Extratropical control of tropical climate, the atmospheric bridge and oceanic tunnel
- 11 March 2003
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 30 (5)
- https://doi.org/10.1029/2002gl016492
Abstract
A coupled ocean‐atmosphere model study shows that the extratropical impact on tropical climate is as strong as the tropical impact on extratropical climate. A 2°C SST warming in the global extratropics increases equatorial ocean temperature by ∼1°C in the surface and subsurface. The surface temperature change is caused by the atmospheric bridge of the Hadley circulation (70%) and the oceanic tunnel of thermocline subduction (30%), while the subsurface temperature change is forced predominantly through the oceanic tunnel. Furthermore, the dominant influence on the equator comes from the southern hemisphere atmosphere and ocean.This publication has 10 references indexed in Scilit:
- Tropical cooling at the last glacial maximum and extratropical ocean ventilation1Geophysical Research Letters, 2002
- Climate Change Across the HemispheresScience, 2001
- The role of the Indonesian Throughflow in equatorial Pacific thermocline ventilationJournal of Geophysical Research: Oceans, 1999
- Interdecadal interactions between the tropics and midlatitudes in the Pacific BasinGeophysical Research Letters, 1999
- The Role of Ocean in the Response of Tropical Climatology to Global Warming: The West–East SST ContrastJournal of Climate, 1998
- Meridional Circulation Cells and the Source Waters of the Pacific Equatorial UndercurrentJournal of Physical Oceanography, 1998
- Interdecadal Climate Fluctuations That Depend on Exchanges Between the Tropics and ExtratropicsScience, 1997
- Interactions between Global SST Anomalies and the Midlatitude Atmospheric CirculationBulletin of the American Meteorological Society, 1997
- Thermodynamic regulation of ocean warming by cirrus clouds deduced from observations of the 1987 El NiñoNature, 1991
- Nonlinear Axially Symmetric Circulations in a Nearly Inviscid AtmosphereJournal of the Atmospheric Sciences, 1980