ASSESSMENT OF THE LOW LEVEL JETS EFFECTS ON MCSS FORMATION IN THE SOUTHWEST 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.

RAFATI SOMAYEH; FATHNIA AMANOLLAH; KARIMI MOSTAFA

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

Journal Paper

Paper Information

Journal: Physical Geography Research Year:2016 | Volume:48 | Issue:1 Page(s): 69-82

Download Full-Text

Persian Verion

View:

902

Download:

250

Cites:

Information Journal Paper

Title

ASSESSMENT OF THE LOW LEVEL JETS EFFECTS ON MCSS FORMATION IN THE SOUTHWEST IRAN

Author(s)

RAFATI SOMAYEH | FATHNIA AMANOLLAH | KARIMI MOSTAFA | Issue Writer Certificate

Keywords

LOW LEVEL JETQ2

MESOSCALE CONVECTIVE SYSTEMSQ1

MOISTURE FLUXQ1

SOUTHWEST IRANQ2

WIND SPEEDQ1

Abstract

IntroductionThe most notable convective systems are MESOSCALE CONVECTIVE SYSTEMS (MCSs). These systems are developed when clouds occurring in response to convective instability organize upscale into a single cloud system with a very large cirriform cloud structure and rainfall covering large contiguous areas (Houz, 2004). Detection and monitoring of MCSs is very important in SOUTHWEST IRAN because they produce hazardous weather, such as lightning, heavy rainfall, hail and strong winds. Several factors influence the development of MCSs such as the flow generated by a weak midlevel trough and the occurrence of LOW LEVEL JETs (LLJs). LLJs transport moisture at the jet level, increase the low-level convergence and are responsible for sustaining convection especially at night.

Cites

No record.

References

Cite

APA: Copy

RAFATI, SOMAYEH, FATHNIA, AMANOLLAH, & KARIMI, MOSTAFA. (2016). ASSESSMENT OF THE LOW LEVEL JETS EFFECTS ON MCSS FORMATION IN THE SOUTHWEST IRAN. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, 48(1), 69-82. SID. https://sid.ir/paper/138765/en

Vancouver: Copy

RAFATI SOMAYEH, FATHNIA AMANOLLAH, KARIMI MOSTAFA. ASSESSMENT OF THE LOW LEVEL JETS EFFECTS ON MCSS FORMATION IN THE SOUTHWEST IRAN. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2016;48(1):69-82. Available from: https://sid.ir/paper/138765/en

IEEE: Copy

SOMAYEH RAFATI, AMANOLLAH FATHNIA, and MOSTAFA KARIMI, “ASSESSMENT OF THE LOW LEVEL JETS EFFECTS ON MCSS FORMATION IN THE SOUTHWEST IRAN,” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. 48, no. 1, pp. 69–82, 2016, [Online]. Available: https://sid.ir/paper/138765/en

Related Journal Papers