Calibration of HY-2A satellite significant wave heights with in situ observation
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  • 作者:Hailong Peng ; Mingsen Lin
  • 关键词:total least squares ; NDBC buoys ; HY ; 2A altimeter ; significant wave height
  • 刊名:Acta Oceanologica Sinica
  • 出版年:2016
  • 出版时间:March 2016
  • 年:2016
  • 卷:35
  • 期:3
  • 页码:79-83
  • 全文大小:1,567 KB
  • 参考文献:Bacon S, Carter D J T. 1991. Wave climate changes in the North Atlantic and North Sea. International Journal of Climatology, 11(5): 545–558CrossRef
    Challenor P G, Cotton P D. 1999. The joint calibration of altimeter and in situ wave heights. In: Preprints CLIMAR’99, WMO Workshop on Advances in Marine Climatology. Vancouver, Canada: WMO, 121–129
    Durrant T H, Greenslade D J M. 2007. Validation and application of Jason-1 and Envisat significant wave heights. In: Proceedings of the 10th International Workshop on Wave Hindcasting and Forecasting. Oahu, Hawaii, USA: AGBM
    Durrant T H, Greenslade D J M. 2009. Validation of Jason-1 and Envisat remotely sensed wave heights. Journal of Atmospheric and Ocean Technology, 26(1): 123–134CrossRef
    Fu L L, Cazenave A. 2001. Satellite Altimetry and Earth Sciences-A Handbook of Techniques and Applications: International Ge—ophysical Series, Vol. 69. San Diego: Academic Press
    Hwang P A, Teague W J, Jacobs G A, et al. 1998. A statistical comparison of wind speed, wave height and wave period derived from satellite altimeters and ocean buoys in Gulf of Mexico region. Journal of Geophysical Research: Oceans, 103(C5): 10451–10468CrossRef
    Korobkin M, D’Sa E. 2008. Significant wave height in the gult of Mexico: validation of Jason-1 measurement against buoy data. In: Proceedings of the 12th Conference on IOAS-AOLS Adjourns. New Orleans, USA
    Petráš I, Bednárová D, škovránek T, et al. 2009. Total least squares method: Matlab toolbox (Functions and Demos). http://​www.​tuke.​sk/​petras/​TLS/​[2011-4-19/2013-4-11]
    Queffeulou P. 2003. Validation of ENVISAT RA-2 and JASON-1 altimeter wind and wave measurements. In: Proceedings of 2003 IEEE International Geoscience and Remote Sensing Symposium. Toulouse, France: IEEE, 5: 2987–2989
    Queffeulou P. 2004. Long-term validation of wave height measurements from altimeters. Marine Geodesy, 27(3–4): 495–510CrossRef
    Queffeulou P. 2006. Altimeter wave height validation-an update. In: Proceedings of OSTST Meeting. Venice, Italy: WMO
    Ray R D, Beckley B D. 2012. Calibration of ocean wave measurements by the TOPEX, Jason-1, and Jason-2 satellites. Marine Geodesy, 35(S1): 238–275CrossRef
    Soukissian T, Kechris C. 2007. About applying linear structural method on ocean data: Adjustment of satellite wave data. Ocean Engineering, 34(3–4): 371–389CrossRef
    Wang Jichao, Zhang Jie, Yang Jungang. 2013. The validation of HY-2 altimeter measurements of a significant wave height based on buoy data. Acta Oceanologica Sinica, 32(11): 87–90CrossRef
    Xu Guangjun, Yang Jingsong, Xu Yuan, et al. 2014. Validation and calibration of significant wave height from HY-2 satellite altimeter. Journal of Remote Sensing, 18(1): 206–214
    Xu Yuan, Yang Jingsong, Zheng Gang, et al. 2014. Calibration and verification of sea surface wind speed from satellite altimeters. Acta Oceanologica Sinica (in Chinese), 36(7): 125–132
  • 作者单位:Hailong Peng (1) (2) (3)
    Mingsen Lin (2) (3)

    1. College of Information Science and Engineering, Ocean University of China, Qingdao, 266100, China
    2. Nation Satellite Ocean Application Service, State Oceanic Administration, Beijing, 100081, China
    3. Key Laboratory of Space Ocean Remote Sensing and Application, State Oceanic Administration, Beijing, 100081, China
  • 刊物主题:Oceanography; Climatology; Ecology; Engineering Fluid Dynamics; Marine & Freshwater Sciences; Environmental Chemistry;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1869-1099
文摘
Significant wave height (SWH) can be computed from the returning waveform of radar altimeter, this parameter is only raw estimates if it does not calibrate. But accurate calibration is important for all applications, especially for climate studies. HY-2a altimeter has been operational since April 2012 and its products are available to the scientific community. In this work, SWH data from HY-2A altimeters are calibrated against in situ buoy data from the National Data Buoy Center (NDBC), Distinguished from previous calibration studies which generally regarded buoy data as “truth”, the work of calibration for HY-2A altimeter wave data against in situ buoys was applied a more sophisticated statistical technique—the total least squares (TLS) method which can take into account errors in both variables. We present calibration results for HY-2A radar altimeter measurement of wave height against NDBC buoys. In addition, cross-calibration for HY-2A and Jason-2 wave data are talked over and the result is given.

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