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Information Journal Paper

Title

THE MAPPING OF THE LATE FROST IN KHORASAN RAZAVI PROVINCE USING THE OUTPUT CLIMATE MODEL

Pages

  83-93

Abstract

 the main aim of this research applied using the output climate model for study of the event LATE FROST. For this purpose, we've used data output from GCM ECHO-G (A1).and we has investigated the effects of CLIMATE CHANGE on light and heavy LATE FROST in future climate period. The data was downscaled by using the LARS-WG model for future climate period 2039-2010.Analysis was performed on six synoptic stations the three stations located in inside to the khorasan Razavi province (Mashhad, Sabzevar and Torbat-e-Heydarieh). The final map of the LATE FROST show that the LATE FROST data occurrence following the arrangement of topography. Significant results show that the average occurrence of light and heavy LATE FROST will be completed 13 days and 7 days earlier than average of past time. The frequency of occurrence and severity of LATE FROST significant decrease compared to past periods of climate. In other words, the rate of light LATE FROST probability will be reduced.

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    Cite

    APA: Copy

    ESMAILI, R., & KOHI, M.. (2012). THE MAPPING OF THE LATE FROST IN KHORASAN RAZAVI PROVINCE USING THE OUTPUT CLIMATE MODEL. JOURNAL OF PHYSICAL GEOGRAPHY, 5(17), 83-93. SID. https://sid.ir/paper/184988/en

    Vancouver: Copy

    ESMAILI R., KOHI M.. THE MAPPING OF THE LATE FROST IN KHORASAN RAZAVI PROVINCE USING THE OUTPUT CLIMATE MODEL. JOURNAL OF PHYSICAL GEOGRAPHY[Internet]. 2012;5(17):83-93. Available from: https://sid.ir/paper/184988/en

    IEEE: Copy

    R. ESMAILI, and M. KOHI, “THE MAPPING OF THE LATE FROST IN KHORASAN RAZAVI PROVINCE USING THE OUTPUT CLIMATE MODEL,” JOURNAL OF PHYSICAL GEOGRAPHY, vol. 5, no. 17, pp. 83–93, 2012, [Online]. Available: https://sid.ir/paper/184988/en

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