Enhanced warming over the global subtropical western boundary currents

被引：3

作者：

Lixin Wu

Wenju Cai

Liping Zhang

Hisashi Nakamura

Axel Timmermann

Terry Joyce

Michael J. McPhaden

Michael Alexander

Bo Qiu

Martin Visbeck

Ping Chang

Benjamin Giese

机构：

[1] Physical Oceanography Laboratory,Department of Earth

[2] Ocean University of China,Physical Oceanography Department

[3] CSIRO Marine and Atmosphere Research,Department of Oceanography

[4] Planetary Science,undefined

[5] University of Tokyo,undefined

[6] International Pacific Research Center,undefined

[7] University of Hawaii,undefined

[8] Woods Hole Oceanographic Institution,undefined

[9] National Oceanic and Atmospheric Administration/Pacific Marine Environmental Laboratory,undefined

[10] Seattle,undefined

[11] National Oceanic and Atmospheric Administration/Earth System Research Laboratory,undefined

[12] Leibniz-Institut für Meereswissenschaften,undefined

[13] IFM-GEOMAR,undefined

[14] Texas A&M University,undefined

来源：

Nature Climate Change | 2012年 / 2卷 / 3期

关键词：

D O I：

10.1038/nclimate1353

中图分类号：

学科分类号：

摘要：

An analysis indicates that the warm, powerful currents that flow along the western edges of ocean basins warmed more than twice as quickly than the global ocean as a whole over the past century. This enhanced warming could have important effects on climate because these currents affect the air–sea exchange of heat, moisture and carbon dioxide.

引用

页码：161 / 166

页数：5

共 50 条

[1] Enhanced warming over the global subtropical western boundary currents
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[J]. NATURE CLIMATE CHANGE, 2012, 2 (03) : 161 - 166
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