Degree | University | Year | Stream |
---|---|---|---|
Advanced Meteorological Training | India Meteorology Department | 1997 | Meteorology |
D.Phil | Allahabad University | 1992 | Fluid Dynamics |
M.Sc. | Allahabad University | 1985 | Mathematics |
Modelling ground water flow
Monsoon prediction and variability studies
Analysis of fluid flow instabilities
Use of Artificial Neural Networks for prediction and data analysis
Climate change studies using climate models and observations
Ocean and atmosphere coupled modelling
Award Name | Awarded By | Awarded For | Year |
---|---|---|---|
3rd IITM Golden Jubilee Biennial Award | Indian Institute of Tropical Meteorology | Outstanding Research Contributions | 2016 |
21st Silver Jubilee Award | Indian Institute of Tropical Meteorology, Pune | Best Research paper | 2008 |
Certificate of Merit Award | Ministry of Earth Sciences, Govt. of India | Outstanding contribution in the field of Atmospheric Science and Technology | 2008 |
3rd Brazallian Symposium | Brazillian Congress of Meteorology | Best Research paper | 2004 |
16th Silver Jubilee Award | Indian Institute of Tropical Meteorology, Pune | Best Research paper | 2003 |
IMS Prize | Indian Mathematical Society | Best Research paper | 1995 |
Year | Designation | Institute |
---|---|---|
2015-Present | Scientist G | Indian Institute of Tropical Meteorology, Pune |
2017 (Jan)-2018 (Nov) | Head, Office of Climate Research and Services | India Meteorological Department (IMD), Pune |
2010-2015 | Scientist F | Indian Institute of Tropical Meteorology, Pune |
2005-2010 | Scientist E | Indian Institute of Tropical Meteorology, Pune |
2001-2005 | Scientist D | Indian Institute of Tropical Meteorology, Pune |
1996-2001 | Senior Scientific Officer Gr.I | Indian Institute of Tropical Meteorology, Pune |
1991-1996 | Lecturer | Allahabad Degree College, Allahabad University |
Moisture dynamics of the northward and eastward propagating boreal summer intraseasonal oscillations: possible role of tropical Indo-west Pacific SST and circulation
Boreal summer intraseasonal oscillation (BSISO) has complex spatial structure due to the co-existence of equatorial eastward and off-equatorial northward propagation in the equatorial Indian Ocean. As a result, equatorial Indian Ocean convection has simultaneous northward and eastward (NE), northward only (N-only) and eastward only (E-only) propagations.