River discharge into the Bay of Bengal in an inverse ocean model

Details River discharge into the Bay of Bengal in an inverse ocean model River discharge into the Bay of Bengal in an inverse ocean model

Aug 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005georl..3216605y&link_type=abstract

Geophysical Research Letters, Volume 32, Issue 16, CiteID L16605

Mathematics

Logic

6

Global Change: Water Cycles (1836), Hydrology: Hydrological Cycles And Budgets (1218, 1655), Atmospheric Processes: Precipitation (1854), Oceanography: General: Descriptive And Regional Oceanography, Oceanography: General: Ocean Data Assimilation And Reanalysis (3225)

Scientific paper

The seasonal cycle of river runoff in the Bay of Bengal is estimated by assimilating climatological salinity/temperature and precipitation data into an ocean model of intermediate complexity. The resulting optimized river-transport field fits independent land-based observations within their error bars. Six precipitation products are discussed for their ability to reproduce the observed salinity field within the Bay.

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