Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data
Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Potekaev, A. I. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
spatiotemporal dynamics of the turbulent and mean kinetic wind energy components |
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| Anmerkung: |
© Springer Science+Business Media, LLC, 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: Russian physics journal - New York, NY [u.a.] : Consultants Bureau, 1965, 65(2023), 12 vom: 25. März, Seite 2238-2244 |
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| Übergeordnetes Werk: |
volume:65 ; year:2023 ; number:12 ; day:25 ; month:03 ; pages:2238-2244 |
| Links: |
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| DOI / URN: |
10.1007/s11182-023-02896-2 |
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| Katalog-ID: |
SPR049943146 |
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| 520 | |a Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. | ||
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| 650 | 4 | |a spatiotemporal dynamics of the turbulent and mean kinetic wind energy components |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a minisodar measurements |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Shamanaeva, L. G. |4 aut | |
| 700 | 1 | |a Krasnenko, N. P. |4 aut | |
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10.1007/s11182-023-02896-2 doi (DE-627)SPR049943146 (SPR)s11182-023-02896-2-e DE-627 ger DE-627 rakwb eng Potekaev, A. I. verfasserin aut Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Science+Business Media, LLC, 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. Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. atmospheric boundary layer (dpeaa)DE-He213 spatiotemporal dynamics of the turbulent and mean kinetic wind energy components (dpeaa)DE-He213 minisodar measurements (dpeaa)DE-He213 Shamanaeva, L. G. aut Krasnenko, N. P. aut Enthalten in Russian physics journal New York, NY [u.a.] : Consultants Bureau, 1965 65(2023), 12 vom: 25. März, Seite 2238-2244 (DE-627)325572518 (DE-600)2037572-4 1573-9228 nnns volume:65 year:2023 number:12 day:25 month:03 pages:2238-2244 https://dx.doi.org/10.1007/s11182-023-02896-2 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_101 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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 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_2008 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_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 65 2023 12 25 03 2238-2244 |
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10.1007/s11182-023-02896-2 doi (DE-627)SPR049943146 (SPR)s11182-023-02896-2-e DE-627 ger DE-627 rakwb eng Potekaev, A. I. verfasserin aut Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Science+Business Media, LLC, 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. Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. atmospheric boundary layer (dpeaa)DE-He213 spatiotemporal dynamics of the turbulent and mean kinetic wind energy components (dpeaa)DE-He213 minisodar measurements (dpeaa)DE-He213 Shamanaeva, L. G. aut Krasnenko, N. P. aut Enthalten in Russian physics journal New York, NY [u.a.] : Consultants Bureau, 1965 65(2023), 12 vom: 25. März, Seite 2238-2244 (DE-627)325572518 (DE-600)2037572-4 1573-9228 nnns volume:65 year:2023 number:12 day:25 month:03 pages:2238-2244 https://dx.doi.org/10.1007/s11182-023-02896-2 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_101 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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 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_2008 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_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 65 2023 12 25 03 2238-2244 |
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10.1007/s11182-023-02896-2 doi (DE-627)SPR049943146 (SPR)s11182-023-02896-2-e DE-627 ger DE-627 rakwb eng Potekaev, A. I. verfasserin aut Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Science+Business Media, LLC, 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. Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. atmospheric boundary layer (dpeaa)DE-He213 spatiotemporal dynamics of the turbulent and mean kinetic wind energy components (dpeaa)DE-He213 minisodar measurements (dpeaa)DE-He213 Shamanaeva, L. G. aut Krasnenko, N. P. aut Enthalten in Russian physics journal New York, NY [u.a.] : Consultants Bureau, 1965 65(2023), 12 vom: 25. März, Seite 2238-2244 (DE-627)325572518 (DE-600)2037572-4 1573-9228 nnns volume:65 year:2023 number:12 day:25 month:03 pages:2238-2244 https://dx.doi.org/10.1007/s11182-023-02896-2 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_101 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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 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_2008 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_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 65 2023 12 25 03 2238-2244 |
