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Volume 24 Issue 5
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Article Navigation >  Acta Oceanologica Sinica  > 2005  >  (5): 46-49
ZHENG Chongwei, PAN Jing, TAN Yanke, GAO Zhansheng, RUI Zhenfeng, CHEN Chaohui. The seasonal variations in the significant wave height and sea surface wind speed of the China's seas[J]. Acta Oceanologica Sinica, 2015, 34(9): 58-64. doi: 10.1007/s13131-015-0738-0
Citation: YANG Jingsong, HUANG Weigen, XIAO Qingmei, ZHOU Chenghu, HSU Mingkuang. Oceanic pycnocline depth retrieval from SAR imagery in the existence of solitary internal waves[J]. Acta Oceanologica Sinica, 2005, (5): 46-49.
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Oceanic pycnocline depth retrieval from SAR imagery in the existence of solitary internal waves

  • 1.

    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

  • 2.

    State Laboratory of Resources and Environment Information System, Institute of Geographical Sciences and Natural Resources, Chinese Academy of Sciences, Beijing 100101, China

  • 3.

    Department of Oceanography, National Taiwan Ocean University, Taibei, China

  • Received Date: 2005-04-19
  • Rev Recd Date: 2005-07-05
    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.
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    2. Bahareh Kamranzad, Khalid Amarouche, Adem Akpinar. Linking the long-term variability in global wave energy to swell climate and redefining suitable coasts for energy exploitation. Scientific Reports, 2022, 12(1) doi:10.1038/s41598-022-18935-w
    3. Yuhan Cao, Changming Dong, Ian R. Young, et al. Global Wave Height Slowdown Trend during a Recent Global Warming Slowdown. Remote Sensing, 2021, 13(20): 4096. doi:10.3390/rs13204096
    4. Yuru Li, Shuyang Ma, Caihong Fu, et al. Appraising the Status of Fish Community Structure in the Yellow Sea Based on an Indicator-Testing Framework. Frontiers in Marine Science, 2021, 8 doi:10.3389/fmars.2021.646733
    5. Shuyang Ma, Yang Liu, Jianchao Li, et al. Climate-induced long-term variations in ecosystem structure and atmosphere-ocean-ecosystem processes in the Yellow Sea and East China Sea. Progress in Oceanography, 2019, 175: 183. doi:10.1016/j.pocean.2019.04.008
    6. Zhuxiao Shao, Bingchen Liang, Huajun Li, et al. Extreme significant wave height of tropical cyclone waves in the South China Sea. Natural Hazards and Earth System Sciences, 2019, 19(10): 2067. doi:10.5194/nhess-19-2067-2019
    7. Yanda Ou, Fangguo Zhai, Peiliang Li. Interannual wave climate variability in the Taiwan Strait and its relationship to ENSO events. Journal of Oceanology and Limnology, 2018, 36(6): 2110. doi:10.1007/s00343-019-7301-3
    8. Bijoy Thompson, Pavel Tkalich, Paola Malanotte-Rizzoli. Regime shift of the South China Sea SST in the late 1990s. Climate Dynamics, 2017, 48(5-6): 1873. doi:10.1007/s00382-016-3178-4
    9. Chongwei Zheng, Chongyin Li, Hailang Wu, et al. 21st Century Maritime Silk Road: Construction of Remote Islands and Reefs. Springer Oceanography, doi:10.1007/978-981-10-8114-9_4
    10. Tiago C.A. Oliveira, Pavel Tkalich, Bien Aik Tan, et al. High-resolution wind-wave model for the Sea Surface Wave Height forecasting and hindcasting. Global Oceans 2020: Singapore – U.S. Gulf Coast, doi:10.1109/IEEECONF38699.2020.9389087

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