A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint
Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness...
Ausführliche Beschreibung
Autor*in: |
Gao, J. [verfasserIn] Xue, M. [verfasserIn] Lee, S.-Y. [verfasserIn] Shapiro, A. [verfasserIn] Xu, Q. [verfasserIn] Droegemeier, K. K. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2006 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Meteorology and atmospheric physics - Wien [u.a.] : Springer, 1948, 94(2006), 1-4 vom: 31. Juli, Seite 11-26 |
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Übergeordnetes Werk: |
volume:94 ; year:2006 ; number:1-4 ; day:31 ; month:07 ; pages:11-26 |
Links: |
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DOI / URN: |
10.1007/s00703-005-0170-7 |
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Katalog-ID: |
SPR007306385 |
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100 | 1 | |a Gao, J. |e verfasserin |4 aut | |
245 | 1 | 2 | |a A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint |
264 | 1 | |c 2006 | |
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520 | |a Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. | ||
650 | 4 | |a Radar |7 (dpeaa)DE-He213 | |
650 | 4 | |a Radial Velocity |7 (dpeaa)DE-He213 | |
650 | 4 | |a Doppler Radar |7 (dpeaa)DE-He213 | |
650 | 4 | |a Tangential Wind |7 (dpeaa)DE-He213 | |
650 | 4 | |a Advanced Regional Prediction System |7 (dpeaa)DE-He213 | |
700 | 1 | |a Xue, M. |e verfasserin |4 aut | |
700 | 1 | |a Lee, S.-Y. |e verfasserin |4 aut | |
700 | 1 | |a Shapiro, A. |e verfasserin |4 aut | |
700 | 1 | |a Xu, Q. |e verfasserin |4 aut | |
700 | 1 | |a Droegemeier, K. K. |e verfasserin |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Meteorology and atmospheric physics |d Wien [u.a.] : Springer, 1948 |g 94(2006), 1-4 vom: 31. Juli, Seite 11-26 |w (DE-627)25463091X |w (DE-600)1462145-9 |x 1436-5065 |7 nnns |
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856 | 4 | 0 | |u https://dx.doi.org/10.1007/s00703-005-0170-7 |z lizenzpflichtig |3 Volltext |
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912 | |a GBV_ILN_73 | ||
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912 | |a GBV_ILN_90 | ||
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912 | |a GBV_ILN_110 | ||
912 | |a GBV_ILN_120 | ||
912 | |a GBV_ILN_138 | ||
912 | |a GBV_ILN_150 | ||
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912 | |a GBV_ILN_161 | ||
912 | |a GBV_ILN_170 | ||
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912 | |a GBV_ILN_213 | ||
912 | |a GBV_ILN_224 | ||
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912 | |a GBV_ILN_281 | ||
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912 | |a GBV_ILN_370 | ||
912 | |a GBV_ILN_602 | ||
912 | |a GBV_ILN_636 | ||
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912 | |a GBV_ILN_2003 | ||
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912 | |a GBV_ILN_2025 | ||
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912 | |a GBV_ILN_2027 | ||
912 | |a GBV_ILN_2031 | ||
912 | |a GBV_ILN_2034 | ||
912 | |a GBV_ILN_2037 | ||
912 | |a GBV_ILN_2038 | ||
912 | |a GBV_ILN_2039 | ||
912 | |a GBV_ILN_2044 | ||
912 | |a GBV_ILN_2048 | ||
912 | |a GBV_ILN_2049 | ||
912 | |a GBV_ILN_2050 | ||
912 | |a GBV_ILN_2055 | ||
912 | |a GBV_ILN_2057 | ||
912 | |a GBV_ILN_2059 | ||
912 | |a GBV_ILN_2061 | ||
912 | |a GBV_ILN_2064 | ||
912 | |a GBV_ILN_2065 | ||
912 | |a GBV_ILN_2068 | ||
912 | |a GBV_ILN_2070 | ||
912 | |a GBV_ILN_2086 | ||
912 | |a GBV_ILN_2088 | ||
912 | |a GBV_ILN_2093 | ||
912 | |a GBV_ILN_2106 | ||
912 | |a GBV_ILN_2107 | ||
912 | |a GBV_ILN_2108 | ||
912 | |a GBV_ILN_2110 | ||
912 | |a GBV_ILN_2111 | ||
912 | |a GBV_ILN_2112 | ||
912 | |a GBV_ILN_2113 | ||
912 | |a GBV_ILN_2116 | ||
912 | |a GBV_ILN_2118 | ||
912 | |a GBV_ILN_2119 | ||
912 | |a GBV_ILN_2122 | ||
912 | |a GBV_ILN_2129 | ||
912 | |a GBV_ILN_2143 | ||
912 | |a GBV_ILN_2144 | ||
912 | |a GBV_ILN_2147 | ||
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912 | |a GBV_ILN_2152 | ||
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912 | |a GBV_ILN_2336 | ||
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912 | |a GBV_ILN_4336 | ||
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912 | |a GBV_ILN_4393 | ||
912 | |a GBV_ILN_4700 | ||
