It has long been believed that the transport of heat by the ocean circulation is of importance to atmospheric climate. Circulation of the Atlantic Ocean warms and moistens western Europe, the argument goes, and, because of the pivotal role of the Atlantic/Arctic region, also affects global climate (e.g., Stommel 1979). Indeed, major oceanographic field programs have been launched by many nations, based on this premise. In the US, NOAA issues quarterly assessments of subtropical North Atlantic meridional heat transport (http://www.aoml.noaa.gov/phod/soto/mht/reports/ index.php). Estimates from ocean observations show the annual-mean, northward heat transport by the global circulation to decrease by about 1.5 pW (1015W) between latitudes 25° N and 50° N, with nearly 1 pW of that within the narrow Atlantic sector alone (see Bryden and Imawaki 2001, who estimate the uncertainty of individual section heat transports at 0.3 pW). This effect of the oceanic meridional overturning forces an enormous upward flux of heat and moisture in subtropical latitudes, providing a significant fraction of the zonally integrated atmospheric northward energy flux (which peaks at between 3 and 5.2 pW, as discussed further below). Occurring dominantly in wintertime, oceanic warmth and moisture energize the Pacific and Atlantic storm tracks. Combined action of atmosphere and ocean carries this energy northward, with great impact on all facets of high-latitude climate.
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References
Adler, R.F., G.J. Huffman, A. Chang, R. Ferraro, P-P. Xie, J. Janowiak, B. Rudolf, U. Schneider, S. Curtis, D. Bolvin, A. Gruber, J. Susskind, P. Arkin and E. Nelkin (2003) The Version-2 Global Precipitation Climatology Project (GPCP) Monthly Precipitation Analysis (1979–Present). J. Hydromet., 4: 1147–1167.
Bailey, D.A., P.B. Rhines and S. Häkkinen (2005) Pathways and formation of North Atlantic Deep Water in a coupled model of the Arctic-North Atlantic Oceans. Clim. Dyn., 24, doi:10. 1007/s00382–005-0050–3
Biastoch, A. and R.H. Käse (2003) The sensitivity of the Greenland-Scotland Ridge overflow to forcing changes. J. Phys. Oceanogr., 33: 2307–2319.
Boccaletti, G., R. Ferrari, A. Adcroft, D. Ferreira and J. Marshall (2005) The vertical structure of ocean heat transport. Geophys. Res. Lett., 32, doi:10.1029/2005GL022474.
Boyle, E. and L.D. Keigwin (1982) Deep circulation of the North Atlantic over the last 20, 000 years: geochemical evidence. Science, 218: 784–787.
Boyle, E. and L.D. Keigwin (1987) North Atlantic thermohaline circulation during the past 20, 000 years linked to high latitude surface temperature. Nature, 334: 333–335.
Bryden, H. and S. Imawaki (2001) Ocean heat transport. In Ocean Circulation and Climate, Siedler, Church and Gould (Eds.). Academic Press, London; 455–474.
Bunker, A.F. (1976) Computations of surface energy flux and annual air-sea interaction cycles of the North Atlantic Ocean. Mon. Wea. Rev., 104: 1122–1140.
Cronin, M.F., N.A. Bond, Fairall, C.W. and R.A. Weller (2006) Surface cloud forcing in the East Pacific stratus deck/cold tongue/ITCZ complex. J. Clim., 19(3): 392–409.
Curry, R., B. Dickson and I. Yashayaev (2003) A change in the freshwater balance of the Atlantic Ocean over the past four decades. Nature, 426: 826–829.
da Silva, A.M., C.C. Young and S. Levitus (1994) Atlas of Surface Marine Data Vol. 1: Algorithms and Procedures. NOAA Atlas series, pp. 74.
Dickson, R.R., T.J. Osborn, J.W. Hurrell, J. Meincke, J. Blindheim, B. Adlandsvik, T. Vinje, G. Alekseev and W. Maslowski (2000) The Arctic Ocean response to the North Atlantic Oscillation. J. Clim., 13: 2671–2696.
Dong, B. and R.T. Sutton (2005) Mechanism of interdecdal thermohaline circulation variability in a coupled ocean-atmosphere GCM. J. Clim., 18: 1117–1135.
