julien emile-geay
DESCRIPTION
Warren revisited : atmospheric freshwater fluxes and “Why is no deep water formed in the North Pacific ?”. Julien Emile-Geay. with Mark Cane, Richard Seager, Amy Clement, Naomi Naik and Alexander van Geen. THC. “A notable and well-known asymmetry in the deep ocean circulation - PowerPoint PPT PresentationTRANSCRIPT
Julien Emile-GeayJulien Emile-Geay
withMark Cane, Richard Seager, Amy Clement, Naomi Naik
and Alexander van Geen
Warren revisited : atmospheric freshwater fluxes and Warren revisited : atmospheric freshwater fluxes and “Why is no deep water formed in the “Why is no deep water formed in the
North Pacific ?”North Pacific ?”
THC
“A notable and well-known asymmetry in the deep ocean circulationis that deep water forms in the North Atlantic, and not at all in the North Pacific” (adapted from Bruce Warren)
What keeps deep water from sinking in the nNP ?
Why is the nNP so fresh relative to its Atlantic counterpart?
VBS,SSss
VWB,SSWBWB
Vu,SSuu
VN,SSWBWB VS,SSss
F=P-E
V’S’Eddy salt fluxes
Interior flow :VN –VS ≈ Sverdrup transportSalt transport MS= SWBVN – SsVS
Runoff
Western Boundary
flow
SWB ~ 34 psuSu = 34.6
V’S’
H=200m
A box model for the nNPA box model for the nNP(based on Warren 1983)(based on Warren 1983)
?
Conservations equations :Conservations equations :
• Freshwater budget :
€
R + F + Vu + Vwb = VBS + (VN −VS )
Interior flow = VN - VS
VWB is computed as a residual
• Salt budget (southward VWB) :€
SuVu+SWBVN+V'S'+W'S'=Ss[VBS+VS−VWB]
Eddy salt fluxes Outflow V0
Interior salt flux MS = SWBVN - SsVS
Subtropical inflowUpwelling
Results and sensitivity analysis
€
Ss =Fs
V0
≈160
4.8×10−3 = 32.93psu
Seasonal freshwater budget
Solid line :nNP
Dash-dotted :nNA
Thin solid :nNP-nNA
Why is the nNP so rainy despite its low evaporation rate?
WINTER
Moisture is pickedfrom the Warm Pooland converged into the nNP
€
rM (x, y) =
1
g(uq,vq) dp
1000
300
∫
SUMMER
Most of the northwardmoisture transport is associated with the Asian Monsoon
€
rM (x, y) =
1
g(uq,vq) dp
1000
300
∫
Conclusions
•Warren was essentially right : small throughflow rate and large (P-E) make the nNP so fresh• But it’s P, not E : Large atmospheric moisture transports, especially the Asian Monsoon, seem to explain this excess (in NCEP at least).
Why this is not happening in the North Atlantic : • different land/sea configuration (weaker Monsoon)• skinnier basin
Ultimately, the asymmetries of the land-sea configuration can explain THC asymmetries
Mass balance at the Southern Boundary
Warren’s box model (1983) CONFUSINGWarren’s box model (1983) CONFUSING : :
Freshwater fluxes :•F=P-E•R
+ Eddy Transports ..
Julien Emile-Geay:
Julien Emile-Geay:Julien Emile-
Geay:
Julien Emile-Geay:
VBS,SSss
VWB,SSWBWB
Vu,SSuu
VN,SSWBWB VS,SSss
F=P-E
A box model for the nNPA box model for the nNP(based on Warren 1983)(based on Warren 1983)
V’S’Eddy salt fluxes
Interior flow :VN –VS ≈ Sverdrup transportSalt transport MS= SWBVN – SsVS
Runoff
Western Boundary
flow
SWB ~ 34 psuSu = 34.6
V’S’ D =200m