Articles | Volume 26, issue 7
https://doi.org/10.5194/acp-26-4633-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-26-4633-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evaluation of reanalysis precipitable water vapor under typhoon conditions using multi-source observations
Jiaqi Shi
GNSS Research Center, Wuhan University, Wuhan, 430079, China
School of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, China
Min Li
CORRESPONDING AUTHOR
GNSS Research Center, Wuhan University, Wuhan, 430079, China
School of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, China
Andrea K. Steiner
Wegener Center for Climate and Global Change, University of Graz, 8010 Graz, Austria
Sebastian Scher
Wegener Center for Climate and Global Change, University of Graz, 8010 Graz, Austria
Department of Geography and Regional Sciences, University of Graz, 8010 Graz, Austria
Minghao Zhang
School of Environment Science and Spatial Informatics, China University of Mining and Technology, Xuzhou, 221116, China
GNSS Research Center, Wuhan University, Wuhan, 430079, China
School of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, China
Wenliang Gao
GNSS Research Center, Wuhan University, Wuhan, 430079, China
School of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, China
Yongzhao Fan
GNSS Research Center, Wuhan University, Wuhan, 430079, China
School of Geodesy and Geomatics, Wuhan University, Wuhan, 430079, China
School of Earth Sciences and Engineering, Hohai University, Nanjing, 211100, China
Kefei Zhang
School of Environment Science and Spatial Informatics, China University of Mining and Technology, Xuzhou, 221116, China
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Florina Roana Schalamon, Sebastian Scher, Andreas Trügler, Lea Hartl, Wolfgang Schöner, and Jakob Abermann
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Major sudden stratospheric warmings (SSWs) and atmospheric blocking can markedly influence winter extratropical surface weather. To study the relationship between SSWs and blocking, we examine dynamic stratosphere–troposphere coupling using vertically highly resolved observations from global navigation satellite system radio occultation for 2007–2019. Our results provide a purely observational view of the evolution of major SSWs, their link to blocking, and their effect on the polar tropopause.
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Karina von Schuckmann, Audrey Minière, Flora Gues, Francisco José Cuesta-Valero, Gottfried Kirchengast, Susheel Adusumilli, Fiammetta Straneo, Michaël Ablain, Richard P. Allan, Paul M. Barker, Hugo Beltrami, Alejandro Blazquez, Tim Boyer, Lijing Cheng, John Church, Damien Desbruyeres, Han Dolman, Catia M. Domingues, Almudena García-García, Donata Giglio, John E. Gilson, Maximilian Gorfer, Leopold Haimberger, Maria Z. Hakuba, Stefan Hendricks, Shigeki Hosoda, Gregory C. Johnson, Rachel Killick, Brian King, Nicolas Kolodziejczyk, Anton Korosov, Gerhard Krinner, Mikael Kuusela, Felix W. Landerer, Moritz Langer, Thomas Lavergne, Isobel Lawrence, Yuehua Li, John Lyman, Florence Marti, Ben Marzeion, Michael Mayer, Andrew H. MacDougall, Trevor McDougall, Didier Paolo Monselesan, Jan Nitzbon, Inès Otosaka, Jian Peng, Sarah Purkey, Dean Roemmich, Kanako Sato, Katsunari Sato, Abhishek Savita, Axel Schweiger, Andrew Shepherd, Sonia I. Seneviratne, Leon Simons, Donald A. Slater, Thomas Slater, Andrea K. Steiner, Toshio Suga, Tanguy Szekely, Wim Thiery, Mary-Louise Timmermans, Inne Vanderkelen, Susan E. Wjiffels, Tonghua Wu, and Michael Zemp
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Longjiang Li, Suqin Wu, Kefei Zhang, Xiaoming Wang, Wang Li, Zhen Shen, Dantong Zhu, Qimin He, and Moufeng Wan
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The zenith hydrostatic delay (ZHD) derived from blind models are of low accuracy, especially in mid- and high-latitude regions. To address this issue, the ratio of the ZHD to zenith total delay (ZTD) is firstly investigated; then, based on the relationship between the ZHD and ZTD, a new ZHD model was developed using the back propagation artificial neural network (BP-ANN) method which took the ZTD as an input variable. The model outperforms blind models.
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In hydrology, it is often necessary to infer from a daily sum of precipitation a possible distribution over the day – for example how much it rained in each hour. In principle, for a given daily sum, there are endless possibilities. However, some are more likely than others. We show that a method from artificial intelligence called generative adversarial networks (GANs) can
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Short summary
This study evaluates how three reanalysis datasets represent precipitable water vapor (PWV) during more than 100 typhoons from 2020 to 2024 using multi-source observations. The fifth-generation European Centre for Medium-Range Weather Forecasts Reanalysis (ERA5) performs best, the Japanese Reanalysis for Three Quarters of a Century (JRA-3Q) improves during typhoons, and the Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2) is less stable
This study evaluates how three reanalysis datasets represent precipitable water vapor (PWV)...
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