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  • English  (1,156)
  • 1960-1964  (1,117)
  • 1945-1949  (41)
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  • 1
    Keywords: DDC 515/.37 ; LC QA372
    Pages: Online-Ressource (viii, 134 pages)
    ISBN: 9780124370562
    Language: English
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  • 2
    Unknown
    New York : Academic Press
    Keywords: DDC 515/.353 ; LC QA373
    Pages: Online-Ressource (viii, 186 pages)
    ISBN: 9780126962505
    Language: English
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  • 3
    Keywords: DDC 515/.353 ; LC QA373
    Pages: Online-Ressource (vi, 369 pages)
    ISBN: 9780123749178
    Language: English
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  • 4
    Unknown
    New York : Academic Press
    Keywords: DDC 515/.353 ; LC QA373
    Pages: Online-Ressource (x, 203 pages)
    ISBN: 9780122596506
    Language: English
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  • 5
    Unknown
    New York : Academic Press
    Keywords: DDC 515/.353 ; LC QA373
    Pages: Online-Ressource (viii, 457pages)
    ISBN: 9780125894500
    Language: English
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  • 6
    Unknown
    Amsterdam : North-Holland Pub. Co
    Keywords: DDC 510/.01 ; LC QA9
    Pages: Online-Ressource (xix, 183 pages)
    ISBN: 9780444534019
    Language: English
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  • 7
    Unknown
    New York : Academic Press
    Keywords: DDC 512.8 ; LC QA3
    Pages: Online-Ressource (v, 385 pages)
    ISBN: 9780123480507
    Language: English
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  • 8
    Unknown
    New York : Academic Press
    Keywords: DDC 515/.353 ; LC QA373 ; Differential-difference equations
    Pages: Online-Ressource (xvi, 462 pages)
    ISBN: 9780080955148
    Language: English
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  • 9
    Unknown
    New York : Academic Press
    Keywords: DDC 526.8 ; LC QA3 ; Curvature ; Homology theory ; Riemann surfaces
    Pages: Online-Ressource (315 pages)
    ISBN: 9780123745620
    Language: English
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  • 10
    Description / Table of Contents: Part 1: Introduction --- Frederick Henry Stewart: Arthur Holmes / Geological Society, London, Special Publications, 1:1-11, doi:10.1144/GSL.SP.1964.001.01.03 --- L. R. Wager: The history of attempts to establish a quantitative time-scale / Geological Society, London, Special Publications, 1:13-28, doi:10.1144/GSL.SP.1964.001.01.04 --- N. J. Snelling: A review of recent Phanerozoic time-scales / Geological Society, London, Special Publications, 1:29-36, doi:10.1144/GSL.SP.1964.001.01.05 --- J. D. Hudson: Sedimentation rates in relation to the Phanerozoic time-scale / Geological Society, London, Special Publications, 1:37-42, doi:10.1144/GSL.SP.1964.001.01.06 --- R. St J. Lambert: The relationship between radiometric ages obtained from plutonic complexes and stratigraphical time / Geological Society, London, Special Publications, 1:43-54, doi:10.1144/GSL.SP.1964.001.01.07 --- F. J. Fitch and J. A. Miller: The geological significance of radiometric age studies on volcanic and hypabyssal rocks / Geological Society, London, Special Publications, 1:55-69, doi:10.1144/GSL.SP.1964.001.01.08 --- Part 2: Radiometric Methods with Respect to the Time-Scale --- A. G. Darnley: Uranium–thorium–lead age-determinations with respect to the phanerozoic time-scale / Geological Society, London, Special Publications, 1:73-86, doi:10.1144/GSL.SP.1964.001.01.09 --- Stephen Moorbath: The rubidium–strontium method / Geological Society, London, Special Publications, 1:87-99, doi:10.1144/GSL.SP.1964.001.01.10 --- John Alfred Miller and Frank John Fitch: Potassium—argon methods with special reference to basic igneous rocks / Geological Society, London, Special Publications, 1:101-117, doi:10.1144/GSL.SP.1964.001.01.11 --- Halfdan Baadsgaard and Martin Henry Dodson: Potassium—argon ages of sedimentary and pyroclastic rocks / Geological Society, London, Special Publications, 1:119-127, doi:10.1144/GSL.SP.1964.001.01.12 --- Alan Gilbert Smith: Potassium—argon decay constants and age tables / Geological Society, London, Special Publications, 1:129-141, doi:10.1144/GSL.SP.1964.001.01.13 --- Part 3: Original Data --- Martin Henry Dodson , David