Observed Vertical Structure of Precipitation over the Southeastern Tibetan Plateau in Summer 2021
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Materials Science
Link
https://link.springer.com/content/pdf/10.1007/s13351-023-2108-8.pdf
Reference65 articles.
1. Adirosi, E., L. Baldini, N. Roberto, et al., 2016: Improvement of vertical profiles of raindrop size distribution from micro rain radar using 2D video disdrometer measurements. Atmos. Res., 169, 404–415, doi: https://doi.org/10.1016/j.atmosres.2015.07.002.
2. Atlas, D., R. C. Srivastava, and R. S. Sekhon, 1973: Doppler radar characteristics of precipitation at vertical incidence. Rev. Geophys., 11, 1–35, doi: https://doi.org/10.1029/RG011i001p00001.
3. Barros, A. P., M. Joshi, J. Putkonen, et al., 2000: A study of the 1999 monsoon rainfall in a mountainous region in central Nepal using TRMM products and rain gauge observations. Geophys. Res. Lett., 27, 3683–3686, doi: https://doi.org/10.1029/2000GL011827.
4. Bringi, V. N., V. Chandrasekar, J. Hubbert, et al., 2003: Raindrop size distribution in different climatic regimes from disdrometer and dual-polarized radar analysis. J. Atmos. Sci., 60, 354–365, doi: https://doi.org/10.1175/1520-0469(2003)060<0354:RSDIDC>2.0.CO;2.
5. Chang, Y., and X. L. Guo, 2016: Characteristics of convective cloud and precipitation during summer time at Naqu over Tibetan Plateau. Chinese Sci. Bull., 61, 1706–1720, doi: https://doi.org/10.1360/N972015-01292. (in Chinese)
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