Elevation-dependent warming in mountainregions of the world

doi:10.1038/NCLIMATE2563

IEECAS OpenIR > 古环境研究室

	Elevation-dependent warming in mountainregions of the world
	Pepin,N[1]; Bradley,R.S.[2]; Diaz,H.F.[3]; Baraer,M.[4]; Caceres,E.B.[5]; Forsythe,N.[6]; Fowler,H.[6]; Greenwood,G.[7]; Hashmi,M.Z.[8]; Liu,XD[9]; Miller,J.R.[10]; Ning,L.[11]; Ohmura[12]; Palazzi,E.[13]; Rangwala,I.[14]; Schöner,W.[15]; Severskiy,I.[16]; Shahgedanova,M.[17]; Wang,MB[18]; Williamson,SN[19]; Yang,DQ[20]
	2015-05
发表期刊	NATURE CLIMATE CHANGE
卷号	5 期号:2015 页码:424-430
文章类型	期刊论文
摘要	There is growing evidence that the rate of warming is amplifed with elevation, such that high-mountain environments experience more rapid changes in temperature than environments at lower elevations. Elevation-dependent warming (EDW) can accelerate the rate of change in mountain ecosystems, cryospheric systems, hydrological regimes and biodiversity. Here we review important mechanisms that contribute towards EDW: snow albedo and surface-based feedbacks; water vapour changes and latent heat release; surface water vapour and radiative ﬂux changes; surface heat loss and temperature change; and aerosols. All lead to enhanced warming with elevation (or at a critical elevation), and it is believed that combinations of these mechanisms may account for contrasting regional patterns of EDW. We discuss future needs to increase knowledge of mountain temperature trends and their controlling mechanisms through improved observations, satellite-based remote sensing and model simulations.
DOI	10.1038/NCLIMATE2563
收录类别	SCI
语种	英语
引用统计	被引频次：1687[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/9462
专题	古环境研究室
作者单位	1.Department of Geography, Buckingham Building, Lion Terrace, University of Portsmouth, Portsmouth PO1 3HE, UK; 2.Climate System Research Center,University of Massachusetts, Amherst, Massachusetts 01003, USA; 3.CIRES, National Oceanic and Atmospheric Administration, Boulder, Colorado 80305,USA; 4.ETS–University of Quebec, Montreal, Quebec H3C 1K3, Canada; 5.Instituto Nacional de Meterología e Hidrología, Loja, Iñaquito 700 y Corea, Ecuador; 6.School of Civil Engineering and Geosciences, Newcastle University, Newcastle upon Tyne NE1 7RU, UK; 7.University of Bern, 3012 Bern, Switzerland; 8.Water Resources Section, Global Change Impact Studies Centre (GCISC), PO BOX 3022, Islamabad, Pakistan; 9.SKLLQG, Institute of Earth Environment,Chinese Academy of Sciences and CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China; 10.Department of Marine and CoastalSciences, Rutgers University, New Jersey 08901, USA; 11.University of Massachusetts, Amherst, Massachusetts 01003, USA; 12.ETH Zurich, 8092 Zurich,Switzerland; 13.Institute of Atmospheric Sciences and Climate – National Research Council (ISAC-CNR), I-10133 Torino, Italy; 14.CIRES/Western WaterAssessment; Physical Sciences Division, NOAA ESRL, Boulder, Colorado 80305, USA; 15.University of Graz, 8010 Graz, Austria; 16.Institute of Geography,050010 Almaty, Kazakhstan; 17.University of Reading, Reading RG6 6AH, UK; 18.Shanxi University, 030006 Taiyuan, China; 19.University of Alberta, Edmonton, Alberta TG6 2R3, Canada; 20.National Hydrology Research Centre, Environment Canada, S7N 3H5 Saskatoon, Canada
推荐引用方式 GB/T 7714	Pepin,N[1],Bradley,R.S.[2],Diaz,H.F.[3],et al. Elevation-dependent warming in mountainregions of the world[J]. NATURE CLIMATE CHANGE,2015,5(2015):424-430.
APA	Pepin,N[1].,Bradley,R.S.[2].,Diaz,H.F.[3].,Baraer,M.[4].,Caceres,E.B.[5].,...&Yang,DQ[20].(2015).Elevation-dependent warming in mountainregions of the world.NATURE CLIMATE CHANGE,5(2015),424-430.
MLA	Pepin,N[1],et al."Elevation-dependent warming in mountainregions of the world".NATURE CLIMATE CHANGE 5.2015(2015):424-430.

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