Water regime of Disraeli Fiord, Ellesmere Island / by John E. Keys. : DR52-17/27-1978E-PDF

"The mouth of Disraeli Fiord in northern Ellesmere Island is dammed by the Ward Hunt Ice Shelf from the surface to a depth of 44 metres. The fiord contains virtually fresh water to this depth, overlying cold salt water. A perennial ice cover precludes any wind induced mixing. Fresh water enters the fiord in the form of melt streams which flow down to the pycnocline. This water flows out beneath the shelf, carrying some of the underlying salt water with it. Heat flows downward across the pycnocline causing formation of frazil ice in the lower part of the fresh layer. This ice floats up to adhere to the fiord ice. Salt water flowing out under the ice shelf is replaced by water of Atlantic origin entering at the bottom"--Abstract, page iii.

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Renseignements sur la publication
Ministère/Organisme Defence Research Establishment Ottawa, issuing body.
Canada. Department of National Defence. Research and Development Branch, issuing body.
Titre Water regime of Disraeli Fiord, Ellesmere Island / by John E. Keys.
Titre de la série DREO report ; no. 792
Type de publication Série - Voir l'enregistrement principal
Langue [Anglais]
Format Électronique
Document électronique
Note(s) "Unclassified."
"Project no. 97-67-05."
Digitized edition from print [produced by Defence Research and Development Canada].
Includes bibliographical references (pages 56-58).
Includes abstracts in English and French.
Information sur la publication Ottawa : Defence Research Establishment Ottawa, December 1978.
Auteur / Contributeur Keys, John E., author.
Description 1 online resource (vii, 58 pages, 2 unnumbered pages) : illustrations, maps, graphs, photographs.
Numéro de catalogue
  • DR52-17/27-1978E-PDF
Descripteurs Hydrographic surveying -- Nunavut -- Ellesmere Island.
Fjords -- Nunavut -- Ellesmere Island.
Levés hydrographiques -- Nunavut -- Ellesmere, Île d'.
Fjords -- Nunavut -- Ellesmere, Île d'.
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