Variability and Trend of Annual Maximum Daily Rainfall in Northern Algeria

The daily rainfall dataset of 35 weather stations covering the north of Algeria was studied for a period up to 43 years, recorded after 1970s. The variability and trends in annual maximum daily rainfall (AMDR) time series and their contributions in annual rainfall (AR) were investigated. The analysi...

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Main Authors: Abderrahmane Nekkache Ghenim, Abdesselam Megnounif
Format: Article
Language:English
Published: Hindawi Limited 2016-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2016/6820397
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spelling doaj-87594d4bf532444d810b2f2a5e51dc4d2020-11-25T00:08:12ZengHindawi LimitedInternational Journal of Geophysics1687-885X1687-88682016-01-01201610.1155/2016/68203976820397Variability and Trend of Annual Maximum Daily Rainfall in Northern AlgeriaAbderrahmane Nekkache Ghenim0Abdesselam Megnounif1“Eau et Ouvrage dans Leur Environnement” Laboratory, Tlemcen University, BP 230, 13000 Tlemcen, Algeria“Eau et Ouvrage dans Leur Environnement” Laboratory, Tlemcen University, BP 230, 13000 Tlemcen, AlgeriaThe daily rainfall dataset of 35 weather stations covering the north of Algeria was studied for a period up to 43 years, recorded after 1970s. The variability and trends in annual maximum daily rainfall (AMDR) time series and their contributions in annual rainfall (AR) were investigated. The analysis of the series was based on statistical characteristics, Burn’s seasonality procedure, Mann-Kendall test, and linear regression technique. The contribution of the AMDR to AR analysis was subjected to both the Buishand test and the double mass curve technique. The AMDR characteristics reveal a strong temporal irregularity and have a wide frequency of occurrence in the months of November and December while the maximum intensity occurred in October. The observed phenomenon was so irregular that there was no dominant season and the occurrence of extreme event can arrive at any time of the year. The AMDR trends showed that only six of 35 stations have significant trend. For other stations, no clear trend was highlighted. This result was confirmed by the linear regression procedure. On the contrary, the contribution of AMDR in annual totals exhibited a significant increasing trend for 57% of the sites studied with a growth rate of up to 50%.http://dx.doi.org/10.1155/2016/6820397
collection DOAJ
language English
format Article
sources DOAJ
author Abderrahmane Nekkache Ghenim
Abdesselam Megnounif
spellingShingle Abderrahmane Nekkache Ghenim
Abdesselam Megnounif
Variability and Trend of Annual Maximum Daily Rainfall in Northern Algeria
International Journal of Geophysics
author_facet Abderrahmane Nekkache Ghenim
Abdesselam Megnounif
author_sort Abderrahmane Nekkache Ghenim
title Variability and Trend of Annual Maximum Daily Rainfall in Northern Algeria
title_short Variability and Trend of Annual Maximum Daily Rainfall in Northern Algeria
title_full Variability and Trend of Annual Maximum Daily Rainfall in Northern Algeria
title_fullStr Variability and Trend of Annual Maximum Daily Rainfall in Northern Algeria
title_full_unstemmed Variability and Trend of Annual Maximum Daily Rainfall in Northern Algeria
title_sort variability and trend of annual maximum daily rainfall in northern algeria
publisher Hindawi Limited
series International Journal of Geophysics
issn 1687-885X
1687-8868
publishDate 2016-01-01
description The daily rainfall dataset of 35 weather stations covering the north of Algeria was studied for a period up to 43 years, recorded after 1970s. The variability and trends in annual maximum daily rainfall (AMDR) time series and their contributions in annual rainfall (AR) were investigated. The analysis of the series was based on statistical characteristics, Burn’s seasonality procedure, Mann-Kendall test, and linear regression technique. The contribution of the AMDR to AR analysis was subjected to both the Buishand test and the double mass curve technique. The AMDR characteristics reveal a strong temporal irregularity and have a wide frequency of occurrence in the months of November and December while the maximum intensity occurred in October. The observed phenomenon was so irregular that there was no dominant season and the occurrence of extreme event can arrive at any time of the year. The AMDR trends showed that only six of 35 stations have significant trend. For other stations, no clear trend was highlighted. This result was confirmed by the linear regression procedure. On the contrary, the contribution of AMDR in annual totals exhibited a significant increasing trend for 57% of the sites studied with a growth rate of up to 50%.
url http://dx.doi.org/10.1155/2016/6820397
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