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10.1007/s11182-023-02896-2 doi (DE-627)SPR049943146 (SPR)s11182-023-02896-2-e DE-627 ger DE-627 rakwb eng Potekaev, A. I. verfasserin aut Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Science+Business Media, LLC, 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. Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. atmospheric boundary layer (dpeaa)DE-He213 spatiotemporal dynamics of the turbulent and mean kinetic wind energy components (dpeaa)DE-He213 minisodar measurements (dpeaa)DE-He213 Shamanaeva, L. G. aut Krasnenko, N. P. aut Enthalten in Russian physics journal New York, NY [u.a.] : Consultants Bureau, 1965 65(2023), 12 vom: 25. März, Seite 2238-2244 (DE-627)325572518 (DE-600)2037572-4 1573-9228 nnns volume:65 year:2023 number:12 day:25 month:03 pages:2238-2244 https://dx.doi.org/10.1007/s11182-023-02896-2 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_101 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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 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_2008 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_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 65 2023 12 25 03 2238-2244 |
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10.1007/s11182-023-02896-2 doi (DE-627)SPR049943146 (SPR)s11182-023-02896-2-e DE-627 ger DE-627 rakwb eng Potekaev, A. I. verfasserin aut Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer Science+Business Media, LLC, 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. Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. atmospheric boundary layer (dpeaa)DE-He213 spatiotemporal dynamics of the turbulent and mean kinetic wind energy components (dpeaa)DE-He213 minisodar measurements (dpeaa)DE-He213 Shamanaeva, L. G. aut Krasnenko, N. P. aut Enthalten in Russian physics journal New York, NY [u.a.] : Consultants Bureau, 1965 65(2023), 12 vom: 25. März, Seite 2238-2244 (DE-627)325572518 (DE-600)2037572-4 1573-9228 nnns volume:65 year:2023 number:12 day:25 month:03 pages:2238-2244 https://dx.doi.org/10.1007/s11182-023-02896-2 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_101 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_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 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_2008 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_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 65 2023 12 25 03 2238-2244 |
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Potekaev, A. I. |
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Potekaev, A. I. misc atmospheric boundary layer misc spatiotemporal dynamics of the turbulent and mean kinetic wind energy components misc minisodar measurements Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data |
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Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data atmospheric boundary layer (dpeaa)DE-He213 spatiotemporal dynamics of the turbulent and mean kinetic wind energy components (dpeaa)DE-He213 minisodar measurements (dpeaa)DE-He213 |
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misc atmospheric boundary layer misc spatiotemporal dynamics of the turbulent and mean kinetic wind energy components misc minisodar measurements |
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spatiotemporal dynamics of the average and turbulent components of the kinetic wind energy in the lower atmosphere from minisodar data |
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Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data |
| abstract |
Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. © Springer Science+Business Media, LLC, 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 |
Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. © Springer Science+Business Media, LLC, 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 |
Based on post-processing of diurnal hourly measurements of three wind velocity components and their variances with an AV4000 minisodar in the lower 200-meter layer of the atmosphere, statistical analysis of the turbulent, ETКE, and average, EMКE, kinetic wind energy components has been performed. It was shown that for the diurnal period of continuous minisodar observations, the turbulent kinetic energy component in the ground atmospheric layer to altitudes of ~50 m was low. At altitudes in the range from 50 to 100 m, the turbulent kinetic energy ETКE increased, at altitudes exceeding 100 m, its growth rate intensified, and the maximum ETКE values were observed at altitudes of 150–200 m. It was established that the results of observations influenced significantly by time of the day. However, at any time, the maximum turbulent energy was localized at altitudes of ~100–200 m, which posed the greatest danger to light small-sized unmanned vehicles. The approach to revealing times and altitudes of maximum and minimum kinetic wind energy values from the minisodar data, that is, the most and least favorable time and altitude range for flights of light small-sized unmanned aerial vehicles has been proposed, and its efficiency has been illustrated. © Springer Science+Business Media, LLC, 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 |
| title_short |
Spatiotemporal Dynamics of the Average and Turbulent Components of the Kinetic Wind Energy in the Lower Atmosphere from Minisodar Data |
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https://dx.doi.org/10.1007/s11182-023-02896-2 |
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Shamanaeva, L. G. Krasnenko, N. P. |
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10.1007/s11182-023-02896-2 |
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2024-07-04T02:52:13.427Z |
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| score |
7.4003954 |