“…Here we are more concerned about the rainfall in JJA, during which Indian subcontinent gets maximum rainfall. This newly defined break period selection matches well with several earlier studies (Krishnan et al 2009;Rajeevan et al 2010Rajeevan et al , 2013Singh 2013). The defined excess and deficit/break episodes match well with India Meteorological Department (IMD) rain gauge observations.…”
Section: Identification Of Monsoon Break Days From Trmm Datasupporting
to be one of the major causes of dry spell/break episodes in ISM. Additionally, the presence of cold air over Central India reduces the north-south thermal contrast over the monsoon region thereby modifying the local Hadley circulation over the region.
“…Here we are more concerned about the rainfall in JJA, during which Indian subcontinent gets maximum rainfall. This newly defined break period selection matches well with several earlier studies (Krishnan et al 2009;Rajeevan et al 2010Rajeevan et al , 2013Singh 2013). The defined excess and deficit/break episodes match well with India Meteorological Department (IMD) rain gauge observations.…”
Section: Identification Of Monsoon Break Days From Trmm Datasupporting
to be one of the major causes of dry spell/break episodes in ISM. Additionally, the presence of cold air over Central India reduces the north-south thermal contrast over the monsoon region thereby modifying the local Hadley circulation over the region.
“…The snow is mostly above 550 hPa, and there is a snow maximum around 78-84°E. These east-west cross sections compare well with the active period composite shown in Rajeevan et al (2013), where the longitude-height variation of the cloud and ice liquid water content is investigated. During the active period, which is when most of the LPS develop, there are positive anomalies of convective plumes across the central Indian continent.…”
Section: Sensitivity Of Areal Mean Precipitation and Runoff To Increasupporting
“…ISM rainfall (ISMR) is important due to its impact on agrarian economies of countries like India (e.g., Gadgil 1996). The country receives more than 80 % of the annual rainfall during a short span of 4 months from June to September (e.g., Rajeevan et al 2013). Kripalani et al (2007) studied the ability of global climate models (GCMs) in simulating the ISMR and its variability and found several discrepancies in the simulation of regional precipitation.…”
followed by a low-level dry (moist) anomaly. The model is inadequately representing the temporal evolution of vertical moist and thermodynamic processes. The evolution of vertical structures of temperature and WVMR is better simulated in the break phase compared to that of active phase. The evolution of cyclonic vorticity in the model is different from the observations during the convective phase. In short the model has limitations in representing convectively unstable regimes. It is anticipated that these findings will significantly contribute to the regional climate model assessment programs.
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