gesjGEOGRAPHY, ENVIRONMENT, SUSTAINABILITYGEOGRAPHY, ENVIRONMENT, SUSTAINABILITY2071-93882542-1565Russian Geographical Society10.24057/2071-9388-2012-5-4-24-32gesj-159Research ArticleGEOGRAPHYГеографияSPREADING OF ANTARCTIC BOTTOM WATER IN THE ATLANTIC OCEANMorozovEugeneegmorozov@mail.ruTarakanovRomanrtarakanov@gmail.comZenkWalterwzenk@geomar.de201201122012542432Copyright © Morozov E., Tarakanov R., Zenk W., 20122012Morozov E., Tarakanov R., Zenk W.Morozov E., Tarakanov R., Zenk W.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://ges.rgo.ru/jour/article/view/159Abyssal channelsVemaRomancheChainKanebottom waterReferencesHogg N.G., Owens W.B. (1999). Direct measurement of the deep circulation within theHogg N.G., Owens W.B. (1999). Direct measurement of the deep circulation within theBrazil Basin, Deep-Sea Res. II, Vol. 46, pp. 335–353.Brazil Basin, Deep-Sea Res. II, Vol. 46, pp. 335–353.Mantyla A.W., Reid J.L. (1983). Abyssal characteristics of the World Ocean waters, Deep-Mantyla A.W., Reid J.L. (1983). Abyssal characteristics of the World Ocean waters, Deep-Sea Res., Vol. 30, N 8, pp. 805–833.Sea Res., Vol. 30, N 8, pp. 805–833.McCartney M.S., Bennet S.L., Woodgate-Jones M.E. (1991). Eastward flow through theMcCartney M.S., Bennet S.L., Woodgate-Jones M.E. (1991). Eastward flow through theMid-Atlantic ridge at 11° N and its influence on the abyss of the Eastern basin, J. Phys.Mid-Atlantic ridge at 11° N and its influence on the abyss of the Eastern basin, J. Phys.Oceanogr., Vol. 21, N 8, pp. 1089–1121.Oceanogr., Vol. 21, N 8, pp. 1089–1121.Messias M.-J., Andrie C., Memery L., Mercier H. (1999). Tracing the North Atlantic DeepMessias M.-J., Andrie C., Memery L., Mercier H. (1999). Tracing the North Atlantic DeepWater through the Romanche and Chain fracture zones with chlorofluoromethanes,Water through the Romanche and Chain fracture zones with chlorofluoromethanes,Deep-Sea Res. Vol. 46, pp. 1247–1278.Deep-Sea Res. Vol. 46, pp. 1247–1278.Morozov E.G., Demidov A.N., Tarakanov R.Y., Zenk W. (2010). Abyssal Channels of the AtlanticMorozov E.G., Demidov A.N., Tarakanov R.Y., Zenk W. (2010). Abyssal Channels of the AtlanticOcean: Water Structure and Flows, Springer, 266 p.Ocean: Water Structure and Flows, Springer, 266 p.Orsi A.H., Johnsson G.C., Bullister J.L. (1999). Circulation, mixing, and production of AntarcticOrsi A.H., Johnsson G.C., Bullister J.L. (1999). Circulation, mixing, and production of AntarcticBottom Water, Progress in Oceanography, Vol. 43, pp. 55–109.Bottom Water, Progress in Oceanography, Vol. 43, pp. 55–109.Saunders P.M. (1987). Flow through Discovery Gap, J. Phys. Oceanogr., Vol. 17, N. 5, pp.Saunders P.M. (1987). Flow through Discovery Gap, J. Phys. Oceanogr., Vol. 17, N. 5, pp.–643.–643.Wüst G. (1936). Schichtung und Zirkulation des Atlantischen Ozeans, Das BodenwasserWüst G. (1936). Schichtung und Zirkulation des Atlantischen Ozeans, Das Bodenwasserund die Stratosphäre. In: A. Defant (Ed.), Wissenschaftliche Ergebnisse, Deutsche Atlantischeund die Stratosphäre. In: A. Defant (Ed.), Wissenschaftliche Ergebnisse, Deutsche AtlantischeExpedition auf dem Forschungs – und Vermessungsschiff „Meteor“ 1925–1927, 6 (1), WalterExpedition auf dem Forschungs – und Vermessungsschiff „Meteor“ 1925–1927, 6 (1), Walterde Gruyter & Co, Berlin, 411 pg.de Gruyter & Co, Berlin, 411 pg.Zenk W., Morozov E. (2007). Decadal warming of the coldest Antarctic Bottom Water flowZenk W., Morozov E. (2007). Decadal warming of the coldest Antarctic Bottom Water flowthrough the Vema Channel, Geophysical Research Letters, Vol. 34, N 14, L14607.through the Vema Channel, Geophysical Research Letters, Vol. 34, N 14, L14607.Zenk W., Speer K.G., Hogg N.G. (1993). Bathymetry at the Vema Sill, Deep-Sea Res., Vol. 40,Zenk W., Speer K.G., Hogg N.G. (1993). Bathymetry at the Vema Sill, Deep-Sea Res., Vol. 40,pp. 1925–1933.pp. 1925–1933.Zenk W., Visbeck M. (2012). Structure and evolution of the abyssal jet in the Vema ChannelZenk W., Visbeck M. (2012). Structure and evolution of the abyssal jet in the Vema Channelof the South Atlantic. Deep-Sea Research II (accepted).of the South Atlantic. Deep-Sea Research II (accepted).
The authors declare that there are no conflicts of interest present.