The Tropics in Paleoclimate

被引:101
作者
Chiang, John C. H. [1 ,2 ]
机构
[1] Univ Calif Berkeley, Dept Geog, Berkeley, CA 94720 USA
[2] Univ Calif Berkeley, Ctr Atmospher Sci, Berkeley, CA 94720 USA
关键词
paleoclimatology; tropical climate dynamics; abrupt climate change; El Nino-Southern Oscillation; SEA-SURFACE TEMPERATURE; NINO-SOUTHERN OSCILLATION; OCEAN-ATMOSPHERE SYSTEM; LAST GLACIAL MAXIMUM; EL-NINO; CLIMATE-CHANGE; THERMOHALINE CIRCULATION; ENSO SUPPRESSION; AFRICAN MONSOON; PACIFIC;
D O I
10.1146/annurev.earth.031208.100217
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The past decade saw a surge ill interest in the role of the Tropics in paleoclimate changes. This was motivated by the emergence of outstanding questions in paleoclimate that pointed to a role for the Tropics in addition to advances in tropical climate dynamics. This article reviews these developments, starting from a historical perspective. Three properties of tropical dynamics are prominent in paleoclimate: the sensitivity of the tropical climate to change; the ability of the tropical climate to reorganize; and the ability of the tropical climate to project its influence globally. The El Nino-Southern Oscillation (ENSO) system exemplifies these properties, making ENSO particularly prominent in paleoclimate. Summaries of three paleoclimate cases in which the science developed over the past decade-mid-Holocene ENSO, abrupt climate change during the most recent glacial period,and the mid-Pliocene permanent El Nino scenario-illustrate how the tropical hypothesis worked its way into paleoclimate research. This review closes with a discussion of prevailing views of the Tropics in the paleoclimate changes.
引用
收藏
页码:263 / 297
页数:35
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