GIS-Based Rainfall Analysis Using Remotely Sensed Data in Kirkuk Province, Iraq Rainfall Analysis

الشريط الجانبي للمقالة

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منشور: 2022-12-25
محدث: 2022-12-25
النسخ:
2022-12-25 (2)
DOI: https://doi.org/10.25130/tjes.29.4.6
الكلمات المفتاحية:
Drought

محتوى المقالة الرئيسي

Arzu M. W. Mohammed Hadi
Environment and Pollution Engineering Department, Technical Engineering College of Kirkuk, Northern Technical University, Kirkuk, Iraq.
https://orcid.org/0000-0003-2544-9405
Akram Mohammed
a:1:{s:5:"en_US";s:17:"Tikrit University";}
https://orcid.org/0000-0002-5786-8236
Huda J. Jumaah
Environment and Pollution Engineering Department, Technical Engineering College of Kirkuk, Northern Technical University, Kirkuk, Iraq.
https://orcid.org/0000-0002-3438-3033
Mohammed H. Ameen
Environmental Eng. Department, College of Engineering, Tikrit University, Tikrit, Iraq.
https://orcid.org/0000-0002-9701-6361
Bahareh Kalantar
RIKEN Center of Advanced Intelligence Project, The Goal-Oriented Technology Research Group, Disaster Resilience Science Team, Tokyo, Japan
Hossein Mojaddadi Rizeei
The Centre for Advanced Modelling and Geospatial Information Systems (CAMGIS), Faculty of Engineering and Information Technology, University of Technology. Sydney, Sydney, New South Wales, Australia.
Zainab Talib Abidzaid Al-Sharify
Chemical Engineering, Birmingham University, UK.
https://orcid.org/0000-0002-3870-3815

الملخص

     يهدف هذا البحث إلى حساب معدل هطول الأمطار لعامين متتاليين 2018 و 2019 لدراسة وتحليل فترات الجفاف خلال هذه السنوات. تم إجراء البحث في محافظة كركوك شمال العراق ، من خلال تقسيم منطقة الدراسة إلى خمس مناطق بناءً على خمس محطات لسجلات الأمطار. نوعان من البيانات تم استخدامها في الدراسة:  بيانات الاستشعار عن بعد للأمطار اليومية من الأقمار الصناعية ومعدل الامطار الشهرية من تطبيق Power التابع لوكالة ناسا. تضمنت المنهجية حساب معدل سقوط الأمطار بثلاث طرق؛ المتوسط، ومضلعات ثيسين، وتقنية Isohyet. تم تحليل البيانات وإنتاج الخرائط النهائية باستخدام نظم المعلومات الجغرافية. بالنسبة لعام 2018، كان متوسط ​​معدل هطول الأمطار السنوي الناتج عن طريق المتوسط، ومضلعات ثيسين، وتقنية Isohyet؛ 1.376 و 1.341 و 1.343 على التوالي. ولكن، بالنسبة لعام 2019، كان متوسط ​​معدل هطول الأمطار السنوي الناتج عن طريق المتوسط، ومضلعات ثيسين، وتقنية Isohyet؛ 0.966 و 0.932 و 0.882 على التوالي. أظهرت النتائج قلة المياه وقلة هطول الأمطار خلال سنوات الدراسة مما  كان له تأثير كبير على تعرض المنطقة للجفاف المتمثل في جفاف الأنهار.

تفاصيل المقالة

إصدار

مجلد 29 عدد 4 (2022): Vol29, No.4, 2022

القسم

Articles
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هذا العمل مرخص بموجب Creative Commons Attribution 4.0 International License.

THIS IS AN OPEN ACCESS ARTICLE UNDER THE CC BY LICENSE http://creativecommons.org/licenses/by/4.0/

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