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Information Journal Paper

Title

ANALYSIS OF JET STREAMS FREQUENCY OCCURRENCE DURING HEAVY PRECIPITATION OVER KURDISTAN PROVINCE

Pages

  95-113

Abstract

 Introduction: Jet stream is a strong narrow current concentrated by strong vertical and lateral wind shears (Vasantha et al., 2002). According to World Meteorological Organization nomenclature, jet stream formed when the speed of wind greater than 60 knots or 30 m/s. The major characteristics of the troposphere and lower stratosphere in the vicinity of JET STREAMS were pointed out by a group of meteorologists at the University of Chicago (Rossby, 1974; Rossby et al., 1974). These characteristics are the tropopause discontinuities, the intense horizontal temperature gradients considerably below the jet stream core, and the associated frontal systems (Endlich, 1953). JET STREAMS possess a considerable amount of kinetic energy with velocities comparable to horizontal phase velocities of atmospheric waves (Vasantha et al., 2002).

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    APA: Copy

    DARAND, MOHAMMAD. (2015). ANALYSIS OF JET STREAMS FREQUENCY OCCURRENCE DURING HEAVY PRECIPITATION OVER KURDISTAN PROVINCE. GEOGRAPHY AND ENVIRONMENTAL HAZARDS, 4(13), 95-113. SID. https://sid.ir/paper/226716/en

    Vancouver: Copy

    DARAND MOHAMMAD. ANALYSIS OF JET STREAMS FREQUENCY OCCURRENCE DURING HEAVY PRECIPITATION OVER KURDISTAN PROVINCE. GEOGRAPHY AND ENVIRONMENTAL HAZARDS[Internet]. 2015;4(13):95-113. Available from: https://sid.ir/paper/226716/en

    IEEE: Copy

    MOHAMMAD DARAND, “ANALYSIS OF JET STREAMS FREQUENCY OCCURRENCE DURING HEAVY PRECIPITATION OVER KURDISTAN PROVINCE,” GEOGRAPHY AND ENVIRONMENTAL HAZARDS, vol. 4, no. 13, pp. 95–113, 2015, [Online]. Available: https://sid.ir/paper/226716/en

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