Charles Rex , Raymond Casey, and Percival Allen: Glauconite dates from the Upper Jurassic and Lower Cretaceous / Geological Society, London, Special Publications, 1:145-158, doi:10.1144/GSL.SP.1964.001.01.14 --- Frank Joseph Fitch and John Alfred Miller: The age of the paroxysmal Variscan orogeny in England / Geological Society, London, Special Publications, 1:159-175, doi:10.1144/GSL.SP.1964.001.01.15 --- Part 4: Stratigraphical Review --- Brian Michael Funnell: The Tertiary period / Geological Society, London, Special Publications, 1:179-191, doi:10.1144/GSL.SP.1964.001.01.16 --- Raymond Casey: The Cretaceous period / Geological Society, London, Special Publications, 1:193-202, doi:10.1144/GSL.SP.1964.001.01.17 --- Michael Kingsley Howarth: The Jurassic period / Geological Society, London, Special Publications, 1:203-205, doi:10.1144/GSL.SP.1964.001.01.18 --- Edward Timothy Tozer: The Triassic period / Geological Society, London, Special Publications, 1:207-209, doi:10.1144/GSL.SP.1964.001.01.19 --- Denys Barker Smith: The Permian period / Geological Society, London, Special Publications, 1:211-220, doi:10.1144/GSL.SP.1964.001.01.20 --- Edward Howel Francis and Austin William Woodland: The Carboniferous period / Geological Society, London, Special Publications, 1:221-232, doi:10.1144/GSL.SP.1964.001.01.21 --- Peter Furneaux Friend and Michael Robert House: The Devonian period / Geological Society, London, Special Publications, 1:233-236, doi:10.1144/GSL.SP.1964.001.01.22 --- I. Strachan: The Silurian period / Geological Society, London, Special Publications, 1:237-240, doi:10.1144/GSL.SP.1964.001.01.23 --- H. B. Whittington and A. Williams: The Ordovician period / Geological Society, London, Special Publications, 1:241-254, doi:10.1144/GSL.SP.1964.001.01.24 --- J. W. Cowie: The Cambrian period / Geological Society, London, Special Publications, 1:255-258, doi:10.1144/GSL.SP.1964.001.01.25 --- GENERAL DISCUSSION OF PAPERS IN PART 4S / Geological Society, London, Special Publications, 1:259, doi:10.1144/GSL.SP.1964.001.01.26 --- Summary of the Phanerozoic time-scale: the Geological Society Phanerozoic time-scale 1964 / Geological Society, London, Special Publications, 1:260-262, doi:10.1144/GSL.SP.1964.001.01.27 --- Part 5: Abstracts of Published Radiometric and Stratigraphical Data with Comments --- Introduction / Geological Society, London, Special Publications, 1:265-268, doi:10.1144/GSL.SP.1964.001.01.28 --- Items / Geological Society, London, Special Publications, 1:269-442, doi:10.1144/GSL.SP.1964.001.01.29 --- Erratum --- Errata / Geological Society, London, Special Publications, 1:ERR, doi:10.1144/GSL.SP.1964.001.01.01 --- Errata / Geological Society, London, Special Publications, 1:ERR, doi:10.1144/GSL.SP.1964.001.01.02 --- Corrigenda / Geological Society, London, Special Publications, 1:ERR, doi:10.1144/GSL.SP.1964.001.01.30
    Pages: Online-Ressource (VIII, 458 Seiten) , Illustrationen
    Language: English
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  • 11
    Description / Table of Contents: After previous meetings in Zuerich in 1959 and in Copenhagen in 1960, the Third General Meeting of the International Mineralogical Association was held in Washington, D. C., April 17-20, 1962, sponsored by the Mineralogical Society of America, and supported financially by a generous grant from the National Science Foundation. The scientific program was arranged by D. Jerome Fisher, A. J. Frueh, Jr., and C. E. Tilley, and the sessions were held at the United States National Museum, Smithsonian Institution. The chairmen for each of the three sessions were C. E. Tilley, Symposium on Layered Intrusions (April 18), C. S. Hurlbut, Jr., General Session (April 19), and A. J. Frueh, Jr., Symposium on the Mineralogy of the Sulfides (April 20). These three gentlemen also served as editors of the papers of their sessions. The publication of the papers and proceedings of the Third General Meeting has been made possible by the financial support of the National Science Foundation and is here gratefully acknowledged. The Association is also appreciative of the work of E. Wm. Heinrich, Editor of the American Mineralogist, who served as Co-ordinating Editor of this volume, and of Marjorie Hooker, Treasurer of the Mineralogical Society of America, who administered the National Science Foundation grants in support of the meeting and of this publication.
