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Transport Measures

Transport Measures. Meridional overturning, MOC:. MOC on density surfaces:. Heat transport (rel. 0 o C):. Freshwater transport (rel. 35 psu):. Ganachaud&Wunsch. K-7. Keith (1995) Trenberth & Solomon (1994) Macdonald & Wunsch (1996) Garnier et al (2001) De las Heras & Schlitzer(1999)

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Transport Measures

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  1. Transport Measures Meridional overturning, MOC: MOC on density surfaces: Heat transport (rel. 0oC): Freshwater transport (rel. 35 psu):

  2. Ganachaud&Wunsch K-7 • Keith (1995) • Trenberth & Solomon (1994) • Macdonald & Wunsch (1996) • Garnier et al (2001) • De las Heras & Schlitzer(1999) • Bryden et al (1991) • Ganachaud & Wunsch • (2000) Heat transports Heat transports Mass transports heat transports are indicated by the arrows and red numbers (positive northward/eastward). The white box at the tail end of each arrow is the one-standard-deviation uncertainty. Between sections, ocean-atmosphere heat transfers are indicated by the zonal length of the coloured boxes (blue for ocean cooling; red for ocean heating), with the length of the white box inside indicating the uncertainty.

  3. Global Heattransport K-7 Ganachaud&Wunsch(1996)

  4. North Atlantic Heattr. ENSEBLES Ganachaud&Wunsch(1996)

  5. Indo-Pac. Heattransport K-7 Ganachaud&Wunsch(1996)

  6. Wijffels et al (2001)/Macdonald&Wunsch(1996) Wijffels et al (2001) Macdonald&Wunsch(1996)

  7. Global Freshwater transp. K-7 Wijffels et. al. (2001)

  8. Atlantic and IndoPac freshwater transports K-7 Indo-Pacific Atlantic

  9. Heat transport 25oN K-7

  10. Heat transport 48oN K-7

  11. Heat/FW transport ENSEBLES

  12. Bryden et al (2005) K-7 Transport per unit depth (in m2 s-1) represents the zonally averaged northward geostrophic velocity times the zonal distance across the section at each depth. a, Top-to-bottom profile showing the general similarity in vertical structure of the flow for each section with southward flow in the upper waters, a northward flow of intermediate waters, a southward flow of deep waters at 1,200-5,000 m depth, and a northward flow in the bottom waters. b, Expanded profile of the thermocline flow showing the stronger southward flow in the 1998 and 2004 sections. c, Expanded profile below 1,000 m depth showing the two cores of southward flowing upper NADW centred at about 2,000 m depth and lower NADW centred at 4,000 m depth. u-NADW l-NADW AABW

  13. Max. MOC 25oN K-7 Bryden et al. (2005) ECMWF

  14. Max. MOC 48oN K-7

  15. ECCO-50y Global MOC ECCO-SIO ECCO-GODAE ECCO-JPL GFDL INGV SODA

  16. ECCO-50y Atlantic MOC ECCO-SIO ECCO-GODAE ECCO-JPL GFDL INGV SODA

  17. ECCO-50y IndoPac MOC ECCO-SIO ECCO-GODAE ECCO-JPL GFDL INGV SODA

  18. MOC ENSEBLES

  19. ---------------- AWI

  20. Willebrand et al (2000) Level ISOPYCNIC Level ISOPYCNIC AtlanticMOC vs. density AtlanticMOC vs. depth SIGMA SIGMA 1styr Level SIGMA Roemmich&Wunsch (1985) ISOPYCNIC 10th yr

  21. ECCO-JPL ECCO-JPL

  22. ECCO-SIO ECCO-SIO

  23. ECCO-50y ECCO-50y

  24. ECCO-GODAE ECCO-GODAE

  25. ECMWF ECMWF

  26. GFDL SODA

  27. INGV INGV

  28. SODA SODA

  29. ECCO-SIO/50y + Ref. ECCO-SIO Bryden et al. (2005)

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