The Bay of Bengal (BoB) is the import basin where tropical cyclone has been forming frequently compared to global perspective. The number and frequency of cyclone over the BoB varies year to year. The recent climatology of tropical cyclone and its track and landfall is very important to minimize casualties and damages. A statistical attempt has been made to know the seasonal number of cyclones over the BoB during 1891-2020 using BMD and IMD cyclone eAtlas data and the most devastating cyclones’ tracks of 1991, 1994, 2007, 2008, 2009 and 2020 are also drawn over the BoB. From the analysis it is found that the total number of cyclones formed over the BoB are 35, 123, 97 and 28 during pre-monsoon, monsoon, post-monsoon and winter seasons respectively whereas 58, 33, 103 and 26 for severe cyclonic storms respectively. The cyclone of all intensity over the BoB follows initially Westward/Northwestwards tracks, some of them re-curved and follows north/northeastwards tracks. Sometimes looping track is also found over the Bay of Bengal. It is also found that some cyclones have completed their journey in the BoB without landfall. This variation of cyclone makes the BoB basin more vulnerable and more challenging for forecasting of tropical cyclones.
Published in | International Journal of Atmospheric and Oceanic Sciences (Volume 5, Issue 2) |
DOI | 10.11648/j.ijaos.20210502.11 |
Page(s) | 20-28 |
Creative Commons |
This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
Copyright |
Copyright © The Author(s), 2021. Published by Science Publishing Group |
Cyclonic Disturbances, BOB, E-atlas, Track, Cyclone (CS & SCS) etc
[1] | Kh. Hafizur Rahman, Neeru Jaiswal1, C. M. Kishtawal, Md. Bazlur Rashid and S. M. Quamrul Hassan, Prediction of the Tropical Cyclogenesis over the Bay of Bengal using the OSCAT derived surface wind fields. The Atmosphere-ISSN 2311-486X, vol-5, no-1, July-2015, pp-1-8. |
[2] | Mohammad Abdur Rahman Khan, Dr. C. M. Kishtawal, Md. Rashaduzzaman, and Md. SanaulHoque Mondal, Development of Emperical Track Prediction for Landfalling Tropical Cyclones over Bangladesh and east Indian coast line. The Atmosphere-ISSN 2311-486X, vol-5, no-1, July-2015, pp-36-46. |
[3] | MehrunNessa and Suraiya Begum, Satellite Observation & Intensity Estimation of Tropical Cyclone Using D’Vorak Algorithm. The Atmosphere-ISSN 2311-486X, vol-5, no-1, July-2015, pp-130-134. |
[4] | Md. Abdur Rahman, P. C. Joshi and B. M. Rao. Tropical Cyclone Track Prediction Using INSAT-VHRR Data. DEW-DROP-ISSN 2414 6056, March-2016, Vol-2, No-1. Pp-53-59. (a Scientific Journal of Meteorology and Geo-Physics). |
[5] | M. A. K. Mallik, M. A. M. Chowdhury, Shamsuddin Ahmed, M. N. Ahsan, Md. A. E. Akhter, S. M. Q. Hassan, Md. Omar Faruk, A Study of the Trend, Track and Frequency of Monsoon Depression over the Bay of Bengal. DEW-DROP-ISSN 2414 6056, March-2016, Vol-2, No.-1, pp-31-36. |
[6] | Samarendra Karmaker, Dewan Abdul Quadir and Md. Abdul Mannan. Trends in maximum temperature and thunderstorms, their correlation and impacts on the livelihood of Bangladesh. The Atmosphere-ISSN 2311-486X, vol-5, no-1, July-2015, pp-113-129. |
[7] | Md. A. E. Akhter, Md. M Alam and M. A. K. Mallik, SIMULATION OF THE STRUCTURE AND TRUCK OF THE TROPICAL CYCLONE RASHMI USING NUMERICAL MODELS. DEW-DROP-ISSN 2414 6056, March-2016, Vol-2, No.-1, pp-60-74. |
[8] | P. V. S. Raju • Jayaraman Potty • U. C. Mohanty, Prediction of severe tropical cyclones over the Bay of Bengal during 2007–2010 using high-resolution mesoscale model, Received: 8 October 2010 / Accepted: 2 July 2011 / Published online: 17 August 2011 Springer Science+Business Media B. V. 2011, Nat Hazards (2012) 63: 1361–1374 DOI 10.1007/s11069-011-9918-1. |
