Convectional Influences on The Weather Pattern of Northern Sri Lanka

There are three precipitation processes, such as monsoon circulation, frontal process, and the convectional process that influence the rainfall of the Northern region of Sri Lanka. Several natural and anthropogenic factors influence the weather pattern of the study area. Even though, recently, conve...

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Main Authors: Nagamuthu, Piratheeparajah, Chan, Ngai Weng
Format: Article
Language:English
Published: European Publisher 2019
Subjects:
Online Access:http://eprints.usm.my/47977/
http://eprints.usm.my/47977/1/Convectional%20Influences%20on%20The%20Weather%20Pattern%20of%20Northern%20Sri%20Lanka.pdf
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author Nagamuthu, Piratheeparajah
Chan, Ngai Weng
author_facet Nagamuthu, Piratheeparajah
Chan, Ngai Weng
author_sort Nagamuthu, Piratheeparajah
building USM Institutional Repository
collection Online Access
description There are three precipitation processes, such as monsoon circulation, frontal process, and the convectional process that influence the rainfall of the Northern region of Sri Lanka. Several natural and anthropogenic factors influence the weather pattern of the study area. Even though, recently, convectional influences on the weather pattern are vital. This paper examines the importance of the convectional process in the weather pattern of the Northern Region of Sri Lanka. The main objective of this paper is, to identify the influence of the convectional process in the weather pattern of Northern Sri Lanka. This study uses meteorological data such as rainfall, temperature, relative humidity, and atmospheric pressure. The data were analysed employing the descriptive statistical method using average, standard deviation, and trend analysis via Microsoft Excel worksheet, and results were mapped using Arc Map 11.2 version. Results show that there are significant influences of the convection process in the weather pattern of the study area. Convection contributes more than 38% of the total rainfall, and this is the leading cause of rainfall during the first inter-monsoon season (FIMS) and the southwest monsoon season (SWMS). The Convectional process is also the primary cause for the variations in the temperature range between day and night during March, April, May, June, July, and August. Convection creates an unstable evaporation rate, which leads to the high rates of relative humidity in the nights during the FIMS. Convectional processes contributing to the unstable atmospheric pressure and resulted in unexpected weather disturbance in the study area.
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spelling usm-479772020-12-11T02:40:36Z http://eprints.usm.my/47977/ Convectional Influences on The Weather Pattern of Northern Sri Lanka Nagamuthu, Piratheeparajah Chan, Ngai Weng QC924-926.2 Rain and Rainfall QC980-999 Climatology and Weather There are three precipitation processes, such as monsoon circulation, frontal process, and the convectional process that influence the rainfall of the Northern region of Sri Lanka. Several natural and anthropogenic factors influence the weather pattern of the study area. Even though, recently, convectional influences on the weather pattern are vital. This paper examines the importance of the convectional process in the weather pattern of the Northern Region of Sri Lanka. The main objective of this paper is, to identify the influence of the convectional process in the weather pattern of Northern Sri Lanka. This study uses meteorological data such as rainfall, temperature, relative humidity, and atmospheric pressure. The data were analysed employing the descriptive statistical method using average, standard deviation, and trend analysis via Microsoft Excel worksheet, and results were mapped using Arc Map 11.2 version. Results show that there are significant influences of the convection process in the weather pattern of the study area. Convection contributes more than 38% of the total rainfall, and this is the leading cause of rainfall during the first inter-monsoon season (FIMS) and the southwest monsoon season (SWMS). The Convectional process is also the primary cause for the variations in the temperature range between day and night during March, April, May, June, July, and August. Convection creates an unstable evaporation rate, which leads to the high rates of relative humidity in the nights during the FIMS. Convectional processes contributing to the unstable atmospheric pressure and resulted in unexpected weather disturbance in the study area. European Publisher 2019-10-30 Article PeerReviewed application/pdf en http://eprints.usm.my/47977/1/Convectional%20Influences%20on%20The%20Weather%20Pattern%20of%20Northern%20Sri%20Lanka.pdf Nagamuthu, Piratheeparajah and Chan, Ngai Weng (2019) Convectional Influences on The Weather Pattern of Northern Sri Lanka. European Proceedings of Social and Behavioural Sciences, 89. pp. 477-487. ISSN 2357-1330 https://www.europeanproceedings.com/proceedings/EpSBS/volumes/ich2019
spellingShingle QC924-926.2 Rain and Rainfall
QC980-999 Climatology and Weather
Nagamuthu, Piratheeparajah
Chan, Ngai Weng
Convectional Influences on The Weather Pattern of Northern Sri Lanka
title Convectional Influences on The Weather Pattern of Northern Sri Lanka
title_full Convectional Influences on The Weather Pattern of Northern Sri Lanka
title_fullStr Convectional Influences on The Weather Pattern of Northern Sri Lanka
title_full_unstemmed Convectional Influences on The Weather Pattern of Northern Sri Lanka
title_short Convectional Influences on The Weather Pattern of Northern Sri Lanka
title_sort convectional influences on the weather pattern of northern sri lanka
topic QC924-926.2 Rain and Rainfall
QC980-999 Climatology and Weather
url http://eprints.usm.my/47977/
http://eprints.usm.my/47977/
http://eprints.usm.my/47977/1/Convectional%20Influences%20on%20The%20Weather%20Pattern%20of%20Northern%20Sri%20Lanka.pdf