Dominant climate change event for salinity intrusion in the GBM delta

Abstract

This research makes a comparative analysis of reduced upstream discharge, sea level rise, and cyclonic conditions to find which factor predominates in the impacts of salinity intrusion. Findings show that a reduced upstream discharge causes increased saltwater intrusion in the entire region. A rising sea level causes increased salinity in the shallower coast. The cyclonic impact on saltwater intrusion is confined within the landfall zone. Salinity intrusion through the estuaries in low-lying tide-dominated deltas is a serious threat. Different levels of impacts are evident in the Ganges-Brahmaputra-Meghna (GBM) delta and along the Bangladesh coast.

Description

Keywords

SEA LEVEL RISE, COASTAL ZONE MANAGEMENT, CLIMATE CHANGE VULNERABILITY, HYDROLOGY, DELTAS, SALINIZATION, SALT WATER INTRUSION, DISASTER PREPAREDNESS, ESTUARIES, BANGLADESH, SOUTH ASIA

Citation

DOI