PCMDI

CAPT

Cloud Feedbacks

CMIP5

CMIP3

Other MIPs

Software

Publications

Google Calendar

Lab Calendar


Site Map

UCRL-WEB-152471

Privacy & Legal Notice

Thanks to Our Sponsors:

PCMDI > WCRP CMIP3 Model Output > Diagnostic Subprojects Printer Friendly Version
 
<< Back to WCRP CMIP3 Subprojects

  • Hazeleger, W., 2005: Can global warming affect tropical ocean heat transport. Geoph. Res. Lett., 32, 10.1029/2005GL023450.

Tropical meridional ocean heat transport is studied in six coupled ocean-atmosphere models in which atmospheric CO2 concentration has been increased. In the Indo-Pacific, the strength of Subtropical Cells (STCs) changes in response to changes in the trade winds. However, the change is not consistent among models. In contrast, in all models the tropical Indo-Pacific heat transport remains nearly constant over time due to compensation of STC and the horizontal gyre variations. Even under strong atmospheric radiative forcing the tropical Indo-Pacific ocean heat transport trends are determined by changes in circulation, rather than changes in the stratification. Ocean heat transport in the tropical Atlantic responds to weakening of the basin-wide meridional overturning circulation (MOC). The trends in the South Atlantic STC do not affect ocean heat transport


Last Updated: 2006-03-06

<< Back to WCRP CMIP3 Subprojects
 
For questions or comments regarding this website, please contact the Webmaster.
 
Lawrence Livermore National Laboratory  |  Physical & Life Sciences Directorate