Trends in extreme rainfall events in Sri Lanka,1961–2010

Abstract

Abstract: Many parts of Sri Lanka are vulnerable to extreme UDLQIDOO HYHQWV OHDGLQJ WR ÀRRGV DQG GURXJKWV 7KLV VWXG\ was focused on a trend analysis of climate extremes derived from daily rainfall records. The daily rainfall data from 13 PHWHRURORJLFDO VWDWLRQV UHSUHVHQWLQJ GL൵HUHQW JHRJUDSKLFDO regions in Sri Lanka for the period 1961–2010 were chosen. The analysis was carried out separately for summer half year (March-August) and winter half year (September-February) to capture the possible changes in two growing seasons, Yala and Maha. Magnitudes of trends were derived using linear regression DQDO\VLV ZKLOH WKH VWDWLVWLFDO VLJQL¿FDQFH ZDV GHWHUPLQHG XVLQJ the Mann-Kendall test. Spatial maps were used to study the UHJLRQDO GL൵HUHQFHV LQ FOLPDWH H[WUHPHV ([WUHPH UDLQIDOO HYHQWV were found to be isolated events without coherent increasing or GHFUHDVLQJ WUHQGV +RZHYHU VWDWLVWLFDOO\ VLJQL¿FDQW LQFUHDVLQJ (decreasing) trends were observed for number of dry days (wet days) ranging from 1.1 to 3.1 days/decade in most parts of the island during the summer half year, except for the coastal areas of the dry zone. No increasing or decreasing trends in extremes were observed for the winter half year. Based on the analysis, it was concluded that there is widespread climate change leading to increasing (decreasing) dry days (wet days) during the summer half year receiving rainfall predominantly from the South-West monsoon. However, mixed results were obtained for the winter half year.