Tropical cooling at the last glacial maximum and extratropical ocean ventilation

Zhengyu Liu; Sang Ik Shin; Bette Otto-Bliesner; John E. Kutzbach; Esther C. Brady; Dong Eun Lee

doi:10.1029/2001gl013938

Tropical cooling at the last glacial maximum and extratropical ocean ventilation

Zhengyu Liu
, Sang Ik Shin
, Bette Otto-Bliesner
, John E. Kutzbach
, Esther C. Brady
, Dong Eun Lee

Paleo and Polar Climate

Research output: Contribution to journal › Article › peer-review

43 Scopus citations

Abstract

The NCAR CSM is used to simulate the climate at Last Glacial Maximum. The CSM simulates a tropical SST cooling of 2.1°C. It is shown that about half of this tropical cooling is associated with the upper ocean circulation, especially the ventilation of thermocline and intermediate waters from the mid/ high latitude South Pacific.

Original language	English
Pages (from-to)	48-1-48-4
Journal	Geophysical Research Letters
Volume	29
Issue number	10
DOIs	https://doi.org/10.1029/2001gl013938
State	Published - May 15 2002

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10.1029/2001gl013938

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title = "Tropical cooling at the last glacial maximum and extratropical ocean ventilation",

abstract = "The NCAR CSM is used to simulate the climate at Last Glacial Maximum. The CSM simulates a tropical SST cooling of 2.1°C. It is shown that about half of this tropical cooling is associated with the upper ocean circulation, especially the ventilation of thermocline and intermediate waters from the mid/ high latitude South Pacific.",

author = "Zhengyu Liu and Shin, \{Sang Ik\} and Bette Otto-Bliesner and Kutzbach, \{John E.\} and Brady, \{Esther C.\} and Lee, \{Dong Eun\}",

year = "2002",

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doi = "10.1029/2001gl013938",

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journal = "Geophysical Research Letters",

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AU - Liu, Zhengyu

AU - Shin, Sang Ik

AU - Otto-Bliesner, Bette

AU - Kutzbach, John E.

AU - Brady, Esther C.

AU - Lee, Dong Eun

PY - 2002/5/15

Y1 - 2002/5/15

N2 - The NCAR CSM is used to simulate the climate at Last Glacial Maximum. The CSM simulates a tropical SST cooling of 2.1°C. It is shown that about half of this tropical cooling is associated with the upper ocean circulation, especially the ventilation of thermocline and intermediate waters from the mid/ high latitude South Pacific.

AB - The NCAR CSM is used to simulate the climate at Last Glacial Maximum. The CSM simulates a tropical SST cooling of 2.1°C. It is shown that about half of this tropical cooling is associated with the upper ocean circulation, especially the ventilation of thermocline and intermediate waters from the mid/ high latitude South Pacific.

UR - https://www.scopus.com/pages/publications/0037095903

U2 - 10.1029/2001gl013938

DO - 10.1029/2001gl013938

M3 - Article

AN - SCOPUS:0037095903

SN - 0094-8276

VL - 29

SP - 48-1-48-4

JO - Geophysical Research Letters

JF - Geophysical Research Letters

IS - 10

ER -

Tropical cooling at the last glacial maximum and extratropical ocean ventilation

Abstract

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