Global Drag-Coefficient Estimates From Scatterometer Wind and Wave Steepness

Global Drag-Coefficient Estimates From Scatterometer Wind and Wave Steepness
复制标题

DOI:
10.1109/tgrs.2010.2082554
复制
发表时间:
2011-05
影响因子:
8.2
通讯作者:
Guoqiang Liu;Yijun He;Hui Shen;Jie Guo
Guoqiang Liu;Yijun He;Hui Shen;Jie Guo
中科院分区:
工程技术1区
文献类型:
--
作者:
Guoqiang Liu;Yijun He;Hui Shen;Jie Guo

文献摘要

被引文献

相似文献

建立了一个神经网络模型,用于从ERS-1/2上的欧洲遥感散射计中反演海浪陡度(δ),以表征海况(尤其是波浪状态)。利用反演的δ和散射计风速,计算并检验了全球海洋的阻力系数。结果表明,当计算中包括波陡时,CD发生显著变化。结合波陡和风速,CD平均增加近14%。这种变化是空间变化的,从热带东太平洋的-18.76%到南大洋的104%不等。
A neural-network model was developed to retrieve the wave steepness (δ), which was used to represent the sea state (particularly wave state), from the European Remote Sensing (ERS) scatterometer onboard ERS-1/2. Using the retrieved δ and scatterometer wind speed, we calculated and examined the drag coefficient ( CD) over the global ocean. The results show that CD changes significantly when wave steepness is included in the calculation. Combining wave steepness and wind speed increases CD by nearly 14% on average. That change is spatially variable, ranging from -18.76% for the tropical Eastern Pacific Ocean to 104% for the Southern Ocean.