Model projections of an imminent transition to a more arid climate in southwestern North America

被引:1638
作者
Seager, Richard [1 ]
Ting, Mingfang
Held, Isaac
Kushnir, Yochanan
Lu, Jian
Vecchi, Gabriel
Huang, Huei-Ping
Harnik, Nili
Leetmaa, Ants
Lau, Ngar-Cheung
Li, Cuihua
Velez, Jennifer
Naik, Naomi
机构
[1] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[2] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
[3] Princeton Univ, Dept Geosci, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA
[4] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[5] Tel Aviv Univ, IL-69978 Tel Aviv, Israel
关键词
D O I
10.1126/science.1139601
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
How anthropogenic climate change will affect hydroclimate in the arid regions of southwestern North America has implications for the allocation of water resources and the course of regional development. Here we show that there is a broad consensus among climate models that this region will dry in the 21st century and that the transition to a more arid climate should already be under way. If these models are correct, the levels of aridity of the recent multiyear drought or the Dust Bowl and the 1950s droughts will become the new climatology of the American Southwest within a time frame of years to decades.
引用
收藏
页码:1181 / 1184
页数:4
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