Characteristics of observed tropopause height derived from L-band sounder over the Tibetan Plateau and surrounding areas
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
http://link.springer.com/content/pdf/10.1007/s13143-016-0035-7.pdf
Reference46 articles.
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3. Fan, J., J. M. Comstock, and M. Ovchinnikov, 2010: The cloud condensation nuclei and ice nuclei effects on tropical anvil characteristics and water vapor of the tropical tropopause layer. Environ. Res. Lett., 5, 044005, doi:10.1088/1748-9326/5/4/044005.
4. Feng, S., Y. Fu, and Q. Xiao, 2011: Is the tropopause higher over the Tibetan Plateau? Observational evidence from Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMOC) data. J. Geophys. Res., 116, D21121, doi:10.1029/2011JD016140.
5. Fu, R., Y. Hu, J. S. Wright, J. H. Jiang, R. E. Dickinson, M. Chen, M. Filipiak, W. G. Read, J. W. Waters, and D. L. Wu, 2006: Short circuit of water vapor and polluted air to the global stratosphere by convective transport over the Tibetan Plateau. Proc. the National Academy of Sciences of the United States of America, 103, 5664–5669.
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