Publications des scientifiques de l'IRD

Durand Fabien, Papa Fabrice, Rahman A., Bala S. K. (2011). Impact of Ganges-Brahmaputra interannual discharge variations on Bay of Bengal salinity and temperature during 1992-1999 period. Journal of Earth System Science, 120 (5), p. 859-872. ISSN 0253-4126.

Titre du document
Impact of Ganges-Brahmaputra interannual discharge variations on Bay of Bengal salinity and temperature during 1992-1999 period
Année de publication
2011
Type de document
Article référencé dans le Web of Science WOS:000297078900007
Auteurs
Durand Fabien, Papa Fabrice, Rahman A., Bala S. K.
Source
Journal of Earth System Science, 2011, 120 (5), p. 859-872 ISSN 0253-4126
This study investigates the impact of monthly Ganges-Brahmaputra river discharge variations on Bay of Bengal salinity and temperature during the period 1992-1999. The Ganges-Brahmaputra river discharge is characterized by a well-defined seasonal cycle with strong interannual variations. The highest/lowest yearly peak discharge occurs in summer 1998/summer 1992, with 1998 value amounting to twice that of 1992. This river discharge is then used to force an ocean general circulation model. Our main result is that the impact of these rivers on the variability of Bay of Bengal sea surface salinity is strong in the northern part, with excess run-off forcing fresh anomalies, and vice versa. Most of the years, the influence of the interannual variability of river discharge on the Bay salinity does not extend south of similar to 10 degrees N. This stands in contrast with the available observations and is probably linked to the relatively coarse resolution of our model. However, the extreme discharge anomaly of 1998 is exported through the southern boundary of the Bay and penetrates the south-eastern Arabian Sea a few months after the discharge peak. In response to the discharge anomalies, the model simulates significant mixed-layer temperature anomalies in the northern Bay of Bengal. This has the potential to influence the climate of the area. From our conclusions, it appears necessary to use a numerical model with higher resolution (both on the horizontal and vertical) to quantitatively investigate the upper Bay of Bengal salinity structure.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Limnologie physique / Océanographie physique [032] ; Hydrologie [062]
Localisation
Fonds IRD [F B010054191]
Identifiant IRD
fdi:010054191
Contact