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• 11. Climate Report

  that exhibited the greatest increase in an index of vegetation. Different vegetation types react differently, for instance in some environments, an increase in shrubs and vascular plants may lead to a decrease in mosses and lichens. Experiments that use geothermal heating to examine the effects of warming dry soils on vegetation found ecosystems to have substantial tolerance to warming /climatology/iceland/climate-report/

• 12. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  and the various scenarios of greenhouse gas emissions therefore still stay relatively close to one another for the next few decades. On the 3 other hand, the atmospheric concentrations of carbon dioxide and other long-lived greenhouse gases react relatively slowly to the changes in emissions. Modelling uncertainty is in the short run more important than scenario uncertainty, and it also increases /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 13. raisanen_ruosteenoja_CES_D2.2

  -lived greenhouse gases react relatively slowly to the changes in emissions. Modelling uncertainty is in the short run more important than scenario uncertainty, and it also increases with time. The larger the greenhouse gas forcing becomes, the larger absolute effect model errors will have in simulating the response to this forcing. Analogously, the modelling uncertainty is (in the long run /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 14. GA_2009_91A_4_Andreassen

  of ice melt at the AWS location will increase from c. 40 to c. 80 days. Key words: glacier, mass balance, albedo, temperature, precipita-tion, precipitation, climate IntroductionTo predict how a glacier will react to climate change or to reconstruct a glacier’s mass balanceback in time, a mass balance model is needed to relate the surface mass balance to prevailing cli- mate conditions. A whole /media/ces/GA_2009_91A_4_Andreassen.pdf

• 15. VI_2020_005

  Brown, et al., 2018; Wong et al., 2014). One of these challenges is the increased frequency of oceanic floods. The more frequent high sea level events further generate in- creased flooding and/or erosion risk and will affect marine ecosystems. Hence, coastal communities can be significantly impacted and need to react to the changes (Wahl, Brown, et al., 2018). A further complication follows /media/vedurstofan-utgafa-2020/VI_2020_005.pdf