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Information Journal Paper

Title

THERMODYNAMIC-STATISTICAL ANALYSIS OF THUNDERSTORMS IN IRAN

Pages

  53-56

Abstract

 Ascent rainfall mechanism is “one of the most important factors in leading to various rainfall behaviors in different regions, such as various atmospheric PRECIPITATION seen in different time scales” (Masoompour, Miri, Zolfaghari, & Yarahmadi, 2013, p.299). In fact, some of them can be called atmospheric phenomena due to their special nature. One of these atmospheric phenomena is thunderstorm. Not only this storm and its accompanying phenomena like lightening, tornado, hail, strong winds, and heavy PRECIPITATION (see Changnon, 1925, 2001), but also atmospheric hazard phenomena in aviation, such asturbulence, frost, and wind shear (Tajbakhsh et al., 2009) cause remarkable damage to human and natural environments. Therefore, recognizing the features of these phenomena has been attracting the attention of researchers.

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    • Cite

    APA: Copy

    MASOOMPOUR SAMAKOSH, JAFAR, & FAJAD, AHMAD. (2016). THERMODYNAMIC-STATISTICAL ANALYSIS OF THUNDERSTORMS IN IRAN. JOURNAL OF GEOGRAPHY AND REGIONAL DEVELOPMENT, 13(2 (25)), 53-56. SID. https://sid.ir/paper/706159/en

    Vancouver: Copy

    MASOOMPOUR SAMAKOSH JAFAR, FAJAD AHMAD. THERMODYNAMIC-STATISTICAL ANALYSIS OF THUNDERSTORMS IN IRAN. JOURNAL OF GEOGRAPHY AND REGIONAL DEVELOPMENT[Internet]. 2016;13(2 (25)):53-56. Available from: https://sid.ir/paper/706159/en

    IEEE: Copy

    JAFAR MASOOMPOUR SAMAKOSH, and AHMAD FAJAD, “THERMODYNAMIC-STATISTICAL ANALYSIS OF THUNDERSTORMS IN IRAN,” JOURNAL OF GEOGRAPHY AND REGIONAL DEVELOPMENT, vol. 13, no. 2 (25), pp. 53–56, 2016, [Online]. Available: https://sid.ir/paper/706159/en

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