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:: Volume 30, Issue 3 (2015) ::
geores 2015, 30(3): 105-120 Back to browse issues page
Analysis and Recognition of Thickness Anomaly Patterns During Extreme Cold Days in Iran
Mohammad Darand *1, Seyed Abolfazl Masoodian2
1- Department Of Climatology ,Kurdistan University,Sanandaj,Iran , m.darand@uok.ac.ir
2- Department Of climatology ,Esfahan University,Esfehan,Iran
Abstract:   (1301 Views)
To do this research daily interpolated temperature data from Asfezari data base have been used.In order to recognition extreme cold days, the Normalized Temperature Deviation Index (NTDI) applied. Then the index sorted according to extensive and severity and first 500 days selected for analysis. The geopotential height data extracted from www.esrl.noaa.gov data base. The thickness anomaly calculated for each day and classified by cluster analysis and Ward method. The thickness mean and temperature anomaly maps has been showed during each pattern. The results showed that 5 thickness anomaly pattern observed during extreme cold day'soccurrence in Iran. The response of Iran absolute temperature anomaly to thickness anomaly are different. The coldest extreme low temperature on Iran occurred when located negative anomaly in thickness over Siberian and northeastern parts of Iran and observed positive anomaly over Barents Sea, Groland and Europe. The mean air temperature anomaly of Iran accompany to this circumstance of thickness anomaly is -5.9° centigrade. 
Keywords: Extreme colds, Thickness, Anomaly, Iran.
Full-Text [PDF 2534 kb]   (430 Downloads)    
Article Type: Original Research | Subject: Climatology
Received: 2014/07/27 | Accepted: 2015/04/14 | Published: 2015/12/19
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Darand M, Masoodian S A. Analysis and Recognition of Thickness Anomaly Patterns During Extreme Cold Days in Iran. geores. 2015; 30 (3) :105-120
URL: http://georesearch.ir/article-1-136-en.html


Volume 30, Issue 3 (2015) Back to browse issues page
فصلنامه تحقیقات جغرافیایی Geographical Researches Quarterly Journal
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