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By Arnold L. Gordon, F. W. G. Baker

Annals of the overseas Geophysical yr, quantity forty six: Oceanography covers this system of oceanographic reviews carried out throughout the overseas Geophysical yr (IGY). this system contains lengthy wave and sea point recording, deep water stream, polar entrance survey, and multipleship present size.
This booklet consists of six chapters and starts with the target and goals of the oceanographic application and the nationwide contributions to this application. The succeeding chapters talk about the matter in delineating sea-level cycle and the result of the North Atlantic Polar entrance Survey within the IGY. those themes are via a survey of the implications from many oceanographical expeditions. quite solid effects have been acquired in the course of the IGY interval via unique large-scale precision automated recorders of the phototelegraph station sort. The final bankruptcy describes the synthetic radioactivity within the oceans consisting more often than not of fission items of U235, Pu239 and U238 from reactors and nuclear explosion units.
This publication is of price to geophysicists, and marine scientists and researchers.

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1951. Climatic implications of glacier research. Compendium of Meteorology, American Meteoro­ logical Society. GUTENBERG, B. 1941. Changes in sea level, postglacial uplift, and mobility on the Earth's interior. Bull. Geol. Soc. America, 52. HARRIS, D. L. and LINDSAY, C. V. 1957. An index of tide gauges and tide-gauge records for the Atlantic and Gulf Coasts of the United States. National Hurricane Research Project Report No. 7. HELA, I. 1944. Über die Schwankungen des Wasserstandes in der Ostsee.

ISELIN, C. O. D. 1940. Preliminary report on long-period variations in the transport of the Gulf Stream system. Pap. Phys. Oceanogr. Meteor. 8. KÄÄRIÄINEN, E. 1953. On the recent uplift of the Earth's crust in Finland. Fennia, 77, 2. KUENEN, Ph. H. 1950. Marine Geology. New York. KUKKAMAKI, T. J.

E. Hydrographie levelling. F. The study of long-term changes in the mean sea-level height. G. The study of deviations between the geoid and "the surface determined by the local mean sea-level heights". H. Possibly, a few other special problems. This article deals with the problem of the mean sea level. Its main purpose is to give an account of the differences between the geoid and the surface determined by the heights of the local mean sea level. The normal practice, when determining the local mean sea level at tide gauges or poles is simply to take the arithmetic means, or average, of all the tidal heights recorded at regular intervals over a given period of time, usually one year or longer.

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