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Record #153368:

Hydrographic observations in Denmark Strait on the VEINS expedition in August-September 1997. Technical report / Bert Rudels, Patrick Eriksson, Hannu Grönvall, Riikka Hietala, Jouko Launiainen, Tero Purokoski.

Title: Hydrographic observations in Denmark Strait on the VEINS expedition in August-September 1997. Technical report / Bert Rudels, Patrick Eriksson, Hannu Grönvall, Riikka Hietala, Jouko Launiainen, Tero Purokoski.
Author(s): Rudels, Bert.
Eriksson, Patrick.
Grönvall, Hannu.
Hietala, Riikka.
Launiainen, Jouko.
Purokoski, Tero.
Date: 1999.
In: Meri. (1999.), Vol. 39 (1999)
Abstract: Observations were taken from RV Aranda. They indicate that densest waters crossing 610 m deep sill are mainly drawn from intermediate waters of East Greenland Current. Overflow plume is stratified and capped by less saline layer as it sinks to 2000 m. Entrainment of ambient water is small and downstream evolution of plume is due to mixing within it of initial overflow. Low-salinity, dense water of current flowing southward over shelf further west may cross shelf break south of sill and sink down slope, adding less dense fraction to Deep Northern Boundary Current.
Notes:

Meri. Vol. 39 :1-57 (1999).

Keywords: 551.46.06 -- Oceanography, observational data.
551.465 -- Oceanography, dynamics.
551.465.4 -- Oceanography, stratification.
551.465.5 -- Ocean currents.
C -- Oceanography, hydrography and hydrology.
(*3) -- Arctic regions.
(*61) -- North Atlantic Ocean.
(*614) -- Greenland waters.
(*616) -- Iceland waters.
SPRI record no.: 153368

MARCXML

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008 220926s1999####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-153368
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245 00 ‡aHydrographic observations in Denmark Strait on the VEINS expedition in August-September 1997. Technical report /‡cBert Rudels, Patrick Eriksson, Hannu Grönvall, Riikka Hietala, Jouko Launiainen, Tero Purokoski.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 1-57 :‡bdiags., tables, maps.
500 ## ‡aMeri. Vol. 39 :1-57 (1999).
520 3# ‡aObservations were taken from RV Aranda. They indicate that densest waters crossing 610 m deep sill are mainly drawn from intermediate waters of East Greenland Current. Overflow plume is stratified and capped by less saline layer as it sinks to 2000 m. Entrainment of ambient water is small and downstream evolution of plume is due to mixing within it of initial overflow. Low-salinity, dense water of current flowing southward over shelf further west may cross shelf break south of sill and sink down slope, adding less dense fraction to Deep Northern Boundary Current.
650 07 ‡a551.46.06 -- Oceanography, observational data.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.4 -- Oceanography, stratification.‡2udc
650 07 ‡a551.465.5 -- Ocean currents.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc
651 #7 ‡a(*614) -- Greenland waters.‡2udc
651 #7 ‡a(*616) -- Iceland waters.‡2udc
700 1# ‡aRudels, Bert.
700 1# ‡aEriksson, Patrick.
700 1# ‡aGrönvall, Hannu.
700 1# ‡aHietala, Riikka.
700 1# ‡aLauniainen, Jouko.
700 1# ‡aPurokoski, Tero.
773 0# ‡7nnas ‡tMeri. ‡gVol. 39 (1999) ‡wSPRI-140453
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220926