Characteristics of diurnal condensational heating at the Western Maritime Continent during MJO eastward propagation
Author:
Funder
National Natural Science Foundation of China
Natural Science Research of Jiangsu Higher Education Institutions of China
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s00382-023-06761-3.pdf
Reference41 articles.
1. Adames ÁF, Wallace JM (2014) Three-dimensional structure and evolution of the MJO and its relation to the mean flow. J Atmos Sci 71:2007–2026
2. Chang C, Wang Z, Ju J, Li T (2004) On the relationship between western maritime continent monsoon rainfall and ENSO during northern winter. J Clim 17:665–672
3. Chang C, Harr PA, Chen H-J (2005) Synoptic disturbances over the equatorial South China Sea and western Maritime Continent during boreal winter. Mon Weather Rev 133:489–503
4. Chen G (2021) Diversity of the global teleconnections associated with the Madden–Julian oscillation. J Clim 34:397–414
5. Hagos SM et al (2016) The impact of the diurnal cycle on the propagation of M adden-J ulian O scillation convection across the M aritime C ontinent. J Adv Model Earth Syst 8:1552–1564
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