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YANG Jingsong,HUANG Weigen,XIAO Qingmei,ZHOU Chenghu,HSU Mingkuang. 2005. Oceanic pycnocline depth retrieval from SAR imagery in the existence of solitary internal waves. Acta Oceanologica Sinica, (5):46-49
Oceanic pycnocline depth retrieval from SAR imagery in the existence of solitary internal waves
Oceanic pycnocline depth retrieval from SAR imagery in the existence of solitary internal waves
Received:April 19, 2005  Revised:July 05, 2005
DOI:
Key words:SAR  pycnocline depth  solitary internal waves
中文关键词:  SAR  pycnocline depth  solitary internal waves
基金项目:
Author NameAffiliationE-mail
YANG Jingsong Key Laboratory of Ocean Dynamic Processes and Satellite Oceanography, State Oceanic Administration, Hangzhou 310012, China
Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China 
isyang@mail.hz.zi.cn 
HUANG Weigen Key Laboratory of Ocean Dynamic Processes and Satellite Oceanography, State Oceanic Administration, Hangzhou 310012, China
Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China 
 
XIAO Qingmei Key Laboratory of Ocean Dynamic Processes and Satellite Oceanography, State Oceanic Administration, Hangzhou 310012, China
Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China 
 
ZHOU Chenghu State Laboratory of Resources and Environment Information System, Institute of Geographical Sciences and Natural Resources, Chinese Academy of Sciences, Beijing 100101, China  
HSU Mingkuang Department of Oceanography, National Taiwan Ocean University, Taibei, China  
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Abstract:
      Oceanic pycnocline depth is usually inferred from in situ measurements.It is attempted to estimate the depth remotely.As solitary internal waves occur on oceanic pycnocline and propagate along it, it is possible to retrieve the depth indirectly in virtue of the solitary internal waves.A numerical model is presented for retrieving the pycnocline depth from synthetic aperture radar (SAR) images where the solitary internal waves are visible and when ocean waters are fully stratified.This numerical model is constructed by combining the solitary internal wave model and a two-layer ocean model.It is also assumed that the observed groups of solitary internal wave packets on the SAR imagery are generated by local semidiurnal tides.A case study in the East China Sea shows a good agreement with in situ CTD (conductivity-temperature-depth) data.
中文摘要:
      Oceanic pycnocline depth is usually inferred from in situ measurements.It is attempted to estimate the depth remotely.As solitary internal waves occur on oceanic pycnocline and propagate along it, it is possible to retrieve the depth indirectly in virtue of the solitary internal waves.A numerical model is presented for retrieving the pycnocline depth from synthetic aperture radar (SAR) images where the solitary internal waves are visible and when ocean waters are fully stratified.This numerical model is constructed by combining the solitary internal wave model and a two-layer ocean model.It is also assumed that the observed groups of solitary internal wave packets on the SAR imagery are generated by local semidiurnal tides.A case study in the East China Sea shows a good agreement with in situ CTD (conductivity-temperature-depth) data.
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