256 MAUSAM, 62, 2 (April 2011) Das, P. K., 1988, “The Monsoons”, National Book Trust, New Delhi. E. KULANDAIVELU M. SOUNDARARAJ* Kulandaivelu, E., 1996, “Glacier Expedition–An experience”, Vayu M. V. GUHAN Mandal, 26, 3-4, 85-88. Puniah, K. B. and De, A. C., 1974, “Cloud burst over Calcutta Airport”, Indain J. Met. Hydrol. & Geophysics, 25, 3 & 4, 503-504. Regional Meteorological Centre, Chennai-6. *Meteorological Office, Airport, Tiruchirapalli. Rauf, M. A., 1978, “Some aspects of cloud burst at the onset of southwest monsoon”, Indian J. Met. Hydrol. & Geophysics, 29, (Received 5 November 2008, Modified 4 August 2010) 1 & 2, 453-458. e mail :
[email protected] 551.509.324.2 : 551.509.335 : 556.51 resulting rainstorms over Gomti catchment and prepared synoptic analogue of forecast range for areal rainfall. Ram SEMI - QUANTITATIVE PRECIPITATION et al. (1999) also studied similar type of synoptic situation FORECASTS FOR RIVER SHARDA CATCHMENT for semi quantitative precipitation forecast in Ghaghara BY SYNOPTIC ANALOGUE METHOD catchment. 1. The technique of synoptic analogue is the most Table 1 shows the details of all gauge sites of Sharda convenient method from the view of day-to-day River for flood forecasting purposes. Statement showing operational forecasting. The dominant factor in by middle Ganga division-1 Central water commission forecasting qualitative precipitation amount is the synoptic Lucknow in “Flood Appraisal Report, Monsoon season, meteorological situation. Out of all the aspects of 2005”. Meteorology and Climatology of river basin, the most important for flood forecasting are the conditions under which flood producing heavy rains are possible in the The present paper also attempts to predict the basin.