Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia

Extreme rainfall is expected to increase as the climate warms, with the rate of increase at 7% per degree of warming following the Clausius-Clapeyron (CC) relationship. However, studies showed that the rate of increase might not necessarily follow the relationship. This study investigates temporal a...

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Published in:International Journal on Advanced Science, Engineering and Information Technology
Main Author: Baharudin S.A.; Asmat A.
Format: Article
Language:English
Published: Insight Society 2022
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-85125953427&doi=10.18517%2fijaseit.12.1.14096&partnerID=40&md5=b71269ccacd64ddcf0e0f42c7223b34b
id 2-s2.0-85125953427
spelling 2-s2.0-85125953427
Baharudin S.A.; Asmat A.
Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
2022
International Journal on Advanced Science, Engineering and Information Technology
12
1
10.18517/ijaseit.12.1.14096
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85125953427&doi=10.18517%2fijaseit.12.1.14096&partnerID=40&md5=b71269ccacd64ddcf0e0f42c7223b34b
Extreme rainfall is expected to increase as the climate warms, with the rate of increase at 7% per degree of warming following the Clausius-Clapeyron (CC) relationship. However, studies showed that the rate of increase might not necessarily follow the relationship. This study investigates temporal and spatial variations of daily rainfall relationship with surface air temperature in Peninsular Malaysia using data from the Global Historical Climatology Network (GHCN) using a fixed temperature interval binning method and quantile regression method. Investigation reveals that a negative scaling of daily extreme rainfall was observed for all surface air temperature and percentiles investigated, in contrast with the expectations from the CC relationship. The largest seasonal variation at 99th percentile was observed in December-January (DJF), while the lowest scaling rate was in March-May (MAM). The scaling rate tends to be higher in Subang and Melaka, and lower in Bayan Lepas, Kota Bharu and Kuantan. The scaling rate also tends to be stronger at 99th percentile compared to the lower rainfall events at 95th and 75th percentile and in warmer seasons compared to colder seasons. Further, the results show that the intensity of daily extreme rainfall in Peninsular Malaysia is decreasing with increasing surface air temperature. © IJASEIT is licensed under a Creative Commons Attribution-Share Alike 4.0 International License.
Insight Society
20885334
English
Article
All Open Access; Hybrid Gold Open Access
author Baharudin S.A.; Asmat A.
spellingShingle Baharudin S.A.; Asmat A.
Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
author_facet Baharudin S.A.; Asmat A.
author_sort Baharudin S.A.; Asmat A.
title Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
title_short Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
title_full Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
title_fullStr Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
title_full_unstemmed Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
title_sort Temporal and Spatial Evaluations of Extreme Rainfall Relationship with Daily Surface Air Temperature in Peninsular Malaysia
publishDate 2022
container_title International Journal on Advanced Science, Engineering and Information Technology
container_volume 12
container_issue 1
doi_str_mv 10.18517/ijaseit.12.1.14096
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-85125953427&doi=10.18517%2fijaseit.12.1.14096&partnerID=40&md5=b71269ccacd64ddcf0e0f42c7223b34b
description Extreme rainfall is expected to increase as the climate warms, with the rate of increase at 7% per degree of warming following the Clausius-Clapeyron (CC) relationship. However, studies showed that the rate of increase might not necessarily follow the relationship. This study investigates temporal and spatial variations of daily rainfall relationship with surface air temperature in Peninsular Malaysia using data from the Global Historical Climatology Network (GHCN) using a fixed temperature interval binning method and quantile regression method. Investigation reveals that a negative scaling of daily extreme rainfall was observed for all surface air temperature and percentiles investigated, in contrast with the expectations from the CC relationship. The largest seasonal variation at 99th percentile was observed in December-January (DJF), while the lowest scaling rate was in March-May (MAM). The scaling rate tends to be higher in Subang and Melaka, and lower in Bayan Lepas, Kota Bharu and Kuantan. The scaling rate also tends to be stronger at 99th percentile compared to the lower rainfall events at 95th and 75th percentile and in warmer seasons compared to colder seasons. Further, the results show that the intensity of daily extreme rainfall in Peninsular Malaysia is decreasing with increasing surface air temperature. © IJASEIT is licensed under a Creative Commons Attribution-Share Alike 4.0 International License.
publisher Insight Society
issn 20885334
language English
format Article
accesstype All Open Access; Hybrid Gold Open Access
record_format scopus
collection Scopus
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