Abstract:
In this research work we have tried to find out the multiple correlation between five
meteorological parameters dry bulb temperature, wet bulb temperature, minimum
temperature, maximum temperature and rainfall of pre-monsoon season with the rainfall
of monsoon season over Bangladesh. Initially correlation coefficients (CC) between
different parameters of pre-monsoon season and rainfall of the monsoon have been
studied. The correlation coefficients between these parameters with the monthly and
seasonal rainfall have been studied.
In this research work we have used the data of thirty meteorological stations during 1951
to 2000 all over Bangladesh. We have collected these raw data from Bangladesh
Meteorological Department (BMD). We processed these raw data and obtained the
monthly and seasonal average. Using these processed data we have analyzed:
1. The average dry bulb temperature (DBT), wet bulb temperature (WBT), minimum
temperature (MinT), maximum temperature (MaxT) and rainfall for the month of
March, April and May and pre-monsoon season itself.
2. The average rainfall for the month of June, July, August and September and the
monsoon season itself.
3. The correlation coefficients between the monthly/seasonal rainfall of monsoon
season with the monthly/seasonal DBT, WBT, MinT, MaxT and rainfall of premonsoon
season. The multiple correlations between the monthly/seasonal rainfall
of monsoon season with the monthly/seasonal DBT, WBT, MinT, MaxT and
rainfall of pre-monsoon season.
The average DBT gradually increases from the northeastern to the southwestern part of
the country. The southern part of the country has the maximum WBT whereas the
northern part has the minimum. Starting from the central part of the country the minimum
temperature increases towards south and decreases towards north during this season. The
highest maximum average temperature exits at
Satkhira belt and the lowest at Sylhet. Jessore and some northern part of the country have
the minimum rainfall during pre-monsoon season. During monsoon season the maximum
rainfall has been recorded at Teknaf, Cox's Bazar and Sylhet region and the minimum
rainfall at Jessore, Chandpur and other west and north western belt.
From the analysis it has been observed that the correlation coefficient between the premonsoon
maximum temperature and monsoon rainfall is positive at most of the places of
the central (especially Chandpur and Madaripur), southwestern and a few places of the
northern part of the country. It has been found that the correlation co-efficient between
the pre-monsoon WBT and monsoon rainfall is positive mostly at the southern,
southwestern and the extreme northern part of the country. From this study it has been
also found that the multiple correlation co-efficient between the DBT, WBT, MinT,
MaxT and rainfall of pre-monsoon and the rainfall of monsoon has a positive value all
over the country.
Description:
This thesis is submitted to the Department of Physics, Khulna University of Engineering & Technology in partial fulfillment of the requirements for the degree of Master of Philosophy in Physics, June, 2008.
Cataloged from PDF Version of Thesis.
Includes bibliographical references (pages 128-130)