Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain
Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distribu...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jiang, Fanying [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Stochastic environmental research and risk assessment - Berlin : Springer, 1987, 37(2023), 12 vom: 29. Juli, Seite 4589-4606 |
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| Übergeordnetes Werk: |
volume:37 ; year:2023 ; number:12 ; day:29 ; month:07 ; pages:4589-4606 |
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| DOI / URN: |
10.1007/s00477-023-02529-7 |
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SPR053583655 |
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| 520 | |a Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. | ||
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| 650 | 4 | |a Mixed wind climate |7 (dpeaa)DE-He213 | |
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| 650 | 4 | |a Peaks-over-threshold |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Generalized Pareto distribution |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Zhang, Jinxiang |4 aut | |
| 700 | 1 | |a Zhang, Mingjin |4 aut | |
| 700 | 1 | |a Qin, Jingxi |4 aut | |
| 700 | 1 | |a Li, Yongle |4 aut | |
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10.1007/s00477-023-02529-7 doi (DE-627)SPR053583655 (SPR)s00477-023-02529-7-e DE-627 ger DE-627 rakwb eng Jiang, Fanying verfasserin aut Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. Mountain canyon (dpeaa)DE-He213 Mixed wind climate (dpeaa)DE-He213 Extreme wind speed (dpeaa)DE-He213 Wind classification (dpeaa)DE-He213 Peaks-over-threshold (dpeaa)DE-He213 Generalized Pareto distribution (dpeaa)DE-He213 Zhang, Jinxiang aut Zhang, Mingjin aut Qin, Jingxi aut Li, Yongle aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 37(2023), 12 vom: 29. Juli, Seite 4589-4606 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:37 year:2023 number:12 day:29 month:07 pages:4589-4606 https://dx.doi.org/10.1007/s00477-023-02529-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 37 2023 12 29 07 4589-4606 |
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10.1007/s00477-023-02529-7 doi (DE-627)SPR053583655 (SPR)s00477-023-02529-7-e DE-627 ger DE-627 rakwb eng Jiang, Fanying verfasserin aut Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. Mountain canyon (dpeaa)DE-He213 Mixed wind climate (dpeaa)DE-He213 Extreme wind speed (dpeaa)DE-He213 Wind classification (dpeaa)DE-He213 Peaks-over-threshold (dpeaa)DE-He213 Generalized Pareto distribution (dpeaa)DE-He213 Zhang, Jinxiang aut Zhang, Mingjin aut Qin, Jingxi aut Li, Yongle aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 37(2023), 12 vom: 29. Juli, Seite 4589-4606 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:37 year:2023 number:12 day:29 month:07 pages:4589-4606 https://dx.doi.org/10.1007/s00477-023-02529-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 37 2023 12 29 07 4589-4606 |
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10.1007/s00477-023-02529-7 doi (DE-627)SPR053583655 (SPR)s00477-023-02529-7-e DE-627 ger DE-627 rakwb eng Jiang, Fanying verfasserin aut Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. Mountain canyon (dpeaa)DE-He213 Mixed wind climate (dpeaa)DE-He213 Extreme wind speed (dpeaa)DE-He213 Wind classification (dpeaa)DE-He213 Peaks-over-threshold (dpeaa)DE-He213 Generalized Pareto distribution (dpeaa)DE-He213 Zhang, Jinxiang aut Zhang, Mingjin aut Qin, Jingxi aut Li, Yongle aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 37(2023), 12 vom: 29. Juli, Seite 4589-4606 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:37 year:2023 number:12 day:29 month:07 pages:4589-4606 https://dx.doi.org/10.1007/s00477-023-02529-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 37 2023 12 29 07 4589-4606 |
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10.1007/s00477-023-02529-7 doi (DE-627)SPR053583655 (SPR)s00477-023-02529-7-e DE-627 ger DE-627 rakwb eng Jiang, Fanying verfasserin aut Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. Mountain canyon (dpeaa)DE-He213 Mixed wind climate (dpeaa)DE-He213 Extreme wind speed (dpeaa)DE-He213 Wind classification (dpeaa)DE-He213 Peaks-over-threshold (dpeaa)DE-He213 Generalized Pareto distribution (dpeaa)DE-He213 Zhang, Jinxiang aut Zhang, Mingjin aut Qin, Jingxi aut Li, Yongle aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 37(2023), 12 vom: 29. Juli, Seite 4589-4606 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:37 year:2023 number:12 day:29 month:07 pages:4589-4606 https://dx.doi.org/10.1007/s00477-023-02529-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 37 2023 12 29 07 4589-4606 |
