Mesoscale anomalous three-dimensional atmospheric circulation underpinned regional heavy rainfall events in the eastern foot of Tibetan Plateau
Author:
Funder
National Natural Science Foundation of China
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00382-024-07108-2.pdf
Reference34 articles.
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2. Chen B, Xu X (2016) Spatiotemporal structure of the moisture sources feeding heavy precipitation events over the Sichuan Basin. Int J Climatol 36:3446–3457
3. Chen H, Yu R, Li J et al (2010) Why nocturnal long-duration rainfall presents an eastward-delayed diurnal phase of rainfall down the Yangtze river valley. J Clim 23:905–917
4. Chen H, Li J, Yu R (2018) Warm season nocturnal rainfall over the eastern periphery of the Tibetan Plateau and its relationship with rainfall events in adjacent regions. Int J Climatol 38:4786–4801
5. Chen Y, Wang X, Huang L et al (2021) Spatial and temporal characteristics of abrupt heavy rainfall events over Southwest China during 1981–2017. Int J Climatol 41:3286–3299
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