भारतीय उष्णदेशीय मौसम विज्ञान संस्थान
Indian Institute of Tropical Meteorology
पृथ्वी विज्ञान मंत्रालय, भारत सरकार का एक स्वायत्त संस्थान
An Autonomous Institute of the Ministry of Earth Sciences, Govt. of India
Scientist Profile
Dr.(Smt.) Deepa J. S.
Designation
: Scientist D
Phone
: +91-(0)20-25904230
Fax
: +91-(0)20-25865142
Email ID
: deepa[dot]cat[at]tropmet[dot]res[dot]in
Sea level variability, Indian Ocean climate variability
| Degree | University | Year | Stream |
|---|---|---|---|
| Ph.D. | Savitribai Phule Pune University | 2016 -2020 | Atmospheric and Space Sciences |
| M.Sc. | IIT Madras | 2011 | Mathematics |
| B.Sc. | Amrita School of Arts and Sciences, Amrita Vishwa Vidyapeetham | 2009 | Physics , Mathematics |
The sea level variability and trends in the Indian Ocean
Indonesian through flow
Ocean modelling
The Indian Ocean climate variability
| Award Name | Awarded By | Awarded For | Year |
|---|---|---|---|
| Best paper presentation award | Indian Meteorological Society, Pune Chapter | Best paper presentation in the Annual Monsoon E-Workshop 2019-2020 and National E-Symposium on Cloud and Precipitation Processes | 2021 |
| 32nd Silver Jubilee Award for the year 2019 | Indian Institute of Tropical Meteorology | Best Research paper | 2020 |
| Reviewer excellence award | Indian Academy of Sciences (IAS) | Outstanding contribution as a reviewer for the Journal of Earth System Sciences | 2020 |
| Year | Designation | Institute |
|---|---|---|
| 2022-Present | Scientist D | Indian Institute of Tropical Meteorology, Pune |
| 2018-2021 | Scientist C | Indian Institute of Tropical Meteorology, Pune |
| 2014-2017 | Scientist B | Indian Institute of Tropical Meteorology, Pune |
| 2012-2013 | Trainee Scientist | Indian Institute of Tropical Meteorology, Pune |
Research Highlight
The tropical Indian Ocean decadal sea level response to the Pacific Decadal Oscillation forcing
The study establishes the relationship between the Pacific Decadal Oscillation (PDO) phases and the decadal sea level variability over the thermocline ridge region of the Indian Ocean (TRIO). Analysis reveals that the decadal variability in the sea level pattern in the TRIO in accordance with the PDO phase shifts is primarily caused by the changes in the surface wind forcing over the Indian Ocean as a response to PDO.