Fairall, C.W., E.F. Bradley, J.E. Hare, A.A. Grachev and J.B. Edson (2003) Bulk parameterization of air-sea fluxes: Updates and verification for the COARE algorithm. J. Clim., 16(4): 571–591.
Fox, A.D. and K. Haines (2003) Interpretation of water mass formation deduced from data assimilation. J.Clim., 33: 485–498.
Grist, J.P. and S.A. Josey (2003) Inverse analysis of the SOC air-sea flux climatology using ocean heat transport constraints, J. Clim., 16: 3274–3295.
Grist, J.P., S.A. Josey and B. Sinha (2007) Impact on the ocean of extreme Greenland Sea heat loss in the HadCM3 coupled ocean-atmosphere model. J. Geophys. Res., 112, C04014, doi:10.1029/2006JC003629.
Gulev, S., T. Jung and E. Ruprecht (2007) Estimation of the impact of sampling errors in the VOS observations on air–sea fluxes. Part I: uncertainties in climate means. J. Clim., 20: 279–301.
Hadfield, N.C. Wells, S.A.Josey and J. J-M Hirschi (2007) Accurac of North Atlantic temperature and heat storage fields from ARGO. J. Geophys Res., 112, C01009, doi:10.1029/2006JC003825.
Hall, M.M. and H.L. Bryden (1982) Direct estimates and mechanisms of ocean heat transport. Deep-Sea Res., 29: 339–359.
Häkkinen, S. and P.B. Rhines (2004) Decline of the North Atlantic subpolar circulation in the 1990s. Science, 304: 555–559.
Häkkinen, S., F. Dupont, M. Karcher, F. Kauker, D. Worthen J. and Zhang (2007a) Model simulation of Greenland Sea upper-ocean variability J. Geophys. Res., 112, No. C6, C06S9010.1029/2006JC003687
Häkkinen, S. and P.B. Rhines (2007b) Shifting circulations in the northern Atlantic Ocean. Science, submitted.
Hallberg, R. and Gnanadesekin, A. (2006) The role of eddies in determining the structure and response of the wind-driven Southern Hemisphere overturning: results from the modeling eddies in the Southern Ocean (MESO) project. J. Phys. Oceanogr., 36: 2232–2252.
Hátún, H., A.B. Sandø, H. Drange, B. Hansen and H. Valdimarsson (2005) Influence of the Atlantic subpolar gyre on the thermohaline circulation. Science, 309: 1841–1844.
Hátún, H., C.E. Eriksen, P.B. Rhines and J. Lilly (2007) Buoyant eddies entering the Labrador Sea observed with gliders and altimetry. J. Phys. Oceanogr., Dec.
Held, I., M.F. Ting and H. Wang (2002) Northern stationary waves: theory and modeling. J. Clim., 15: 2125–2144.
Keith, D.W. (1995) Meridional energy transport: uncertainty in zonal means. Tellus, 47A: 30–44.
Josey, S.A., E.C. Kent and P.K. Taylor (1999) New insights into the ocean heat budget closure problem from analysis of the SOC air-sea flux climatology. J. Clim., 12(9): 2856–2880.
Josey, S.A. and R. Marsh (2005) Surface freshwater flux variability and recent freshening of the North Atlantic in the Eastern Subpolar Gyre. J. Geophys. Res., 110, C05008, doi:10.1029/ 2004JC002521.
Josey, S.A. and S.R. Smith (2006) Guidelines for Evaluation of Air-Sea Heat, Freshwater and Momentum Flux Datasets, CLIVAR Global Synthesis and Observations Panel (GSOP) White Paper, July 2006, pp. 12. Available at http://www.noc.soton.ac.uk/JRD/MET/gsopfg.pdf.
Kistler, R., E. Kalnay, W. Collins, S. Saha, G. White, J. Woollen, M. Chelliah, W. Ebisuzaki, M. Kanamitsu, V. Kousky, H. van den Dool, R. Jenne and M. Fiorino (2001) The NCEP–NCAR 50-year reanalysis: monthly means CD-ROM and documentation. Bull. Am. Met. Soc., 82: 247–267.
