Open WL Archief (OWA)

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Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.

Dit archief wordt uitgebouwd en beheerd volgens de principes van de Open Access Movement, en het daaruit ontstane Open Archives Initiative.

Basisinformatie over ‘Open Access to scholarly information'.

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one publication added to basket [7221]

The movements of sea-bed and sea-surface drifters in the Irish Sea, 1965-1967 Harvey, J. (1968). The movements of sea-bed and sea-surface drifters in the Irish Sea, 1965-1967. Sarsia 34(1): 227-242. https://dx.doi.org/10.1080/00364827.1968.10413385 In: Sarsia. University of Bergen. Universitetsforlaget: Bergen. ISSN 0036-4827; e-ISSN 1503-1128, meer Ook verschenen in: Brattström, H.; Matthews, J.B.L. (Ed.) (1968). The Importance of Water Movements for Biology and Distribution of Marine Organisms: 2nd European Symposium on Marine Biology, Bergen 24-28 August 1967. European Marine Biology Symposia, 2. Sarsia, 34. 398 pp., meer

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Beschikbaar in	Auteur
VLIZ: Non-open access 148666 [ aanvragen ]

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Trefwoorden

Aquatic organisms > Marine organisms > Aquatic birds > Marine birds Drift Ocean floor Stranding Surfaces > Sea surface ANE, Ierse Zee [Marine Regions] Marien/Kust

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Auteur		Top
Harvey, J.

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Abstract

500 sea-bed and 500 sea-surface drifters were released in the Irish Sea on each of four occasions. The overall mean return rate of each type of drifter was about 34% within six months of release. Marked differences were found between the movements of sea-surface drifters released on different occasions, whereas there were some similarities in the movements of sea-bed drifters released on different occasions. The movements of the different types of drifters were generally unrelated. The movements of the sea-surface drifters were shown to be closely related to the wind, and the wind factor, k, was estimated to lie between 1.5% and 2.0%. Attention was drawn to the marked vertical shear in residual currents in the Irish Sea indicated by the drifter movements.

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