Zobrazeno 1 - 10
of 102
pro vyhledávání: '"Naresh Krishna Vissa"'
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-11 (2024)
Abstract India experienced several unprecedented floods in the recent decades. The increase in the extreme rainfall events (EREs) is the primary cause for these floods, manifesting its societal impacts. The daily downscaled and bias corrected (DBC) C
Externí odkaz:
https://doaj.org/article/288f2c79c8ed48428ab04cfe387f29ef
Autor:
Mohan Murali Krishna Gorja, Venkata Sai Gulakaram, Naresh Krishna Vissa, Yesubabu Viswanadhapalli, Bhishma Tyagi
Publikováno v:
Atmosphere, Vol 14, Iss 2, p 333 (2023)
The present study investigates the variation in large-scale environments during the maximum intensity of tropical cyclones (TCs) formed in the Bay of Bengal. TC tracks are classified into four groups based on their direction of movement using the k-m
Externí odkaz:
https://doaj.org/article/6f4adc7cb49c4b8abd4f60964f31d3a9
Publikováno v:
Climate, Vol 11, Iss 2, p 35 (2023)
In recent years, and particularly from 2000 onwards, the North Indian Ocean (NIO) has been acting as a major sink of ocean heat that is clearly visible in the sub-surface warming trend. Interestingly, a part of the NIO—the Arabian Sea (AS) sector
Externí odkaz:
https://doaj.org/article/ceabd304299642019752ce8070f0574f
Publikováno v:
Toxics, Vol 10, Iss 11, p 653 (2022)
The spread of the COVID-19 pandemic forced the administration to lock down in many countries globally to stop the spread. As the lockdown phase had only the emergency use of transportation and most of the industries were shut down, there was an appar
Externí odkaz:
https://doaj.org/article/fd1a30f9610f412f8b2af9b1f733184f
Publikováno v:
Atmosphere, Vol 13, Iss 8, p 1261 (2022)
El-Niño and La-Niña are believed to change the intensity and frequencies of extreme weather events globally. The present study aims to analyse the impact of El-Niño and La-Niña on the lightning activities of cloud systems and their associated pre
Externí odkaz:
https://doaj.org/article/395eb2c50f644cdfbac30967eede8f30
Publikováno v:
Journal of Ocean Engineering and Science, Vol 3, Iss 4, Pp 343-354 (2018)
Our study aims to understand the variability of oceanic mesoscale eddies during contrasting (2009 and 2013) monsoon seasons and the role of such eddies on atmospheric deep convection over the Bay of Bengal (BoB). Oceanic eddies are detected and track
Externí odkaz:
https://doaj.org/article/10d7d46045ef499abee541a4a6774f6a
Publikováno v:
Ocean Dynamics. 73:165-179
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ac10876659b847cf93cfde7968adcc1
https://doi.org/10.1007/s10236-023-01547-x
https://doi.org/10.1007/s10236-023-01547-x
Autor:
Viswanadhapalli Yesubabu, Vijaya Kumari Kattamanchi, Naresh Krishna Vissa, Hari Prasad Dasari, Vijaya Bhaskara Rao Sarangam
Publikováno v:
Meteorological Applications, Vol 27, Iss 1, Pp n/a-n/a (2020)
Abstract The sensitivity of the simulated tropical cyclone (TC) intensity and tracks to the different ocean mixed‐layer depth (MLD) initializations is studied using coupled weather research and forecasting (WRF) and ocean mixed‐layer (OML) models
Externí odkaz:
https://doaj.org/article/39e62c884f8c4353b912453934cd2edd
Autor:
Dibyashakti Panda, Bhaskar Kundu, Vineet K. Gahalaut, Roland Bürgmann, Birendra Jha, Renuhaa Asaithambi, Rajeev Kumar Yadav, Naresh Krishna Vissa, Amit Kumar Bansal
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
The interaction between seasonally-induced non-tectonic and tectonic deformation along the Himalayan plate boundary is still debated. Here, the authors propose that seasonal hydrological loading can influence tectonic deformation along this plate bou
Externí odkaz:
https://doaj.org/article/fefc73cd8f374f219009eff20ffe0f9e
Autor:
Gopinadh Konda, Naresh Krishna Vissa
Publikováno v:
Climate Dynamics. 60:1023-1042
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b520e04cbac061baa202df5006b68f97
https://doi.org/10.1007/s00382-022-06367-1
https://doi.org/10.1007/s00382-022-06367-1