Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan Plateau
Wind profile light detection and ranging (LiDAR) is an important tool for observing features within the atmospheric boundary layer. Observations of the wind field and boundary layer height from coherent Doppler wind LiDARs (CDWLs) under sandy and dusty weather conditions were evaluated using observa...
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MDPI AG
2022-10-01
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Online Access: | https://www.mdpi.com/2072-4292/14/20/5264 |
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author | Meiqi Song Yu Wang Ali Mamtimin Jiacheng Gao Ailiyaer Aihaiti Chenglong Zhou Fan Yang Wen Huo Cong Wen Bo Wang |
author_facet | Meiqi Song Yu Wang Ali Mamtimin Jiacheng Gao Ailiyaer Aihaiti Chenglong Zhou Fan Yang Wen Huo Cong Wen Bo Wang |
author_sort | Meiqi Song |
collection | DOAJ |
description | Wind profile light detection and ranging (LiDAR) is an important tool for observing features within the atmospheric boundary layer. Observations of the wind field and boundary layer height from coherent Doppler wind LiDARs (CDWLs) under sandy and dusty weather conditions were evaluated using observations from two CDWLs and one GTS radio sounding located at the northern edge of the Tibetan plateau from 1 May to 30 August 2021. The results showed that CDWL has good applicability in reproducing wind fields in dust, precipitation, and in clear-sky conditions, and that it is superior to the <i>v</i> wind field for real measurements of the <i>u</i> wind fields. In terms of the planetary boundary layer height (PBLH), the validity of the inversion of PBLH in dusty weather was higher than that under clear-sky conditions. It was found that the PBLH retrieved by the CDWL at 20:00 (BJT) was better than that at 08:00 (BJT). The diurnal variation amplitude of the PBLH before the occurrence of a sandstorm was larger than the diurnal variation amplitude of the PBLH occurring during a sandstorm. |
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issn | 2072-4292 |
language | English |
last_indexed | 2024-03-09T19:31:57Z |
publishDate | 2022-10-01 |
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series | Remote Sensing |
spelling | doaj.art-ad8d91c8595b4725adc5f4e21bc3d49e2023-11-24T02:22:19ZengMDPI AGRemote Sensing2072-42922022-10-011420526410.3390/rs14205264Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan PlateauMeiqi Song0Yu Wang1Ali Mamtimin2Jiacheng Gao3Ailiyaer Aihaiti4Chenglong Zhou5Fan Yang6Wen Huo7Cong Wen8Bo Wang9Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaInstitute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, ChinaXinjiang Meteorological Service Center, Urumqi 830002, ChinaWind profile light detection and ranging (LiDAR) is an important tool for observing features within the atmospheric boundary layer. Observations of the wind field and boundary layer height from coherent Doppler wind LiDARs (CDWLs) under sandy and dusty weather conditions were evaluated using observations from two CDWLs and one GTS radio sounding located at the northern edge of the Tibetan plateau from 1 May to 30 August 2021. The results showed that CDWL has good applicability in reproducing wind fields in dust, precipitation, and in clear-sky conditions, and that it is superior to the <i>v</i> wind field for real measurements of the <i>u</i> wind fields. In terms of the planetary boundary layer height (PBLH), the validity of the inversion of PBLH in dusty weather was higher than that under clear-sky conditions. It was found that the PBLH retrieved by the CDWL at 20:00 (BJT) was better than that at 08:00 (BJT). The diurnal variation amplitude of the PBLH before the occurrence of a sandstorm was larger than the diurnal variation amplitude of the PBLH occurring during a sandstorm.https://www.mdpi.com/2072-4292/14/20/5264coherent doppler wind LiDARnorthern edge of Tibetan plateaudusty weathermonitoring application assessment |
spellingShingle | Meiqi Song Yu Wang Ali Mamtimin Jiacheng Gao Ailiyaer Aihaiti Chenglong Zhou Fan Yang Wen Huo Cong Wen Bo Wang Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan Plateau Remote Sensing coherent doppler wind LiDAR northern edge of Tibetan plateau dusty weather monitoring application assessment |
title | Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan Plateau |
title_full | Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan Plateau |
title_fullStr | Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan Plateau |
title_full_unstemmed | Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan Plateau |
title_short | Applicability Assessment of Coherent Doppler Wind LiDAR for Monitoring during Dusty Weather at the Northern Edge of the Tibetan Plateau |
title_sort | applicability assessment of coherent doppler wind lidar for monitoring during dusty weather at the northern edge of the tibetan plateau |
topic | coherent doppler wind LiDAR northern edge of Tibetan plateau dusty weather monitoring application assessment |
url | https://www.mdpi.com/2072-4292/14/20/5264 |
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