Current,Température and Salinity Observations in the Terra Nova Bay
173
Acknowledgements. The authors are grateful to colleagues of the CLIMA Project
whose participation in the field campaign allowed collection of the data.
References
1. Kurtz DD, Bromwich DH (1985) A recurring atmospherically forced polynya in Terra Nova Bay.
In: Jacobs SS (ed) Oceanology of the Antarctic Continental Shelf. Antarct Res Ser 43:173-202,AGU
2. Smith SD, Muench RD, Pease CH (1990) Polynyas and Leads: an overview of physical processes
and environment. J Geophys Res 95:9461-9479
3. Pease CH (1987) The size of wind-driven Coastal polynya. J Geophys Res 92:7049-7059
4. Bromwich DH, Kurtz DD (1984) Katabatic wind forcing of the Terra Nova Bay polynya. J Geophys
Res 89:3561-3572
5. Stocchino C, Manzella GMR (1991) Analisi delle correnti marine di Baia Terra Nova (Mare di
Ross-Antartide). CNR-ARIGE, pp 56
6. Jacobs S, Fairbanks GR, Horibe Y(1985) Origin and évolution of water masses near the Antarctic
continental margin: evidence from H218O/ H216O ratio in sea water. In: Jacobs SS (ed) Oceanology
of the Antarctic Continental Shelf. Antarct Res Ser 43:59-86, AGU, Washington, DC
7. Topp R, Johnson M (1997) Winter intensification and water mass évolution from year long current
meters in the northeast Polynya. J Marine Systems 10:157-198
8. Minnet PJ, Bignami F, Bohm E, Budeus G, Galbraith PS, Gudmansen P, Hopkins TS, Ingram RG,
Johmson MA, Niebauer HJ, Ramseier RO, Schneider W (1997) A summary of the formation and
seasonal progression of the northeast Polynya. J Marine Systems 10:79-86
9. Van Woert M (1998) Wintertime expansion and contraction of the Terra Nova Bay polynya
(This Volume)
10. Gawarkoewicz G, Chapman DC (1995) A numerical study of dense water formation and transport
on a shallow, sloping continental shelf. J Geophys Res 100:4489-4507
Précédent

- 185/298

Suivant