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10.1007/s00703-005-0170-7 doi (DE-627)SPR007306385 (SPR)s00703-005-0170-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Gao, J. verfasserin aut A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. Radar (dpeaa)DE-He213 Radial Velocity (dpeaa)DE-He213 Doppler Radar (dpeaa)DE-He213 Tangential Wind (dpeaa)DE-He213 Advanced Regional Prediction System (dpeaa)DE-He213 Xue, M. verfasserin aut Lee, S.-Y. verfasserin aut Shapiro, A. verfasserin aut Xu, Q. verfasserin aut Droegemeier, K. K. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 94(2006), 1-4 vom: 31. Juli, Seite 11-26 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:94 year:2006 number:1-4 day:31 month:07 pages:11-26 https://dx.doi.org/10.1007/s00703-005-0170-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 94 2006 1-4 31 07 11-26 |
spelling |
10.1007/s00703-005-0170-7 doi (DE-627)SPR007306385 (SPR)s00703-005-0170-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Gao, J. verfasserin aut A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. Radar (dpeaa)DE-He213 Radial Velocity (dpeaa)DE-He213 Doppler Radar (dpeaa)DE-He213 Tangential Wind (dpeaa)DE-He213 Advanced Regional Prediction System (dpeaa)DE-He213 Xue, M. verfasserin aut Lee, S.-Y. verfasserin aut Shapiro, A. verfasserin aut Xu, Q. verfasserin aut Droegemeier, K. K. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 94(2006), 1-4 vom: 31. Juli, Seite 11-26 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:94 year:2006 number:1-4 day:31 month:07 pages:11-26 https://dx.doi.org/10.1007/s00703-005-0170-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 94 2006 1-4 31 07 11-26 |
allfields_unstemmed |
10.1007/s00703-005-0170-7 doi (DE-627)SPR007306385 (SPR)s00703-005-0170-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Gao, J. verfasserin aut A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. Radar (dpeaa)DE-He213 Radial Velocity (dpeaa)DE-He213 Doppler Radar (dpeaa)DE-He213 Tangential Wind (dpeaa)DE-He213 Advanced Regional Prediction System (dpeaa)DE-He213 Xue, M. verfasserin aut Lee, S.-Y. verfasserin aut Shapiro, A. verfasserin aut Xu, Q. verfasserin aut Droegemeier, K. K. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 94(2006), 1-4 vom: 31. Juli, Seite 11-26 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:94 year:2006 number:1-4 day:31 month:07 pages:11-26 https://dx.doi.org/10.1007/s00703-005-0170-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 94 2006 1-4 31 07 11-26 |
allfieldsGer |
10.1007/s00703-005-0170-7 doi (DE-627)SPR007306385 (SPR)s00703-005-0170-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Gao, J. verfasserin aut A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. Radar (dpeaa)DE-He213 Radial Velocity (dpeaa)DE-He213 Doppler Radar (dpeaa)DE-He213 Tangential Wind (dpeaa)DE-He213 Advanced Regional Prediction System (dpeaa)DE-He213 Xue, M. verfasserin aut Lee, S.-Y. verfasserin aut Shapiro, A. verfasserin aut Xu, Q. verfasserin aut Droegemeier, K. K. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 94(2006), 1-4 vom: 31. Juli, Seite 11-26 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:94 year:2006 number:1-4 day:31 month:07 pages:11-26 https://dx.doi.org/10.1007/s00703-005-0170-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 94 2006 1-4 31 07 11-26 |
allfieldsSound |
10.1007/s00703-005-0170-7 doi (DE-627)SPR007306385 (SPR)s00703-005-0170-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Gao, J. verfasserin aut A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. Radar (dpeaa)DE-He213 Radial Velocity (dpeaa)DE-He213 Doppler Radar (dpeaa)DE-He213 Tangential Wind (dpeaa)DE-He213 Advanced Regional Prediction System (dpeaa)DE-He213 Xue, M. verfasserin aut Lee, S.-Y. verfasserin aut Shapiro, A. verfasserin aut Xu, Q. verfasserin aut Droegemeier, K. K. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 94(2006), 1-4 vom: 31. Juli, Seite 11-26 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:94 year:2006 number:1-4 day:31 month:07 pages:11-26 https://dx.doi.org/10.1007/s00703-005-0170-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 94 2006 1-4 31 07 11-26 |
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Enthalten in Meteorology and atmospheric physics 94(2006), 1-4 vom: 31. Juli, Seite 11-26 volume:94 year:2006 number:1-4 day:31 month:07 pages:11-26 |
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Radar Radial Velocity Doppler Radar Tangential Wind Advanced Regional Prediction System |
