The role of climatic models in morphoclimatic risks and their environmental impacts in Babil Governorate

Authors

  • Maher Hamood Kadhem, Phd. Ministry of Education / Baghdad Directorate of Education - Second Karkh

DOI:

https://doi.org/10.31973/aj.v2i143.3915

Keywords:

morphoclimatic risks, climate models, human activity

Abstract

The research dealt with the role of climate models and their impact on morpho-climatic risks and their reflection on the environment that were studied according to statistical methods to build (extreme) thermal and rain climatic models, which amounted to (12) recurrences in the study stations. In addition to the natural characteristics of (geology, elevations and slopes, soil, natural vegetation), while the highest amount of water for rain intensity was recorded in (Al-Kifl, Al-Qasim) station, which has an effective role in varying the severity of morpho-climatic risks in the region. The volume of water erosion was estimated according to (Furniah, Gavrilovic) model, and the region was within the category (moderate - high), and its correlation with climatic models reached the strongest with the wet cold model, by (0.72), As for wind erosion, according to (chepil), which is considered very high, and its relationship is stronger with the hot and dry model by (0.80). And building a model for morphoclimatic risks (water erosion risks, sand dune encroachment risks) to determine the degrees of risk for water erosion risks, as high-risk lands occupied (42%), medium-risk (39.7%) and low-risk (18.3%), while the degree of risk of dune encroachment risks sandy sand is high risk (29%), medium risk (53.6%), low risk (17.4%), Then it was evaluated and matched with the map of human uses, as it was found that human activities (agricultural lands, transportation routes, religious and archaeological sites, tourism) have more impact on the risks of water erosion and encroachment of sand dunes that fall within high-risk lands, and the correlation between them is (very strong).

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References

Anwa Barwar، Naseira Slewam . (1991). The Geology Of Sammara Quadrangle. State Establishment Of Geological Survey And Mining Department Of Geological Suvey.

الدراسة الميدانية . (22 , 7, 2019). بابل.

انور مصطفى برواري، و آخرون. (1992). تقرير عن جيولوجية لوحة الكوت (أن أي 38_15), (جي أم _27). الهيئة العامة للمسح الجيولوجي والتعدين.

خطاب عطا نعيم الطائي. (،2007). مظاهر أشكال سطح الأرض لنهر دجلة بين شيخ سعد وعلي الغربي، رسالة ماجستير (غير منشورة). ص 39. كلية التربية للبنات ،جامعة بغداد.

سحر شفيق. (بلا تاريخ). اوصاف شدة انواع الهطول. الهيئة العامة للأنواء الجوية والرصد الزلزالي( بيانات غير منشورة).

سرحان نعيم الخفاجي. (2008). هيدروجيومورفولوجية نهر الفرات بين المناطق الخضر والقرنة، اطروحة دكتوراه (غير منشورة). ص23. كلية الآداب ، جامعة بغداد.

سفير جاسم حسين . (2007). جيومورفولوجية مجرى نهر الغراف، أطروحة دكتوراه (غير منشورة). ص 39. قسم الجغرافية ، كلية الآداب ، جامعة بغداد

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Published

2022-12-15

How to Cite

Kadhem, M. H. (2022). The role of climatic models in morphoclimatic risks and their environmental impacts in Babil Governorate. Al-Adab Journal, 2(143), 383-432. https://doi.org/10.31973/aj.v2i143.3915

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