Comparison among sea surface roughness schemes

Sha Wenyu; Gui Qijun; Pan Yuping; Min Jinzhong; Yin Zhijun

doi:10.1007/BF02842680

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Comparison among sea surface roughness schemes

OriginalPaper | Updated：2023-05-16

- Comparison among sea surface roughness schemes
- Comparison among sea surface roughness schemes
- 海洋湖沼学报（英文） 2005年23卷第4期页码：376-382
- Affiliations：
  
  1. Jiangsu Key Laboratory of Meteorological Disaster Nanjing University of Information Science & Technology
  2. The College of Meterology the Institute of Science and Engineering of the P.. A,L
  3. The Weather Center of the P.L.A. Nanjing Military Area Air Command
- Author bio：
- Funds：
  
  This work is supported by Nanjing University of Information Science & Technology, Jiangsu Key Laboratory of Meterological Disaster Program (KLME 050210).
- DOI：10.1007/BF02842680
  中图分类号：
- 纸质出版：2005
- Accepted：
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Comparison among sea surface roughness schemes[J]. 海洋湖沼学报（英文）, 2005,23(4):376-382.

Wenyu, S., Qijun, G., Yuping, P. et al. Comparison among sea surface roughness schemes., Chin. J. Ocean. Limnol. 23, 376–382 (2005). https://doi.org/10.1007/BF02842680
Comparison among sea surface roughness schemes[J]. 海洋湖沼学报（英文）, 2005,23(4):376-382. DOI： 10.1007/BF02842680.

Wenyu, S., Qijun, G., Yuping, P. et al. Comparison among sea surface roughness schemes., Chin. J. Ocean. Limnol. 23, 376–382 (2005). https://doi.org/10.1007/BF02842680 DOI：

摘要

Abstract

Based on the measurements from the US National Data Buoy Center 3-m discus buoy site No. 44004 (38.5°N

70.47°W) from January 1 to March 31 of 2003

with the COARE algorithm (Version 3.0)

the results from four parameterization schemes developed recently for sea surface aerodynamic roughness length were compared with each other. Calculations of frictional speedu*

drag coefficientC d and wind stress τ indicate that the calculated frictional velocities from the four schemes (8.50%–16.20%

the normalized standard error estimate

or NSEE)

the computed drag coefficients and wind stress (respectively 15.08%–28.67% and 17.26%–50.59% NSEE) are reasonable. Schemes YT96 and GW03 are consistent. The O02 scheme gives over-estimated values foru* andC d. Schemes TY01 and GW03 display discontinuous characteristics in handling young wave data.

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references

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Donelan, M., F. W. Dobson, S. D. Smith and R. J. Anderson, 1993. On the dependence of sea surface roughness on wave development.J. Phys. Oceanog. 23: 2143–2149.

Fairall, C. W., E. F. Bradley, D. P. Rogers, J. B. Edson and G. S. Young, 1996. Bulk parameterization of air-sea fluxes for TOGA COARE.J. Geophys. Res. 101: 3747–3764.

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