Abstract. Long term changes of near surface air temperature over Bangladesh have been studied using the available historical data collected by the Bangladesh Meteorological Department (BMD). Maximum and minimum daily temperature data of last sixty years (1948-2007) collected from 34 stations of BMD located all over the Bangladesh have been used in this study. It has been found that daily maximum temperature shows a positive trend of increase at a rate of 0.621 ± 0.491 0C per 100 year. The maximum increase occurred during November at a rate of 2.7 0C per 100 year. However, daily minimum temperature shows more significant trend of increase at a rate of 1.536 ± 0.461 0C per 100 year. The maximum increase occurred during February at a rate of 3...
Abstract: This study aims to determine trends in the long-term monthly total data series using non-p...
Analysis of meteorological records from four stations (Chittagong, Cox’s Bazar, Rangamati, Sitakunda...
The amount of rainfall received over an area is an important factor in assessing availability of wat...
Diurnal temperature range (DTR) is a meteorological indicator independent of internal climate variat...
Surface air temperature distribution over the Ganges Delta Region of southwest Bangladesh and its te...
Due to the importance of climatic variability, an assessment detecting the changes and trends has be...
The present study is carried out to determine the trends in changes in temperature at Dhaka and Khul...
The climate of Bangladesh is very likely to be influenced by global climate change. To quantify the ...
Climate change-derived extreme heat phenomena are one of the major concerns across the globe, includ...
Bangladesh has been undergoing hazardous climatic changes. Monsoon is changing its pattern. Variatio...
Heat Index describes the combined effect of temperature and humidity on human body. This combined ef...
Dhaka, the capital of Bangladesh, is a fast growing megacity with a population of 12.8 million. Due ...
The terms “climate change" and “climate change impacts"” have become ubiquitous in the 21st century...
Climate change is one of the biggest threats for the new millennium, and Bangladesh is considered as...
Climate change is one of the biggest threats for the new millennium, and Bangladesh is considered as...
Abstract: This study aims to determine trends in the long-term monthly total data series using non-p...
Analysis of meteorological records from four stations (Chittagong, Cox’s Bazar, Rangamati, Sitakunda...
The amount of rainfall received over an area is an important factor in assessing availability of wat...
Diurnal temperature range (DTR) is a meteorological indicator independent of internal climate variat...
Surface air temperature distribution over the Ganges Delta Region of southwest Bangladesh and its te...
Due to the importance of climatic variability, an assessment detecting the changes and trends has be...
The present study is carried out to determine the trends in changes in temperature at Dhaka and Khul...
The climate of Bangladesh is very likely to be influenced by global climate change. To quantify the ...
Climate change-derived extreme heat phenomena are one of the major concerns across the globe, includ...
Bangladesh has been undergoing hazardous climatic changes. Monsoon is changing its pattern. Variatio...
Heat Index describes the combined effect of temperature and humidity on human body. This combined ef...
Dhaka, the capital of Bangladesh, is a fast growing megacity with a population of 12.8 million. Due ...
The terms “climate change" and “climate change impacts"” have become ubiquitous in the 21st century...
Climate change is one of the biggest threats for the new millennium, and Bangladesh is considered as...
Climate change is one of the biggest threats for the new millennium, and Bangladesh is considered as...
Abstract: This study aims to determine trends in the long-term monthly total data series using non-p...
Analysis of meteorological records from four stations (Chittagong, Cox’s Bazar, Rangamati, Sitakunda...
The amount of rainfall received over an area is an important factor in assessing availability of wat...