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Indicator Assessment
Mean annual sea surface temperature trend in European seas
Note: Spatial distribution of sea surface temperature trend over the past 25 years (1987-2011) for the European seas as calculated from the HADISST1 dataset. The units are °C/yr. Source: HADSST1 dataset (http://hadobs.metoffice.com/hadisst/data/download.html), masked where ice coverage constituted more than 20% of the sea water.
Past trends
Sea surface temperature (SST) has been increasing globally and in Europeans seas over the last 100 years at a faster rate than the global ocean. The rate of increase in European seas has been particularly rapid over the last 25 years (Figure 1) [i]. The rate of warming varies across European seas; the fastest warming has been observed in the Black Sea (Figure 2). The observed patterns of change in the subsurface ocean are consistent with changes in the surface ocean in response to climate change and natural variability and with known physical and biogeochemical processes in the ocean [ii].
Projections
It is very likely that globally-averaged surface and vertically-averaged ocean temperatures will further increase in the near-term and beyond. Due to the thermal inertia of the ocean, global SST is projected to rise more slowly than atmospheric temperature [iii].
It is not generally possible to project changes in SST for individual regional seas across Europe due to the insufficient spatial resolution of the applied coupled ocean-climate models. However, detailed projections are available for some regions. For the Baltic Sea, the increase in summer SST during the 21st century under medium to high emissions scenarios is projected to be about 2 °C in the southern parts and about 4 °C in the northern parts [iv].
[i] S. Levitus et al., ‘Global Ocean Heat Content 1955–2008 in Light of Recently Revealed Instrumentation Problems’,Geophysical Research Letters 36, no. 7 (11 April 2009), doi:10.1029/2008GL037155; M. Rhein et al., ‘Observations: Ocean’, inClimate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, ed. T. F. Stocker et al. (Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 2013), Chapter 3, http://www.climatechange2013.org/images/report/WG1AR5_Chapter03_FINAL.pdf; HELCOM,Climate Change in the Baltic Sea Area - HELCOM Thematic Assessment in 2013, Baltic Sea Environment Proceedings (Helsinki: HELCOM, 2013), http://helcom.fi/Lists/Publications/BSEP137.pdf.
[ii] Rhein et al., ‘Observations: Ocean’.
[iii] Gerald A. Meehl et al., ‘Climate Change Projections for the Twenty-First Century and Climate Change Commitment in the CCSM3’,Journal of Climate 19, no. 11 (June 2006): 2597–2616, doi:10.1175/JCLI3746.1; B. Kirtman et al., ‘Near-Term Climate Change: Projections and Predictability’, inClimate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, ed. T. F. Stocker et al. (Cambridge, United Kingdom and New York, NY, USA: Cambridge University Press, 2013), Chapter 11, http://www.climatechange2013.org/images/report/WG1AR5_Chapter11_FINAL.pdf.
[iv] HELCOM,Climate Change in the Baltic Sea Area - HELCOM Thematic Assessment in 2013.
In April 2013 the European Commission presented the EU Adaptation Strategy Package (http://ec.europa.eu/clima/policies/adaptation/what/documentation_en.htm). This package consists of the EU Strategy on adaptation to climate change /* COM/2013/0216 final */ and a number of supporting documents. One of the objectives of the EU Adaptation Strategy is Better informed decision-making, which should occur through Bridging the knowledge gap and Further developing Climate-ADAPT as the ‘one-stop shop’ for adaptation information in Europe. Further objectives include Promoting action by Member States and Climate-proofing EU action: promoting adaptation in key vulnerable sectors. Many EU Member States have already taken action, such as by adopting national adaptation strategies, and several have also prepared action plans on climate change adaptation.
The European Commission and the European Environment Agency have developed the European Climate Adaptation Platform (Climate-ADAPT, http://climate-adapt.eea.europa.eu/) to share knowledge on observed and projected climate change and its impacts on environmental and social systems and on human health; on relevant research; on EU, national and subnational adaptation strategies and plans; and on adaptation case studies.
No targets have been specified.
Sea surface temperature datasets stem from the Hadley Centre (HADISST1 (global)), MOON-ENEA (Mediterranean Sea), and Bundesamt für Seeschifffahrt und Hydrographie (Baltic and North Seas), and MyOcean.
Not applicable
Not applicable
In general, changes related to the physical and chemical marine environment are better documented than biological changes because links between cause and effect are better understood and often time series of observations are longer. For example, systematic observations of both sea-level and sea surface temperature were started around 1880 and are today complemented by observations from space that have high resolution in time and geographical coverage and by Argo floats that also automatically measure temperature and salinity below the ocean surface.
Further information on uncertainties is provided in Section 1.7 of the EEA report on Climate change, impacts, and vulnerability in Europe 2012 (http://www.eea.europa.eu/publications/climate-impacts-and-vulnerability-2012/)
No uncertainty has been specified
For references, please go to https://www.eea.europa.eu/data-and-maps/indicators/sea-surface-temperature-1/assessment-1 or scan the QR code.
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