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Massachusetts Institute of Technology

On the meridional heat transport and its partition between the atmosphere and oceans

Abstract

dc:description.abstract

In this thesis I study the meridional heat transport of the climate system and its partition between the atmosphere and oceans using models and data. I focus on three primary questions: (1) What is the total heat transport and its partition between the two fluids? (2) What sets the magnitude of the total heat transport and to what extent is it sensitive to the details of atmospheric and oceanic circulation? (3) How robust is the partition of heat transport between the two fluids and how sensitive is it to bathymetric constraints on ocean circulation? For these studies I employ a series of aqua-planet calculations using a coupled atmosphere-ocean-ice model in which idealized ocean basins impose various geometrical constraints on ocean circulation. A wide range of ocean heat transports and heat transport partitions are found, but with more modest variations in the total heat transport. Differences in the total heat transport are associated with the presence or absence of polar ice which is found to be sensitive to the ability of the ocean to carry heat to high latitudes. These model results, as well as data, are analyzed in the context of earlier work suggesting that the total meridional heat transport should be insensitive to the details of the atmospheric and oceanic circulation. The heat transport partitions in these aqua-planet calculations are also analyzed. The calculations all feature the same gross partition as the present climate with the ocean dominating near the equator and the atmosphere dominating at middle and high latitudes. While this suggests that this overall partition may be a robust feature of the climate system, there are important differences associated with the presence or absence of a meridional barrier to zonal flow in the ocean.

Degree

thesis:*
Department dc:contributor.department
Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences.
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2009

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Enderton, Daniel
Advisor dc:contributor.advisor
  • John Marshall.

Subjects

dc:subject × 1

Rights

dc:rights
Statement dc:rights
  • M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/47842
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/47842

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Enderton, Daniel. On the meridional heat transport and its partition between the atmosphere and oceans. Massachusetts Institute of Technology, 2009. http://hdl.handle.net/1721.1/47842