期刊文献+

太平洋海面粗糙度的计算及在ENSO期间的变化

Calculation and ahanging of roughness of sea surface in Pacific Ocean in ENSO period
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摘要 利用TOPEX高度计风速资料,实现了对太平洋海面粗糙度(Zo)的计算。1997~1999年正是厄尔尼诺与拉尼娜事件发生时期,作者研究了1997~1999年Zo在ENSO期间的变化后发现:(1)EINion发生期间赤道附近翱最大值在A,C,B3个站点上移动;最小值在B,A2个站点上移动。(2)LiNina发生期间赤道附近2。最小值在A站点,最大值主要在B站点上。LiNina发生期间,1999年15个站点翱均大于正常年份和EINion发生期间的15个站点2。。(3)ENSO期间,四季Zo与正常年份相比都有显著改变。 We calculated values of roughness in 15 points using wind speed by TOPEX satellite Altimeter. We studied the changes of roughness during 1997-1999 (ENSO period) and compared them with roughness in 1996. We find some characteristics as follows: The largest roughness nearby equator is moving from station A to station C to station B and the smallest roughness is moving from station B to station A during the EI Nion period. The smallest roughness is in station A and the largest roughness is in station B during LI Nina period. The roughness of 15 stations in 1999 is bigger than those in 1996, 1997, 1998. The roughness of 4 seasons has prominent change during ENSO period when compared with 1996.
出处 《海洋科学》 CAS CSCD 北大核心 2006年第6期87-91,共5页 Marine Sciences
关键词 ENSO 厄尔尼诺 拉尼娜 海面粗糙度(Zo) 海面风速 高度计 ENSO EI Nion La Nina the roughness of the sea surfaee sea surfaee wind speed satellite altimeter
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参考文献8

  • 1斯塔尔RB.边界层气象学导论[M].青岛:青岛海洋大学出版社,1991.1457.
  • 2冯士笮,李凤岐,李少菁.海洋科学导论[M].北京:高等教育出版社,2003.1-503.
  • 3方立新,陈戈.AVHRR和WEDGIS热带太平洋海洋温度分析系统[D].青岛:中国海洋大学,2003.1-76.
  • 4Blackadar A K,Tennekes H, Asymptotic similarity in neutral barotropic planetary boundary layers [J]. J Atmos Sci, 1968,25 : 1 015-1 020.
  • 5Tennekes H, Free convection in the turbulent Ekman layer of the atmosphere [J], J Atmos Sci, 1970, 27:1 027-1 034.
  • 6王秀芹,钱成春,王伟.风应力拖曳系数选取对风暴潮数值模拟的影响[J].青岛海洋大学学报(自然科学版),2001,31(5):640-646. 被引量:22
  • 7Wu J. Wind stress and surface roughness at air-sea interface [J]. Geophys Res, 1969 ,21(5): 707-714.
  • 8周良明,郭佩芳.利用卫星高度计风速资料研究海面粗糙度[J].海洋湖沼通报,2005(4):10-14. 被引量:6

二级参考文献14

  • 1Fedor,L.s.,and Brown,G.s.,waveheight and wind speed measurements from the seasat altimeter[J].G.R,1982,87(C5):3254-3260.
  • 2Chelton D B.,McCabe P J.,1985.a review of satellite altimeter measurement of sea surface wind speed:with a proposed new algorithm[J].J.G.R.,90(C3):4707-4720.
  • 3Chelton D.B.,and Wentz F.J.,1986.further development of an improved altimeter wind speed algorithm[J].J.G.R.,91:14250-14260.
  • 4Witter D L.,and Chelton D B.1991.A Geosat altimeter wind speed algorithm and a method for altimeter wind speed algorithm development[J].J.G.R.,96:8853-8860.
  • 5Blackadar A K amd Tennekes H,asymptotic similarity in neutral barotropic planetary boundary layers[J].J.Atmos.Sci.,1968,25:1015-1020.
  • 6Tennekes H,free convection in the turbulent Ekman layer of the atmosphere [J].J.Atmos.Sci.,1970,27:1027-1034.
  • 7R.B.斯塔尔.边界层气象学导论[M].青岛海洋大学出版社,1991.262-265.
  • 8Wu,J.,wind stress and surface roughness at air-sea interface[J].Geophys,res 21(5) 707-714,1969.
  • 9Smith,S.D.,wind stress and heat flux over the ocean in gale force winds[J].J.P.O,1980,10,709-726.
  • 10Carratt J R.review of coefficients over oceans and continents [J].Monthly weather review,1977,105:915-929.

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