Volume 25, Issue 78 (9-2025)
jgs 2025, 25(78): 0-0 |
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Mohammadi R, saligheh M, Naserzadeh M H, Akbari M. (2025). An analysis of cyclonic dominant patterns on cold period precipitation in the mid-western of Iran. jgs. 25(78), doi:10.61186/jgs.25.78.2
URL: http://jgs.khu.ac.ir/article-1-3935-en.html
URL: http://jgs.khu.ac.ir/article-1-3935-en.html
1- Ph.D. student in climatology, Kharazmi University, std_rastegar365@khu.ac.ir , std_rastegar365@khu.ac.ir
2- Associated Professor of climatology, kharazmi University, Tehran, Iran ., salighe1338@gmail.com
3- Assistant Professor of climatology, kharazmi University, Tehran, Iran ., Nasserzadeh2100@yahoo.com
4- Associated Professor of climatology, kharazmi University, Tehran, Iran ., mehryakbary@khu.ac.ir
2- Associated Professor of climatology, kharazmi University, Tehran, Iran ., salighe1338@gmail.com
3- Assistant Professor of climatology, kharazmi University, Tehran, Iran ., Nasserzadeh2100@yahoo.com
4- Associated Professor of climatology, kharazmi University, Tehran, Iran ., mehryakbary@khu.ac.ir
Abstract: (4599 Views)
Extratropical cyclones according to the frequency, duration, and intensity, the major cause of mid-and high-latitude precipitation across the Mediterranean during winter and autumn. For this research using network data of ECMWF climatic variables with 6-hour time resolution and 0.25 × 0.25 spatial resolution from1979-2016 and were used of 4 Basin stations precipitation data from the Asfezari database from 1979-2016. The results showed that the first pattern is the Mediterranean trough pattern which has the highest frequency of 42%. In this pattern, the low-level due to the presence of a high-level that acts as a barrier have caused the deepening of the Mediterranean low-level and its axis extends to the Red Sea, and due to the collision of low-level and high-level on the region, instability is intensified and has caused the most rainfall among the patterns. In contrast to the first pattern, The fourth pattern has the lowest frequency of 10% Which is the trough pattern of western winds which is located on the Caspian Sea but due to high-level in the south of the region has prevented the entry of low-level and is located in the northern part of the study area due to this, the isobar in the north of the region have become orbital as a result, fewer cyclones enter the area, resulting in less rainfall between patterns. The results also showed that the frequency of cold-core cyclones was 60% in winter and 40% in autumn, but the frequency of hot core cyclones was 62% in winter and 38% in autumn, which in winter, the frequency of hot core cyclones has increased compared to cold-core cyclones, while in the fall the frequency of hot-core cyclones has decreased compared to cold-core. In the last decade, both the frequency of occurrence of cyclones and their intensity has decreased compared to the last two decades. In terms of cyclogenesis places, the western part of the study area has always been active, And with the onset of the cold season from autumn to winter, cyclogeneses places are gradually becoming more active.
Type of Study: Research |
Subject:
climatology
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