The physical development processes along the coast are influenced by a multitude of factors, comprising wave motions, micro and macro-tidal cycles and long shore currents typical to the coastal tract. The shore currents vary greatly along with the
monsoon. These are also affected by
cyclonic action. Erosion and accretion through these forces maintains varying levels, as yet not properly measured, of physiographic change whilst the mangrove vegetation itself provides a remarkable stability to the entire system. During each monsoon season almost all the Bengal Delta is submerged, much of it for half a year. The sediment of the lower delta plain is primarily advected inland by monsoonal coastal setup and cyclonic events. One of the greatest challenges people living on the
Ganges Delta may face in coming years is the threat of rising sea levels caused mostly by
subsidence in the region and partly by climate change. In many of the Bangladesh's mangrove wetlands, freshwater reaching the mangroves was considerably reduced from the 1970s because of diversion of freshwater in the upstream area by neighbouring
India through the use of the
Farakka Barrage bordering
Rajshahi, Bangladesh. Also, the Bengal
Basin is slowly tilting towards the east because of neo-
tectonic movement, forcing greater freshwater input to the Bangladesh Sundarbans. As a result, the salinity of the Bangladesh Sundarbans is much lower than that of the Indian side. A 1990 study noted that there "is no evidence that environmental degradation in the
Himalayas or a 'greenhouse' induced rise in sea level have aggravated floods in Bangladesh"; however, a 2007 report by UNESCO, "Case Studies on Climate Change and World Heritage" has stated that an anthropogenic rise in sea level (likely by the end of the 21st century, according to the Intergovernmental Panel on Climate Change), combined with other forms of anthropogenic stress on the Sundarbans, could lead to the destruction of 75 percent of the Sundarbans mangroves. Already,
Lohachara Island and
New Moore Island/South Talpatti Island have disappeared under the sea, and
Ghoramara Island is half submerged. In a study conducted in 2012, the Zoological Society of London (ZSL) found out that the Sunderban coast was retreating up to in a year. Agricultural activities had destroyed around of mangroves within three decades (1975–2010). Shrimp cultivation had destroyed another . Researches from the School of Oceanographic Studies, Jadavpur University, estimated the annual rise in sea level to be in 2010. It had doubled from recorded in 2000. The rising sea levels had also submerged around of forest areas. This, coupled with an around rise in surface water temperatures and increased levels of salinity have posed a problem for the survival of the indigenous flora and fauna. The Sundari trees are exceptionally sensitive to salinity and are being threatened with extinction. Mangroves mitigate the effects of cyclones and tsunamis on coastal areas. Protecting mangrove health is therefore an urgent concern. Climate change-linked worsening of tidal and storm surges is causing flight to the mainland; about 13% of residents relocated in the decade of 2000–2010. A 2015 ethnographic study, conducted by a team of researchers from Heidelberg university in Germany, found a crisis brewing in the Sunderbans. The study contended that poor planning on the part of the India and Bangladesh governments coupled with natural ecological changes were forcing the flight of human capital from the region ==Hazards==