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DOI: 10.1002/2016GL068064
Title:
Fast and slow precipitation responses to individual climate forcers: A PDRMIP multimodel study
Author: Samset B.H.; Myhre G.; Forster P.M.; Hodnebrog Ø.; Andrews T.; Faluvegi G.; Fläschner D.; Kasoar M.; Kharin V.; Kirkevåg A.; Lamarque J.-F.; Olivié D.; Richardson T.; Shindell D.; Shine K.P.; Takemura T.; Voulgarakis A.
Source Publication: Geophysical Research Letters
ISSN: 0094-9205
EISSN: 1944-8936
Indexed By: SCI-E ; EI
Publishing Year: 2016
Volume: 43, Issue:6
pages begin: 2782
pages end: 2791
Language: 英语
Keyword: climate drivers ; PDRMIP ; precipitation
Scopus Keyword: Atmospheric radiation ; Atmospheric temperature ; Carbon dioxide ; Climate change ; Precipitation (chemical) ; Solar radiation ; Anthropogenic climate changes ; Atmospheric absorption ; Global climate model ; Intermodel variability ; PDRMIP ; Precipitation change ; Radiative forcings ; Surface temperature changes ; Climate models ; adsorption ; black carbon ; carbon dioxide ; climate change ; climate forcing ; climate modeling ; global climate ; methane ; precipitation (climatology) ; radiative forcing ; sulfate ; surface temperature
Subject in Chinese: ; 大气辐射 ; 吸收 ; 辐射强迫[作用]) ; 太阳辐射 ; 大气温度 ; 地表温度 ; 降水 ; 二氧化碳 ; 吸附作用 ; 甲烷
Subject: CARBON ; ATMOSPHERIC RADIATION ; ABSORPTION ; RADIATIVE FORCING ; SOLAR RADIATION ; ATMOSPHERIC TEMPERATURE ; SURFACE TEMPERATURE ; PRECIPITATION ; CARBON DIOXIDE ; METHANE
English Abstract: Precipitation is expected to respond differently to various drivers of anthropogenic climate change. We present the first results from the Precipitation Driver and Response Model Intercomparison Project (PDRMIP), where nine global climate models have perturbed CO2, CH4, black carbon, sulfate, and solar insolation. We divide the resulting changes to global mean and regional precipitation into fast responses that scale with changes in atmospheric absorption and slow responses scaling with surface temperature change. While the overall features are broadly similar between models, we find significant regional intermodel variability, especially over land. Black carbon stands out as a component that may cause significant model diversity in predicted precipitation change. Processes linked to atmospheric absorption are less consistently modeled than those linked to top-of-atmosphere radiative forcing. We identify a number of land regions where the model ensemble consistently predicts that fast precipitation responses to climate perturbations dominate over the slow, temperature-driven responses. ©2016. American Geophysical Union. All Rights Reserved.
Related Link: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84971595207&doi=10.1002%2f2016GL068064&partnerID=40&md5=271b6ec3703edffda3a4b8f8884d8bdc
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被引频次[WOS]:49   [查看WOS记录]     [查看WOS中相关记录]
Document Type: 期刊论文
Identifier: http://119.78.100.177/globalchange/handle/2HF3EXSE/10168
Appears in Collections:科学计划与规划
气候变化与战略

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Affiliation: Center for International Climate and Environmental Research, Oslo, Norway

Recommended Citation:
Samset B.H.,Myhre G.,Forster P.M.,et al. Fast and slow precipitation responses to individual climate forcers: A PDRMIP multimodel study[J]. Geophysical Research Letters,2016-01-01,43(6).
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