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First, UWPBL model(the university of washington planetary boundary layer model) is used to retrieve YaGi typhoon sea level pressure from sea surface wind data of SeaWinds which are obtained from QuikSCAT(called direct retrieving) and these strength results are analyzed. Then the variational method is used to decompose the sea surface winds field into two parts: vortex and irrotational environmental flow field, the UWPBL model is used again to retrieve YaGi typhoon sea level pressure from the vortex flow field, the results of typhoon central positions are analyzed by comparing the results with the results of direct retrieving, NCEP data and typhoon annual reports. It turns out that the accuracy of the typhoon sea level pressure central position is obviously improved. This method offers a new idea for the study of typhoon from microwave scatterometer data.
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Keywords:
- scatterometer-derived sea surface winds /
- variational method /
- typhoon /
- sea level pressure field
[1] Brown R A, Levy G 1986 Mon. Wea. Rev. 114 2197
[2] [3] Brown R A, Zeng L 1994 J. Appl. Meteor. 33 1088
[4] Hsu C S,Wurtele M G 1997 J. Appl. Meteor. 9 1249
[5] [6] Zierden D F, Bourassa M A, OBrien J J 2000 J. Geophys. Res. 105 23967
[7] [8] Patoux J, Brown R A 2002 J. Appl. Meteor. 41 133
[9] [10] Patoux J, Foster R C, Brown R A 2003 J. Appl. Meteor. 42 813
[11] [12] [13] Patoux J, Hakim G J, Brown R A 2005 Mon. Wea. Rev. 133 863
[14] [15] Patoux J, Foster R C, Brown R A 2008 J. Appl. Meteor. 47 835
[16] Zhang F, Liu Y D 2008 Progress in Natural Science 11 1288 (in Chinese) [张 帆、刘宇迪 2008自然科学进展11 1288]
[17] [18] Zhang L, Huang S X, Liu Y D, Zhong J 2010 Acta Phys. Sin. 59 2889 (in Chinese) [张 亮、黄思训、刘宇迪、钟 剑 2010 59 2889]
[19] [20] [21] Huang S X, Cai Q F, Xiang J, Zhang M 2007 Acta Phys. Sin. 56 3022 (in Chinese)[黄思训、蔡其发、项 杰、张 铭 2007 56 3022]
[22] [23] Cao X Q, Huang S X, Du H D 2008 Acta Phys. Sin. 57 3912 (in Chinese) [曹小群、黄思训、杜华栋 2008 57 3912]
[24] [25] Zhang L, Huang S X, Zhong J, Du H D 2010 Acta Phys. Sin. 59 7478 (in Chinese) [张 亮、黄思训、钟 剑、杜华栋 2010 59 7478]
[26] [27] Stevens B, Duan J, McWilliams J C, Munnich M, Neelin J D 2002 J. Clim. 15 30
[28] Zhao M, Miao M Q, Wang Y C 1991 A course of Boundary Layer Meteorology (Beijing:Meteorology Press) p1 (in Chinese)[赵 鸣、苗曼倩、王彦昌 1991 边界层气象学教程(北京:气象出版社)第1页]
[29] [30] [31] Press W H, Teukolsky S A, Vetterling W T, Flannery B P 1992 Numerical Recipes in FORTRAN: the art of Scientifc Computing (New York: Cambridge University Press) p1
[32] [33] Troen I, Mahrt L 1986 Bound.-Layer Meteorol. 37 129
[34] -
[1] Brown R A, Levy G 1986 Mon. Wea. Rev. 114 2197
[2] [3] Brown R A, Zeng L 1994 J. Appl. Meteor. 33 1088
[4] Hsu C S,Wurtele M G 1997 J. Appl. Meteor. 9 1249
[5] [6] Zierden D F, Bourassa M A, OBrien J J 2000 J. Geophys. Res. 105 23967
[7] [8] Patoux J, Brown R A 2002 J. Appl. Meteor. 41 133
[9] [10] Patoux J, Foster R C, Brown R A 2003 J. Appl. Meteor. 42 813
[11] [12] [13] Patoux J, Hakim G J, Brown R A 2005 Mon. Wea. Rev. 133 863
[14] [15] Patoux J, Foster R C, Brown R A 2008 J. Appl. Meteor. 47 835
[16] Zhang F, Liu Y D 2008 Progress in Natural Science 11 1288 (in Chinese) [张 帆、刘宇迪 2008自然科学进展11 1288]
[17] [18] Zhang L, Huang S X, Liu Y D, Zhong J 2010 Acta Phys. Sin. 59 2889 (in Chinese) [张 亮、黄思训、刘宇迪、钟 剑 2010 59 2889]
[19] [20] [21] Huang S X, Cai Q F, Xiang J, Zhang M 2007 Acta Phys. Sin. 56 3022 (in Chinese)[黄思训、蔡其发、项 杰、张 铭 2007 56 3022]
[22] [23] Cao X Q, Huang S X, Du H D 2008 Acta Phys. Sin. 57 3912 (in Chinese) [曹小群、黄思训、杜华栋 2008 57 3912]
[24] [25] Zhang L, Huang S X, Zhong J, Du H D 2010 Acta Phys. Sin. 59 7478 (in Chinese) [张 亮、黄思训、钟 剑、杜华栋 2010 59 7478]
[26] [27] Stevens B, Duan J, McWilliams J C, Munnich M, Neelin J D 2002 J. Clim. 15 30
[28] Zhao M, Miao M Q, Wang Y C 1991 A course of Boundary Layer Meteorology (Beijing:Meteorology Press) p1 (in Chinese)[赵 鸣、苗曼倩、王彦昌 1991 边界层气象学教程(北京:气象出版社)第1页]
[29] [30] [31] Press W H, Teukolsky S A, Vetterling W T, Flannery B P 1992 Numerical Recipes in FORTRAN: the art of Scientifc Computing (New York: Cambridge University Press) p1
[32] [33] Troen I, Mahrt L 1986 Bound.-Layer Meteorol. 37 129
[34]
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