THE IMPACTS OF THE ATMOSPHERIC FORCING ON THERMOCLINE LAYER STRUCTURE IN THE CASPIAN SEA

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.

SHIEA MARYAM; ALIAKBARI BIDOKHTI ABBAS ALI

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

Journal Paper

Paper Information

Journal: HYDROPHYSICS Year:2016 | Volume:2 | Issue:1 Page(s): 25-33

Download Full-Text

Persian Verion

View:

681

Download:

Cites:

Information Journal Paper

Title

THE IMPACTS OF THE ATMOSPHERIC FORCING ON THERMOCLINE LAYER STRUCTURE IN THE CASPIAN SEA

Author(s)

SHIEA MARYAM | ALIAKBARI BIDOKHTI ABBAS ALI | Issue Writer Certificate

Keywords

CASPIAN SEAQ2

THERMOCLINEQ1

COHERENS MODELQ1

TEMPERATUREQ2

SEASONAL VARIATIONQ2

Abstract

In this study, the structure of THERMOCLINE layer in the Middle CASPIAN SEA (MCS) and Southern CASPIAN SEA (SCS) for 2004 was investigated using the three-dimensional ocean model COHERENS. The simulation results for three transects (along South-North, in Southern CASPIAN SEA "along 38.91N", in Middle CASPIAN SEA "along 42.45N" show that, in winter, season THERMOCLINE is almost eliminated and the TEMPERATURE is uniform up to a depth of 100 m. After the erosion of surface THERMOCLINE in winter, this layer is recreated in spring. The results show the formation of a strong THERMOCLINE in summer and in the beginning of autumn, the thickness of the THERMOCLINE is reduced. In general, seasonal variability of water TEMPERATURE is conﬁned to the upper 120m layers. Also transects of Southern and Middle CASPIAN SEA show some special regions in which THERMOCLINE layer structure is stronger. Thus THERMOCLINE layer is created at a depth less than 25m from the sea surface water in eastern coast of SCS and at a depth less than 20m from the sea surface water in western coast of MCS during the summer.

Cites

No record.

References

No record.

Cite

APA: Copy

SHIEA, MARYAM, & ALIAKBARI BIDOKHTI, ABBAS ALI. (2016). THE IMPACTS OF THE ATMOSPHERIC FORCING ON THERMOCLINE LAYER STRUCTURE IN THE CASPIAN SEA. HYDROPHYSICS, 2(1 ), 25-33. SID. https://sid.ir/paper/264854/en

Vancouver: Copy

SHIEA MARYAM, ALIAKBARI BIDOKHTI ABBAS ALI. THE IMPACTS OF THE ATMOSPHERIC FORCING ON THERMOCLINE LAYER STRUCTURE IN THE CASPIAN SEA. HYDROPHYSICS[Internet]. 2016;2(1 ):25-33. Available from: https://sid.ir/paper/264854/en

IEEE: Copy

MARYAM SHIEA, and ABBAS ALI ALIAKBARI BIDOKHTI, “THE IMPACTS OF THE ATMOSPHERIC FORCING ON THERMOCLINE LAYER STRUCTURE IN THE CASPIAN SEA,” HYDROPHYSICS, vol. 2, no. 1 , pp. 25–33, 2016, [Online]. Available: https://sid.ir/paper/264854/en

Related Journal Papers