TREND ANALYSIS OF THE RECENT SEASONAL CHANGES IN SUBTROPICAL JET STREAM IN CLIMATEOF IRAN

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

ASAKEREH HOSSEIN; GHAEMI HUSHANG; BEYRANVAND AZAR

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: Physical Geography Research Year:2015 | Volume:47 | Issue:1 Page(s): 8-9

Download Full-Text

Persian Verion

View:

1,331

Download:

308

Cites:

Information Journal Paper

Title

TREND ANALYSIS OF THE RECENT SEASONAL CHANGES IN SUBTROPICAL JET STREAM IN CLIMATEOF IRAN

Author(s)

ASAKEREH HOSSEIN | GHAEMI HUSHANG | BEYRANVAND AZAR | Issue Writer Certificate

Keywords

JET STREAMQ2

MERIDIONAL COMPONENTQ2

TRENDQ2

ZONAL COMPONENTQ2

Abstract

Introduction: According to the definition of World Meteorology Organization (WMO), as the speed of the air mass is more than 30 meters per second, the jetstream will arise. The core of the jetstream is with baroclinic atmosphere due to the large difference in temperature and wind speed. There are two west jetstreams in the northern hemisphere. The northern JET STREAM is called polar front jetstream and the southern is called subtropical jetstream. Polar Front JET STREAM produce intense temperature gradient by polar air mass and tropical Polar Front JET STREAM is produced by strong temperature gradient of polar and subtropical air. The subtropical jetstream is produced by temperature gradient in tropopause as limited to the upper troposphere.

Cites

No record.

References

Cite

APA: Copy

ASAKEREH, HOSSEIN, GHAEMI, HUSHANG, & BEYRANVAND, AZAR. (2015). TREND ANALYSIS OF THE RECENT SEASONAL CHANGES IN SUBTROPICAL JET STREAM IN CLIMATEOF IRAN. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, 47(1), 8-9. SID. https://sid.ir/paper/395242/en

Vancouver: Copy

ASAKEREH HOSSEIN, GHAEMI HUSHANG, BEYRANVAND AZAR. TREND ANALYSIS OF THE RECENT SEASONAL CHANGES IN SUBTROPICAL JET STREAM IN CLIMATEOF IRAN. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2015;47(1):8-9. Available from: https://sid.ir/paper/395242/en

IEEE: Copy

HOSSEIN ASAKEREH, HUSHANG GHAEMI, and AZAR BEYRANVAND, “TREND ANALYSIS OF THE RECENT SEASONAL CHANGES IN SUBTROPICAL JET STREAM IN CLIMATEOF IRAN,” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. 47, no. 1, pp. 8–9, 2015, [Online]. Available: https://sid.ir/paper/395242/en

Related Journal Papers