations, so are more likely to be representative; areas with significant long-term trends are indicated by black dots. Right panel: projected changes in near-surface air temperature by the period 2071-2100, compared with 1971-2000 for RCP4.5 and 8.5 emissions scenarios; simulations are based on the multi-model ensemble average of simulations of the EURO-CORDEX initiative.
Figure Projected change in meteorological drought frequency between the present (1981-2010) and the mid-century 21st century (2041-2070) in Europe, under two emissions scenarios Left map: Scenario RCP4.5; right map: Scenario RCP8.5. The lines represent the areas in which at least two-third of the simulations used agree on the sign of the change.
Figure Projected linear trend in heating (HDD) and cooling degree days (CDD) over the period 1981-2100 under two scenarios These maps show the trend in heating degree days (left) and cooling degree days (right) from 1981-2100 for all EEA member and cooperating countries, based on the median of an ensemble of 11 EURO-CORDEX simulations.
Figure Projected change in the frequency of meteorological droughts The maps show changes in the frequency of meteorological droughts for two future periods (2041-2070, left and 2071-2100, right) and for two emissions scenarios (RCP4.5, top and RCP8.5, bottom). Drought frequency is defined as the number of months in a 30 year period with the Standardised Precipitation Index accumulated over a 6 month period (SPI-6) having a value below -2.
Figure Projected changes in annual mean temperature (left) and annual precipitation (right) Projected changes are for 2071-2100, compared to 1971-2000, based on the average of a multi-model ensemble forced with the RCP8.5 high emissions scenario. All changes marked with a colour (i.e. not white) are statistically significant. Individual models from the EURO-CORDEX ensemble or high-resolution models for smaller regions may show different results.
Figure Projected changes in heavy precipitation in winter and summer Projected changes in heavy precipitation (in %) in winter and summer from 1971-2000 to 2071–2100 for the RCP8.5 scenario based on the ensemble mean of different regional climate models (RCMs) nested in different general circulation models (GCMs).
Figure Projected change in the length of dry spells Projected changes in the length of dry spell (in days) from 1971-2000 to 2071–2100 for the RCP8.5 scenario based on the ensemble mean of different regional climate models (RCMs) nested in different general circulation models (GCMs).
Figure Projected changes in annual, summer and winter temperature Projected changes in annual (left), summer (middle) and winter (right) near-surface air temperature (°C) in the period 2071-2100, compared with the baseline period 1971-2000 for the forcing scenarios RCP 4.5 (top) and RCP 8.5 (bottom). Model simulations are based on the multi-model ensemble average of RCM simulations from the EURO-CORDEX initiative.
Figure Projected change in annual and summer precipitation Projected changes in annual (left) and summer (right) precipitation (%) in the period 2071-2100 compared to the baseline period 1971-2000 for the forcing scenario RCP 8.5. Model simulations are based on the multi-model ensemble average of RCM simulations from the EURO-CORDEX initiative.
Figure
Draft
Observed annual mean temperature change from 1960 to 2019 (left panel) and projected change under different emissions scenarios (right panels) in Europe Left panel: boxes outlined in black indicate areas with at least three stations, so are more likely to be representative; areas with significant long-term trends are indicated by black dots. Right panel: projected changes in near-surface air temperature by the period 2071-2100, compared with 1971-2000 for RCP4.5 (Representative Concentration Pathway) and 8.5 emissions scenarios; simulations are based on the multi-model ensemble average of simulations of the EURO-CORDEX initiative.
Figure
Draft
Projected change in meteorological drought frequency between the periods 1981-2010 and 2041-2070 under two climate change scenarios Left map: Scenario RCP4.5 (Representative Concentration Pathway). Right map: Scenario RCP8.5 (Representative Concentration Pathway).The line pattern represents the areas in which at least two-third of the simulations used agree on the sign of the change.

