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1.
Tad Murty 《Marine Geodesy》2013,36(1):85-87
Oceanography, Units 1–16 edited by J. Stewart (Open University Press, 1977), 755 pp. The Thermohaline Fine Structure of the Ocean by K. N. Fedorov (New York: Pergamon Press, Pergamon Marine Series. Volume 2, 1978). Translated from Russian by D. A. Brown, Technical Editor: J. S. Turner, 170 pp., no price listed. The Ocean Basins and Margins edited by Alan E. M. Nairn and Francis G. Stehli, with William H. Kanes (New York: Plenum Press, Vol. 1–4A, 4B, 1973, 1979, 1975, 1977, and 1978) approx. 3,000 pp. Recent Crustal Movements, 1977 edited by C.A. Whitten, R. Green, and B.K. Meade (New York: Elsevier Scientific Publishing Co., 1979), 663 pp., hardcover, $78.00. The Alaskan Shelf‐Hydrographic, Sedimentary, and Geotechnical Environment by Ghanshyam Datt Sharma (New York: Springer Verlag, 1979), 498 pp., hardcover, $29.80. 相似文献
2.
Z. J. Slouka 《Marine Georesources & Geotechnology》2013,31(1):69-70
The Control of the Sea‐bed: A New International Issue by Evan Luard. Taplinger Publishing Co., Inc., New York, 1974. 309 pp. $14.95. 相似文献
3.
Wolfgang Torge. Gravimetry. New York: Walter de Gruyter, 1989. 465 pp. U.S. $94.95. W. H. Berger, V. S. Smetacek, and G. Wefer (eds.). Productivity of the Ocean: Present and Past. Chichester: John Wiley and Sons, 1989. 471 pp. Hardcover. U.S. $146.00. 相似文献
4.
A Re-Evaluation of the Offset in the Australian Height Datum Between Mainland Australia and Tasmania
Applications of Marine Geodesy in Support of National Objectives in Ocean Science, Engineering and Operations a study prepared for the Marine Technology Society, by Narendra Saxena, College of Engineering, University of Hawaii, 1980, 176 pages. Plate Tectonics and Crustal Evolution by K.E. Condie (New York: Pergamon Press, 1979), 288 pages, $35.00. Bottom‐Interacting Ocean Accoustics by W.A. Kuperman and F.B. Jensen (eds.). NATO Conference Series, Series IV: Marine Sciences, Volume 5 (New York: Plenum Press, 1980), 717 pages, hardcover, U.S. $75.00. 相似文献
5.
Terence J. Hirst 《Marine Georesources & Geotechnology》2013,31(4):371-373
Ocean Floor Mining by John S. Pearson. Noyes Data Corporation, Park Ridge, New Jersey, 1975. 201 pp., $24.00. Offshore Drilling Technology by Frank R. Carmichael. Noyes Data Corporation, Park Ridge, New Jersey, 1975. 392 pp., $36.00. 相似文献
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Mechanics of Sediment Transport. Edited by B. Mutlu Sumer and A. Muller. Proceedings of Euromech 156, Istanbul, 12–14 July 1982. Rotterdam: A. A. Balkema, 1983. 285 pp. $45.00. Gear Drive Systems: Design and Application, Peter Lynwander, New York and Basel: Marcel Dekker, Inc., 1983. Price: $49.50. 相似文献
8.
Offshore Soil Mechanics edited by Philip George and David Wood. Cambridge University Engineering Department and Lloyd's Register of Shipping, London, 1976. 468 pp. £7.50 + shipping. Beach Processes and Sedimentation by Paul D. Komar. Prentice‐Hall, Inc. Englewood Cliffs, New Jersey, 1976. 429 pp., $26.95. 相似文献
9.
R. H. Bennett, W. R. Bryant, and M. H. Hulbert, Eds. 1991. Microstructure ofFine‐Grained Sediments—from Shale to Mud. New York: Springer‐Verlag. 582 pp. $98.00. 相似文献
10.
Scott E. Drummond Jr. 《Marine Geodesy》2013,36(2):143-144
Electronic Surveying and Navigation by Simon H. Laurila (New York: John Wiley &; Sons, 1976), 545 pages, hardcover, $25.00. 相似文献
11.
