Research output: Contribution to journal › Article
Injection of oxygenated Persian Gulf Water into the southern Bay of Bengal. / Sheehan, Peter M F; Webber, Ben G M; Sanchez-Franks, Alejandra; Matthews, Adrian J; Heywood, Karen J; Vinayachandran, P N.
In: Geophysical Research Letters, Vol. 47, No. 14, e2020GL087773, 28.07.2020.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Injection of oxygenated Persian Gulf Water into the southern Bay of Bengal
AU - Sheehan, Peter M F
AU - Webber, Ben G M
AU - Sanchez-Franks, Alejandra
AU - Matthews, Adrian J
AU - Heywood, Karen J
AU - Vinayachandran, P N
PY - 2020/7/28
Y1 - 2020/7/28
N2 - Persian Gulf Water (PGW) is an oxygenated, high-salinity water mass that has recently been detected in the Bay of Bengal (BoB). However, little is known about the transport pathways of PGW into the BoB. Ocean glider observations presented here demonstrate the presence of PGW in the southwestern BoB. Output from an ocean reanalysis product shows that this PGW signal is associated with a northward-flowing filament of high-salinity water. Particle tracking experiments reveal two pathways: one in the eastern Arabian Sea that takes a minimum of 2 years and another in the western Arabian Sea that takes a minimum of 3 years. The western pathway connects to the BoB via equatorial currents. The greatest influx of PGW occurs between 82° and 87°E during the southwest monsoon. We propose that injection of PGW to the BoB oxygen minimum zone (OMZ) contributes to keeping oxygen concentrations in the BoB above the level at which denitrification occurs.
AB - Persian Gulf Water (PGW) is an oxygenated, high-salinity water mass that has recently been detected in the Bay of Bengal (BoB). However, little is known about the transport pathways of PGW into the BoB. Ocean glider observations presented here demonstrate the presence of PGW in the southwestern BoB. Output from an ocean reanalysis product shows that this PGW signal is associated with a northward-flowing filament of high-salinity water. Particle tracking experiments reveal two pathways: one in the eastern Arabian Sea that takes a minimum of 2 years and another in the western Arabian Sea that takes a minimum of 3 years. The western pathway connects to the BoB via equatorial currents. The greatest influx of PGW occurs between 82° and 87°E during the southwest monsoon. We propose that injection of PGW to the BoB oxygen minimum zone (OMZ) contributes to keeping oxygen concentrations in the BoB above the level at which denitrification occurs.
KW - Bay of Bengal
KW - Persian Gulf
KW - ocean gliders
KW - oxygen-minimum zones
KW - particle tracking
KW - water masses
UR - http://www.scopus.com/inward/record.url?scp=85088571283&partnerID=8YFLogxK
U2 - 10.1029/2020GL087773
DO - 10.1029/2020GL087773
M3 - Article
VL - 47
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 14
M1 - e2020GL087773
ER -
ID: 182298278