Rainfall and temperature data recorded at 17 meteorological stations over the time period 1958-2007 were used to assess recent changes in the climate of Bangladesh. The results show increasing mean, mean maximum and mean minimum temperatures at a rate of 0.103, 0.091 and 0.097°C per decade, respectively. More warming was observed for winter compared to other seasons. Increases in annual and pre-monsoon rainfall were also observed at a rate of 5.53 and 2.47 mm yr -1 , respectively. The spatial pattern of rainfall trends shows an increase in annual, monsoon and premonsoon rainfall in the western part of Bangladesh. The findings of the present study are consistent with the results obtained in other parts of the Indian subcontinent.
KEY WORDS: Climate variability · Trend analysis · GIS · Bangladesh
Resale or republication not permitted without written consent of the publisherClim Res 42: [185][186][187][188][189][190][191][192][193] 2010 ing the period 1961-1991 with a maximum increase in September followed by that in July. The only work carried out so far on temperature trends in Bangladesh is by Jones (1995), who analyzed the monthly mean maximum and minimum temperatures over the period and found no significant change in annual mean minimum and maximum temperatures. This contradicts the results obtained in the regions of India bordering Bangladesh (Pant & Rupa Kumar 1997). A large amount of scientific literature is available on the variability of rainfall and temperature of India (Mooley & Parthasarathy 1984, Rupa Kumar et al. 1992, Pant & Rupa Kumar 1997, Sinha Ray & De 2003, Arora et al. 2005, Guhathakurta & Rajeevan, 2008. These studies show an increase in the annual mean temperature over India in the last 100 yr, with a higher increase in winter temperature compared to pre-monsoon summer temperature. On the other hand, no statistically significant trend has been observed in monsoon rainfall over India as a whole (Thapliyal & Kulshrestha 1991, Pant & Rupa Kumar 1997. However, Rupa Kumar et al. (1992) reported that there are areas over India with decreasing rainfall, and other areas with increasing trends.Climate models have been used to predict the change in rainfall and temperature of Bangladesh and India (Manabe et al. 1991, Stephenson et al. 2001, Kripalani et al. 2003, Agrawala et al. 2003, May 2004, Dash et al. 2006, Immerzeel 2008. However, consensus has not yet been reached on the projected strength of monsoon circulation and the quantum of rainfall. May (2004) used a climate model to study the rainfall pattern over the tropical Indian Ocean and predicted an increase in intensity of heavy rainfall events in Bangladesh. Immerzeel (2008) predicted seasonal increases in precipitation from 2000 to 2100, with more increases in the monsoon season compared to other seasons for the Brahmaputra basin. Rupa Kumar et al. (2006) projected a marked increase in both rainfall and temperature in India towards the end of the 21st century under scenarios of increasing greenhouse gas concentrations. Kripalani...