The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing

Author:

Stevens C. L.12,McPhee M. G.3,Forrest A. L.45,Leonard G. H.6,Stanton T.7,Haskell T. G.8

Affiliation:

1. Marine Physics; National Institute of Water and Atmospheric Research; Greta Point Wellington New Zealand

2. Physics Department; University of Auckland; Auckland New Zealand

3. McPhee Research Company; Naches Washington USA

4. Australian Maritime College; University of Tasmania; Launceston Tasmania Australia

5. Tahoe Environmental Research Center; University of California Davis; Davis California USA

6. School of Surveying; University of Otago; Dunedin New Zealand

7. Naval Postgraduate School; Monterey California USA

8. Industrial Research Ltd.; Lower Hutt New Zealand

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference38 articles.

1. Observation of sub-inertial internal tides in McMurdo Sound, Antarctica;Albrecht;Geophys. Res. Lett.,2006

2. A mathematical model of turbulent heat and mass transfer in stably stratified shear flow;Barenblatt;J. Fluid Mech.,1993

3. Current patterns in McMurdo Sound, Antarctica and their relationship to local biotic communities;Barry;Polar Biol.,1988

4. The glacier tongues of McMurdo Sound;Debenham;Geogr. J.,1965

5. Radio echosounding of Erebus Glacier Tongue;DeLisle;N. Z. Antarct. Rec.,1989

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