An overview of the opportunities and challenges in the Ganges-Brahmaputra Delta and the Bay of Bengal in reference to climate change impact
Author: Aftab Alam KhanDOI: doi.org/10.70279/bmj-v5-i2-1025
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Ganges-Brahmaputra Delta and its extension in the Bay of Bengal is genetically related to delta progradation. Sediments of the Ganges-Brahmaputra Delta have been the principal source of opportunities in the perspective of georesources and ecosystem. Simultaneously the same sediments have been the major cause of many challenges this delta is facing since its formation. Terrestrial sediments from the Himalaya, deposited over the oceanic floor of the Bay of Bengal are the major source of oil, gas, gas hydrates, metallic and radioactive minerals in addition to all kinds of nutrients being supplied to the living organisms. Supply of more than one billion tons of sediments in the offshore delta every year provide opportunities in building prograding delta by accretion wherein one of the largest continental shelf advancing seaward through accumulating sediments to form numerous sand-bars and islands. However, all these opportunities are countered by the major challenges due to the recurring adverse events viz., massive siltation, inland and coastal flooding, deterioration of navigation routes, large scale land loss by bank erosion, submarine landslides, high pressure mud formation, free natural gas escape, cyclone, storm surge, saline water encroachment, security and pollution. These opportunities and challenges are not associated with climate change impact. Climate change is a natural phenomena that occurs in about hundred thousand years cycle of glacial and interglacial periods while the present Earth is passing through the interglacial period. The notion of climate change is an idea that circulates international diplomacy and domestic politics, and not the climate change in reality of the anthropocene time frame. Opportunities and challenges are associated with the variable physical and anthropogenic process operating in decadal to millennium time scale. The opportunities need to explore and nourish for the benefits of sustainable economic development. While, challenges are needed to face and manage by the good governance and by the proper professional human resource development and management.
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Article Volume | Volume 05 |
Article Issue | Issue 02 |
Article DOI | doi.org/10.70279/bmj-v5-i2-1025 |
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Article Slug | an-overview-of-the-opportunities-and-challenges-in-the-ganges-brahmaputra-delta-and-the-bay-of-bengal-in-reference-to-climate-change-impact |
Article Keyword | Opportunities; Challenges; Climate Change; Ganges-Brahmaputra Delta; Bay of Bengal |
Article Entry Time | 10:52:34 |
Article References | Alley, R. B., 2000. The Younger Dryas cold interval as viewed from central Greenland. Quaternary Science Reviews, 19 (1–5), 213-226. doi:10.1016/S0277-3791(99)00062-1 Broecker, W.S., 1975. Climate Change - Are we on the brink of a pronounced global warming? SCIENCE 189, p. 460 - 463. Broecker, W., 2017. When climate change predictions are right for the wrong reasons. Climatic Change 142, p. 1–6. https://doi.org/10.1007/s10584-017-1927-y Davis, B. A. S., Brewer, S., Stevenson, A. C., Guiot, J., 2003. Quaternary Science Reviews 22: 1701-1716. doi:10.1016/S0277-3791(03)00173-2 EPICA community members, 2004. Eight glacial cycles from an Antarctic ice core. Nature 429 (6992): 623-628. doi:10.1038/nature02599 Goodbred, Jr., S.L. and Kuehl, S.A., 2000. The significance of large sediment supply, active tectonism, and eustasy on margin sequence development: Late Quaternary stratigraphy and evolution of the Ganges–Brahmaputra delta. Sedimentary Geology 133, 227–248. Kawamura, K., Parrenin, F., Lisiecki, L., Uemura, R., Vimeux, F., Severinghaus, J. P., Hutterli, M. A., Nakazawa, T., Aoki, S., Jouzel, J., Raymo, M. E., Matsumoto, K., Nakata, H., Motoyama, H., Fujita, S., Goto-Azuma, K., Fujii, Y &Okitsugu Watanabe, O 2007. Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years. Nature 448, 912–916.doi:10.1038/nature06015 Khan, A.A., Akhter, S.H., Alam, S.M.M., 2000. Evidence of Holocene transgression, dolomitization and the source of arsenic in the Bengal delta. Geoengineering in Arid Lands, Mohamed & Al Hosani (eds), Balkema, Rotterdam, ISBN 90 5809 160 0 Khan, A.A., 1984. Interpretation of a buried channel in the Bay of Bengal using seismic reflection and gravity data. Bang. Jour. Geol., v.3, p.35-42. Köppen, W. 1884. Translated by Volken, E.; Brönnimann, S. "Die Wärmezonen der Erde, nach der Dauer der heissen, gemässigten und kalten Zeit und nach der Wirkung der Wärme auf die organische Welt betrachtet" [The thermal zones of the earth according to the duration of hot, moderate and cold periods and to the impact of heat on the organic world)]. Meteorologische Zeitschrift (published 2011). 20 (3): 351–360. Kuehl, S.A., Levy, B.M., Moore, W.S., Allison, M.A., 1997. Subaqueous delta of the Ganges-Brahmaputra river system. Mar. Geol. 144:81–96 Lea, D. W., Pak, D. K., Peterson, L. C., Hughen, K. A., 2003. Synchroneity of tropical and high-latitude Atlantic temperatures over the last glacial termination. Science 301 (5638): 1361-1364. doi:10.1126/science.1088470 Mahmuduzzaman, M., Ahmed, Z. U., Nuruzzaman, A. K. M., Ahmed, F. R. S., 2014. Causes of Salinity Intrusion in Coastal Belt of Bangladesh. International Journal of Plant Research, 4(4A): 8-13. DOI: 10.5923/s.plant.201401.02 Milliman, J. D., and Syvitski, J. P. M., 1992, Geomorphic/tectonic control of sediment discharge to the ocean: The importance of small mountainous rivers: Journal of Geology, v. 100, p. 525–544. Petit J. R., Jouzel J., Raynaud D., Barkov N. I., Barnola J. M., Basile I., Bender M., Chappellaz J., Davis J., Delaygue G., Delmotte M., Kotlyakov V. M., Legrand M., Lipenkov V., Lorius C., Pépin L., Ritz C., Saltzman E., Stievenard, M., 1999. Climate and Atmospheric History of the Past 420,000 years from the Vostok Ice Core, Antarctica. Nature 399: 429-436. doi:10.1038/20859 Rennell, J.J. 1776. An actual survey of the provinces of Bengal, Bahar etc. by Major General James Rennell, Surveyor to the Honourable East India Company (as referenced in Bristow, 1999). Rogers, K. G., Goodbred Jr, S. L., Khan, S. R., 2015. Shelf-to-canyon connections: Transport-related morphology and mass balance at the shallow-headed, rapidly aggrading Swatch of No Ground (Bay of Bengal). Marine Geology 369, 288–299. Stocker, T.F., D. Qin, G.-K. Plattner, L.V. Alexander, S.K. Allen, N.L. Bindoff, F.-M. Bréon, J.A. Church, U. Cubasch, S. Emori, P. Forster, P. Friedlingstein, N. Gillett, J.M. Gregory, D.L. Hartmann, E. Jansen, B. Kirtman, R. Knutti, K. Krishna Kumar, P. Lemke, J. Marotzke, V. Masson-Delmotte, G.A. Meehl, I.I. Mokhov, S. Piao, V. Ramaswamy, D. Randall, M. Rhein, M. Rojas, C. Sabine, D. Shindell, L.D. Talley, D.G. Vaughan and S.-P. Xie, 2013: Technical Summary. In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. Stott, L. D., Cannariato, K. G., Thunell, R., Haug, G. H., Koutavas, A., Lund, S., 2004. Decline of surface temperature and salinity in the western tropical Pacific Ocean in the Holocene epoch. Nature 431: 56-59. doi:10.1038/nature02903 Thompson, L.G., Mosley-Thompson, E., Davis, M. E., Henderson, K. A., Brecher, H. H., Zagorodnov, V. S., Mashiotta, T. A., Lin, P.-N., Mikhalenko, V. N., Hardy, D. R., Beer. J., 2002. Kilimanjaro Ice Core Records: Evidence of Holocene Climate Change in Tropical Africa. Science 298 (5593): 589-593. doi:10.1126/science.1073198 Wilson, C.A. and Goodbred Jr., S.L., 2015. Construction and Maintenance of the Ganges-Brahmaputra-Meghna Delta: Linking Process, Morphology, and Stratigraphy. Annu. Rev. Mar. Sci. 7:67–88. Zhao, M., Beveridge, N. A. S., Shackleton, N. J., Sarnthein, M., Eglinton. G., 1995. Molecular stratigraphy of cores off northwest Africa: Sea surface temperature history over the last 80 ka. Paleoceanography 10 (3): 661-675. doi:10.1029/94PA03354 Zavala, C., M. Arcuri, H. Gamero, C. Contreras, and M. Di Meglio. 2011. A genetic facies tract for the analysis of sustained hyperpycnal flow deposits. In Sediment Transfer from Shelf to Deep Water — Revisiting the Delivery System, ed. R.M. Slatt and C. Zavala. AAPG Studies in Geology, vol. 61, 31–51. https://www.iceagenow.info/temperatures-have-been-falling-for-8000-years/ https://commons.wikimedia.org/wiki/File:Holocene_Temperature_Variations.png |