The atmospheric wet pool: definition and comparison with the oceanic warm pool

Caiyun Zhang; Ge Chen

doi:10.1007/s00343-008-0440-6

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The atmospheric wet pool: definition and comparison with the oceanic warm pool

OriginalPaper | Updated：2023-05-16

- The atmospheric wet pool: definition and comparison with the oceanic warm pool
- The atmospheric wet pool: definition and comparison with the oceanic warm pool
- 海洋湖沼学报（英文） 2008年26卷第4期页码：440-449
- Affiliations：
  
  1. Program of Geospatial Information Sciences University of Texas at Dallas
  2. Ocean Remote Sensing Institute Ocean University of China
- Author bio：
- Funds：
  
  Supported by the National Natural Science Foundation of China under projects (Nos. 40730530, 40675016, 40706056)
- DOI：10.1007/s00343-008-0440-6
  中图分类号：
- 网络首发：2009-01-23，
  
  纸质出版：2008
- Accepted：
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The atmospheric wet pool: definition and comparison with the oceanic warm pool[J]. 海洋湖沼学报（英文）, 2008,26(4):440-449.

Zhang, C., Chen, G. The atmospheric wet pool: definition and comparison with the oceanic warm pool., Chin. J. Ocean. Limnol. 26, 440–449 (2008). https://doi.org/10.1007/s00343-008-0440-6
The atmospheric wet pool: definition and comparison with the oceanic warm pool[J]. 海洋湖沼学报（英文）, 2008,26(4):440-449. DOI： 10.1007/s00343-008-0440-6.

Zhang, C., Chen, G. The atmospheric wet pool: definition and comparison with the oceanic warm pool., Chin. J. Ocean. Limnol. 26, 440–449 (2008). https://doi.org/10.1007/s00343-008-0440-6 DOI：

摘要

Abstract

The oceanic warm pool (OWP) defined by sea surface temperature (SST) is known as the “heat reservoir” in the ocean. The warmest portion in the ocean mirrors the fact that the wettest region with the largest accumulation of water vapor (WV) in the atmosphere

termed atmospheric wet pool (AWP)

should be identified because of the well-known Clausius-Clapeyron relationship between SST and WV. In this study

we used 14-year simultaneous observations of WV and SST from January 1988 to December 2001 to define the AWP and investigate its coupling and co-variations with the OWP. The joint examination of the area variations

centroid locations

and zonal migrations of the AWP and OWP lead to a number of interesting findings. The results hopefully can contribute to our understanding of the air-sea interaction in general and characterization of El Niño/La Niña events in particular.

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references

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