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DOI	10.1175/JCLI-D-19-0232.1
	The role of zonally averaged climate change in contributing to intermodel spread in CMIP5 predicted local precipitation changes
	Garfinkel C.I.; Adam O.; Morin E.; Enzel Y.; Elbaum E.; Bartov M.; Rostkier-Edelstein D.; Dayan U.
发表日期	2020
ISSN	0894-8755
起始页码	1141
结束页码	1154
卷号	33 期号:3
英文摘要	While CMIP5 models robustly project drying of the subtropics and more precipitation in the tropics and subpolar latitudes by the end of the century, the magnitude of these changes in precipitation varies widely across models: for example, some models simulate no drying in the eastern Mediterranean while others simulate more than a 50% reduction in precipitation relative to the model-simulated present-day value. Furthermore, the factors leading to changes in local subtropical precipitation remain unclear. The importance of zonal-mean changes in atmospheric structure for local precipitation changes is explored in 42 CMIP5 models. It is found that up to half of the local intermodel spread over the Mediterranean, northern Mexico, East Asia, southern Africa, southern Australia, and southern South America is related to the intermodel spread in large-scale processes such as the magnitude of globally averaged surface temperature increases, Hadley cell widening, polar amplification, stabilization of the tropical upper troposphere, or changes in the polar stratosphere. Globally averaged surface temperature increases account for intermodel spread in land subtropical drying in the Southern Hemisphere but are not important for land drying adjacent to the Mediterranean. The factors associated with drying over the eastern Mediterranean and western Mediterranean differ, with stabilization of the tropical upper troposphere being a crucial factor for the former only. Differences in precipitation between the western and eastern Mediterranean are also evident on interannual time scales. In contrast, the global factors examined here are unimportant over most of the United States, and more generally over the interior of continents. Much of the rest of the spread can be explained by variations in local relative humidity, a proxy also for zonally asymmetric circulation and thermodynamic changes. © 2020 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).
英文关键词	Atmospheric humidity; Atmospheric structure; Atmospheric temperature; Climate models; Drying; Stabilization; Surface properties; Tropics; Troposphere; Eastern Mediterranean; Interannual time scale; Polar amplifications; Precipitation change; Southern south america; Surface temperatures; Thermodynamic changes; Western Mediterranean; Climate change; atmospheric modeling; climate change; CMIP; computer simulation; precipitation (climatology); prediction; Southern Hemisphere; stratosphere; troposphere; Australia; Far East; Mediterranean Region; Mexico [North America]; South America; Southern Africa
语种	英语
来源期刊	Journal of Climate
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/171475
作者单位	Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University, Jerusalem, Israel; Department of Natural Sciences, Open University of Israel, Raanana, Israel; Department of Applied Mathematics, Environmental Sciences Division, Israel Institute for Biological Research, Ness-Ziona, Israel; Department of Geography, Hebrew University, Jerusalem, Israel
推荐引用方式 GB/T 7714	Garfinkel C.I.,Adam O.,Morin E.,et al. The role of zonally averaged climate change in contributing to intermodel spread in CMIP5 predicted local precipitation changes[J],2020,33(3).
APA	Garfinkel C.I..,Adam O..,Morin E..,Enzel Y..,Elbaum E..,...&Dayan U..(2020).The role of zonally averaged climate change in contributing to intermodel spread in CMIP5 predicted local precipitation changes.Journal of Climate,33(3).
MLA	Garfinkel C.I.,et al."The role of zonally averaged climate change in contributing to intermodel spread in CMIP5 predicted local precipitation changes".Journal of Climate 33.3(2020).