| Type of Material: | Thesis |
| Title: | Effect of Arabian Sea Cyclones during the Onset Phase of Indian Summer Monsoon |
| Researcher: | Baburaj, P P |
| Guide: | Abhilash, S |
| Department: | Department of Marine Science |
| Publisher: | Cochin University of Science & Technology, Cochin |
| Place: | Cochin |
| Year: | 2022 |
| Language: | English |
| Subject: | Geosciences | Geosciences Multidisciplinary | Indian Summer Monsoon | Physical Sciences | Tropical Cyclone | Oceanography | Physical and Basic Sciences |
| Dissertation/Thesis Note: | PhD; Department of Marine Science, Cochin University of Science & Technology, Cochin, Cochin; 2022 |
| Fulltext: | Shodhganga |
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| 001 | 456501 | |
| 003 | IN-AhILN | |
| 005 | 2024-10-10 14:42:13 | |
| 008 | __ | 241010t2022||||ii#||||g|m||||||||||eng|| |
| 035 | __ | |a(IN-AhILN)th_456501 |
| 040 | __ | |aCUST_682022|dIN-AhILN |
| 041 | __ | |aeng |
| 100 | __ | |aBaburaj, P P|eResearcher |
| 110 | __ | |aDepartment of Marine Science|bCochin University of Science & Technology, Cochin|dCochin|ein|0U-0253 |
| 245 | __ | |aEffect of Arabian Sea Cyclones during the Onset Phase of Indian Summer Monsoon |
| 260 | __ | |aCochin|bCochin University of Science & Technology, Cochin|c2022 |
| 300 | __ | |a170|dDVD |
| 502 | __ | |cDepartment of Marine Science, Cochin University of Science & Technology, Cochin, Cochin|d2022|bPhD |
| 518 | __ | |d2023|oDate of Award |
| 518 | __ | |oDate of Registration|d2016 |
| 520 | __ | |aThe Indian Summer Monsoon (ISM) is one of the popular and strongest monsoon systems in the world due to its inherent variability in the quantum of rainfall, spatial extent and duration of four months (June to September). The Monsoon Onset over Kerala (MOK) is considered the most awaited weather singularity in the Indian Subcontinent and marks the beginning of the rainy season over India.The onset process starts in May and is characterised by many dynamical and thermodynamical changes over South Asia and the Indian Ocean region. The pre-monsoon thermal field over the Indian landmass has an important bearing on the land-sea heating contrast in the region, consequently influencing the establishment of monsoon over India. The Outgoing Long-wave Radiation (OLR) pattern, depth of westerlies over the Lakshadweep area and rainfall over the Southwest coast are taken into account for the declaration of MOK. The normal date of MOK is around 1st June with a standard deviation of 5 6 days. The strengthening of Low-Level |
| 650 | __ | |aOceanography|2UGC |
| 650 | __ | |aPhysical and Basic Sciences|2AIU |
| 653 | __ | |aGeosciences |
| 653 | __ | |aGeosciences Multidisciplinary |
| 653 | __ | |aIndian Summer Monsoon |
| 653 | __ | |aPhysical Sciences |
| 653 | __ | |aTropical Cyclone |
| 700 | __ | |eGuide|aAbhilash, S |
| 856 | __ | |uhttp://shodhganga.inflibnet.ac.in/handle/10603/474581|yShodhganga |
| 905 | __ | |afromsg |
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