    Pages: Online-Ressource (VIII, 332 Seiten)
    Language: English
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  • 12
    Unknown
    New York : Academic Press
    Keywords: DDC 517.521 ; LC QA3 ; Topology
    Pages: Online-Ressource (xi, 317 pages)
    ISBN: 9780123745668
    Language: English
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  • 13
    Unknown
    New York : Academic Press
    Keywords: DDC 519.1 ; LC HE369 ; Probabilities ; Queuing theory ; Traffic surveys
    Pages: Online-Ressource (xi, 242 pages)
    ISBN: 9780080955155
    Language: English
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  • 14
    Unknown
    Amsterdam : North-Holland Pub. Co
    Keywords: DDC 510/.01 ; LC QA9
    Pages: Online-Ressource (v, 651 pages)
    ISBN: 9780444533982
    Language: English
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  • 15
    Unknown
    Amsterdam : North-Holland Pub. Co
    Keywords: DDC 510/.01 ; LC QA9
    Pages: Online-Ressource (vi, 100 pages)
    ISBN: 9780444533968
    Language: English
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  • 16
    Unknown
    Amsterdam : North-Holland Pub. Co
    Keywords: DDC 510/.01 ; LC QA9
    Pages: Online-Ressource (iv, 224 pages)
    ISBN: 9780444533937
    Language: English
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  • 17
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Longmans
    Call number: AWI P7-17-90975
    Type of Medium: Monograph available for loan
    Pages: XVI, 328 S. , Ill., Kt., graph. Darst.
    Edition: 1st publ.
    Series Statement: Geographies for advanced study
    Language: English
    Note: Contents: Preface. - 1. Introduction. - 2. History of Arctic exploration. - 3. The meteorology and climate of the Arctic. - 4. Landforms of the Arctic. - 5. The Arctic Seas. - 6. Arctic flora and fauna. - 7. Native peoples. - 8. Transportation. - 9. Political geography of the Arctic. - 10. Regional description of the Canadian Arctic. - 11. Alaska. - 12. The Soviet Arctic. - 13. Svalbard. - 14. Greenland. - 15. The history of Antarctic exploration. - 16. The Antarctic continent. - 17. Meteorology and climate of the Antarctic. - 18. The Antarctic Seas. - 19. The sub-Antarctic islands. - Index.
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  • 18
    Call number: MOP 31266 ; MOP 41304
    In: Meteorologische Abhandlungen
    Type of Medium: Series available for loan
    Pages: 57 S. , graph. Darst., Kt.
    Series Statement: Meteorologische Abhandlungen Bd. 32, H. 4
    Language: English
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 19
    Series available for loan
    Series available for loan
    Golden : Colorado School of Mines
    Associated volumes
    Call number: Z 92.0189(57)
    In: Quarterly of the Colorado School of Mines
    Type of Medium: Series available for loan
    Pages: 111 Seiten , 445 Seiten , 71 Seiten , 171 Seiten , Illustrationen, 1 Karte
    Series Statement: Quarterly of the Colorado School of Mines 57, 1-4
    Language: English
    Location: Lower compact magazine
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  • 20
    Series available for loan
    Series available for loan
    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-53
    In: Research report / Cold Regions Research and Engineering Laboratory, 53
    Description / Table of Contents: Summary: The results of investigations on the structural changes of Greenland snow during age-hardening in the first 49 hr after ejection by a Peter snow miller from a trench 4.7 ft deep are reported, and the method of study is described. The samples of snow were taken at various distances from the trench 1, 3, 14, 25, and 49 hr after deposition, and their changes were studied as a function of time and distance from the trench. The porosity remained constant at an average of 50 ± 3%. The number of grains/cm^2 decreased with time and increased with distance from the trench because of the different speeds of sedimentation and wind sifting. The mean grain cross-section showed a similar dependence. The relative length of grain boundaries increased with time and slightly with distance from the trench, while the mean length of new grain-to-grain boundaries increased with age and decreased with distance from the trench. The mean number of adjacent grains per grain vs. relative length of grain boundaries showed a linear relation. A slight increase of new boundaries with increasing number of neighbors was also observed. Suggestions for a precise study of the age-hardening process of snow are made.
