Coast sea level and Asian monsoon system a downscaling exercise for Chinese coast

Cui Mao-chang; Lian Shu-min; Yang Dong-fang; Eduardo Zorita

doi:10.1007/BF02845176

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Coast sea level and Asian monsoon system a downscaling exercise for Chinese coast

Updated：2023-05-16

- Coast sea level and Asian monsoon system a downscaling exercise for Chinese coast
- Journal of Oceanology and Limnology Vol. 16, Issue 2, Pages: 108-121(1998)
- Affiliations：
  
  1. Institute of Oceanology
  2. Institute of Hydrophysics
- Author bio：
- Funds：
- DOI：10.1007/BF02845176
  CLC：
- Published：1998
- Accepted：
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Mao-chang, C., Shu-min, L., Dong-fang, Y. et al. Coast sea level and Asian monsoon system a downscaling exercise for Chinese coast., Chin. J. Ocean. Limnol. 16, 108–121 (1998). https://doi.org/10.1007/BF02845176
DOI：

Mao-chang, C., Shu-min, L., Dong-fang, Y. et al. Coast sea level and Asian monsoon system a downscaling exercise for Chinese coast., Chin. J. Ocean. Limnol. 16, 108–121 (1998). https://doi.org/10.1007/BF02845176 DOI：

摘要

Abstract

In this study

the authors examined the relationship between monthly sea level data and concurrent large-scale monthly mean sea level pressure and SST data for 1960 to 1990

which are reasonably well simulated by present day climate models; sea level variations due to variations of regional atmospheric forcing and oceanic circulation

are not adequately simulated by a global climate model because of insufficient spatial resolution. The authours applied a statistical “down scaling” strategy to sea level along the Chinese coast. Two interrelated processes were identified: one process is the local wind or wave set-up of water due to Asian monsoon wind anomalies; the other is the rainfall diluting effect in spring. At interdecadal time scale

the later becomes more important and most likely plays a major role in the planetary scale atmosphere-ocean interaction taking place in the eastern North Pacific.

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Keywords

references

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