[9] | Siddiki, UbaydurRahaman, Islam, Md. Nurul and Ansari, Mohammad Nayeem Aziz, Cyclonic track analysis using GIS over the Bay of Bengal, Int. Journal of Applied Sciences and Engineering Research, Vol. 1, Issue 5, 2012 www.ijaser.com © 2012 by the authors – Licensee IJASER- Under Creative Commons License 3.0 editorial@ijaser.com Research article, ISSN 2277–9442, DOI: 10.6088/ijaser.0020101070. |
[10] | Shyama Mohanty, Raghu Nadimpalli, Krishna K Osuri, Sujata Pattanayak, U C Mohanty and SouravSil, Role of Sea Surface Temperature in Modulating Life Cycle of Tropical Cyclones over Bay of Bengal, Tropical Cyclone Research and Review, Vol-8, No-2, pp 68-83. |
[11] | AbhijitMitra, JoystuDutta, AnkitaMitra and TarunThakur, AmphanSupercyclone: A death knell for Indian Sundarbans, eJournal of Applied Forest Ecology (eJAFE), Vol. 8, No. 1 (2020) 41-48 Available online at www.ejafe.com ISSN: 2347-4009, Research Gate, Article june-20,: https://www.researchgate.net/publication/342477802. |
[12] | Sridhar Balasubramanian and Vamsi K Chalamalla, Super Cyclone Amphan: A Dynamical Case Study, Research Gate, Preprint July 2020, arXiv: 2007.02982v1 [physics.ao-ph] 6 Jul 2020, https://www.researchgate.net/publication/342763311. |
[13] | Muhammad Al-Amin Hoque, Stuart Phinn, Chris Roelfsema, A systematic review of tropical cyclone disaster management research using remote sensing and spatial analysis, ELSEVIER, Ocean & Coastal Management 146 (2017) 109e120. |
[14] | SamarendraKarmaker, Trends In The Annual Frequency Of Cyclonic Disturbances And Storms In The Bay of Bengal, south asian association for regional cooperation (SAARC), proceedings of SAARC seminar on climate variability in the south Asian region and its impacts, 10-12 December 2002. |
[15] | https://www.shutterstock.com/image-photo/super-cyclonic-storm-amphan-currently-very-1734314534. |
[16] | https://www.gettyimages.com/photos/cyclone?phrase=cyclone&sort=mostpopular. |
[17] | https://weheartit.com/entry/278263605?context_page=6&context_set=81676047-lighthouse&context_type=collection. |
APA Style
Shahanaj Sultana, Kawsar Parvin, Mohammad Abdul Mannan, Mohammad Abur Rahman Khan, Abul Kalam Mallik, et al. (2021). The Seasonal Climatology of Tropical Disturbances and Its Associated Tracks over the Bay of Bengal During 1891-2020. International Journal of Atmospheric and Oceanic Sciences, 5(2), 20-28. https://doi.org/10.11648/j.ijaos.20210502.11
ACS Style
Shahanaj Sultana; Kawsar Parvin; Mohammad Abdul Mannan; Mohammad Abur Rahman Khan; Abul Kalam Mallik, et al. The Seasonal Climatology of Tropical Disturbances and Its Associated Tracks over the Bay of Bengal During 1891-2020. Int. J. Atmos. Oceanic Sci. 2021, 5(2), 20-28. doi: 10.11648/j.ijaos.20210502.11
AMA Style
Shahanaj Sultana, Kawsar Parvin, Mohammad Abdul Mannan, Mohammad Abur Rahman Khan, Abul Kalam Mallik, et al. The Seasonal Climatology of Tropical Disturbances and Its Associated Tracks over the Bay of Bengal During 1891-2020. Int J Atmos Oceanic Sci. 2021;5(2):20-28. doi: 10.11648/j.ijaos.20210502.11
