The Sundarban and Its Environment

  • Avijit Mistri
  • Bhaswati Das


The Sundarban is the UNESCO designated World Biosphere Reserve (in 2001) and inscribed as the Natural World Heritage Site in 1987. It is the largest halophytic mangrove forest in a single block, famous for in-situ conservation of endangered endemics and magnificent biodiversity of flora and fauna. The mangrove forest and associates, marsh grass, phytoplankton, molluscs and other coastal vegetation in the Sundarban sequester a huge amount of ‘Blue Carbon’ that reduces the global warming. Nowadays, low-lying coastal areas and islands like the Sundarban are in the limelight of climate change. Sea level rise, sea surface temperature, both the intensity and frequency of tropical cyclones, air temperature, rainfall, salinity, surface water pH and water transparency, all the environmental indicators in the Sundarban, are increasing in trend. This chapter provides insights into the detailed examination of the environment in the Sundarban based on the existing literatures.


Sundarban Biosphere Reserve (SBR) Sundarban Tiger Reserve (STR) Environmental change Sea level rise Tropical cyclone Salinity 


  1. B. A. E. & S. (2011). District statistical handbook, South 24 Parganas and North 24 Parganas. Department of Statistics and Programme Implementation, The Government of West Bengal. Kolkata, New Secretariat Buildings: Bureau of Applied Economics and Statistics (B.A.E. & S). Accessed 22 Nov 2018.
  2. Bhattacharya, S. (2007). Lesson learn for vulnerability and adaptation assessment from India’s first national communication. Paper 7 of BASIC project, Winrock International. Accessed 30 Sept 2016.
  3. Bindoff, N., Willebrand, J., Artale, V., Cazenave, A., Gregory, J., Gulev, S., Hanawa, K., Quéré, L., & Co-authors. (2007). Observations: Oceanic climate change and sea level. In S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt, M. Tignor, & H. L. Miller (Eds.), Climate change 2007: The physical science basis. Contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change (pp. 385–432). Cambridge: Cambridge University Press.Google Scholar
  4. Chand, B. K., Trivedi, R. K., Dubey, S. K., & Beg, M. M. (2012). Aquaculture in changing climate of Sundarban: Survey report on climate change vulnerabilities, aquaculture practices and coping measures in Sagar and Basanti blocks of Indian Sundarban. Kolkata: West Bengal University of Animal and Fishery Sciences.Google Scholar
  5. Dinse, K. (2012). Climate variability and climate change: What is the difference? Accessed 15 Feb 2013.
  6. Doney, N. M., & Levine, C. D. (2006). How long can the ocean slow global warming? How much excess carbon dioxide can the ocean hold and how will it affect marine life? Oceanus Magazine. Accessed 8 Jan 2014.
  7. DPD. (2009). Human development report, south 24 Parganas. Development and Planning Department (DPD), Government of West Bengal, Kolkata: HDRCC.Google Scholar
  8. Ghosh, A. (2012). Living with changing climate: Impact, vulnerability and adoption challenges in Indian Sundarbans. New Delhi: Centre for Science and Environment (CSE). Accessed 20 Dec 2013.Google Scholar
  9. Goshthakur, D. (2009, December 4). Sundarbaner Bastutantra Nonarbish (Poison of Salinity in the Ecosystem of Sundarban). Annadabazar Patrika, p. 4.Google Scholar
  10. Hazra, S., Ghosh, T., DasGupta, R., & Sen, G. (2002). Sea level and associated changes in the Sundarbans. Science and Culture, 68(9–12), 309–321.Google Scholar
  11. Hazra, S., Samanta, K., Mukhopadhyay, A., & Akhandet, A. (2010). Temporal change detection (2001–2008) study of Sundarban. Final report. School of Oceanographic Studies, Jadavpur University. Accessed 23 Jan 2013.
