Please use this identifier to cite or link to this item: https://dspace.iiti.ac.in/handle/123456789/3706
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dc.contributor.authorDas, Saurabhen_US
dc.date.accessioned2022-03-17T01:00:00Z-
dc.date.accessioned2022-03-17T15:30:00Z-
dc.date.available2022-03-17T01:00:00Z-
dc.date.available2022-03-17T15:30:00Z-
dc.date.issued2021-
dc.identifier.citationChakravarty, K., Bhangale, R., Das, S., Yadav, P., Kannan, B. A. M., & Pandithurai, G. (2021). Unraveling the characteristics of precipitation microphysics in summer and winter monsoon over mumbai and chennai – t the two urban-coastal cities of indian sub-continent. Atmospheric Research, 249 doi:10.1016/j.atmosres.2020.105313en_US
dc.identifier.issn0169-8095-
dc.identifier.otherEID(2-s2.0-85094191687)-
dc.identifier.urihttps://doi.org/10.1016/j.atmosres.2020.105313-
dc.identifier.urihttps://dspace.iiti.ac.in/handle/123456789/3706-
dc.description.abstractThe characteristic features of inter-seasonal variability of precipitation microphysics for the year 2019 over Mumbai and Chennai – the two urban-coastal cities of Indian sub-continent have been studied in this paper. The importance of choosing the regions lies in the fact that these two cities are well-known for the occurrences of severe rainfall events due to the effect of south-west and north-east monsoon during the summer and winter season of Indian sub-continent respectively. It has been observed that raindrops of diameter 2-–4 mm dominate the summer rainfall over Chennai with respect to winter rainfall. Correspondingly, while comparing the two cities together, the impact of the south-west and north-east monsoon in conjunction with the interplay of the continental and maritime effect on the microphysics of precipitation over these cities is strongly visible in the analysis. The study reveals that the rainfall evolving from the continental clouds along with contrasting surface temperature produces distinct diurnal variation for the summer (winter) rainfall over Chennai (Mumbai) while such variations are not visible for the maritime clouds. It has been observed that the drops of larger diameter along with higher radar reflectivity dominated the summer rainfall of Chennai with respect to Mumbai. While for the winter rainfall, such distinct variations are visible only for higher rainfall regimes from 16 mm/h and above where the domination of larger drops is visible for the Mumbai rainfall. Thus the difference in surface temperature which in turn escalates the convective environment in the atmosphere can be termed as one of the important factors responsible for this inter-seasonal variability of precipitation microphysics. © 2020 Elsevier B.V.en_US
dc.language.isoenen_US
dc.publisherElsevier Ltden_US
dc.sourceAtmospheric Researchen_US
dc.subjectAtmospheric temperatureen_US
dc.subjectAtmospheric thermodynamicsen_US
dc.subjectDropsen_US
dc.subjectSurface propertiesen_US
dc.subjectDiurnal variationen_US
dc.subjectMicrophysics of precipitationsen_US
dc.subjectPrecipitation microphysicsen_US
dc.subjectRadar reflectivitiesen_US
dc.subjectRainfall regimeen_US
dc.subjectSeasonal variabilityen_US
dc.subjectSummer rainfallen_US
dc.subjectSurface temperaturesen_US
dc.subjectRainen_US
dc.subjectcloud coveren_US
dc.subjectcoastal zoneen_US
dc.subjectmonsoonen_US
dc.subjectprecipitation (climatology)en_US
dc.subjectraindropen_US
dc.subjectrainfallen_US
dc.subjectsummeren_US
dc.subjecturban areaen_US
dc.subjectwinteren_US
dc.subjectChennaien_US
dc.subjectIndiaen_US
dc.subjectMaharashtraen_US
dc.subjectMumbaien_US
dc.subjectTamil Naduen_US
dc.titleUnraveling the characteristics of precipitation microphysics in summer and winter monsoon over Mumbai and Chennai – t the two urban-coastal cities of Indian sub-continenten_US
dc.typeJournal Articleen_US
Appears in Collections:Department of Astronomy, Astrophysics and Space Engineering

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