@Article{NellipudiRaPoRaYeRa:2022:ImMoLa,
               author = "Nellipudi, Nanaji Rao and Ramakrishna, S. S. V. S. and Podeti, 
                         Srinivasa Rao and Rao, B. Ravi Srinivasa and Yesubabu, V. and Rao, 
                         Brahmananda Vadlamudi",
          affiliation = "{National Atmospheric Research Laboratory} and {Andhra University} 
                         and {Andhra University} and {Andhra University} and {National 
                         Atmospheric Research Laboratory} and {Instituto Nacional de 
                         Pesquisas Espaciais (INPE)}",
                title = "Impact of the moisture and land surface processes on the 
                         sustenance of the cyclonic storm Yemyin over land using the 
                         WRF-ARW model",
              journal = "Natural Hazards",
                 year = "2022",
               volume = "114",
                pages = "495--519",
                month = "June",
             keywords = "Cyclone, Re-intensifcation, Transport of moisture, Soil moisture, 
                         Land, surface processes.",
             abstract = "In this study, an attempt is made to analyze the sensitivity of 
                         land surface process and the associated moisture budget 
                         characteristics of the cyclonic storm Yemyin (2007), which 
                         originated over the Bay of Bengal, crossed the entire Indian 
                         subcontinent, entered into the Arabian Sea and made a 2nd landfall 
                         at the Pakistan Coast. Sensitivity of land surface processes is 
                         carried using the WRF-ARW model with a focus on the sustainability 
                         and reintensifcation of the system over land along with the 
                         available observations. Our results suggest that the transport of 
                         moisture and soil moisture played a major role in the maintenance 
                         and re-intensifcation of the system over land. Transport of the 
                         strong moisture by the monsoon currents from the Arabian Sea to 
                         land furnished the energy required for the system. The transport 
                         of the vertically integrated moisture helped to increase the 
                         moisture convergence over the Indian landmass which gave the 
                         energy to sustain the system on land. An early period of rainfall 
                         before reaching the system helped to increase the soil moisture 
                         which releases the latent heat over land. Evaporation over land 
                         played an important role in amplifying the mid-tropospheric 
                         moisture, which contributed to the precipitation along with 
                         moisture fux convergence. The Noah and RUC land surface physics 
                         produced the least errors in the movement of the system while the 
                         RUC scheme gives signifcant results for intensifcation. The soil 
                         moisture zero experiment failed to provide the good results for 
                         movement and intensity of the system compared to other 
                         experiments. The soil moisture zero experiment did not yield give 
                         good results due to lack of sufcient soil moisture.",
                  doi = "10.1007/s11069-022-05399-4",
                  url = "http://dx.doi.org/10.1007/s11069-022-05399-4",
                 issn = "0921-030X",
             language = "en",
           targetfile = "s11069-022-05399-4.pdf",
        urlaccessdate = "04 maio 2024"
}