气候变化领域集成服务门户(CCPortal): Response of global evaporation to major climate modes in historical and future Coupled Model Intercomparison Project Phase 5 simulations

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DOI	10.5194/hess-24-1131-2020
	Response of global evaporation to major climate modes in historical and future Coupled Model Intercomparison Project Phase 5 simulations
	Le T.; Bae D.-H.
发表日期	2020
ISSN	1027-5606
起始页码	1131
结束页码	1143
卷号	24 期号:3
英文摘要	Climate extremes, such as floods and droughts, might have severe economic and societal impacts. Given the high costs associated with these events, developing early-warning systems is of high priority. Evaporation, which is driven by around 50% of solar energy absorbed at surface of the Earth, is an important indicator of the global water budget, monsoon precipitation, drought monitoring and the hydrological cycle. Here we investigate the response of global evaporation to main modes of interannual climate variability, including the Indian Ocean Dipole (IOD), the North Atlantic Oscillation (NAO) and the El Niño-Southern Oscillation (ENSO). These climate modes may have an influence on temperature, precipitation, soil moisture and wind speed and are likely to have impacts on global evaporation. We utilized data of historical simulations and RCP8.5 (representative concentration pathway) future simulations derived from the Coupled Model Intercomparison Project Phase 5 (CMIP5). Our results indicate that ENSO is an important driver of evaporation for many regions, especially the tropical Pacific. The significant IOD influence on evaporation is limited in western tropical Indian Ocean, while NAO is more likely to have impacts on evaporation of the North Atlantic European areas. There is high agreement between models in simulating the effects of climate modes on evaporation of these regions. Land evaporation is found to be less sensitive to considered climate modes compared to oceanic evaporation. The spatial influence of major climate modes on global evaporation is slightly more significant for NAO and the IOD and slightly less significant for ENSO in the 1906-2000 period compared to the 2006-2100 period. This study allows us to obtain insight about the predictability of evaporation and hence, may improve the early-warning systems of climate extremes and water resource management. © 2020 Authors.
语种	英语
scopus关键词	Atmospheric pressure; Budget control; Climatology; Drought; Evaporation; Oceanography; Soil moisture; Solar energy; Tropics; Water management; Wind; Coupled Model Intercomparison Project; Historical simulation; Indian ocean dipoles; Interannual climate variability; Monsoon precipitation; North Atlantic oscillations; Tropical Indian ocean; Waterresource management; Climate models; air-sea interaction; climate modeling; drought; early warning system; evaporation; flood; Indian Ocean Dipole; Indian Ocean tsunami 2004; North Atlantic Oscillation; Atlantic Ocean; Atlantic Ocean (North); Pacific Ocean; Pacific Ocean (Tropical)
来源期刊	Hydrology and Earth System Sciences
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/159477
作者单位	Le, T., Department of Civil and Environmental Engineering, Sejong University, Seoul, South Korea, Climate Change Adaptation for Water Resources, Sejong University, Seoul, South Korea; Bae, D.-H., Department of Civil and Environmental Engineering, Sejong University, Seoul, South Korea, Climate Change Adaptation for Water Resources, Sejong University, Seoul, South Korea
推荐引用方式 GB/T 7714	Le T.,Bae D.-H.. Response of global evaporation to major climate modes in historical and future Coupled Model Intercomparison Project Phase 5 simulations[J],2020,24(3).
APA	Le T.,&Bae D.-H..(2020).Response of global evaporation to major climate modes in historical and future Coupled Model Intercomparison Project Phase 5 simulations.Hydrology and Earth System Sciences,24(3).
MLA	Le T.,et al."Response of global evaporation to major climate modes in historical and future Coupled Model Intercomparison Project Phase 5 simulations".Hydrology and Earth System Sciences 24.3(2020).