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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
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Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 1 to 10 of 17 (0.078 seconds)Spelling suggestions: "subject:"eea ice drift."" "subject:"area ice drift.""
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An evaluation of hot-film anemometry for Reynolds stress measurements under sea ice.Koutitonsky, Vladimir G. January 1973 (has links)
No description available.
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| 2 |
Arctic sea ice dynamics : drifts and ridging in numerical models and observations = Arktische Meereisdynamik : Drift und Presseisrückenbildung in numerischen Modellen und Beobachtungsdaten /Martin, Torge. January 2007 (has links)
Univ., Diss.--Bremen, 2007.
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| 3 |
Drifter observations in the Northeast PacificUkita, Jinro January 1987 (has links)
From the position data of 23 drifters over the four years period, 1982 to 1985, the upper layer kinematics of the Northeast Pacific were investigated. The focus of this study was upon the topographic influence, wind forcing, and Rossby waves. The notions of homogeneity and stationarity were applied to both the Eulerian and Lagrangian analysis. A new computational scheme was proposed and tested in order to explicitly take into account the Lagrangian characteristics of the drifter data. The Eulerian analysis showed that the spatial and temporal distributions of the mean current and the mean wind stress were in good agreement. Three of the four eddy kinetic energy maxima found in the region geographically corresponded to topographic features. Also the velocity field of this region appeared to be strongly inhomogeneous, non-stationary, and anisotropic. The results from the Lagrangian analysis showed that the spectral slope for the periods shorter than 5 days followed the -2 law, and suggested that the direct wind forcing was a dominant mechanism for those periods. The spectrum of the eddy component of the velocity appeared to be white for the periods longer than 10 days. The results showed that the linear Rossby waves were not dominant mechanism for upper layer dynamics of this region. The rotary spectra illustrated some evidence of the rotational preference of the cyclonic over anti-cyclonic motions at a period of 10 days. The new scheme provided meaningful information about the eddy component of the velocity. / Science, Faculty of / Earth, Ocean and Atmospheric Sciences, Department of / Graduate
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| 4 |
An evaluation of hot-film anemometry for Reynolds stress measurements under sea ice.Koutitonsky, Vladimir G. January 1973 (has links)
No description available.
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| 5 |
Internal stress in a floating cover of sea iceWright, B. D. January 1974 (has links)
No description available.
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| 6 |
Internal stress in a floating cover of sea iceWright, B. D. January 1974 (has links)
No description available.
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| 7 |
Ice drift in the Gulf of St. Lawrence.Ingram, Richard Grant, 1945- January 1967 (has links)
No description available.
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A thermodynamic and dynamic Lagrangian model for icebergs a data-model intercomparison for the Southern Ocean /Abrahamowicz, Maria. January 1900 (has links)
Thesis (M.Sc.). / Written for the Dept. of Atmospheric and Oceanic Sciences. Title from title page of PDF (viewed 2008/05/13). Includes bibliographical references.
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| 9 |
Ice drift in the Gulf of St. Lawrence.Ingram, Richard Grant, 1945- January 1967 (has links)
No description available.
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| 10 |
Observations on ice movement in the gulf of St. LawrenceFarmer, David M. January 1969 (has links)
No description available.
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