See also

Used in indicators

Indicator Specification Heating and cooling degree days This indicator looks at the following: Time series of population-weighted heating and cooling degree days averaged over Europe; Observed trends in heating and cooling degree days; Projected trends in heating and cooling degree days.
Indicator Specification
Archived
Global and European temperature This indicator shows absolute changes and rates of change in average near-surface temperature for the globe and for a region covering Europe. Near-surface air temperature gives one of the clearest and most consistent signals of global and regional climate change, especially in recent decades. It has been measured for many decades — even centuries at some locations — and a dense network of stations across the globe, especially in Europe, provides regular monitoring of temperature, using standardised measurements, quality control and homogeneity procedures. Global average annual temperature deviations (anomalies) are discussed relative to a ‘pre-industrial’ period between 1850 and 1899 (the beginning of instrumental temperature records). During this time, anthropogenic greenhouse gases from the industrial revolution (between 1750 and 1850) are considered to have had a relatively small influence on the climate compared with natural influences. However, it should be noted that owing to earlier changes in the climate due to internal and forced natural variability, there was not one single pre-industrial climate and it is not clear that there is a rigorous scientific definition of the term ‘pre-industrial climate’. Temperature changes also influence other aspects of the climate system that can have an impact on human activities, including sea level, intensity and frequency of floods and droughts, biota and food productivity, and infectious diseases. In addition to the global average target, seasonal variations and spatial distributions of temperature change are important, for example, to understand the risks that the current climate poses to human and natural systems, and to assess how these may be impacted by future climate change.
Indicator Specification Global and European temperature This indicator shows absolute changes and rates of change in average near-surface temperature for the globe and for a region covering Europe. Near-surface air temperature gives one of the clearest and most consistent signals of global and regional climate change, especially in recent decades. It has been measured for many decades — even centuries at some locations — and a dense network of stations across the globe, especially in Europe, provides regular monitoring of temperature, using standardised measurements, quality control and homogeneity procedures. Global average annual temperature deviations (anomalies) are discussed relative to a ‘pre-industrial’ period between 1850 and 1899 (the beginning of instrumental temperature records). During this time, anthropogenic greenhouse gases from the industrial revolution (between 1750 and 1850) are considered to have had a relatively small influence on the climate compared with natural influences. However, it should be noted that owing to earlier changes in the climate due to internal and forced natural variability, there was not one single pre-industrial climate and it is not clear that there is a rigorous scientific definition of the term ‘pre-industrial climate’. Temperature changes also influence other aspects of the climate system that can have an impact on human activities, including sea level, intensity and frequency of floods and droughts, biota and food productivity, and infectious diseases. In addition to the global average target, seasonal variations and spatial distributions of temperature change are important, for example, to understand the risks that current climate poses to human and natural systems and to assess how these may be impacted by future climate change.
Indicator Specification Heavy precipitation in Europe Heavy precipitation is defined as the maximum annual 5-day consecutive precipitation. Trends are calculated for the period between 1960 and 2015. Projected changes in heavy precipitation are defined as changes in the 95th percentile of daily precipitation (only days with precipitation >1 mm/day are considered). Changes between the 1971-2000 and 2071-2100 are calculated using a multi-model ensemble forced by RCP8.5.
Indicator Specification Mean precipitation Observed trends in annual and summer precipitation across Europe 1960-2015 Projected changes in mean annual and summer precipitation (%) in the period 2071–2100 compared with the baseline period 1971–2000 for the forcing scenario RCP8.5. Model simulations are based on the multi-model ensemble average of many different RCM simulations from the EURO-CORDEX initiative.
Indicator Specification
Archived
Global and European temperature This indicator shows absolute changes and rates of change in average near-surface temperature for the globe and for a region covering Europe. Near-surface air temperature gives one of the clearest and most consistent signals of global and regional climate change, especially in recent decades. It has been measured for many decades - even centuries at some locations - and a dense network of stations across the globe, especially in Europe, provides regular monitoring of temperature, using standardised measurements, quality control and homogeneity procedures. Global average annual temperature deviations, ‘anomalies’, are discussed relative to a ‘pre-industrial’ period between 1850 and 1899 (the beginning of instrumental temperature records). During this time, anthropogenic greenhouse gases from the industrial revolution (between 1750 and 1850) are considered to have a relatively small influence on the climate compared to natural influences. However, it should be noted that owing to earlier changes in the climate due to internal and forced natural variability, there was not one single pre-industrial climate and it is not clear that there is a rigorous scientific definition of the term ‘pre-industrial climate’. Temperature changes also influence other aspects of the climate system that can have an impact on human activities, including sea level, intensity and frequency of floods and droughts, biota and food productivity, and infectious diseases. In addition to the global average target, seasonal variations and spatial distributions of temperature change are important, for example, to understand the risks that current climate poses to human and natural systems and to assess how these may be impacted by future climate change.
Indicator Specification
Archived
Global and European temperatures This indicator shows absolute changes and rates of change in average near-surface temperature for the globe and for a region covering Europe. Near-surface air temperature gives one of the clearest and most consistent signals of global and regional climate change, especially in recent decades. It has been measured for many decades or even centuries at some locations and a dense network of stations across the globe, and especially in Europe, provide regular monitoring of temperature, using standardised measurements, quality control and homogeneity procedures. This indicator provides guidance for the following policy-relevant questions:  Will the global average temperature increase stay within the UNFCCC policy target of 2.0°C above pre-industrial levels?  Will the rate of global average temperature increase stay below the indicative proposed target of 0.2°C increase per decade? Temperature changes also influence other aspects of the climate system which can impact on human activities, such as sea level rise, intensity and frequency of floods and droughts, biota and crop productivity and vector-borne diseases. In consideration with the target of limiting the rise in global average temperature, understanding seasonal variations and spatial distributions of temperature change are important, for example to manage the risks that current climate poses to human and natural systems and to assess how these may be impacted by future climate change.
Indicator Specification
Archived
Precipitation extremes Trends in consecutive wet days and consecutive dry days Projected changes in heavy precipitation in summer and winter
Indicator Specification
Archived
Mean precipitation Trends in annual precipitation across Europe Projected changes in annual and summer precipitation
Indicator Specification
Archived
Global and European temperature This indicator shows absolute changes and rates of change in average near-surface temperature for the globe and for a region covering Europe. Near-surface air temperature gives one of the clearest and most consistent signals of global and regional climate change, especially in recent decades. It has been measured for many decades or even centuries at some locations and a dense network of stations across the globe, and especially in Europe, provide regular monitoring of temperature, using standardised measurements, quality control and homogeneity procedures. This indicator provides guidance for the following policy-relevant questions:  Will the global average temperature increase stay within the UNFCCC policy target of 2.0°C above pre-industrial levels?  Will the rate of global average temperature increase stay below the indicative proposed target of 0.2°C increase per decade? Global average annual temperature deviations, ‘anomalies’, are discussed relative to a ‘pre-industrial’ period between 1850 and 1899 (beginning of instrumental temperature records).  During this time, anthropogenic greenhouse gases from the industrial revolution (between 1750 and 1850) are considered to have a relatively small influence on climate compared to natural influences. However it should be noted that owing to earlier changes in the climate due to internal and forced natural variability there was not one single pre-industrial climate and it is not clear that there is a rigorous scientific definition of the term ‘pre-industrial climate’. Temperature changes also influence other aspects of the climate system which can impact on human activities, including sea level, intensity and frequency of floods and droughts, biota and food productivity and infectious diseases. In addition to the global average target, seasonal variations and spatial distributions of temperature change are important, for example to understand the risks that current climate poses to human and natural systems and to assess how these may be impacted by future climate change.

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