Rongxing Li 《Marine Geodesy》2013,36(1):57-59
J. Albertz. Grundlagen der Interpretation von Luft‐und Satellitenbildern: eine Einfuhrung in die Fernerkundung (Fundamentals of Interpretation of Aerial and Satellite Images: An Introduction to Remote Sensing). Darmstadt: Wissenschaftliche Buchgesellschaft, 1991. 204 pp. Hardcover. U.S. $40.00–45.00. ISBN 3–534–07838–1. International Symposium on Marine Positioning Proceedings, “Marine Positioning into the 1990's.” Marine Geodesy Committee/MTS, 1991. 594 pp. Hardcover. U.S. $139.00. ISBN 91–060360. 相似文献
12.
This paper deals with an application of Clough and Penzien's suggestion [(1975), Dynamics of Structures, pp. 549–550. McGraw-Hill, New York] for improving the results obtained by means of the Rayleigh-Ritz method when dealing with forced vibrations problems. Viscous damping is taken into account. 相似文献
13.
《Deep Sea Research Part I: Oceanographic Research Papers》2006,53(4):689-712
Biogeochemical processes in the sea are triggered in various ways by chlorophyll-containing phytoplankton groups. While the variability of chlorophyll concentration at sea has been observed from satellites for several years, these groups are known only from cruises which are limited in space and time. The Geochemistry, Phytoplankton and Color of the Ocean programme (GeP&CO) was set up to describe and understand the variability of phytoplankton composition on large spatial scales under a multi-year sampling strategy. It was based on sea-surface sampling along the route of the merchant ship Contship London which travelled four times a year from Le Havre (France) to Nouméa (New Caledonia) via New York, Panama and Auckland. Observations included the measurement of photosynthetic pigments, counts of picoplanktonic cells by flow cytometry (Prochlorococcus, Synechococcus, and picoeucaryotes) and counting and identification of coccolithophores. The results confirmed that tropical areas have low seasonal variability and are characterized by relatively high divinyl-chlorophyll a and zeaxanthin concentration and that the variability is strongest at high latitudes where the phytoplankton biomass and population structure are found to have large seasonal cycles. Thus, the spring bloom in the North Atlantic and an austral winter bloom north of New Zealand are marked by chlorophyll concentrations which are often higher than 0.5 μg l−1 and by high concentration of fucoxanthin (a pigment used as an indicator for diatoms), while summer populations are dominated by Prochlorococcus sp. and have low chlorophyll concentrations. Apart from this yearly bloom at temperate latitudes, fucoxanthin is scarce, except in the equatorial upwelling zone in the eastern Pacific Ocean, where it is found in moderate amounts. In this region, relatively high chlorophyll concentrations extend generally as far as 14°S and do not respond to the seasonal strengthening of the equatorial upwelling during the austral winter. Prochlorococcus, which is known to dominate in oligotrophic tropical seas and to disappear in cold conditions, in fact has its minimum during the spring bloom in the North Atlantic, rather than during the winter. Coccolithophores are ubiquitous, showing a succession of species in response to oceanic conditions and provinces. 19′Hexanoyloxyfucoxanthin, the pigment generally considered as an indicator of coccolithophores, is relatively abundant at all times and in all regions, but its abundance is generally not tightly correlated with that of coccolithophores. The regional differences revealed by these results are in overall agreement with Longhurst's division of the ocean into ecological provinces. 相似文献
14.
Identification of Seismic Sources—Earthquake or Underground Explosion Proceedings of the NATO Advanced Study Institute held at Voksenåsen, Oslo, Norway, September 8–18, 1980, edited by E. S. Husebye and S. Mykkeltveit. (Dordrecht, The Netherlands: D. Reidel Publishing Company, published in cooperation with NATO Scientific Affairs Division, NATO Advanced Study Institute, Series C, Vol. 74, 1981), 876 p. Current Research in Earthquake Prediction I edited by T. Rikitake, Report No. 2, Developments in Earth and Planetary Sciences, Centre for Academic Publications, Tokyo, (Dordrecht, The Netherlands: D. Reidel Publishing Company, 1981), 383 p. Air‐Sea Interaction: Instruments and Methods edited by F. Dobson, L. Hasse, and R. Davis. (New York: Plenum Press, 1980), 692 p. Structure of Transition Zone edited by S. Asano. Published by Center for Academic Publications Japan, Tokyo. (Dordrecht, The Netherlands: D. Reidel Publishing Company. 1980. The Sea Floor: An Introduction to Marine Geology by E. Seibold and W. H. Berger (Berlin: Springer‐Verlag, 1982), 288 p. $20.00. Reference Coordinate Systems for Earth Dynamics Proceedings of the 56th Colloquium of the International Astronomical Union held in Warsaw, Poland, September 8–12, 1980, edited by E. M. Gaposchkin, Smithsonian Astrophysical Observatory, Cambridge, MA, U.S.A., and B. Kolaczek, Polish Academy of Sciences, Warsaw, Poland (D. Reidel Publishing Company Dordrecht, the Netherlands/Boston, U.S.A./London, England, 1981) 414 p. hard cover. The Geomorphology of the Great Barrier Reef by David Hopley (New York; John Wiley &; Sons, 1982) $59.95. 相似文献
15.
