ENSO variability and teleconnections during glacial climates

被引:78
作者
Merkel, Ute [1 ]
Prange, Matthias [1 ,2 ]
Schulz, Michael [1 ,2 ]
机构
[1] MARUM, Ctr Marine Environm Sci, D-28334 Bremen, Germany
[2] Univ Bremen, Fac Geosci, D-28334 Bremen, Germany
关键词
MERIDIONAL OVERTURNING CIRCULATION; PMIP2 COUPLED SIMULATIONS; SEA-SURFACE TEMPERATURE; EL-NINO-LIKE; TROPICAL PACIFIC; THERMOHALINE CIRCULATION; ISOTOPE STAGE-3; FUTURE CLIMATE; SEASONAL CYCLE; ATLANTIC;
D O I
10.1016/j.quascirev.2009.11.006
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Understanding the origin of sub-Milankovitch and millennial-scale abrupt climate change still poses a major challenge. An important role of communicating the orbital-scale forcing into abrupt climate change on millennial and centennial timescales has been hypothesized for the tropics in earlier studies based on the assumption of stationary teleconnections. This paper presents a modelling study for the Last Glacial Maximum and Marine Isotope Stage 3 using the comprehensive climate model CCSM3. Glacial boundary conditions and freshwater hosing at high latitudes of the North Atlantic are imposed to mimic a Heinrich stadial and Dansgaard-Oeschger stadials and interstadials. It is shown that glacial ENSO variability is strongly enhanced by a substantial slowdown of the Atlantic Meridional Overturning Circulation. The simulations also suggest that glacial boundary conditions induce major modifications to ENSO teleconnections and that the "blueprint" of modern ENSO teleconnections should only be applied with caution to glacial climate periods. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:86 / 100
页数:15
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