Zobrazeno 1 - 8
of 8
pro vyhledávání: '"V. F. C. Veley"'
Publikováno v:
Journal of the Marine Biological Association of the United Kingdom. 29:587-608
A review is given of the results obtained from upwards of 600 days of current measuring at the Seven Stones lightvessel during 1939–41. From the plotted observations, an attempt is made to deduce the association between the total daily water moveme
Publikováno v:
Deutsche Hydrographische Zeitschrift. 3:277-286
Water and wind movements, computed from daily observations at two light vessels in the English Channel and the North Sea, are shown graphically and discussed. In the case of the “Royal Sovereign” light vessel (English Channel), the angle between
Publikováno v:
Journal of the Marine Biological Association of the United Kingdom. 39:659-665
Measurements of current at the Seven Stones Light Vessel, 50° 03·5' N. lat., 6° 05·1' W. long. (for position, see Cooper, 1960b, fig. 1) were first made with the Carruthers Drift Indicator between 17 August and 15 September 1933 (Carruthers, 1934
Publikováno v:
ICES Journal of Marine Science. 18:354-358
Publikováno v:
Nature. 168:317-319
Autor:
V. F. C. Veley, A. L. Lawford
Publikováno v:
Nature. 167:684-684
THE article by R. I. B. Cooper1 describes, interalia, an investigation made by us to determine the effect of change in the ocean's moment of inertia, due to seasonal changes in sea-level, upon the periodic fluctuation in the length of the day.
Publikováno v:
Transactions, American Geophysical Union. 38:584
It seems fortunate that two papers concerning the relationship between wind velocity and movement of the surface water appeared in the same issue. Since both papers show apparently different results, it seems necessary to point out difference in the
Autor:
A. L. Lawford, V. F. C. Veley
Publikováno v:
Transactions, American Geophysical Union. 37:691
Analysis of continuous current measurements aboard four light vessels in the southern North Sea suggests that while the expression connecting wind and surface water movements is linear up to winds of about Beaufort 3, above this strength it appears t