  12. IPCC (2007a). Impacts, adaptation and vulnerability. Contribution of working group II to the fourth assessment report of the intergovernmental panel on climate change. Cambridge: Cambridge University Press.Google Scholar
  13. IPCC (2007b). Climate change 2007: The physical science basis. Contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge: Cambridge University Press.Google Scholar
  14. Jhala, Y. V., Qureshi, Q., Gopal, R. (Eds.) (2015). The Status of Tigers in India, 2014. National Tiger Conservation Authority, New Delhi and the Wildlife Institute of India, Dehradun. New Delhi: NTCAGoogle Scholar
  15. Khan, T. M. A., Singh, O., & Rahaman, M. S. (2000). Recent sea level and sea surface temperature trends along the Bangladesh coast in relation to the frequency of intense cyclone. Marine Geodesy, 23(2), 23–103.Google Scholar
  16. Lal, M., Singh, K. K., Rathore, L. S., Srinivasan, G., & Saseendran, S. A. (1998). Vulnerability of rice and wheat yields in NW India to future changes in climate. Agricultural and Forest Meteorology, 89(2), 101–114.CrossRefGoogle Scholar
  17. Mistri, A. (2011). Open image in new window (Natural hazard and migration: In the context of Aila). Antorjatik Pathsala, 1(2), 124–140.Google Scholar
  18. Mistri, A., & Das, B. (2015). Environmental legislations and livelihood conflicts of fishermen in Sundarban, India. Asian Profile, 44(3), 389–400.Google Scholar
  19. Mitra, A., Gangopadhyay, A., Dube, A., Schmidt, A. C. K., & Banerjee, K. (2009). Observed changes in water mass properties in the Indian Sundarbans (Northwestern Bay of Bengal) during 1980–2007. Current Science, 97(10), 1445–1452.Google Scholar
  20. Mitra, A., Chowdhury, R., Sengupta, K., & Banerjee, K. (2010). Impact of salinity on mangroves of Indian Sundarbans. Journal of Coastal Environment, 1(1), 71–82.Google Scholar
  21. Nandy, S., & Bandyopadhyay, S. (2011). Trend of sea level change in the Hugli Estuary, India. Indian Journal of Geo-Marine Science, 40(6), 802–812.Google Scholar
  22. Rudra, K. (2010). The proposal of strengthening embankment in Sundarban: Myth and reality. Discussion Paper-I. Accessed 6 Jan 2014.
  23. Rupa Kumar, K., Sahai, A. K., Kumar, K. K., Patwardhan, S. K., Mishra, P. K., Revadekar, J. V., Kamala, K., & Pant, G. B. (2006). High-resolution climate change scenarios for India for the 21st century. Current Science, 90(3), 334–345.Google Scholar
  24. Singh, O. P. (2002). Spatial variation of sea level trend along the Bangladesh coast. Marine Geodesy, 25(3), 2005–2012.CrossRefGoogle Scholar
  25. Singh, O. P. (2007). Long-term trends in the frequency of severe cyclones of bay of Bengal: Observations and simulations. Mausam, 58(1), 59–66.Google Scholar
  26. Singh, O. P., Khan, T. M. A., & Md Rahman, S. (2001). Has the frequency of intense tropical cyclones increased in the North Indian Ocean? Current Science, 80(4), 575–580.Google Scholar
  27. STR. (2015). Administrative units, Government of West Bengal. Accessed 19 June 2015.
  28. Unnikrishnan, A. S., Kumar, K. R., Fernandes, S. E., Michael, G. S., & Patwardhan, S. K. (2006). Sea level changes along the Indian coast: Observations and projections. Current Science, 90(3), 362–368.Google Scholar

Copyright information

© Springer Nature Singapore Pte Ltd. 2020

Authors and Affiliations

  • Avijit Mistri
    • 1
  • Bhaswati Das
    • 2
  1. 1.Department of GeographyNistarini CollegePuruliaIndia
  2. 2.Centre for the Study of Regional Development, School of Social SciencesJawaharlal Nehru UniversityNew DelhiIndia

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