Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China

Water vapor vertical profiles are important in numerical weather prediction, moisture transport, and vertical flux calculation. This study presents the Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) retrieval algorithm for water vapor vertical profiles and the retrieved results a...

Szczegółowa specyfikacja

Opis bibliograficzny
Główni autorzy: Hua Lin, Cheng Liu, Chengzhi Xing, Qihou Hu, Qianqian Hong, Haoran Liu, Qihua Li, Wei Tan, Xiangguang Ji, Zhuang Wang, Jianguo Liu
Format: Artykuł
Język:English
Wydane: MDPI AG 2020-09-01
Seria:Remote Sensing
Hasła przedmiotowe:
Dostęp online:https://www.mdpi.com/2072-4292/12/19/3193
_version_ 1827705099556749312
author Hua Lin
Cheng Liu
Chengzhi Xing
Qihou Hu
Qianqian Hong
Haoran Liu
Qihua Li
Wei Tan
Xiangguang Ji
Zhuang Wang
Jianguo Liu
author_facet Hua Lin
Cheng Liu
Chengzhi Xing
Qihou Hu
Qianqian Hong
Haoran Liu
Qihua Li
Wei Tan
Xiangguang Ji
Zhuang Wang
Jianguo Liu
author_sort Hua Lin
collection DOAJ
description Water vapor vertical profiles are important in numerical weather prediction, moisture transport, and vertical flux calculation. This study presents the Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) retrieval algorithm for water vapor vertical profiles and the retrieved results are validated with corresponding independent datasets under clear sky. The retrieved Vertical Column Densities (VCDs) and surface concentrations are validated with the Aerosol Robotic Network (AERONET) and National Climatic Data Centre (NCDC) datasets, achieving good correlation coefficients (R) of 0.922 and 0.876, respectively. The retrieved vertical profiles agree well with weekly balloon-borne radiosonde measurements. Furthermore, the retrieved water vapor concentrations at different altitudes (100–2000 m) are validated with the corresponding European Centre for Medium-range Weather Forecasts (ECMWF) ERA-interim datasets, achieving a correlation coefficient (R) varying from 0.695 to 0.857. The total error budgets for the surface concentrations and VCDs are 31% and 38%, respectively. Finally, the retrieval performance of the MAX-DOAS algorithm under different aerosol loads is evaluated. High aerosol loads obstruct the retrieval of surface concentrations and VCDs, with surface concentrations more liable to severe interference from such aerosol loads. To summarize, the feasibility of detecting water vapor profiles using MAX-DOAS under clear sky is confirmed in this work.
first_indexed 2024-03-10T15:56:31Z
format Article
id doaj.art-0da8f74be9004383a47684d923f0f375
institution Directory Open Access Journal
issn 2072-4292
language English
last_indexed 2024-03-10T15:56:31Z
publishDate 2020-09-01
publisher MDPI AG
record_format Article
series Remote Sensing
spelling doaj.art-0da8f74be9004383a47684d923f0f3752023-11-20T15:34:42ZengMDPI AGRemote Sensing2072-42922020-09-011219319310.3390/rs12193193Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, ChinaHua Lin0Cheng Liu1Chengzhi Xing2Qihou Hu3Qianqian Hong4Haoran Liu5Qihua Li6Wei Tan7Xiangguang Ji8Zhuang Wang9Jianguo Liu10School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei 230026, ChinaKey Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, ChinaKey Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, ChinaKey Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, ChinaSchool of Environment and Civil Engineering, Jiangnan University, Wuxi 214122, ChinaInstitute of Physical Science and Information Technology, Anhui University, Hefei 230601, ChinaInstitute of Physical Science and Information Technology, Anhui University, Hefei 230601, ChinaKey Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, ChinaSchool of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei 230026, ChinaKey Laboratory of Environmental Optics and Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, ChinaSchool of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei 230026, ChinaWater vapor vertical profiles are important in numerical weather prediction, moisture transport, and vertical flux calculation. This study presents the Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) retrieval algorithm for water vapor vertical profiles and the retrieved results are validated with corresponding independent datasets under clear sky. The retrieved Vertical Column Densities (VCDs) and surface concentrations are validated with the Aerosol Robotic Network (AERONET) and National Climatic Data Centre (NCDC) datasets, achieving good correlation coefficients (R) of 0.922 and 0.876, respectively. The retrieved vertical profiles agree well with weekly balloon-borne radiosonde measurements. Furthermore, the retrieved water vapor concentrations at different altitudes (100–2000 m) are validated with the corresponding European Centre for Medium-range Weather Forecasts (ECMWF) ERA-interim datasets, achieving a correlation coefficient (R) varying from 0.695 to 0.857. The total error budgets for the surface concentrations and VCDs are 31% and 38%, respectively. Finally, the retrieval performance of the MAX-DOAS algorithm under different aerosol loads is evaluated. High aerosol loads obstruct the retrieval of surface concentrations and VCDs, with surface concentrations more liable to severe interference from such aerosol loads. To summarize, the feasibility of detecting water vapor profiles using MAX-DOAS under clear sky is confirmed in this work.https://www.mdpi.com/2072-4292/12/19/3193MAX-DOASwater vaporvertical profilesHEIPRO
spellingShingle Hua Lin
Cheng Liu
Chengzhi Xing
Qihou Hu
Qianqian Hong
Haoran Liu
Qihua Li
Wei Tan
Xiangguang Ji
Zhuang Wang
Jianguo Liu
Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China
Remote Sensing
MAX-DOAS
water vapor
vertical profiles
HEIPRO
title Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China
title_full Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China
title_fullStr Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China
title_full_unstemmed Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China
title_short Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China
title_sort validation of water vapor vertical distributions retrieved from max doas over beijing china
topic MAX-DOAS
water vapor
vertical profiles
HEIPRO
url https://www.mdpi.com/2072-4292/12/19/3193
work_keys_str_mv AT hualin validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT chengliu validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT chengzhixing validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT qihouhu validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT qianqianhong validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT haoranliu validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT qihuali validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT weitan validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT xiangguangji validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT zhuangwang validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina
AT jianguoliu validationofwatervaporverticaldistributionsretrievedfrommaxdoasoverbeijingchina