Prof. Arindam Chakraborty
, Indian Institute of Science
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Publications: Clouds, Convection and Radiation
Jana, K, D Sengupta, S Kundu, Arindam Chakraborty and P Shaw, 2019:
The Statistical Face of a Region Under Monsoon Rainfall in Eastern India
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Journal of the American Statistical Association
, DOI: 10.1080/01621459.2019.1681275
Jain, D., Arindam Chakraborty, and R.S. Nanjundaiah, 2018:
A Mechanism for the Southward Propagation of Mesoscale Convective Systems Over the Bay of Bengal.
Journal of Geophysical Research (Atmospheres), 123, 3893-3913, doi:10.1002/2017JD027470.
Bhattacharya, A, Arindam Chakraborty, and V. Venugopal, 2017:
Role of aerosols in modulating cloud properties during active-break cycle of Indian summer monsoon
. Climate Dynamics, 49(5-6), 2131-2145.
Bhattacharya, A., Arindam Chakraborty and V Venugopal, 2014:
Variability of cloud liquid water and ice over South Asia from TMI estimates
, Climate Dynamics, DOI 10.1007/s00382-013-1978-3. [
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Jain, D. K., Arindam Chakraborty, and R S Nanjundiah, 2013:
Role of the cloud adjustment time scale in simulation of the interannual variability of Indian summer monsoon
, Meteorology and Atmospheric Physics, 122:159-173. [
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Jain, D. K., Arindam Chakraborty, and R S Nanjundiah, 2012:
On the role of cloud adjustment time scale in simulating precipitation with Relaxed Arakawa–Schubert convection scheme
, Meteorology and Atmospheric Physics, 115, 1-13. [
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Krishnamurti, T. N., Arindam Chakraborty, and A. K. Mishra, 2010:
Improving multimodel forecasts of the vertical distribution of heating using the TRMM profiles
, J. Climate, 23, 1089-1094. [
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Chakraborty, A., T. N. Krishnamurti and C. Gnanaseelan, 2007:
Prediction of the Diurnal Cycle using a Multimodel Superensemble. Part II: Clouds
, Monthly Weather Review, 135, 4097-4116. [
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Chakraborty, A., and J. Srinivasan, 2003:
Comparison of radiative fluxes at the top of the atmosphere from INSAT and ERBE
, Mausam, 54, 299-314. [
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Bhat, G. S., Arindam Chakraborty, R. S. Nanjundiah and J. Srinivasan, 2002:
Vertical thermal structure of the atmosphere during active and weak phases of convection over the north Bay of Bengal: Observation and model results
, Current Science, 83, 296-302. [
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