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1)  sea surface wind speed
海面风速
1.
With JASON-1 and TOPEX/POSEIDON measurements taken during the verification phase in the China Seas and Northwest Pacific Ocean,such parameters as the sea surface wind speed,significant wave height,backscatter coefficient and sea surface height are compared systematically,and the coherence of the two missions is analyzed.
利用JASON-1和TOPEX/POSEIDON卫星高度计在相互校正阶段的观测资料,对两者在中国海和西北太平洋测得的海面风速、有效波高、后向散射截面、海平面高度等参数进行一致性分析;利用j,v模型及主要分潮的调和常数,对中国陆架浅海的JASON-1海平面高度数据进行浅海潮汐修正,使用验潮站月平均水位资料对修正结果加以印证。
2.
Based on altimetric observation of sea surface wind speeds over the South China Sea from Geosat satellite during the period between November 1986 to March 1989, the statistical characteristics of the sea surface wind speeds and the seasonal features of the wind field over the area are studied.
利用GEOSAT卫星高度计于1986年11月至1989年3月;司所测的南海海面风速资料,统计分析了南海海面风速的统计特征以及海面风场的分布特点。
2)  extreme sea surfa ce wind speed prediction
极端海面风速预测
3)  wind speed on land and sea
海陆风速
4)  Sea Surface Wind Vector
海面风场
1.
Application of Sea Surface Wind Vector Measured by Satellite-based scatterometer to Anti-ship Missile;
介绍了星载微波散射计测量海面风场技术及其精度,分析了海面风场对反舰导弹射击精度的影响。
5)  sea surface wind
海面风
1.
The temperature data from SODA and sea surface wind data from NCEP during 1950—1999 were used to investigate the interannual variation characters of the surface and subsurface heat contents in Indian Ocean and their relationship with ENSO by EOF analysis.
采用1950年1月至1999年12月SODA海洋上层温度的月平均资料及同期的NCEP月平均风场资料,研究了印度洋表层和次表层热含量年际变化的特征以及与海面风场的关系。
6)  ocean surface wind
海面风场
1.
Research on ocean surface wind field retrievals from SAR;
SAR海面风场反演研究
2.
By the development of the remote sensing, Synthetic Aperture Radar (SAR) becomesa very important measurement on the ocean surface wind because of the capability ofhigh-resolution, working all the time and under all weather conditions.
海面风场是海洋和大气的重要要素。
补充资料:多通道电子风速计(见转杯式风速表)


多通道电子风速计(见转杯式风速表)


  爹豁笔戮翁ng’粗转杯式风速表。
  
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