Helium 3 and dissolved oxygen balances in the upper waters of the Weddell Sea: Implications for oceanic heat fluxes

Publication Type  Journal Article
Year of Publication  2003
Authors  Hohmann, R.; Schlosser, P.; Huber, B.
Journal Title  Journal of Geophysical Research-Oceans
Volume  108
Issue  C3
Pages  -
Journal Date  Mar 18
ISBN Number  0148-0227
Accession Number  ISI:000182224000001
Key Words  tracers; noble gases; water masses; sea ice; winter mixed layer; southern-ocean; deep-water; maud-rise; ice; circulation; tritium; model; he-3; stratification
Abstract  

[1] We present helium 3 (He-3) and dissolved oxygen (DO) distributions in the upper waters of the central Weddell Sea obtained from samples collected during the Winter Weddell Sea Project (WWSP, July to September 1986), and the Antarctic Zone Flux Experiment (ANZFLUX, July to August 1994). The data are discussed in terms of apparent entrainment rates of Weddell Deep Water (WDW) into the Winter Mixed Layer (WML) and the associated apparent heat flux. The fraction of WDW in the WML derived from the He-3 excess (Deltadelta(3) He) and DO deficit in the mixed layer increases with latitude and reaches 10-20% at 68degreesS. The corresponding apparent heat flux during the winter entrainment period is 14 +/- 4 W m(-2), and the apparent annual heat flux is 6 +/- 4 W m(-2). Significantly larger heat fluxes ( winter ocean heat flux of 25 W m(-2); average annual heat flux of 15 W m(-2)) are observed near Maud Rise and in the region southwest of the rise in features that are associated with a Taylor column that apparently forms over the seamount. The entrainment rates and heat fluxes obtained from a one-dimensional numerical model exceed those calculated from the WDW fraction in the WML by about a factor of two, mainly because of the effect of gas exchange through leads on the mass balance of 3 He and DO in the WML. The best agreement between model calculations performed for 62.5degreesS, 65degreesS, and 67.5degreesS and observations is achieved for entrainment rates of 25-35 m yr(-1), 30-40 m yr(-1), and 35-45 m yr(-1), respectively. Daily entrainment rates are practically identical (0.28-0.39 m d(-1)) for the three latitudes. Corresponding simulated heat fluxes for the winter entrainment period and the annual average are 36-50 W m(-2) and 10-17 W m(-2), respectively. Extrapolation of the annual average heat flux to the seasonally ice-covered Weddell Sea yields a value of 0.04-0.07 PW.

Notes  

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URL  <Go to ISI>://000182224000001
DOI  Doi 10.1029/2000jc000474