Determining of atmospheric boundary layer heights and its applications to numerical weather prediction models
The Atmospheric Boundary Layer (ABL) links the free atmosphere and the earth surface (land and ocean), and plays a significant role in the initiation and development of rainfall. The ABL height is a key parameter of ABL, and usually applied to parameterizations of the ABL processes in numerical weat...
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Format: | Article |
Language: | zho |
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Editorial Office of Torrential Rain and Disasters
2022-10-01
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Series: | 暴雨灾害 |
Subjects: | |
Online Access: | http://www.byzh.org.cn/cn/article/doi/10.12406/byzh.2021-078 |
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author | Jin WANG Qianfeng LIAO Shen YAN Yi WANG Jie XIANG |
author_facet | Jin WANG Qianfeng LIAO Shen YAN Yi WANG Jie XIANG |
author_sort | Jin WANG |
collection | DOAJ |
description | The Atmospheric Boundary Layer (ABL) links the free atmosphere and the earth surface (land and ocean), and plays a significant role in the initiation and development of rainfall. The ABL height is a key parameter of ABL, and usually applied to parameterizations of the ABL processes in numerical weather prediction and climate models. Obtaining accurate ABL height data can contribute to improving prediction skills of numerical weather prediction and climate models. The present paper introduces main methods in evaluating the ABL heights from a variety of profile data, such as conventional radiosonde data, satellite remote sensing data, aerosol backscattering intensity data, and global navigation satellite system (GNSS) radio occultation (RO) sounding data. Additionally, some progresses are presented. Three rules are suggested for dealing with the ABL with different ABL height estimates. Particular attention is paid to the application of the parameterization schemes of the ABL processes in numerical weather (or climate) prediction models, such as Weather Research and Forecasting (WRF), which includes application of ABL height data in solving the equation of turbulent eddy dispersion. And some prospects are presented finally. |
first_indexed | 2024-03-13T01:16:08Z |
format | Article |
id | doaj.art-07cb83aac4324caa99b42a9cc442707e |
institution | Directory Open Access Journal |
issn | 2097-2164 |
language | zho |
last_indexed | 2024-03-13T01:16:08Z |
publishDate | 2022-10-01 |
publisher | Editorial Office of Torrential Rain and Disasters |
record_format | Article |
series | 暴雨灾害 |
spelling | doaj.art-07cb83aac4324caa99b42a9cc442707e2023-07-05T10:06:56ZzhoEditorial Office of Torrential Rain and Disasters暴雨灾害2097-21642022-10-0141551552410.12406/byzh.2021-0782856Determining of atmospheric boundary layer heights and its applications to numerical weather prediction modelsJin WANG0Qianfeng LIAO1Shen YAN2Yi WANG3Jie XIANG4Pujiang College, Nanjing Tech University, Nanjing 211222Teaching Office, PLA University of Engineering, Nanjing 210007College of Advanced Interdisciplinary Studies, National University of Defense Technology, Changsha 410028College of Meteorology and Oceanography, National University of Defense Technology, Changsha 410028College of Meteorology and Oceanography, National University of Defense Technology, Changsha 410028The Atmospheric Boundary Layer (ABL) links the free atmosphere and the earth surface (land and ocean), and plays a significant role in the initiation and development of rainfall. The ABL height is a key parameter of ABL, and usually applied to parameterizations of the ABL processes in numerical weather prediction and climate models. Obtaining accurate ABL height data can contribute to improving prediction skills of numerical weather prediction and climate models. The present paper introduces main methods in evaluating the ABL heights from a variety of profile data, such as conventional radiosonde data, satellite remote sensing data, aerosol backscattering intensity data, and global navigation satellite system (GNSS) radio occultation (RO) sounding data. Additionally, some progresses are presented. Three rules are suggested for dealing with the ABL with different ABL height estimates. Particular attention is paid to the application of the parameterization schemes of the ABL processes in numerical weather (or climate) prediction models, such as Weather Research and Forecasting (WRF), which includes application of ABL height data in solving the equation of turbulent eddy dispersion. And some prospects are presented finally.http://www.byzh.org.cn/cn/article/doi/10.12406/byzh.2021-078atmospheric boundary layer (abl)soundingsatellite remote sensingaerosolgnss roparameterization schemes |
spellingShingle | Jin WANG Qianfeng LIAO Shen YAN Yi WANG Jie XIANG Determining of atmospheric boundary layer heights and its applications to numerical weather prediction models 暴雨灾害 atmospheric boundary layer (abl) sounding satellite remote sensing aerosol gnss ro parameterization schemes |
title | Determining of atmospheric boundary layer heights and its applications to numerical weather prediction models |
title_full | Determining of atmospheric boundary layer heights and its applications to numerical weather prediction models |
title_fullStr | Determining of atmospheric boundary layer heights and its applications to numerical weather prediction models |
title_full_unstemmed | Determining of atmospheric boundary layer heights and its applications to numerical weather prediction models |
title_short | Determining of atmospheric boundary layer heights and its applications to numerical weather prediction models |
title_sort | determining of atmospheric boundary layer heights and its applications to numerical weather prediction models |
topic | atmospheric boundary layer (abl) sounding satellite remote sensing aerosol gnss ro parameterization schemes |
url | http://www.byzh.org.cn/cn/article/doi/10.12406/byzh.2021-078 |
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