Fróðskaparrit - 01.01.2004, Side 77

WORKS IN ENGLISH FROM AND ABOUT THE FAROE ISLANDS
75
331: Hansen, B./Malmberg, S.A./Sælen,
O.H./Østerhus, S.: Measurement of flow
north of the Faroe Islands, June 1986
Hansen/Østerhus: North Atlantic-Norwegian
Sea Exchange, Copenhagen 1998, pp. 83-95, 9
figures, references
<A preliminary report of the current measurements
received fronr a line of moorings with currenl meters
deployed north-wards from the Faroe Islands for ten
days in the beginning of June 1986>
332: Hansen, Bogi/Sælen, Odd H./Østerhus,
Svein: The passage of Atlantie Water east of
the Faroes
Hansen/Østerhus: North Atlanlic-Norwegian
Sea Exchange, Copenhagen 1998, pp. 112-123,
6 figures, 1 table, references
<Results of measurements made in June 1986 and
July 1987>
333: Hansen, Bogi/Meldrum, David/Iillett,
David: Satellite-tracked drogue paths over
Faroe Bank and the Iceland-Faroe Ridge
Hansen/Østerhus: North Atlanlic-Norwegian
SeaExchange, Copenhagen 1998, pp. 150-161,
8 figures, 1 table, references
<”Satellite-tracked drogues have conftrmed the
existence of an anticyclonic circulation around Faroe
Bank during three periods of 1986-1989, and also
showed a predicted self-contained circulation in the
upper waters of the Faroe Bank Channel. Upon the
Iceland-Faroe Ridge, drogues mainly followed the
isobaths and were largely consistent with the clas-
sical circulation shemes for the area.” Quoted from
abstract>
334: Hansen, Bogi/Kristiansen, Regin:
Variations of the Faroe Bank Channel over-
flow
in: Rit Fiskideildar. Reykjavík, vol. 16, 1999,
pp. 13-22, 10 figures, 4 tables, references
<”Using results from CTD cruises acquired by the
Faroese Fisheries Laboratory since the early eight-
ies, we discuss temporal variations of the tempera-
ture in the overflow water.” Quoted from abstract>
335: Hansen, B./Østerhus, S.: North Atlantic
- Nordic Seas exchanges
in: Progress in Oceanography, vol. 45, 2000,
no. 2, pp. 109-208, 59 ftgures, 4 tables, biblio-
graphy (pp. 199-208)
<”In this paper, the state of the knowledge on the
exchanges expecially across the eastern part of the
Greenland-Scotland Ridge is reviewed based on
results from the ICES Nansen [...] project, from the
Nordic WOCE project and other sources”. Quoted
from abstract>
336: Hansen, Bogi/Turrell, William R./
Østerhus, Svein: Decreasing overllow froni
the Nordic Seas into the Atlantic Ocean
through the Faroe Bank channel since 1950
in: Nature, vol. 411, June 21, 2001, no. 6840,
pp. 927-931, 4 figures, references
<”New measurements contbined with historic hydro-
graphic data show that the flow of water from the
depth of the Nordic Seas into the Atlantic Ocean has
decreased by at least 20% since 1950. The implica-
tions of this decrease depend on the behaviour of
other overflow sources. But if not counteracted by
an increased flow from elsewhere, the fall could lead
to a reduced inflow into the deep Atlantic Ocean.
Given that the heat transported by the Atlantic
Ocean circulation gives rise to the exceptionally
mild climate of norlhwestern Europe, the trend could
have profounđ implications for European climate if
it continues.” Quoted from above paper. The above
topic was attended to in several newspaper articles,
cf. e.g. ”As the world gets hotter, will Britain get
colder? Plunging lemperatures feared after scicntists
fmd Gulf stream changes” by Tim Radford, in: The
Guardian, Manchester, June 21, 2001, p. 3; ”Cold
Water Flow From Arctic to Atlantic is Falling, Study
Finds” by Andrew C. Revkin, in: The New York
Times, June 21, 2001, section A, p. 5; ”As North
Atlantic current slows, concern rises” by Peter N.
Spotts, in: The Christian Science Monitor, June 21,
2001, p. 15; "Globalski warming; How greenhouse
effect will bring Russian-style winters to Britain”
by Stephen White, in: The Mirror, London, June 22,
2001, p. 23; "Outlook chilly as climate changes” by
James Freeman, in: The Herald, Glasgow, June 21,
2001, p. 11>