Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/113234
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorGao, Z-
dc.creatorZhang, J-
dc.creatorYu, M-
dc.creatorLiu, Z-
dc.creatorYin, R-
dc.creatorZhou, S-
dc.creatorZong, L-
dc.creatorNing, G-
dc.creatorXu, X-
dc.creatorGuo, Y-
dc.creatorWei, H-
dc.creatorYang, Y-
dc.date.accessioned2025-05-29T07:59:31Z-
dc.date.available2025-05-29T07:59:31Z-
dc.identifier.urihttp://hdl.handle.net/10397/113234-
dc.language.isoenen_US
dc.publisherAmerican Geophysical Unionen_US
dc.rights© 2022. The Authors. Earth and Space Science published by Wiley Periodicals LLC on behalf of American Geophysical Union.en_US
dc.rightsThis is an open access article underthe terms of the Creative Commons Attribution-NonCommercial-NoDerivsLicense (http://creativecommons.org/licenses/by-nc-nd/4.0/), which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.en_US
dc.rightsThe following publication Gao, Z., Zhang, J., Yu, M., Liu, Z., Yin, R., Zhou, S., et al. (2022). Role of water vapor modulation from multiple pathways in the occurrence of a record-breaking heavy rainfall event in China in 2021. Earth and Space Science, 9, e2022EA002357 is available at https://doi.org/10.1029/2022EA002357.en_US
dc.titleRole of water vapor modulation from multiple pathways in the occurrence of a record-breaking heavy rainfall event in China in 2021en_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume9-
dc.identifier.issue9-
dc.identifier.doi10.1029/2022EA002357-
dcterms.abstractExtreme torrential rainfall events are low-probability events. A “China-Record Extremely Heavy Rainfall” (CREHR) event with rain rate of 201.9 mm/hr occurred on 20 July in Zhengzhou in North China. Using high-density meteorological observations, ERA5 reanalysis data, remote sensing data from China's FY-4A satellite, and numerical simulation, we revealed that sufficient warm–humid airflows were continuously transported to the Zhengzhou area via multiple pathways that were mainly modulated by the large-scale western Pacific subtropical high to the north along with the anomalies of the westerly belt and a meso-scale binary typhoon system. At the local scale, under the combined action of the vertical circulation that caused low-level convergence and high-level divergence, and the rapid uplift of water vapor related to the blocking by mountainous terrain, this CREHR event was eventually triggered. Particularly, our present work shows the roles of both typhoon Cempaka and meso-scale convective systems to south of Henan province can not be ignored, producing a strong super-thick water vapor transport layer. The existence of the binary typhoon raises the level of uncertainty involved in the water vapor transport of this CREHR event.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationEarth and space science, Sept 2022, v. 9, no. 9, e2022EA002357-
dcterms.isPartOfEarth and space science-
dcterms.issued2022-09-
dc.identifier.scopus2-s2.0-85139148122-
dc.identifier.eissn2333-5084-
dc.identifier.artne2022EA002357-
dc.description.validate202505 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Othersen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThe National Key Research and Development Program of the Ministry of Science and Technology of China (2018YFC1506405); the National Natural Science Foundation of China (Grants 42175082 and 42222503)en_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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