Dynamic Trigger and Moisture Source of Two Typical Meiyu Front Rainstorms Associated with Eastward-Moving Cloud Clusters from the Tibetan Plateau
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Materials Science
Link
https://link.springer.com/content/pdf/10.1007/s13351-022-1179-2.pdf
Reference50 articles.
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3. Chen, G. X., R. Yoshida, W. M. Sha, et al., 2014: Convective instability associated with the eastward-propagating rainfall episodes over eastern China during the warm season. J. Climate, 27, 2331–2339, doi: https://doi.org/10.1175/JCLI-D-13-00443.1.
4. Chen, S.-J., Y.-H. Kuo, W. Wang, et al., 1998: A modeling case study of heavy rainstorms along the Mei-Yu front. Mon. Wea. Rev., 126, 2330–2351, doi:https://doi.org/10.1175/1520-0493(1998)126<2330:AMCSOH>2.0.CO;2.
5. Chen, Z.-M., 2007: Effects of barotropic and baroclinic forces on the excitation and maintenance for torrential rain. Chinese J. Atmos. Sci., 31, 291–297, doi: https://doi.org/10.1387/j.issn.1060-9895.2007.02.10. (in Chinese)
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