Exercise in downscaling on sea surface temperature along Chinese coast

Lian Shu-min; Wang Kai; Cui Mao-chang; Eduardo Zorita

doi:10.1007/BF02842569

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Exercise in downscaling on sea surface temperature along Chinese coast

OriginalPaper | Updated：2023-05-16

- Exercise in downscaling on sea surface temperature along Chinese coast
- Exercise in downscaling on sea surface temperature along Chinese coast
- 海洋湖沼学报（英文） 2000年18卷第2期页码：110-116
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. Institute for Hydrophysics
- Author bio：
- Funds：
  
  Contribution No. 3238 from the Institute of Oceanology, Chinese Academy of Sciences.;Project 49476274 supported by NSFC and the Chinese Academy of Sciences President's fund (YJJZ No. 218), also supported by Key Lab. of Marine Environmental Sciences and Numerical Modelling of SOA.
- DOI：10.1007/BF02842569
  中图分类号：
- 纸质出版：2000
- Accepted：
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Exercise in downscaling on sea surface temperature along Chinese coast[J]. 海洋湖沼学报（英文）, 2000,18(2):110-116.

Shu-min, L., Kai, W., Mao-chang, C. et al. Exercise in downscaling on sea surface temperature along Chinese coast., Chin. J. Ocean. Limnol. 18, 110–116 (2000). https://doi.org/10.1007/BF02842569
Exercise in downscaling on sea surface temperature along Chinese coast[J]. 海洋湖沼学报（英文）, 2000,18(2):110-116. DOI： 10.1007/BF02842569.

Shu-min, L., Kai, W., Mao-chang, C. et al. Exercise in downscaling on sea surface temperature along Chinese coast., Chin. J. Ocean. Limnol. 18, 110–116 (2000). https://doi.org/10.1007/BF02842569 DOI：

摘要

Abstract

The present study examines the relationship between observed variations of regional hydrographic elements and concurrent large-scale climatological parameters. The former were chosen as the monthly sea surface temperature along the Chinese coast; the latter were chosen as monthly mean sea level pressure and sea surface temperature for the period from 1960 to 1990

which are reasonably well simulated by present day climate models. The variations of the former

due to variations of the regional atmospheric forcing and of oceanic circulation

are not adequately simulated by a global climate model because of insufficient spatial resolution. A statistical “downscaling” strategy is applied to the former. To better understand their variation mechanism and study the relationship among the environmental parameters in a group

canonical correlation analysis with combined datasets was carried out. The results show that variations of hydrographic elements are heavily forced by the East Asian monsoon through monsoon wind and rainfall.

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references

Cubasch, U., Hegerl, G., Hellbach, A. et al., 1995. A climate change simulation starting at an early time industrialization.Clim. Dyn. 11: 71–84.

Cui, M., von Storch, H., Zorita, E., 1995. Coast sea level and the large-scale climate state: A downscaling exercise for the Japanese islands.Tellus 47A: 132–144.

Cui Maochang, Lian Shumin, Yang Dongfang et al., 1998. Coastal sea level and Asian monsoon system: a downscaling exercise for Chinese coast.Chin. J. Oceanol. Limnol. 16(2): 108–121.

Li, C., 1990. Interactivity between anomalous winter monsoon in east Asia and El Nino events.Adv. Atmos. Sci. 7: 36–46.

Tao, S. Y., Chen, L. X., 1987. A review of recent research on the East Asian summer monsoon in China.In: Chang C. P. and Krish-namurti, T. N. ed., Monsoon Meteorology. Oxford University Press, p. 60–92.

von Storch, H., Zorita, E., Cubasch, U., 1993. Downscaling of global climate change estimates to regional scales: An application to Iberian rainfall in wintertime.J. Climate 6: 1161–1171.

Webster, P. J., Yang, S., 1992. Monsoon and ENSO: Selectively interactive system.Quart. J. R. Meteorol. Soc. 118: 877–926.

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