The authors investigate the life cycle of a strong subtropical stratospheric intrusion event and propose a hypothesis through which might reduce the intensity of the Indian-summer-monsoon rainfall (ISMR) after the monsoon onset during June 2014. The diagnostic analysis of ERA-Interim data revealed that stratospheric intrusion occurs in the region of Subtropical Westerly Jet (SWJ) due to Rossby Wave Breaking (RWB). The RWB event is associated with eddy shedding. These eddies transport extratropical stratospheric mass and energy fluxes downward and southward to North India (NI). As a result, the intrusion spread dry, cold and ozone rich air deep into the troposphere (~500hPa) over the NI. It enhances the static stability and weakens the North-South upper tropospheric temperature gradient. The intrusion of cold and dry air persisted for the entire June which might have inhibited northward propagation of ISM convection and could be responsible for prolonged hiatus in northward phase propagation of the ISM after onset. We also investigate the relation between stratospheric intrusion events and ISMR from long term data (1979-2007). Our analysis shows that the stronger negative anomalies of rainfall are associated with stratospheric intrusions during break spells. Thus study reveals that stratospheric intrusion is an important factor that may influence ISMR deficit. (Fadnavis S., Chattopadhyay R., Journal of Climate, July 2017)
Read MoreAregionaltree-ring chronology prepared from two species (Piceasmithiana and Cedrusdeodara) over western Himalaya has been used in relation to climate fluctuations in present study. This analysis shows that moisture index and rainfall during (February to May) have significant positive relationship whereas temperature and heat index showed negative relationship with trees growth. But, moisture and heat index indicate more impact to trees growth than rainfall and temperature. The strong association of tree-rings chronology with moisture demonstrates that tree-rings are much more sensitivity to availability of moisture at trees root zone which enabled us to extend it back to AD 1789; consecutive two years moisture deficiency during 1846-1847, 1908-1909, 1921-1922, 1931-1932, 1947-1948, and 1966-1967 was noticed in the present reconstruction. (Somaru Ram and H.P. Borgaonkar, online June 2017)
Read MoreThis paper focused on regional variability in annual and seasonal tropospheric temperature trends during the period 1971-2015 by using the 19 radiosonde stations data.The linear trends in surface and the tropospheric temperatures at five selected isobaric levels (850, 700, 500, 200 and 150 hPa) were examined for all-India, North India and South India. Increasing trend in annual temperatures were observed from surface to 500 hPa levels, but decreasing from 200 to 150 hPa over South India whereas, North India shows an increasing trend at all the levels. The highest increasing trends of 0.36°C and 0.27°C per decade were observed at 700 hPa over North and South India during the winter season, respectively. Annual mean temperature series of North and South India show a significant increasing trend at only surface and 700 hPa level. At the surface, annual mean temperature of South India shows higher increasing trend (0.19°C/decade) than that of the North India (0.17°C/decade). While, at 700 hPa, the reverse is observed, North India temperature shows higher trend of 0.25°C than the South India temperature trend of 0.15°C per decade(Kothawale D.R., Singh H.N., Earth and Space Science, May 2017)
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