2025/12/08 by Keith Richards, Hugh Brammer, Patricia L. Saunders · 1 voice
Earth and Planetary Sciences · Environmental Science · #Flood Risk Assessment and Management #Hydrology and Sediment Transport Processes #Tree-ring climate responses
paper · pdf · doi:10.1111/geoj.70059
openalex publication_date 2025/12/08 · openalex created_date 2025/12/09 · openalex updated_date 2026/07/30
ABSTRACT The Brahmaputra River is one of the world's largest rivers, entering the Bengal Basin from its extensive Himalayan catchment, flowing south through Bangladesh, and joining the Ganges to traverse a complex fan‐delta and enter the Bay of Bengal. When Major James Rennell surveyed the river to establish the ‘Route Surveys’ for the East India Company between 1765 and 1777, it followed a different course, turning to the South‐East into the Sylhet Basin, and joining the Meghna. Some time after this, it changed its course—it avulsed—and a re‐survey was undertaken by Captain Richard Wilcox in 1828–1830 which first showed its present‐day southerly route. However, there is uncertainty about when, why, and how this major adjustment occurred, and these questions can only be answered with recourse to archival materials. This paper accordingly pieces together information in the writings of travellers and East India Company officials in the region in the period between 1787 and 1854; evidence of boundary changes in 1806; archival material indicating that the East India Company was concerned enough about declining flow in the ‘Old’ Brahmaputra to consider engineering works by 1845; and contemporary evidence of the widespread impact of severe monsoon floods in 1787; to conclude that the avulsion probably took place rather earlier than often assumed. And intriguingly, it seems that although Rennell left India in 1777, in the first edition of his Memoir published after those floods had occurred (1788), he inserted a brief reference to the Brahmaputra changing its course.