Cite this paper:
WANG Zhixiong, ZHAO Chaofang, ZOU Juhong, XIE Xuetong, ZHANG Yi, LIN Mingsen. An improved wind retrieval algorithm for the HY-2A scatterometer[J]. Journal of Oceanology and Limnology, 2015, 33(5): 1201-1209

An improved wind retrieval algorithm for the HY-2A scatterometer

WANG Zhixiong1,2, ZHAO Chaofang1, ZOU Juhong2, XIE Xuetong3, ZHANG Yi2, LIN Mingsen2
1 Ocean Remote Sensing Institute, Ocean University of China, Qingdao 266100, China;
2 National Satellite Ocean Application Service, State Oceanic Administration, Beijing 100081, China;
3 Guangzhou University, Guangzhou 510006, China
Abstract:
Since January 2012, the National Satellite Ocean Application Service has released operational wind products from the HY-2A scatterometer (HY2-SCAT), using the maximum-likelihood estimation (MLE) method with a median filter.However, the quality of the winds retrieved from HY2-SCAT depends on the sub-satellite cross-track location, and poor azimuth separation in the nadir region causes particularly low-quality wind products in this region.However, an improved scheme, i.e., a multiple solution scheme (MSS) with a two-dimensional variational analysis method (2DVAR), has been proposed by the Royal Netherlands Meteorological Institute to overcome such problems.The present study used the MSS in combination with a 2DVAR technique to retrieve wind data from HY2-SCAT observations.The parameter of the empirical probability function, used to indicate the probability of each ambiguous solution being the "true" wind, was estimated based on HY2-SCAT data, and the 2DVAR method used to remove ambiguity in the wind direction.A comparison between MSS and ECMWF winds showed larger deviations at both low wind speeds (below 4 m/s) and high wind speeds (above 17 m/s), whereas the wind direction exhibited lower bias and good stability, even at high wind speeds greater than 24 m/s.The two HY2-SCAT wind data sets, retrieved by the standard MLE and the MSS procedures were compared with buoy observations.The RMS error of wind speed and direction were 1.3 m/s and 17.4°, and 1.3 m/s and 24.0° for the MSS and MLE wind data, respectively, indicating that MSS wind data had better agreement with the buoy data.Furthermore, the distributions of wind fields for a case study of typhoon Soulik were compared, which showed that MSS winds were spatially more consistent and meteorologically better balanced than MLE winds.
Key words:    HY-2A scatterometer|wind retrieval|maximum-likelihood estimation (MLE)|multiple solution scheme (MSS)|two-dimensional variational analysis method (2DVAR)|typhoon Soulik   
Received: 2014-06-11   Revised: 2014-07-25
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Articles by WANG Zhixiong
Articles by ZHAO Chaofang
Articles by ZOU Juhong
Articles by XIE Xuetong
Articles by ZHANG Yi
Articles by LIN Mingsen
References:
Gohil B S, Sarkar A, Agarwal V K.2008.A new algorithm for wind-vector retrieval from scatterometers.IEEE Geoscience and Remote Sensing Letters, 5 (3): 387-391.
Gohil B S, Sharma P, Sikhakolli R et al.2010.Directional stability and conservation of scattering (DiSCS)-based directional-ambiguity removal algorithm for improving wind fields from scatterometer: a QuikSCAT example.IEEE Geoscience and Remote Sensing Letters, 7 (3): 592-595.
Lorenc A C.1986.Analysis methods for numerical weather prediction.Quarterly Journal of the Royal Meteorological Society, 112 (474): 1 177-1 194.
Peixdto J P, Oort A H.1992.Physics of Climate.American Institute of Physics, New York, USA.520p.
Pierson W J.1989.Probabilities and statistics for backscatter estimates obtained by a scatterometer.Journal of Geophysical Research: Oceans (1978-2012), 94 (C7): 9 743-9 759.
Portabella A.2002.Wind Field Retrieval from Satellite Radar Systems.Universitat de Barcelona.Science, Netherlands.207p.
Portabella M, Stoffelen A.2001.Rain detection and quality control of SeaWinds.Journal of Atmospheric and Oceanic Technology, 18 (7): 1 171-1 183.
Portabella M, Stoffelen A.2002.Quality Control and Wind Retrieval for Sea Winds.Ministerie van Verkeer en Waterstaat, Koninklijk Nederlands Meteorologisch Institute.
Portabella M, Stoffelen A.2004.A probabilistic approach for SeaWinds data assimilation.Quarterly Journal of the Royal Meteorological Society, 130 (596): 127-152.
Schultz H.1990.A circular median filter approach for resolving directional ambiguities in wind fields retrieved from spaceborne scatterometer data.Journal of Geophysical Research: Oceans (1978-2012), 95 (C4): 5 291-5 303.
Stiles B W, Pollard B D, Dunbar R S.2002.Direction interval retrieval with thresholded nudging: a method for improving the accuracy of QuikSCAT winds.IEEE Transactions on Geoscience and Remote Sensing, 40 (1): 79-89.
Stoffelen A.1998.Scatterometery.PhD thesis, University of Utrecht, ISBN 90-393-1708-9.
Stoffelen A, Anderson D.1997a.Scatterometer data interpretation: measurement space and inversion.Journal of Atmospheric & Oceanic Technology, 14 (6).
Stoffelen A, Portabella M.2006.On Bayesian scatterometer wind inversion.IEEE Transactions on Geoscience and Remote Sensing, 44 (6): 1 523-1 533.
Stoffelen A, Vogelzang J, Verhoef A.2010.Verification of scatterometer winds.In: Forsythe M, Daniels J eds.10th International Winds Workshop.20/2/2010-26/2/2010,Tokyo, Japan, JMA, EUMETSAT.
Stoffelen A, Vries D J, Voorrips A.2001.Towards the Real-Time Use of QuikSCAT Winds.Project Report, KNMI, de Bilt, the Netherlands.
Stoffelen B A, Anderson D.1997b.Ambiguity removal and assimilation of scatterometer data.Quarterly Journal of the Royal Meteorological Society, 123 (538): 491-518.
Verhoef A, Stoffelen A.2012.OSCAT winds validation report.OSI SAF Report.SAF/OSI/CDOP2/KNMI/TEC/RP/196.Available: http://www.eumetsat.int.
Vogelzang J, Stoffelen A, Verhoef A et al.2011.On the quality of high-resolution scatterometer winds.Journal of Geophysical Research: Oceans (1978-2012), 116 (C10033): 1-14.
Vogelzang J.2007.Two-dimensional variational ambiguity removal (2DVAR).NWP SAF NWPSAF-KN-TR-004.Available: http://www.eumetsat.int.
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