@article{10.11648/j.ijaos.20210502.11, author = {Shahanaj Sultana and Kawsar Parvin and Mohammad Abdul Mannan and Mohammad Abur Rahman Khan and Abul Kalam Mallik and Mohammad Kamrujjaman}, title = {The Seasonal Climatology of Tropical Disturbances and Its Associated Tracks over the Bay of Bengal During 1891-2020}, journal = {International Journal of Atmospheric and Oceanic Sciences}, volume = {5}, number = {2}, pages = {20-28}, doi = {10.11648/j.ijaos.20210502.11}, url = {https://doi.org/10.11648/j.ijaos.20210502.11}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijaos.20210502.11}, abstract = {The Bay of Bengal (BoB) is the import basin where tropical cyclone has been forming frequently compared to global perspective. The number and frequency of cyclone over the BoB varies year to year. The recent climatology of tropical cyclone and its track and landfall is very important to minimize casualties and damages. A statistical attempt has been made to know the seasonal number of cyclones over the BoB during 1891-2020 using BMD and IMD cyclone eAtlas data and the most devastating cyclones’ tracks of 1991, 1994, 2007, 2008, 2009 and 2020 are also drawn over the BoB. From the analysis it is found that the total number of cyclones formed over the BoB are 35, 123, 97 and 28 during pre-monsoon, monsoon, post-monsoon and winter seasons respectively whereas 58, 33, 103 and 26 for severe cyclonic storms respectively. The cyclone of all intensity over the BoB follows initially Westward/Northwestwards tracks, some of them re-curved and follows north/northeastwards tracks. Sometimes looping track is also found over the Bay of Bengal. It is also found that some cyclones have completed their journey in the BoB without landfall. This variation of cyclone makes the BoB basin more vulnerable and more challenging for forecasting of tropical cyclones.}, year = {2021} }
TY - JOUR T1 - The Seasonal Climatology of Tropical Disturbances and Its Associated Tracks over the Bay of Bengal During 1891-2020 AU - Shahanaj Sultana AU - Kawsar Parvin AU - Mohammad Abdul Mannan AU - Mohammad Abur Rahman Khan AU - Abul Kalam Mallik AU - Mohammad Kamrujjaman Y1 - 2021/08/18 PY - 2021 N1 - https://doi.org/10.11648/j.ijaos.20210502.11 DO - 10.11648/j.ijaos.20210502.11 T2 - International Journal of Atmospheric and Oceanic Sciences JF - International Journal of Atmospheric and Oceanic Sciences JO - International Journal of Atmospheric and Oceanic Sciences SP - 20 EP - 28 PB - Science Publishing Group SN - 2640-1150 UR - https://doi.org/10.11648/j.ijaos.20210502.11 AB - The Bay of Bengal (BoB) is the import basin where tropical cyclone has been forming frequently compared to global perspective. The number and frequency of cyclone over the BoB varies year to year. The recent climatology of tropical cyclone and its track and landfall is very important to minimize casualties and damages. A statistical attempt has been made to know the seasonal number of cyclones over the BoB during 1891-2020 using BMD and IMD cyclone eAtlas data and the most devastating cyclones’ tracks of 1991, 1994, 2007, 2008, 2009 and 2020 are also drawn over the BoB. From the analysis it is found that the total number of cyclones formed over the BoB are 35, 123, 97 and 28 during pre-monsoon, monsoon, post-monsoon and winter seasons respectively whereas 58, 33, 103 and 26 for severe cyclonic storms respectively. The cyclone of all intensity over the BoB follows initially Westward/Northwestwards tracks, some of them re-curved and follows north/northeastwards tracks. Sometimes looping track is also found over the Bay of Bengal. It is also found that some cyclones have completed their journey in the BoB without landfall. This variation of cyclone makes the BoB basin more vulnerable and more challenging for forecasting of tropical cyclones. VL - 5 IS - 2 ER -