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Falling monsoon depression frequency: a Gray-Sikka conditions perspective.
A G Prajeesh1, K Ashok, D V Bhaskar Rao
1Indian Institute of Tropical Meteorology, Pune, India.
Scientific Reports
|October 22, 2013
Summary
Monsoon depressions (MDs) making landfall on India's east coast are decreasing, particularly south of 20°N. This decline is linked to reduced mid-tropospheric humidity over the Indian region.
Area of Science:
- Meteorology
- Climatology
- Atmospheric Science
Background:
- Monsoon depressions (MDs) are crucial weather systems impacting India.
- A decreasing trend in MD frequency has been observed along the east coast of India.
- This decline is more pronounced in the southern Bay of Bengal.
Purpose of the Study:
- To investigate the reasons behind the weakening frequency of MDs in the southern Bay of Bengal.
- To analyze atmospheric parameters influencing tropical cyclogenesis.
- To validate findings using observational and reanalysis datasets.
Main Methods:
- Analysis of statistically significant trends in MD frequency (1979-2010).
- Examination of seasonal average in-situ atmospheric parameters.
- Utilizing observational data from the India Meteorological Department (IMD) and three reanalysis datasets.
- Conducting numerical sensitivity experiments.
Main Results:
- A statistically significant decreasing trend in annual monsoon depression frequency making landfall on India's east coast from 1979-2010.
- Approximately 80% of this decrease is concentrated south of 20°N.
- The weakening of MD frequency south of 20°N since the 1950s is strongly correlated with a declining trend in mid-tropospheric relative humidity over the Indian region.
Conclusions:
- Declining mid-tropospheric relative humidity is a likely cause for the reduced frequency of monsoon depressions in the southern Bay of Bengal.
- Numerical experiments support the link between reduced humidity and weakened MD activity.
- This finding has implications for understanding regional climate variability and monsoon dynamics.
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