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Information Journal Paper

Title

THE ROLE OF REGIONAL ATMOSPHERIC CIRCULATION OVER THE MIDDLE EAST ON THE OCCURRENCE OF SUMMER DUST-STORMS IN SOUTHWEST IRAN

Pages

  17-46

Abstract

 In middle and lower troposphere, the main control factor of weather and climate over the Middle East is a local to regional scale thermal forcing including forcing from high mountains. In this regard, regional scale atmospheric circulation associated with surface forcing has an important role in the occurrence of summer DUST STORMS over the area. SOUTHWEST OF IRAN experiences a large number of DUST STORMS every year. Many of them occur in warm period when a series of semi-permanent synoptic systems in lower troposphere control weather and climate in regional scale. In spite of large number of works which have been done during two to three last decades, the main governing mechanisms on the occurrence of dust events over the Middle East are not much clear...

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  • Cite

    APA: Copy

    MOFIDI, ABBAS, & JAFARI, SAJAD. (2011). THE ROLE OF REGIONAL ATMOSPHERIC CIRCULATION OVER THE MIDDLE EAST ON THE OCCURRENCE OF SUMMER DUST-STORMS IN SOUTHWEST IRAN. ARID REGIONS GEOGRAPHIC STUDIES, 2(5), 17-46. SID. https://sid.ir/paper/190685/en

    Vancouver: Copy

    MOFIDI ABBAS, JAFARI SAJAD. THE ROLE OF REGIONAL ATMOSPHERIC CIRCULATION OVER THE MIDDLE EAST ON THE OCCURRENCE OF SUMMER DUST-STORMS IN SOUTHWEST IRAN. ARID REGIONS GEOGRAPHIC STUDIES[Internet]. 2011;2(5):17-46. Available from: https://sid.ir/paper/190685/en

    IEEE: Copy

    ABBAS MOFIDI, and SAJAD JAFARI, “THE ROLE OF REGIONAL ATMOSPHERIC CIRCULATION OVER THE MIDDLE EAST ON THE OCCURRENCE OF SUMMER DUST-STORMS IN SOUTHWEST IRAN,” ARID REGIONS GEOGRAPHIC STUDIES, vol. 2, no. 5, pp. 17–46, 2011, [Online]. Available: https://sid.ir/paper/190685/en

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