Abstract
Data collected over five years (1967-71) with a self-recording evaporigraph at the Central Agricultural Meteorological Observatory in Poona, are analysed and discussed.
 The afternoon 3-hour period 1330-1630 IST is found to contribute as much as 24 to 30 percent of the total daily evaporation recorded in any month; whereas the 15-hr period 1930-1030 IST can account for only 26 to 41 percent of the total daily evaporation.
 A statistical analysis of evaporigraph data in comparison with Class A Pan evaporimeter measurements is also presented.
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