East of Iceland, there are several areas in which overflow of dense water passes from the Norwegian Sea across the Iceland-Scotland Ridge into the Atlantic Ocean. Together, these overflows have been estimated (Hansen and Østerhus 2000) to yield a volume transport of similar magnitude to that through the Denmark Strait (Fig. 18.1). These eastern overflows thus contribute about 50% of the dense overflow from the Arctic Mediterranean into the North Atlantic.
The largest eastern overflow occurs in the deepest passage across the Greenland-Scotland Ridge, the Faroe Bank Channel, with a sill depth of 840 m. Some dense water also crosses the shallower ridges between Iceland and Scotland, the Iceland–Faroe Ridge with sill depth around 480 m, and the Wyville Thomson Ridge with a sill depth around 600 m.
During the ASOF period, observations of the eastern overflows were included in the ASOF-MOEN project. These observations included extension of the measurements of dense overflow through the Faroe Bank Channel and new instrumental records have been obtained for the Iceland–Faroe Ridge and Wyville Thomson Ridge.
Reviews on the history of overflow research and its accomplishments are given in Saunders (2001) and Hansen and Østerhus (2000), who focus on the eastern overflows. In this chapter, we offer a brief overview of the eastern overflows, including results from observations made during the last decade in a series of projects: Nordic WOCE, VEINS, ASOF-MOEN.
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References
Bryden H, Candela J, Kinder TH (1994) Exchange through the Strait of Gibraltar. Progress in Oceanography 33:201–248
de Boer CJ (1998) Water mass distribution in the Iceland Basin calculated with an Optimal Parameter Analysis. ICES Cooperative Research Report No 225:228–246
de Boer CJ, van Aken HM, van Bennekom AJ (1998) Hydrographic variability of the overflow water in the Iceland Basin. ICES Cooperative Research Report No 225:136–149
Dietrich G. (1956) Überströmung des Island-Faröer-Rücken in Bodennahe nach Beobachtungen mit dem Forschungsschiff ‘Anton Dohrn’ 1955/56. Deutsche Hydrographische Zeitschrift 9:78–89
Dickson RR, Brown J (1994) The production of North Atlantic Deep Water: sources, rates, and pathways. Journal of Geophysical Research 99:12319–12341
Ellett DJ (1991) Norwegian Sea Deep Water overflow across the Wyville Thomson Ridge during 1987–88. ICES CM1991/C:41
Ellett DJ, Edwards A (1978) A volume transport estimate for Norwegian Sea overflow across the Wyville Thomson Ridge. Overflow’ 73 expedition contribution nr 37. ICES CM1978/C:19, 12 pp
Fogelqvist E, Blindheim J, Tanhua T, Østerhus S, Buch E, Rey F (2003) Greenland-Scotland overflow studied by hydro-chemical multivariate analysis. Deep-Sea Research I 50:73–102
Geyer F, Østerhus S, Hansen B, Quadfasel D (2006) Observations of highly regular oscillations in the overflow plume downstream of the Faroe Bank Channel. Journal of Geophysical Research 111: C12020, doi:10.1029/2006JC003693
Hansen B, Østerhus S (2000) North Atlantic-Nordic Seas exchanges. Progress in Oceanography 45(2):109–208
Hansen B, Turrell WR, Østerhus S (2001) Decreasing overflow from the Nordic seas into the Atlantic Ocean through the Faroe Bank channel since 1950. Nature 411:927–930
Hansen B, Østerhus (2007) Faroe Bank Channel overflow 1995–2001. Progress in Oceanography. doi:10.1016/j.physletb.2003.10.071
Hermann F (1959) Hydrographic Observations in the Faroe Bank Channel and over the Faroe-Iceland Ridge June 1959. Journal du Conseil International pour l’Exploration de la Mer 118, 5 pp
Hermann F (1967) The T-S Diagram Analysis of the Water Masses over the Iceland-Faroe Ridge and in the Faroe Bank Channel (Overflow ‘60). Rapports et Procès-Verbaux des Réunions du Conseil International pour l’Exploration de la Mer 157:139–149
Høyer JL, Quadfasel D (2001) Detection of deep overflows with satellite altimetry. Geophysical Research Letters 28(8):1611–1614
Knudsen M (1898) Den Danske Ingolf-expedition. Bianco Lunos Kgl Hof-Bogtrykkeri (F. Dreyer). København, 1(2):21–154
Kuijpers A, Hansen B, Huhnerbach V, Larsen B, Nielsen T, Werner F (2002) Norwegian Sea overflow through the Faroe-Shetland gateway as documented by its bedforms. Marine Geology 188(1–2):147–164
Meincke J (1972) The Hydrographic Section along the Iceland-Faroe Ridge carried out by R.V. “Anton Dohrn” in 1959–1971. Berichte der Deutschen Wissenschaftlichen Kommission für Meeresforschung 22:372–384
Meincke J (1974) ’Overflow 73–Large-scale Features of the Overflow across the Iceland-Faroe Ridge. ICES CM 1974/C:7, 10 pp
Meincke J (1983) The modern current regime across the Greenland-Scotland Ridge. In: Bott M, Saxov S, Talwani M, Thiede J (eds) Structure and Development of the Greenland-Scotland Ridge. Plenum, New York, pp. 637–650
Nielsen JN (1904) Hydrography of the waters by the Faroe Islands and Iceland during the cruises of the Danish research steamer ‘Thor’ in the summer 1903. Meddelelser fra Kommisionen for havundersøgelser. Serie Hydrografi I(4), 42 pp
Perkins H, Hopkins TS, Malmberg SA, Poulain PM, Warn-Varnas A (1998) Oceanographic conditions east of Iceland. Journal of Geophysical Research 103:21531–21542
Saunders P (1990) Cold outflow from the Faroe Bank Channel. Journal of Physical Oceanography 20:29–43
Saunders PM (1996) The flux of dense cold overflow water southeast of Iceland*. Journal of Physical Oceanography 26:85–95
Saunders PM (2001) The dense northern overflows. In: Siedler G et al. (eds) Ocean Circulation and Climate. Academic, New York, pp. 401–417
Steele JH (1959) Observations of deep water overflow across the Iceland-Faroe Ridge. Deep-Sea Research 6:70–72
Sherwin TJ, Turrell WR (2005) Mixing and advection of a cold water cascade over the Wyville Thomson Ridge. Deep-Sea Research I 52:1392–1413
Sherwin TJ, Griffiths CR, Inall ME, Turrell WR (2007) Quantifying the overflow across the Wyville Thomson Ridge into the Rockall Trough, In press Deep-Sea Research
Tait JB (1967) The Iceland-Faroe Ridge international (ICES) ‘Overflow’ expedition 1960. Rapports et Procès-Verbaux des Réunions du Conseil International pour l’Exploration de la Mer 157:38–149
Wåhlin AK (2002) Topographic steering of dense currents with application to submarine canyons. Deep-Sea Research I 49(2):305–320
Østerhus S, Turrell WR, Hansen B, Lundberg P, Buch E (2001) Observed transport estimates between the North Atlantic and the Arctic Mediterranean in the Iceland-Scotland region. Polar Research 20(4):169–175
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Østerhus, S., Sherwin, T., Quadfasel, D., Hansen, B. (2008). The Overflow Transport East of Iceland. In: Dickson, R.R., Meincke, J., Rhines, P. (eds) Arctic–Subarctic Ocean Fluxes. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-6774-7_19
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