Analysis of an extreme weather event in a hyper-arid region using WRF-Hydro coupling, station, and satellite data
This study investigates an extreme weather event that impacted the United Arab Emirates
(UAE) in March 2016, using the Weather Research and Forecasting (WRF) model version …
(UAE) in March 2016, using the Weather Research and Forecasting (WRF) model version …
Variability of monsoon low‐level jet and associated rainfall over India
Y Viswanadhapalli, HP Dasari… - International Journal …, 2020 - Wiley Online Library
The structure and climatology of the monsoon low‐level jet (MLLJ) is studied based on
dynamically downscaled simulations over a 37‐year period (1980–2016) using the Weather …
dynamically downscaled simulations over a 37‐year period (1980–2016) using the Weather …
Characterization of intertropical convergence zone using SAPHIR/Megha-Tropiques satellite brightness temperature data
The intertropical convergence zone (ITCZ) is a region encircling the globe near the equator
where the surface trade winds of both the hemispheres meet. It is characterized by deep …
where the surface trade winds of both the hemispheres meet. It is characterized by deep …
The dynamic and thermodynamic structure of the monsoon over southern India: New observations from the INCOMPASS IOP
Some of the highest summer monsoon rainfall in South Asia falls on the windward slopes of
the Western Ghats mountains on India's west coast and offshore over the eastern Arabian …
the Western Ghats mountains on India's west coast and offshore over the eastern Arabian …
Is the Monsoon climatology observed over the National Capital Region, Delhi indicative of an Urban-Monsoon linkage on rainfall modification?
JB Chalakkal, M Mohan - Urban Climate, 2022 - Elsevier
Abstract The Indian Summer Monsoon (ISM) plays a vital role in the lives of the National
Capital Region (NCR)-Delhi, the second biggest urban settlement globally. This study …
Capital Region (NCR)-Delhi, the second biggest urban settlement globally. This study …
Study of active and break spell phenomena of Indian summer monsoon using WRF downscaled data
VK Prathipati, Y Viswanadhapalli, VN Chennu… - Pure and Applied …, 2021 - Springer
This study evaluates the performance of a dynamically downscaled Weather Research and
Forecasting (WRF) model by capturing the characteristics of the interseasonal variability in …
Forecasting (WRF) model by capturing the characteristics of the interseasonal variability in …
An assessment of Indian Summer Monsoon (ISM) characteristics observed in continuous Radiosonding from New Delhi, National Capital Region (NCR-Delhi)
JB Chalakkal, M Mohan - Atmospheric Research, 2024 - Elsevier
The geographical location of the New Delhi, National Capital Region (NCR) within the
Northern Gangetic Plains is influenced by the Indian Summer Monsoon (ISM) and its …
Northern Gangetic Plains is influenced by the Indian Summer Monsoon (ISM) and its …
Characteristics of temperature inversion from radiosonde measurements in the Western Ghats region
The characteristics of temperature inversion (TI) are believed to be dependent on
topographical features and synoptic regime. Western Ghats (WGs) mountains located in the …
topographical features and synoptic regime. Western Ghats (WGs) mountains located in the …
Role of vertical structure of cloud microphysical properties on cloud radiative forcing over the Asian monsoon region
Abstract Five years (2006–2010) of clouds and earth's radiant energy system (CERES) and
CloudSat data have been analyzed to examine the role of vertical structure of cloud …
CloudSat data have been analyzed to examine the role of vertical structure of cloud …
Radiative characteristics of fog over the Indo-Gangetic Plains during northern winter
V Sathiyamoorthy, R Arya, CM Kishtawal - Climate Dynamics, 2016 - Springer
Abstract The Indo-Gangetic plains (IGP), spread across northern parts of India, Pakistan and
Bangladesh is a hot-spot for fog formation during northern winter. The unavailability of long …
Bangladesh is a hot-spot for fog formation during northern winter. The unavailability of long …