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Gao, J. @@aut@@ Xue, M. @@aut@@ Lee, S.-Y. @@aut@@ Shapiro, A. @@aut@@ Xu, Q. @@aut@@ Droegemeier, K. K. @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR007306385</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110194105.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s2006 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00703-005-0170-7</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR007306385</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00703-005-0170-7-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.80</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Gao, J.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="2"><subfield code="a">A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2006</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. 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Gao, J. |
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Gao, J. ddc 550 bkl 38.80 misc Radar misc Radial Velocity misc Doppler Radar misc Tangential Wind misc Advanced Regional Prediction System A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint |
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550 ASE 38.80 bkl A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint Radar (dpeaa)DE-He213 Radial Velocity (dpeaa)DE-He213 Doppler Radar (dpeaa)DE-He213 Tangential Wind (dpeaa)DE-He213 Advanced Regional Prediction System (dpeaa)DE-He213 |
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ddc 550 bkl 38.80 misc Radar misc Radial Velocity misc Doppler Radar misc Tangential Wind misc Advanced Regional Prediction System |
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A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint |
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A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint |
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Gao, J. Xue, M. Lee, S.-Y. Shapiro, A. Xu, Q. Droegemeier, K. K. |
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three-dimensional variational single-doppler velocity retrieval method with simple conservation equation constraint |
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A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint |
abstract |
Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. |
abstractGer |
Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. |
abstract_unstemmed |
Summary In this paper, a new three-dimensional variational analysis scheme capable of retrieving three-dimensional winds from single Doppler observations of convective storms is developed. The method incorporates, in a single cost function, Doppler radar observations, a background field, smoothness and mass continuity constraints, and the residual of reflectivity or radial velocity conservation. By minimizing this cost function, an analysis with the desired fit to these constraints is obtained in a single procedure. In tests with both simulated and real thunderstorm cases, detailed structures of the storms are well retrieved in comparison with reference analysis. Unlike most kinematic retrieval methods, our scheme is capable of directly dealing with data voids. When an analysis background is available, say from a proximity sounding, a wind profiler, or a numerical model forecast, the method naturally blends Doppler radar observations with it. Thus, a smooth transition is obtained between data-rich and data-void areas. These features, among others, are important if the analysis is to be used to initialize storm-scale numerical models or for diagnostic studies of storm structures. |
collection_details |
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container_issue |
1-4 |
title_short |
A three-dimensional variational single-Doppler velocity retrieval method with simple conservation equation constraint |
url |
https://dx.doi.org/10.1007/s00703-005-0170-7 |
remote_bool |
true |
author2 |
Xue, M. Lee, S.-Y. Shapiro, A. Xu, Q. Droegemeier, K. K. |
author2Str |
Xue, M. Lee, S.-Y. Shapiro, A. Xu, Q. Droegemeier, K. K. |
ppnlink |
25463091X |
mediatype_str_mv |
c |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s00703-005-0170-7 |
up_date |
2024-07-04T02:45:55.521Z |
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1803614846213685248 |
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score |
7.3984594 |