Freshwater export pathways from the Bay of Bengal
Advanced Search
Select up to three search categories and corresponding keywords using the fields to the right. Refer to the Help section for more detailed instructions.

Search our Collections & Repository

All these words:

For very narrow results

This exact word or phrase:

When looking for a specific result

Any of these words:

Best used for discovery & interchangable words

None of these words:

Recommended to be used in conjunction with other fields

Language:

Dates

Publication Date Range:

to

Document Data

Title:

Document Type:

Library

Collection:

Series:

People

Author:

Help
Clear All

Query Builder

Query box

Help
Clear All

For additional assistance using the Custom Query please check out our Help Page

i

Freshwater export pathways from the Bay of Bengal

Filetype[PDF-20.25 MB]


Select the Download button to view the document
This document is over 5mb in size and cannot be previewed

Details:

  • Journal Title:
    Deep Sea Research Part II: Topical Studies in Oceanography
  • Description:
    Observations from surface drifters and Argo floats elucidate details of two upper-ocean pathways through which freshwater from the Bay of Bengal (BoB) is advected into the tropical Indian Ocean and Arabian Sea (AS). The western route is located along the east coast of India and feeds into the westward Northeast Monsoon Current (NMC) south of Sri Lanka during the winter monsoon, whereas the eastern path is located along the western margin of Sumatra reaching at times as far south as the Indonesian Throughflow plume near 10°S. While the former pathway is highly seasonal and affected by mesoscale variability, the latter is a year-round feature and may be dominant from an annual perspective. The observations do not support the notion of a continuous current system comprised of the NMC and the West India Coastal Current around the Laccadive High in boreal winter that can directly export surface freshwater from the BoB to the AS. Further, the observations indicate an occasional leakage of low-salinity water by a westward coastal current between the eastward Southwest Monsoon Current (SMC) and Sri Lanka in boreal summer that may be caused by equatorial wave processes. The SMC, which exhibits considerable Ekman contributions in contrast to its geostrophically-balanced NMC counterpart in boreal winter, facilitates the transport of saltier AS water into the BoB, with subsequent spreading into the upper thermocline of the BoB setting up an estuary-like circulation pattern.
  • Source:
    Deep Sea Research Part II: Topical Studies in Oceanography, 168: 104645
  • Document Type:
  • Rights Information:
    CC BY
  • Compliance:
    CHORUS
  • Main Document Checksum:
  • File Type:

Supporting Files

More +

You May Also Like

Checkout today's featured content at repository.library.noaa.gov

Version 3.26