Skip to main content
Log in

Contrast between the climatic states of the warm pool in the Indian Ocean and in the Pacific Ocean

  • Research Papers
  • Published:
Journal of Ocean University of Qingdao Aims and scope Submit manuscript

Abstract

Based on the analysis of Levitus data, the climatic states of the warm pool in the Indian Ocean (WPIO) and in the Pacific Ocean (WPPO) are studied. it is found that WPIO has a relatively smaller area, a shallower bottom and a slightly lower seawater temperature than those of WPPO. The horizontal area at different depths, volumes, central positions, and bottom depths of both WPIO and WPPO show quite apparent signals of seasonal variation. The maximum amplitude of WPIO surface area’s seasonal variation is 58% larger over the annual mean value. WPIO’s maximum volume variation amplitude is 66% larger over the annual mean value. The maximum variation amplitudes of the surface area and volume of WPPO are 20.9% and 20.6% larger over the annual mean value respectively. WPIO and WPPO show different temporal and spatial characteristics mainly due to the different wind fields and restriction of ocean basin geometry. For instance, seasonal northern displacement of WPIO is, to some extent, constrained by the basin of the Indian Ocean, while WPPO moves relatively freely in the longitudinal direction. The influence of WPIO and WPPO over the atmospheric motion must be quite different.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Antonov, J., S. Levitus, T. P. Boyer, M. E. Conkright, T. O’Brien, et al., 1998. World Ocean Atlas 1998 Pacific Ocean Temperature fields. Vol. 2, NOAA Atlas NESDIS 28, U. S. Gov. Printing Office, Wash., D. C., 166 pp.

    Google Scholar 

  • Antonov, J., S. Levitus, T. P. Boyer, M. Conkright, T. O’Brien, et al., 1998. World Ocean Atlas 1998. Indian Ocean Temeprature fields. Vol. 3, NOAA Atlas NESDIS 29, U. S. Gov. Printing Office, Wash., D. C., 166 pp.

    Google Scholar 

  • Cornejo-Garrido, A., and P. Stone, 1977. On the heat balance of the walker circulation. J. Atmos. Sci., 34: 1155–1162.

    Article  Google Scholar 

  • Hartmann, D., H. Henden, and R. Houze, 1984. Some implications of the mesoscale circulation in the tropical cloud clusters for large-scale dynamics and climate. J. Atmos. Sci., 41: 113–121.

    Article  Google Scholar 

  • Li, C. Y., and Mu, M. Q., 1999. El Ninño occurrence and sub-structure ocean temperature anomalies in the Pacific warm pool. Chinese Journal of Atmospheric Science, 23: 513–521.

    Google Scholar 

  • Mu, M. Q., and Li, C. Y., 2000. Interactions between subsurface ocean temperature anomalies in the western pacific warm pool of ENSO cycle. Chinese Journal of Atmospheric Science, 24: 447–459.

    Google Scholar 

  • Wyrtki, K., 1989. Some thoughts about the west Pacific warm pool. Proc. Western Pacific Int. Meeting and Workshop on TOGA/COARE. ORSTOM, Noumea (New Caledonia). pp. 99–109.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Meng Xiangfeng.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Xiangfeng, M., Dexing, W. Contrast between the climatic states of the warm pool in the Indian Ocean and in the Pacific Ocean. J Ocean Univ. China 1, 119–124 (2002). https://doi.org/10.1007/s11802-002-0003-y

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11802-002-0003-y

Key words

Navigation