Basic characteristics of the atmospheric boundary layer over the Western Pacific

Song Xi-long; Hu Dun-xin; Lian Shu-min

doi:10.1007/BF02845348

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Basic characteristics of the atmospheric boundary layer over the Western Pacific

OriginalPaper | Updated：2023-05-16

- Basic characteristics of the atmospheric boundary layer over the Western Pacific
- Basic characteristics of the atmospheric boundary layer over the Western Pacific
- 海洋湖沼学报（英文） 1995年13卷第1期页码：43-50
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  Supported by the National Natural Science Foundation of China, No. 49176255.;Contribution No. 2219 from the Institute of Oceanology, Chinese Academy of Sciences.
- DOI：10.1007/BF02845348
  中图分类号：
- 纸质出版：1995
- Accepted：
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Basic characteristics of the atmospheric boundary layer over the Western Pacific[J]. 海洋湖沼学报（英文）, 1995,13(1):43-50.

Xi-long, S., Dun-xin, H. & Shu-min, L. Basic characteristics of the atmospheric boundary layer over the Western Pacific., Chin. J. Ocean. Limnol. 13, 43–50 (1995). https://doi.org/10.1007/BF02845348
Basic characteristics of the atmospheric boundary layer over the Western Pacific[J]. 海洋湖沼学报（英文）, 1995,13(1):43-50. DOI： 10.1007/BF02845348.

Xi-long, S., Dun-xin, H. & Shu-min, L. Basic characteristics of the atmospheric boundary layer over the Western Pacific., Chin. J. Ocean. Limnol. 13, 43–50 (1995). https://doi.org/10.1007/BF02845348 DOI：

摘要

Abstract

The western Pacific

one of the most violent air-sea interaction areas

plays an important role in the formation of ENSO events which greatly affect global climate change. Knowledge on the structure of the atmospheric boundary layer and the air-sea exchange over that area is very important and is the key to understanding the air-sea interaction. Tethered balloon measurements were made successfully during the September–October

1987 cruise of theR/V SCIENCE 1 in the Philippine Sea at the northwest of the Warm Pool. The data collected were used for analysis of the structure of the atmospheric boundary layer showing that the characteristics of the inversion layers (advection layer

capping inversion layer and radiation layer) are different from those over the land and other sea areas. The wind profiles were simulated with the P-exponent method and the values of P under unstable

stable and neutral conditions were obtained. Moreover

the effect of the ship body on the air above was estimated to reach 30 meters high.

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Keywords

references

Atkinson, B. W., 1981. Mesoscale Atmospheric Circulations. Academic Press, New York, pp. 125–224.

Hsu, S. A., 1982. Determination of the power-law wind profile exponent on a Tropical Coast.J. Appl. Meteor.,21: 1187–1190.

Li Ruodun and Sun Ruiben. 1991. The analysis of multiple structure of the Atmospheric Boundary Layer in the Western Tropical Ocean.Scientia Atmospheric Sinica 15(16): 110–116. (in Chinese with English abstract)

Qu Shaohou, 1988. Observation research of the turbulent fluxes of momentum, sensible heart and latent heart over the Western Pacific Tropical Ocean area.Acta Meteorologica Sinica 46(4): 452–460. (in Chinese with English abstract)

Xiong Kang, 1990. The observation study of the turbulent fluxes, sea surface roughness z0 and drag coefficientC D over the Western Tropic Pacific Ocean.Scientia Atmospheric Sinica 14(4): 475–482. (in Chinese with English abstract)

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