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The Central Equatorial Pacific Experiment

  • W. D. Collins
  • V. Ramanathan
  • P. J. Crutzen
  • A. Heymsfield
  • J. P. Kuettner
  • D. Kley
  • R. L. Grossman
  • R. T. Pierrehumbert
Conference paper
Part of the NATO ASI Series book series (volume 35)

Abstract

The tropical Pacific Ocean exhibits several intriguing features. For nearly 50% of the tropical Pacific (30°N to 30°S), sea-surface temperatures (SSTs) are within a narrow range between 300 K and 303 K, and less than 0.01% of the ocean surface has SSTs in excess of 304 K (Figure 1). Furthermore, deep convection is triggered only when SSTs exceed 300 K. In regions of deep convection and warm SST, the reduction of outgoing longwave energy by the atmospheric water vapor increases so rapidly with SST that it exceeds the rate of increase of blackbody surface emission. Thus the surface-atmosphere system in the warm pool loses its ability to radiate excess energy to space. Without some negative feedback process, the greenhouse effect would produce a runaway warming. Ramanathan and Collins [1991] (hereafter RC) found that the warm ocean is also covered by thick cirrus anvil clouds, which reflect a significant amount of solar energy back to space. They concluded that the anvils produced by deep convection act like a thermostat to regulate the flow of solar energy to the ocean.

Keywords

Water Vapor Deep Convection Atmospheric Temperature Warm Pool Surface Energy Budget 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag Berlin Heidelberg 1996

Authors and Affiliations

  • W. D. Collins
    • 1
  • V. Ramanathan
    • 1
  • P. J. Crutzen
    • 1
    • 2
  • A. Heymsfield
    • 1
    • 3
  • J. P. Kuettner
    • 3
  • D. Kley
    • 1
    • 4
  • R. L. Grossman
    • 5
  • R. T. Pierrehumbert
    • 6
  1. 1.Center for Clouds, Chemistry and ClimateScripps Institution of OceanographyUSA
  2. 2.Max-Planck-Institut für ChemieMainzGermany
  3. 3.National Center for Atmospheric ResearchBoulderUSA
  4. 4.Department für Chemie und Dynamik der GeosphäreForschungszentrum JülichJülichGermany
  5. 5.Astrophysical, Planetary and Atmospheric SciencesUniversity of ColoradoBoulderUSA
  6. 6.Department of Geophysical SciencesUniversity of ChicagoChicagoUSA

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