Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan Valley

Flash floods are considered to be one the worst kind of hazard. They are characterized by their suddenness, rarity, small scale, heavy rain and peak discharge, unpredictable, fast and violent movement. It has severe effects on human society in the form life losses, damages to property, roads, commun...

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Main Authors: Ali Mukhlif Sabea, Numman Hussain Atea, Sedeak Mustafa Jasim, Hussain Abid Ismaiel
Format: Article
Language:fas
Published: University of Tehran 2019-12-01
Series:Journal of Information Technology Management
Subjects:
Online Access:https://jitm.ut.ac.ir/article_74761_cfcc3d6ee3ba7dc8fa9d6d3d93befeba.pdf
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author Ali Mukhlif Sabea
Numman Hussain Atea
Sedeak Mustafa Jasim
Hussain Abid Ismaiel
author_facet Ali Mukhlif Sabea
Numman Hussain Atea
Sedeak Mustafa Jasim
Hussain Abid Ismaiel
author_sort Ali Mukhlif Sabea
collection DOAJ
description Flash floods are considered to be one the worst kind of hazard. They are characterized by their suddenness, rarity, small scale, heavy rain and peak discharge, unpredictable, fast and violent movement. It has severe effects on human society in the form life losses, damages to property, roads, communication and on natural settings. Advances in hydrology, meteorology, engineering, using of GIS and remote sensing still not able to increase real time forecast. Researchers from developed countries have stressed to more focus to improve very short time an effective early warning system with collaboration of local communities for flash flood risk supervision. The data were combined with the Geographical Information System to analyze the temporal and spatial distribution of flood events in Salah Al-Din Governorate and Ramadan Valley. The analysis of the spatial distribution of the floods proves that most of the occurrences are recorded in the southern part of the study area. Most of the flooded areas in the study area are mainly pre-classified areas within the areas threatened by the flood due to the low level of its surface and its proximity to the course of the main valley (Wadi Jarnav), which flows into the Tigris River. The proposed method estimates the localization of sites prone to flood, and it may be used for flood hazard assessment mapping and for flood risk management. It was therefore, suggested that government agencies and policy makers should adopt this powerful technique for reliable and well synthesized information which is a vital component of flood risk assessment and planning.
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spelling doaj.art-810fe520a75d49649de4c44b947c09ed2022-12-22T03:24:49ZfasUniversity of TehranJournal of Information Technology Management2008-58932423-50592019-12-01114375510.22059/jitm.2019.7476174761Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan ValleyAli Mukhlif Sabea0Numman Hussain Atea1Sedeak Mustafa Jasim2Hussain Abid Ismaiel3Department of Geography, College of Education for Humanities, Tikrit University, Tikrit, Iraq.Department of Geography, College of Education for Humanities, Tikrit University, Tikrit, Iraq.Department of Geography, College of Education for Humanities, Tikrit University, Tikrit, Iraq.Department of Geography, College of Education for Humanities, Tikrit University, Tikrit, Iraq.Flash floods are considered to be one the worst kind of hazard. They are characterized by their suddenness, rarity, small scale, heavy rain and peak discharge, unpredictable, fast and violent movement. It has severe effects on human society in the form life losses, damages to property, roads, communication and on natural settings. Advances in hydrology, meteorology, engineering, using of GIS and remote sensing still not able to increase real time forecast. Researchers from developed countries have stressed to more focus to improve very short time an effective early warning system with collaboration of local communities for flash flood risk supervision. The data were combined with the Geographical Information System to analyze the temporal and spatial distribution of flood events in Salah Al-Din Governorate and Ramadan Valley. The analysis of the spatial distribution of the floods proves that most of the occurrences are recorded in the southern part of the study area. Most of the flooded areas in the study area are mainly pre-classified areas within the areas threatened by the flood due to the low level of its surface and its proximity to the course of the main valley (Wadi Jarnav), which flows into the Tigris River. The proposed method estimates the localization of sites prone to flood, and it may be used for flood hazard assessment mapping and for flood risk management. It was therefore, suggested that government agencies and policy makers should adopt this powerful technique for reliable and well synthesized information which is a vital component of flood risk assessment and planning.https://jitm.ut.ac.ir/article_74761_cfcc3d6ee3ba7dc8fa9d6d3d93befeba.pdfdry valley floodssalah al-din governorateramadan valley
spellingShingle Ali Mukhlif Sabea
Numman Hussain Atea
Sedeak Mustafa Jasim
Hussain Abid Ismaiel
Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan Valley
Journal of Information Technology Management
dry valley floods
salah al-din governorate
ramadan valley
title Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan Valley
title_full Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan Valley
title_fullStr Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan Valley
title_full_unstemmed Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan Valley
title_short Spatial Analysis of Dry Valley Floods in Salah Al-Din Governorate and Ramadan Valley
title_sort spatial analysis of dry valley floods in salah al din governorate and ramadan valley
topic dry valley floods
salah al-din governorate
ramadan valley
url https://jitm.ut.ac.ir/article_74761_cfcc3d6ee3ba7dc8fa9d6d3d93befeba.pdf
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AT sedeakmustafajasim spatialanalysisofdryvalleyfloodsinsalahaldingovernorateandramadanvalley
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