000 02448nab a22003737a 4500
999 _c61929
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008 180103s2013 xxk|||p|op||| 00| 0 eng d
022 _a1758-678X
022 _a1758-6798 (Online)
024 8 _ahttps://doi.org/10.1038/nclimate1876
040 _aMX-TxCIM
041 _aeng
100 1 _913378
_aMahlstein, I.
245 1 0 _aPace of shifts in climate regions increases with global temperature
260 _aLondon (United Kingdom) :
_bNature Publishing Group,
_c2013.
500 _aPeer review
520 _aHuman-induced climate change causes significant changes in local climates1,2, which in turn lead to changes in regional climate zones. Large shifts in the world distribution of Köppen–Geiger climate classifications by the end of this century have been projected3. However, only a few studies have analysed the pace of these shifts in climate zones4,5, and none has analysed whether the pace itself changes with increasing global mean temperature. In this study, pace refers to the rate at which climate zones change as a function of amount of global warming. Here we show that present climate projections suggest that the pace of shifting climate zones increases approximately linearly with increasing global temperature. Using the RCP8.5 emissions pathway, the pace nearly doubles by the end of this century and about 20% of all land area undergoes a change in its original climate. This implies that species will have increasingly less time to adapt to Köppen zone changes in the future, which is expected to increase the risk of extinction5.
546 _aText in English
650 7 _91045
_aClimate change
_2AGROVOC
650 7 _97940
_aTemperature
_2AGROVOC
650 7 _91558
_aClimate
_2AGROVOC
700 1 _913379
_aDaniel, J.S.
700 1 _913380
_aSolomon, S.
773 0 _gv. 3, no. 8, p. 739-743
_tNature Climate Change
_x1758-6798
_dLondon (United Kingdom) : Nature Publishing Group, 2013.
_wu97377
942 _2ddc
_cJA
_n0