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10.1007/s00477-023-02529-7 doi (DE-627)SPR053583655 (SPR)s00477-023-02529-7-e DE-627 ger DE-627 rakwb eng Jiang, Fanying verfasserin aut Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. Mountain canyon (dpeaa)DE-He213 Mixed wind climate (dpeaa)DE-He213 Extreme wind speed (dpeaa)DE-He213 Wind classification (dpeaa)DE-He213 Peaks-over-threshold (dpeaa)DE-He213 Generalized Pareto distribution (dpeaa)DE-He213 Zhang, Jinxiang aut Zhang, Mingjin aut Qin, Jingxi aut Li, Yongle aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 37(2023), 12 vom: 29. Juli, Seite 4589-4606 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:37 year:2023 number:12 day:29 month:07 pages:4589-4606 https://dx.doi.org/10.1007/s00477-023-02529-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_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_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_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 37 2023 12 29 07 4589-4606 |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. 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Jiang, Fanying |
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Jiang, Fanying misc Mountain canyon misc Mixed wind climate misc Extreme wind speed misc Wind classification misc Peaks-over-threshold misc Generalized Pareto distribution Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain |
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Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain Mountain canyon (dpeaa)DE-He213 Mixed wind climate (dpeaa)DE-He213 Extreme wind speed (dpeaa)DE-He213 Wind classification (dpeaa)DE-He213 Peaks-over-threshold (dpeaa)DE-He213 Generalized Pareto distribution (dpeaa)DE-He213 |
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Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain |
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determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain |
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Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain |
| abstract |
Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstractGer |
Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstract_unstemmed |
Abstract Determining the extreme wind speed and basic wind speed in mountain areas is the fundamental topic in wind-resistant design for engineering structures. The traditional epochal approach commingles all types of wind's maximum speeds in a hybrid set regardless of their respective distributions. While the mountain wind climate is a typical mixed system that consists of local and synoptic wind events, differences in meteorological mechanisms lead to deviation in their wind speed distribution. Therefore, it is necessary to distinguish the mixed wind speed distribution and calculate the combined extreme wind speed. This study extends the extreme wind speed theory in mixed wind climates to the mountain wind field. The measured mountain wind data are classified into periodic thermally-driven winds caused by local thermal gradient, cooling windstorms driven by cold high pressure, and sudden intense winds caused by severe convection. Their respective distribution parameters are determined through the peaks-over-threshold approach with generalized Pareto distribution, and the combined extreme wind speed concluding all types of wind is obtained. The combined extreme wind speeds considering wind direction and attack angle are subsequently obtained. Results show that the combined value is a conservative estimation in mountain mixed wind climates. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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12 |
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Determination of extreme wind speed under different wind directions and attack angles with mixed wind climates in mountain terrain |
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https://dx.doi.org/10.1007/s00477-023-02529-7 |
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Zhang, Jinxiang Zhang, Mingjin Qin, Jingxi Li, Yongle |
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Zhang, Jinxiang Zhang, Mingjin Qin, Jingxi Li, Yongle |
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10.1007/s00477-023-02529-7 |
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2024-07-03T20:34:27.647Z |
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| score |
7.399047 |