Ocean Heat Transport and Water Vapor Greenhouse in a Warm Equable Climate: A New Look at the Low Gradient Paradox
The authors study the role of ocean heat transport (OHT) in the maintenance of a warm, equable, ice-free climate. An ensemble of idealized aquaplanet GCM calculations is used to assess the equilibrium sensitivity of global mean surface temperature ([line over T]) and its equator-to-pole gradient (ΔT...
Main Authors: | Rose, Brian E. J. (Author), Ferreira, David (Contributor) |
---|---|
Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor) |
Format: | Article |
Language: | English |
Published: |
American Meteorological Society,
2013-09-18T12:20:41Z.
|
Subjects: | |
Online Access: | Get fulltext |
Similar Items
-
The early Eocene equable climate problem revisited
by: M. Huber, et al.
Published: (2011-06-01) -
Warm equable palaeoclimates, the role of general circulation model uncertainty in model-data mismatch
by: Sagoo, Navjit
Published: (2014) -
STUDY ON THE PRIMARY SEALING WITH TILT SURFACES AND EQUABLE CENTER DISTANCE
by: Mihaela ISTRATE, et al.
Published: (2016-05-01) -
The future of scientific publication is Open Access, but needs diversity, equability and equality!
by: Jähne Joachim
Published: (2021-04-01) -
Ocean warming, not acidification, controlled coccolithophore response during past greenhouse climate change
by: Gibbs, Samantha J., et al.
Published: (2016)