Large, W.G. and S.G. Yeager (2004) Diurnal to decadal global forcing for ocean and sea-ice models: the data sets and flux climatologies. NCAR Technical Note NCAR/TN-460 + STR, 111 pp.
Leduc, G., L. Vidal, K. Tachikawa1, F. Rostek, C. Sonzogni, L. Beaufort and E. Bard (2007) Moisture transport across Central America as a positive feedback on abrupt climatic changes. Nature, 445, 908–911, doi:10.1038/nature05578
Lilly, J.M., P.B. Rhines, M. Visbeck, R. Davis, J.R.N. Lazier, F. Schott, and D. Farmer (1999) Observing deep convection in the Labrador Sea during winter, 1994–1995. J. Phys. Oceanogr., 29: 2065–2098.
Lilly, J.M., P.B. Rhines, F. Schott, K. Lavender, J. Lazier, U. Send and E. d’Asaro (2003) Observations of the Labrador Sea eddy field. Prog. Oceanogr., 59: 75–176.
Liu, J. and J. Curry (2006) Variability of the tropical and subtropical ocean surface latent heat flux during 1989–2000. Geophys. Res. Lett., 33, doi:10.1029/2005GL023809.
Levitus, S., J. Antonov and T. Boyer (2005) Warming of the world ocean, 1955–2003. Geophys. Res. Lett., 32, doi:10.1029/2004GL021592
Lumpkin, R. and K. Speer (2003) Large-scale vertical and horizontal circulation of the Atlantic Ocean. J. Phys. Oceanogr., 33: 1902–1920.
Manabe, S. and R. Stouffer (1994) Multiple century response of a coupled ocean-atmosphere model to a n increase of atmospheric carbon dioxide. J. Clim., 7: 5–23.
Marsh, R., S.A. Josey, A.J.G. Nurser, B.A. de Cuevas, and A.C. Coward (2006) Water mass transformation in the North Atlantic over 1985–2002 simulated in an eddy-permitting model. Ocean Sci., 1: 127–144.
Peterson, B.J., J. McClelland, R. Curry, R.M. Holmes, J.E. Walsh, K. Aagaard (2006) Trajectory shifts in the Arctic and Subarctic freshwater cycle. Science, 313: 1061–1066.
Pickart, R.S., M.A. Spall, M.H. Ribergaard, G.W.K. Moore and R.F. Milliff (2003) Deep convection in the Irminger Sea forced by the Greenland tip jet Nature, 424: 152–156.
Rhines, P.B. (2006) Sub-Arctic oceans and global climate. Weather, 61: 109–118.
Renfrew, I.A., G.W.K. Moore, P.S. Guest and K. Bumke (2002) A comparison of surface-layer and surface heat flux observations over the Labrador Sea with ECMWF and NCEP reanalyses. J. Phys. Oceanogr., 32: 383–400.
Sarmiento, J.L., N. Gruber, M. Brzezinski and J.P. Dunne (2004) High-latitude controls of thermocline nutrients and low latitude biological productivity. Nature, 427: 56–60.
Schmittner, K. (2005) Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation. Nature, 434: 628–632.
Seager, R., D.S. Battisti, J. Yin, N. Gordon, N. Naik, A.C. Clement, and M.A. Cane (2002) Is the Gulf Stream responsible for Europe’s mild winters? Q. J. Roy. Met. Soc., 128: 2563–2586.
Stammer, D., K. Ueyoshi, A. Kohl, W.G. Large, S.A. Josey and C. Wunsch (2004) Estimating air-sea fluxes of heat, freshwater and momentum through global ocean data assimilation. J. Geophys. Res., 109, C05023, doi:10.1029/2003JC002082.
Stommel, H.M. (1979) Oceanic warming of western Europe. Proc. Nat. Acad. Sci., 76: 2518–2521.
Stommel, H.M. and G.T. Csanady (1980) A relation between the T-S curve and global heat and atmospheric water transports. J. Geophys. Res., 85: 495–501.
van der Swaluw, E., S.S. Drijfhout and W. Hazeleger (2007) Bjerknes compensation at high Northern latitudes: the ocean forcing the atmosphere. J. Clim. submitted.
