THERMOHALINE CIRCULATION AND DYNAMIC STRUCTURE OF THE NORTH AEGEAN
Thermohaline Circulation (THC)
description
Transcript of Thermohaline Circulation (THC)
![Page 1: Thermohaline Circulation (THC)](https://reader036.fdocuments.in/reader036/viewer/2022062323/56815b7d550346895dc97a88/html5/thumbnails/1.jpg)
Thermohaline Thermohaline CirculationCirculation
(THC)(THC)By Ross AlterBy Ross Alter
![Page 2: Thermohaline Circulation (THC)](https://reader036.fdocuments.in/reader036/viewer/2022062323/56815b7d550346895dc97a88/html5/thumbnails/2.jpg)
What is it?What is it? “…that part of the ocean circulation which is
driven by fluxes of heat and freshwater across the sea surface and subsequent interior mixing of heat and salt” (Rahmstorf, 2006)
OneOne driving mechanism driving mechanism of large-scale “deep” of large-scale “deep” ocean circulationocean circulation
Temperature + salinity Temperature + salinity densitydensity ““Thermo-” + “-haline”Thermo-” + “-haline”
Requires Requires turbulent mixingturbulent mixing to complete the to complete the circulationcirculation
PhysicalPhysical concept, not observational concept, not observational
![Page 3: Thermohaline Circulation (THC)](https://reader036.fdocuments.in/reader036/viewer/2022062323/56815b7d550346895dc97a88/html5/thumbnails/3.jpg)
Source: Rahmstorf (2006)
![Page 4: Thermohaline Circulation (THC)](https://reader036.fdocuments.in/reader036/viewer/2022062323/56815b7d550346895dc97a88/html5/thumbnails/4.jpg)
Figure 2: Idealized meridional section representing a zonally averaged picture of the Atlantic Ocean. Straight arrows sketch the MOC. The color shading depicts a zonally averaged density profile derived from observational data [Levitus, 1982].
Source: Kuhlbrodt et al. (2007)
![Page 5: Thermohaline Circulation (THC)](https://reader036.fdocuments.in/reader036/viewer/2022062323/56815b7d550346895dc97a88/html5/thumbnails/5.jpg)
Why is it important?Why is it important? Maintains ocean Maintains ocean stratificationstratification ComparableComparable transport transport to that of the to that of the
surfacesurface Global volume transport ~ 30 SvGlobal volume transport ~ 30 Sv
Climate modulatorClimate modulator Cold water absorbs COCold water absorbs CO22 more efficiently more efficiently THC modulates THC modulates heat transportheat transport
~ 1 PW (10~ 1 PW (101515 W) in N. Atlantic W) in N. Atlantic
![Page 6: Thermohaline Circulation (THC)](https://reader036.fdocuments.in/reader036/viewer/2022062323/56815b7d550346895dc97a88/html5/thumbnails/6.jpg)
Speculation about the Speculation about the future…future…
Global warmingGlobal warming – warming and – warming and fresheningfreshening
Will the THC Will the THC break downbreak down?? Low probabilityLow probability, high impact, high impact Most likely scenario – Most likely scenario – weakeningweakening of of
THCTHC Would take Would take decades todecades to centuriescenturies to to
changechange No “Day After Tomorrow” scenario…No “Day After Tomorrow” scenario…
![Page 7: Thermohaline Circulation (THC)](https://reader036.fdocuments.in/reader036/viewer/2022062323/56815b7d550346895dc97a88/html5/thumbnails/7.jpg)
ReferencesReferences Stewart, R. H., 2002. Stewart, R. H., 2002. Introduction to Physical Introduction to Physical
OceanographyOceanography. . Kuhlbrodt, T., et al., 2007. On the driving Kuhlbrodt, T., et al., 2007. On the driving
processes of the Atlantic meridional processes of the Atlantic meridional overturning circulation, overturning circulation, Rev. Geophys.Rev. Geophys., 45, , 45, RG2001, doi:10.1029/2004RG000166 RG2001, doi:10.1029/2004RG000166
Rahmstorf, S. Thermohaline Ocean Circulation. In: Encyclopedia of Quaternary Sciences, Edited by S. A. Elias. Elsevier, Amsterdam 2006.