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Tropical drought regions in global warming and El Niño teleconnections

Neelin, J. D., Chou, C., Su, H.·2003·Geophysical Research Letters

Abstract

Climate model global warming simulations predict large regional changes in tropical rainfall, including regions of drought. Qualitatively similar changes occur during El Niño interannual variability. Using an intermediate climate model, we have identified a mechanism that creates regional reductions in precipitation at the margins of convection zones during warming. In this “upped‐ante mechanism”, a warm troposphere increases the value of surface boundary layer moisture required for convection to occur. In regions of plentiful moisture supply, moisture simply rises to maintain precipitation, but this increases the moisture gradient relative to neighboring subsidence regions. Reductions in rainfall then result for those margins of convection zones that have strong inflow of air from the subsidence regions and less frequently meet the increased “ante” for convection. In simulations analyzed here, this new mechanism is the leading cause of tropical drought in the global warming case and is dominant in certain El Niño drought regions.

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Metadata

Authors
Neelin, J. D., Chou, C., & Su, H.
Venue
Geophysical Research Letters
Published
2003-12
Volume
30
Issue
24
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2167393797
Cited by
279
References
0
FWCI
14.53
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Tropical drought regions in global warming and El Niño teleconnections. https://app.cochat.ai/papers/10.1029/2003gl018625
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Neelin, J. D., Chou, C., & Su, H. (2003). Tropical drought regions in global warming and El Niño teleconnections. Geophysical Research Letters. https://doi.org/10.1029/2003gl018625

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