Talley, L. (2003) Shallow, deep and intermediate components of the global heat budget. J. Phys. Oceanogr., 33: 530–560.
Thompson, D. and J.M. Wallace (2001) Annular modes in the extratropical circulation: Part I: Month-to-month variability. J. Clim., 13: 1000–1016.
Toggweiler, R. and B.Samuels (1995) Effect of Drake Passage on the global thermohaline circulation. Deep-Sea Res., 42: 477–500.
Toggweiler, R. and B. Samuels (1998) On the ocean’s large-scale circulation near the limit of no vertical mixing. J. Phys. Oceanogr., 28: 1832–1852.
Trenberth, K. and J.M. Caron (2001) Estimates of meridional atmosphere and ocean heat transports. J. Clim., 14: 3433–3443.
Trenberth, K.E., J.M. Caron and D.P. Stepaniak (2001) The atmospheric energy budget and implications for surface fluxes and ocean heat transports. Clim. Dyn., 17: 259–276.
Uppala, S.M., P.W. Kållberg, A.J. Simmons, U. Andrae, V. da Costa Bechtold, M. Fiorino, J.K. Gibson, J. Haseler, A. Hernandez, G.A. Kelly, X. Li, K. Onogi, S. Saarinen, N. Sokka, R.P. Allan, E. Andersson, K. Arpe, M.A. Balmaseda, A.C.M. Beljaars, L. van de Berg, J. Bidlot, N. Bormann, S. Caires, F. Chevallier, A. Dethof, M. Dragosavac, M. Fisher, M. Fuentes, S. Hagemann, E. Hólm, B.J. Hoskins, L. Isaksen, P.A.E.M. Janssen, R. Jenne, A.P. McNally, J.-F. Mahfouf, J.-J. Morcrette, N.A. Rayner, R.W. Saunders, P. Simon, A. Sterl, K.E. Trenberth, A. Untch, D. Vasiljevic, P. Viterbo and J. Woollen (2005) The ERA-40 re-analysis. Q. J. Roy. Met. Soc., 131: 2961–3012. doi:10.1256/qj.04.176.
Wang, J. and J.A. Carton (2002) Seasonal heat budget of the Pacific and Atlantic Oceans. J. Phys. Oceanogr., 32: 3474–3489.
WGASF (2000) Intercomparison And Validation Of Ocean-Atmosphere Energy Flux Fields, Final Report Of The Joint WCRP/SCOR Working Group On Air-Sea Fluxes SCOR Working Group 110, P.K. Taylor (Ed). 312.
Wijffels, S.E. (2001) Ocean transport of fresh water. In Ocean Circulation and Climate, Siedler, Church and Gould (Eds.). Academic Press, London: 475–488.
Wijffels, S.E., R.W. Schmitt, H.L. Bryden and A. Stigebrandt (1992) Transport of freshwater by the oceans. J. Phys. Oceanogr., 22: 155–162.
Willis, J., D. Roemmich and B. Cornuelle (2003) Combining altimetric height with broadscale profile data to estimate steric height, heat storage, subsurface temperature, and sea-surface temperature variability. J. Geophys. Res., 108, doi:10.1029/2002JC001755.
Woodgate, R., K. Aagaard and T. Weingartner (2006) Interannual changes in the Bering Strait fluxes of volume, heat and freshwater between 1991 and 2004. Geophys. Res. Lett., 33, L15609, doi:10.1029/2006GL026931.
Wunsch, C. (2005) The total meridional heat flux and its oceanic and atmospheric partition. J. Clim., 18: 4374–4380.
Wunsch, C. and R. Ferrari (2004) Vertical mixing, energy and the general circulation of the oceans. Ann. Revs. Fluid Mech., 36: 281–314.
Yu, L. and R.A. Weller (2007) Objectively analyzed air–sea heat fluxes for the global ice-free oceans (1981–2005). Bull. Am. Meteor. Soc., 88: 527–539.
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Rhines, P., Häkkinen, S., Josey, S.A. (2008). Is Oceanic Heat Transport Significant in the Climate System?. In: Dickson, R.R., Meincke, J., Rhines, P. (eds) Arctic–Subarctic Ocean Fluxes. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-6774-7_5
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