Alan N. Baker 《新西兰海洋与淡水研究杂志》2013,47(2):401-406
A cranium of Phocoena dioptrica Lahille, 1912, collected at Enderby Island, Auckland Islands, represents the first discovery of the species in the Pacific Ocean, the ten previous records being all from the south‐western. Atlantic. The species may thus have a circumpolar distribution in subantarctic latitudes. A list of six small cetacean species now known from New Zealand's subantarctic region is appended. 相似文献
16.
At interannual to multidecadal time scales, much of the oceanographic and climatic variability in the North Atlantic Ocean can be associated with the North Atlantic Oscillation (NAO). While evidence suggests that there is a relationship between the NAO and zooplankton dynamics in the North Atlantic Ocean, the phytoplankton response to NAO-induced changes in the environment is less clear. Time series of monthly mean phytoplankton colour values, as compiled by the Continuous Plankton Recorder (CPR) survey, are analysed to infer relationships between the NAO and phytoplankton dynamics throughout the North Atlantic Ocean. While a few areas display highly significant (p < 0.05) trends in the CPR colour time series during the period 1948–2000, nominally significant (p < 0.20) positive trends are widespread across the basin, particularly on the continental shelves and in a transition zone stretching across the Central North Atlantic. When long-term trends are removed from both the NAO index and CPR colour time series, the correlation between them ceases to be significant. Several hypotheses are proposed to explain the observed variability in the CPR colour and its relationship with climate in the North Atlantic. 相似文献
17.
The whale‐louse Scutocyamus antipodensis n.sp., ectoparasitic on Hector's dolphin, Cephalorhynchus hectori (van Beneden), is described and figured from material collected in Cloudy Bay, Cook Strait, New Zealand. Morphologically the new species is very close to S. parvus Lincoln & Hurley, the type and only other species of the genus, known only from the North Sea. However, the two species differ in the detailed structure and spinosity of the body and pereopods. 相似文献
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19.
Ronald C. Chaney Marnie D. Chapman William Miller III 《Marine Georesources & Geotechnology》2013,31(3):333-339
Geotechnical Aspects of Coastal and Offshore Structures. Edited by Yudhair and A. S. Balasubramaniam. Proceedings of the Symposium on Geotechnical Aspects of Coastal and Offshore Structures, Bangkok, December 14–18,1981. Rotterdam: A. A. Balkema, 1983. 280 pp. $40.00. The Seaside Naturalist: A Guide to Nature Study at the Seashore. Written and illustrated by D. A. Coulombe. Englewood Cliffs, N.J.: Prentice‐Hall, Inc., 1984. 246 pp. $12.95. Ichnology, Trace Fossils in Sedimentology and Stratigraphy. By A. A. Ekdale, R. G. Bromley, and S. G. Pemberton. Society of Economic Paleontologists and Mineralogists, Short Course No. 15. Tulsa, Okla.: S.E.P.M., 1984. 317 pp. S.E.P.M. members, $16.00; non‐members, $20.00. 相似文献
20.
C. H. Greene A. J. Pershing A. Conversi B. Planque C. Hannah D. Sameoto E. Head P. C. Smith P. C. Reid J. Jossi D. Mountain M. C. Benfield P. H. Wiebe E. Durbin 《Progress in Oceanography》2003,58(2-4):301
Populations of the copepod species Calanus finmarchicus often dominate the springtime biomass and secondary production of shelf ecosystems throughout the North Atlantic Ocean. Recently, it has been hypothesised that interannual to interdecadal fluctuations observed in such populations are driven primarily by climate-associated changes in ocean circulation. Here, we compare evidence from the North Sea and Gulf of Maine/Western Scotian Shelf (GoM/WSS) linking fluctuations in C. finmarchicus abundance to changes in ocean circulation associated with the North Atlantic Oscillation (NAO). A particularly striking contrast emerges from this Trans-Atlantic comparison: whereas the North Sea C. finmarchicus population exhibits a negative correlation with the NAO index, the GoM/WSS population exhibits a more complex, positive association with the index. The physical processes underlying these contrasting population responses are discussed in the context of regional- to basin-scale circulation changes associated with the NAO. 相似文献