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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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) |
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COSMIC COSMIC-2 GNSS RO typhoon track atmospheric boundary layer height Meteorology. Climatology QC851-999 |
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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 |
work_keys_str_mv |
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1718413046504751104 |