Two Typical Synoptic-Scale Weather Patterns of Dust Events over the Tibetan Plateau
Author:
Funder
National Key R&D Program of China
China's Second Tibetan Plateau Scientific Expedition and Research
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s13143-023-00325-5.pdf
Reference40 articles.
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2. Bao, M., Wallace, J.M.: Cluster analysis of northern hemisphere wintertime 500-hPa flow regimes during 1920–2014*. J. Atmos. Sci. 72, 3597–3608 (2015). https://doi.org/10.1175/JAS-D-15-0001.1
3. Bilal, M., Nazeer, M., Qiu, Z., Ding, X., Wei, J.: Global validation of MODIS C6 and C6.1 merged aerosol products over diverse vegetated surfaces. Remote Sens. 10, 475 (2018). https://doi.org/10.3390/rs10030475
4. Chen, S., Huang, J., Zhao, C., Qian, Y., Leung, L.R., Yang, B.: Modeling the transport and radiative forcing of Taklimakan dust over the Tibetan Plateau: a case study in the summer of 2006. J. Geophys. Res. Atmos. 118, 797–812 (2013). https://doi.org/10.1016/j.earscirev.2020.103408
5. Dong, Z., Brahney, J., Kang, S., Elser, J., Wei, T., Jiao, X., Shao, Y.: Aeolian dust transport, cycle and influences in high-elevation cryosphere of the Tibetan Plateau region: new evidences from alpine snow and ice. Earth-Sci. Rev. 211, 103408 (2020). https://doi.org/10.1016/j.earscirev.2020.103408
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