Abstract
The role of land surface processes in land falling tropical cyclones is an area of emerging interest. Tropical cyclones are formed as organized convection over warm water (typically 26.5 °C, Gray, 1968) packing tremendous amounts of energy. Tropical cyclones have a typical size of 200-2000 km with a life span of about one to two weeks. The cyclone and its environment are interlinked. There are a number of environmental factors that are important for sustaining and intensifying a tropical cyclone including low humidity, cooler sea surface temperature (SST), or higher tropopause temperatures, dry air intrusion from land masses, and large vertical wind shear (Gray, 1968; McBride and Zehr, 1981). However a number of environmental conditions can change the evolution of a landfalling storm.
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Acknowledgements
The authors gratefully acknowledge the financial support given by the US National Science Foundation (NSF CAREER AGS-0847472), the Indian National Center for Ocean Information Services (INCOIS), MoES and the Earth System Science Organization, Ministry of Earth Sciences, Government of India (Grant no./Project no MM/SERP/CNRS/2013/INT-10/002) to conduct this research under Monsoon Mission.
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Niyogi, D., Subramanian, S., Osuri, K.K. (2016). The Role of Land Surface Processes on Tropical Cyclones: Introduction to Land Surface Models. In: Mohanty, U.C., Gopalakrishnan, S.G. (eds) Advanced Numerical Modeling and Data Assimilation Techniques for Tropical Cyclone Prediction. Springer, Dordrecht. https://doi.org/10.5822/978-94-024-0896-6_8
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