Monthly, Seasonal and Annual Rainfall Time Series for All-India, Homogeneous Regions and Meteorological Subdivisions: 1871-2016 by Kothawale D.R., Rajeevan M., August 2017
Read MoreMonsoon (June-October) and Post monsoon (October-.November) rainfall amount in south east India exhibit distinct spatial and temporal trends. However, studies are extremely rare on whether similar synoptic scale rainfall variation also exist in multi-decadal time scale beyond the period of instrumental observation. This is possibly due to paucity of annually resolved proxy data from suitable locations. Towards this, tree ring data (~200 years) of Indian Teak (Tectona Grandis L.f.) generated from four locations is presented in this study. The locations are situated from east coast of India to Inland along a south east North West transect. The primary objective of this work is to understand how ring width index data respond to temperature and precipitation in synoptic scale. Ring width data show moderately positive response to monsoon rainfall and negative response to summer (March- May) temperature for all stations suggesting moisture deficit in warm summer. Ring width indices also exhibit positive response with post monsoon rainfall at coastal location but the response gradually reduces towards inland. This preliminary study, thus, suggests that Indian teak has a potential to capture signals of the synoptic variation of post monsoon rainfall from coast to inland. (Sengupta S., Borgaonkar H.P., Joy R.M., Ram S., Theor. Appl. Climatol., November, 2017)
Read MoreThe 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)
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