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Information Journal Paper

Title

EL NINO AND DROUGHT - WET PERIODS IN THE CLIMATE OF IRAN

Pages

  6-6

Abstract

 The purpose of this paper is investigates the EL NINO and drough-wet periods in the climate of Iran. The contents treated in this study are somewhat limited on the precipitation of Iran and it"s relation with EL NINO southern oscillation. Therefore, rainfall anamalies, annual and interannual variations of precipitation above Iran and their relation with SOUTHERN OSCILLATION Index (SOI) are investigated. The results of this study are follows: There exits a almost strong dependencies between annual RAINFALL OF IRAN.and SOI. This relationship shows a negative Correlation Coefficient (r=-0.37, N=30) Which goes to 5% significance level. Among 29 Selected Station, Gazvin Station has most Strony Correlation Coefficenl (r=-0.59) and Birjand station has Weakest correlation coefficient (r=0.005). In addition, it is interesting to note that among the months, most Strong correlation coefficient between monthly rainfall and SOI there is in october.

Cites

References

Cite

APA: Copy

AZIZI, GHASEM. (2000). EL NINO AND DROUGHT - WET PERIODS IN THE CLIMATE OF IRAN. GEOGRAPHICAL RESEARCH QUARTERLY, 32(38), 6-6. SID. https://sid.ir/paper/361158/en

Vancouver: Copy

AZIZI GHASEM. EL NINO AND DROUGHT - WET PERIODS IN THE CLIMATE OF IRAN. GEOGRAPHICAL RESEARCH QUARTERLY[Internet]. 2000;32(38):6-6. Available from: https://sid.ir/paper/361158/en

IEEE: Copy

GHASEM AZIZI, “EL NINO AND DROUGHT - WET PERIODS IN THE CLIMATE OF IRAN,” GEOGRAPHICAL RESEARCH QUARTERLY, vol. 32, no. 38, pp. 6–6, 2000, [Online]. Available: https://sid.ir/paper/361158/en

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