Investigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific

This study investigated the relationship between variations in the atmospheric boundary layer height (ABLH) and typhoons over the Northwest Pacific using global navigation satellite system (GNSS) radio occultation (RO) data during the local summer typhoon season (July–October in the Northern Hemisph...

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Autores principales: Jiaqi Shi, Kefei Zhang, Suqin Wu, Shuangshuang Shi, Zhen Shen
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Lenguaje:EN
Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:d84b68d8b142487aa90367f12de461172021-11-25T16:45:00ZInvestigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific10.3390/atmos121114572073-4433https://doaj.org/article/d84b68d8b142487aa90367f12de461172021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4433/12/11/1457https://doaj.org/toc/2073-4433This study investigated the relationship between variations in the atmospheric boundary layer height (ABLH) and typhoons over the Northwest Pacific using global navigation satellite system (GNSS) radio occultation (RO) data during the local summer typhoon season (July–October in the Northern Hemisphere) from 2007 to 2020. The minimum gradient of refractivity derived from COSMIC and COSMIC-2 was used to determine the ABLH. The RO profiles were co-located with the position of a typhoon track base within a 600 km space window and different time windows. ABLH climatology with a 2.5° × 2.5° horizontal resolution was developed, which can be used to obtain the interpolated mean ABLH at any target position. The mean ABLH at the central typhoon position in a specific year was compared with the results interpolated from the climatology of the same location (excluding the year in which the investigated typhoon occurred). In this paper, the results indicate that the ABLH is lower in the vicinity of typhoons relative to the undisturbed atmosphere by a significant amount, and that the reduction in ABLH ranges from 0.13 km to 0.39 km. It was also found that the ABLH was negatively correlated with wind speed, and that the mean correlation coefficient was −0.607. Moreover, similar results can be obtained via the RO water vapor partial pressure profile compared to the refractivity results.Jiaqi ShiKefei ZhangSuqin WuShuangshuang ShiZhen ShenMDPI AGarticleCOSMICCOSMIC-2GNSS ROtyphoon trackatmospheric boundary layer heightMeteorology. ClimatologyQC851-999ENAtmosphere, Vol 12, Iss 1457, p 1457 (2021)
institution DOAJ
collection DOAJ
language EN
topic COSMIC
COSMIC-2
GNSS RO
typhoon track
atmospheric boundary layer height
Meteorology. Climatology
QC851-999
spellingShingle COSMIC
COSMIC-2
GNSS RO
typhoon track
atmospheric boundary layer height
Meteorology. Climatology
QC851-999
Jiaqi Shi
Kefei Zhang
Suqin Wu
Shuangshuang Shi
Zhen Shen
Investigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific
description This study investigated the relationship between variations in the atmospheric boundary layer height (ABLH) and typhoons over the Northwest Pacific using global navigation satellite system (GNSS) radio occultation (RO) data during the local summer typhoon season (July–October in the Northern Hemisphere) from 2007 to 2020. The minimum gradient of refractivity derived from COSMIC and COSMIC-2 was used to determine the ABLH. The RO profiles were co-located with the position of a typhoon track base within a 600 km space window and different time windows. ABLH climatology with a 2.5° × 2.5° horizontal resolution was developed, which can be used to obtain the interpolated mean ABLH at any target position. The mean ABLH at the central typhoon position in a specific year was compared with the results interpolated from the climatology of the same location (excluding the year in which the investigated typhoon occurred). In this paper, the results indicate that the ABLH is lower in the vicinity of typhoons relative to the undisturbed atmosphere by a significant amount, and that the reduction in ABLH ranges from 0.13 km to 0.39 km. It was also found that the ABLH was negatively correlated with wind speed, and that the mean correlation coefficient was −0.607. Moreover, similar results can be obtained via the RO water vapor partial pressure profile compared to the refractivity results.
format article
author Jiaqi Shi
Kefei Zhang
Suqin Wu
Shuangshuang Shi
Zhen Shen
author_facet Jiaqi Shi
Kefei Zhang
Suqin Wu
Shuangshuang Shi
Zhen Shen
author_sort Jiaqi Shi
title Investigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific
title_short Investigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific
title_full Investigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific
title_fullStr Investigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific
title_full_unstemmed Investigation of the Atmospheric Boundary Layer Height Using Radio Occultation: A Case Study during Twelve Super Typhoons over the Northwest Pacific
title_sort investigation of the atmospheric boundary layer height using radio occultation: a case study during twelve super typhoons over the northwest pacific
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/d84b68d8b142487aa90367f12de46117
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