Ægir - 01.07.1981, Qupperneq 32

14. mynd W.H. Athuganir fyrir Suðausturlandi. Hér á eftir
verða sýnda niðurstöður frá athugunarstöðum 7-19.
International (ICES) „Overflow“ Expedition,
May-June 1960. Rapp. proc. Verb. Reun. 157.
4) Alþjóðahafrannsóknaráðið 1981. ICES Expedition
Overflow’73 Contributions. ICES WG. on Oceanic
Hydrography.
5) Thomas J. Miiller, Jens Meincke, Gerd A. Becker
1979. Overflow’73. The Distribution of Water
Masses on the Greenland-Scotland Ridge in
August-September 1973. A Data Rep. Ber. Inst.
Meeresk. Chr. Albr. Univ. Kiel.
6) Frede Hermann 1967. The TS-Diagrams Analysis of
the water masses over the Iceland-Faroe Ridge and
in the Faroe Bank Channel. Rapp. Proc. Verb.
Reun. 157.
7) Unnsteinn Stefánsson 1961. North Icelandic Wat-
ers. Rit Fiskideildar 3.
8) Unnsteinn Stefánsson 1969. Hafstraumar og sjó-
gerðir í Norður-íshafi, Norður-Grænlandshafi og
íslandshafi. Hafísinn. Ritstj.: Markús Á. Einars-
son. Rv. Alm. bókafél.
"WflLTHER HERWIG’, I
14.-16.RUG.1973
STRT.NO.7-19
15. mynd W.H. TS-línurit á st. 7-19. Hér eru margar sjógerðir,
heitar og kaldar. Sniðið liggur yfir hrygginn um ,,Rennuna“
fyrir Suðausturlandi.
9) Gúnther Dietrich 1957. Schichtung und Zirkulation
der Irminger-See im Juni 1955. Ber. Dtsch. Wiss.
Komm. Meeresf. 14,4.
10) Unnsteinn Stefánsson 1968. Dissolved nutrients,
oxygen and water masses in the northern Irminger
Sea. Deep Sea Res. 15.
11) Svend-Aage Malmberg 1974. A note on the deep
water south of Iceland. — ,,Overflow’73“. ICES
CM 1974/C:32.
12) Jens Meincke 1978. On the Distribution of low
Salinity Intermediate Waters around the Faroes.
Dtsch. Hydr. Zeitschr. 31.
13) Bogi Hansen, Jens Meincke 1979. Eddies and
Meanders in the Iceland-Faroe Ridge area. Deep
Sea Res. 26,9A.
14) Sveinn Sveinbjörnsson 1981. Um kolmunna og kol-
munnaveiðar, Ægir 74 (4).
English summary:
The sea and fishing grounds around Iceland
III Water masses between Iceland and the Faroe Islands
This paper (1,2) deals with water masses in the area between
Iceland and the Faroe Islands (Table 1). The paper is based on a
work done by Thomas J. Múller et al. (5) on the distribution of
water masses during the Overflow’73 investigations on the
384 — ÆGIR