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Figure Annual, winter (December, January, February) and summer (June, July, August) mean temperature deviations in Europe, 1860-2010 (°C)
The lines refer to 10-year moving average European land.
Located in Data and maps Maps and graphs
Figure Observed global annual average temperature deviations in the period 1850–2010 (in ºC)
In blue, the source of the original anomalies is the combined UK Met Office Hadley Centre and Climate Research Unit dataset, HadCRUT3. The global mean annual temperature deviations are in relation to the base period 1961-1990. In red, the source of the original anomalies is NASA's GISS dataset. The anomalies are in the source in relation to the base period 1951-1980. The global mean annual temperature deviations have been adjusted to be relative to the period 1850-1899 (HadCRUT3) and 1880 - 1899 (NASA's GISS). All original data is rounded to the nearest 2 decimal places. The trend lines show the 10-year centred moving average of the original anomalies for both datasets relative to the period 1880-1899. The dotted lines show the annual anomalies of the HadCRUT3 (blue) data set and GISS (red) respectively.
Located in Data and maps Maps and graphs
Figure European annual average temperature deviations, 1850-2010, relative to the 1850-1899 average (in °C).
The lines refer to 10-year moving average, the bars to the annual 'land only' European average. The source of the original data is the Climatic Research Unit of the University of East Anglia. The European mean annual temperature deviations are in the source in relation to the base period 1961-1990. The annual deviations shown in the chart have been adjusted to be relative to the period 1850-1899 to better monitor the EU objective not to exceed 2°C above pre-industrial values. Over Europe average annual temperatures during the real pre-industrial period (1750-1799) were very similar to those during 1850-99. Europe is defined as the area between 35° to 70° Northern latitude, -25° to 30° Eastern longitude, plus Turkey (=35° to 40° North, 30° to 45° East). The resulting temperature anomalies were obtained using KNMI's climate explorer.
Located in Data and maps Maps and graphs
Indicator Assessment Global and European temperature (CSI 012/CLIM 001) - Assessment published May 2011
Global The global (land and ocean) average temperature increase between 1850 and 2010 was 0.81 0 C using combined UK Met Office Hadley centre and University of East Anglia - Climate Research Unit HadCRUT3 dataset compared to the 1850 - 1899 period average temperature and 0.89 0 C using Goddard Institute for Space Studies - GISS dataset compared to the 1880 - 1899 period average temperature.  All used temperature records show the 2000s decade (2001 - 2010) was the warmest decade. For the HadCRUT3 and GISS datasets the rate of the global average has increased from around 0.06 0 C per decade over last 100 years, to 0.18 - 0.22 0 C in last decade. The best estimates for projected global warming in this century are a further rise in the global average temperature from 1.8 to 4.0 0 C for different scenarios that assume no further/additional action to limit emissions. The EU global temperature target is projected to be exceeded between 2040 and 2060, taking into account all six IPCC scenarios. Europe Europe has warmed more than the global average. The average temperature for the European land area for the last decade (2001 - 2010) was 1.2 °C above the 1850 - 1899 average, and for the combined land and ocean area 1.0 °C above. Considering the land area, 8 out of the last 13 years were among the warmest years since 1850. High-temperature extremes like hot days, tropical nights, and heat waves have become more frequent, while low - temperature extremes (e.g. cold spells, frost days) have become less frequent in Europe. The average length of summer heat waves over Western Europe doubled over the period 1850 to 2010 and the frequency of hot days almost tripled. The annual average temperature in Europe is projected to rise in this century with the largest warming over eastern and northern Europe in winter, and over Southern Europe in summer. High temperature events across Europe including temperature extremes such as heat waves are projected to become more frequent, intense and longer this century, whereas winter temperature variability and the number of cold and frost extremes are projected to decrease further. According to the projections, the most affected European regions are going to be the Iberian and the Apennine Peninsula and south - eastern Europe.  
Located in Data and maps Indicators Global and European temperature
Article Forests and their forgotten communities
In May 2008 a helicopter flew over unexplored parts of the Amazon in Acre State in Brazil, near the country’s border with Peru. Onboard were officials from Funai, the Brazilian government's Indian affairs department, on a mission to prove the existence of unknown Amazonian tribes who have never been in contact with the outside world. The few aerial pictures Funai has released show startled and intrigued people and their huts but do not reveal any landmarks which could be used to identify the exact location.
Located in Articles
Article Urban soil sealing in Europe
Soil is the earth's living skin and provides us with essential services for life in our planet: production of food; infiltration and cleansing of water and protection against flooding; habitat for plants; areas for recreation and mental health; micro climate regulation, etc. It is such a crucial resource that it can't be ignored. However, particularly in urban areas, soil is being sealed off with increasing housing and infrastructure.
Located in Articles
SOER Key fact (Deprecated) Adapting to climate change - key fact 3
So far, 11 European countries, and a few regions and cities, have adopted climate adaptation strategies.
Located in The European environment — state and outlook 2015 Adapting to climate change - SOER 2010 thematic assessment Key facts
Figure object code Projected CH4 emissions from 1990 to 2030 , RAINS model - most feasible reduction scenario
Located in Data and maps Maps and graphs
Figure Observed changes in frost days indices 1976-2009 (in days per decade)
Frost day is defined as a day with an average temperature below 0 ºC. Frost days are defined as a day with an average temperature below 0 ºC.
Located in Data and maps Maps and graphs
Indicator Assessment Global and European temperature (CSI 012/CLIM 001) - Assessment published Jun 2010
Global The global (land and ocean) average temperature increase between 1850 and 2009 was 0.74 0 C using combined Hadley centre and CRU datasets compared to the 1850 - 1899 period average temperature and 0.84 0 C using GISS dataset compared to the 1880 - 1899 period average temperature.  All used temperature records show the 2000s decade (2000 - 2009) was the warmest decade. The rate of global average temperature change has increased from around 0.06 0 C per decade over last 100 years, to 0.16 - 0.20 0 C in last decade. The best estimates for projected global warming in this century are a further rise in the global average temperature from 1.8 to 4.0 0 C for different scenarios that assume no further/additional action to limit emissions. The EU global temperature target is projected to be exceeded between 2040 and 2060, taking into account all six IPCC scenarios. Europe Europe has warmed more than the global average. The annual average temperature for the European land area up to 2009 was 1.3 0 C above 1850 - 1899 average temperature, and for the combined land and ocean area 1 0 C above. Considering the land area, nine out of the last 12 years were among the warmest years since 1850. High-temperature extremes like hot days, tropical nights, and heat waves have become more frequent, while low - temperature extremes (e.g. cold spells, frost days) have become less frequent in Europe. The average length of summer heat waves over Western Europe doubled over the period 1850 to 2009 and the frequency of hot days almost tripled. The annual average temperature in Europe is projected to rise in this century with the largest warming over eastern and northern Europe in winter, and over Southern Europe in summer. High temperature events across Europe including temperature extremes such as heat waves are projected to become more frequent, intense and longer this century, whereas winter temperature variability and the number of cold and frost extremes are projected to decrease further. According to the projections, the most affected European regions are going to be the Iberian and the Apennine Peninsula and south - eastern Europe.
Located in Data and maps Indicators Global and European temperature
European Environment Agency (EEA)
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