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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Main Authors: Meiqi Song, Yu Wang, Ali Mamtimin, Jiacheng Gao, Ailiyaer Aihaiti, Chenglong Zhou, Fan Yang, Wen Huo, Cong Wen, Bo Wang
Format: Article
Language:English
Published: MDPI AG 2022-10-01
Series:Remote Sensing
Subjects:
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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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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