    Type of Medium: Series available for loan
    Pages: v, 15, A5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 53
    Language: English
    Note: CONTENTS Preface Summary Methods of testing Sampling Preparation of samples Preparation of structure pictures Results Influence of time and place Porosity Number of grains/cm2 Mean grain cross section Relative length of grain boundaries (KM ratio) Mean number of adjacent grains per grain Number of new boundaries/cm 2 Mean length of new grain-to-grain boundaries Some interrelations of the structure data Structure of a 1-yr old Peter snow Suggestions for an exact study of the age-hardening process of snow References Appendix: Structure pictures
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  • 21
    Monograph available for loan
    Monograph available for loan
    Bad Kissingen : Deutscher Wetterdienst in der US-Zone, Zentralamt
    Call number: MOP 47660 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 40 Seiten
    Language: German , English
    Note: Text zum Teil in Deutsch und Englisch
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  • 22
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-105
    In: Research report / Cold Regions Research and Engineering Laboratory, 105
    Description / Table of Contents: Summary: A principle of particle segregation by freezing is presented. It is demonstrated experimentally by using a transparent freezing cabinet in which a sample of distilled water freezes from the bottom upward. In this way the freezing front line travels vertically and the particles are carried against gravity. By using the same material with different shapes (glass beads and broken quartz or glass) it is demonstrated that an important factor in particle migration is the shape of the particle or its contact area with the interface. By testing other materials with different shapes and sizes, it is demonstrated that another important factor is particle size and rate of freezing. Fine particles migrate under a wide range of rates of freezing; coarser ones migrate at lower and more limited ranges of rates of freezing. It is suggested that, for determining frost behavior of soils in permafrost regions, freezing from the bottom upward is a more reliable test than freezing from the top down. Freezing from the bottom more closely approximates freezing of the active layer above permafrost; also, friction with the cylinder testing wall is eliminated. The implication of this principle in engineering and studies of soil genesis in cold regions is emphasized.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 105
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental procedure Experimental results Conclusions and recommendations References
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  • 23
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-115
    In: Research report / Cold Regions Research and Engineering Laboratory, 115
    Description / Table of Contents: SUMMARY Between 1 July and 7 August 1960, the U.S. Army Snow Ice and Permafrost Research Establishment, Corps of Engineers, supported a £our-man glaciological expedition on the southern dome of the Greenland ice sheet. Measurements of snow temperature, density, ram hardness, and grain size were made at seven pit ~tudies along 191 mileS of over-snow traverse. In addition to the pit studies, 38 Rammsonde profiles were measured and 166 shallow pits were dug to measure temperature in the first meter of snow. The annual accumulation of snow was found to decrease westward, from 97 em water equivalent 50 miles from tP.e east coast, to 40 em 80 miles from the western margin. A possible precipitation shadow was encountered immediately west of the crest line of the ice sheet. The precipitation shadow and the decrease in accumulation westward indicate that the source area for the precipitation lies to the east of the southern dome, in the. Greenland Sea. Temperature profiles in the firn indicated that summer warming was still in progress. During August, melting at an elevation of 2000 m above se~ level was intense (OC in the top 75 em} •. According to the facies classification of glaciers (Benson, 1959, 1960}, most of the study area is in tfie percolation facies, with the possible exception of the westernmost· s.tation (mile l-138) which is at or near the saturation line. The daily heat exchange in the first meter of snow, near the time of maximum melt conditions, is between 20 and '35 cal/cinZ. This is approxi-mately 25o/o of the heat necessary to raise the temperature of a column of firn of unit cross Section and 1 m deep to the melting point. Effective values of thermal conductivity and diffusivity as determined from the temperature curves with no attempt made to isolate radiation and con-vection are, respectively, 4-6 x 10-3 cgs and 20-30 x 10-3 cgs. Radiation and convection in the first meter of firn cause "effective conductivity" values to be 4 to 7 times greater than the value k = 0. 0068pZ given by Abel's (1892), which is the conductivity at greater depths.
    Type of Medium: Series available for loan
    Pages: v, 22, A4, B1 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 115
    Language: English
    Note: CONTENTS Preface Summary Introduction Method of investigation Location Pit studies Temperature Hardness Density Stratigraphic measurements Thermal studies Stratigraphic features Grain size Grain shape Crusts Discussion of results Temperature Altitude gradient Latitude gradient Depth-density relationship Depth-load relationship Densification Stratigraphic analysis Facies relationship Climatological aspects 1960 meteorological observations Temperature Wind Barometric pressure Radiation Cloudiness Visibility Thermal studies Summary and conclusions References Appendix A Appendix B
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  • 24
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-117
    In: Research report / Cold Regions Research and Engineering Laboratory, 117
    Description / Table of Contents: Summary: An experiment was designed to investigate operator-variance in the determination of the plastic limit of cohesive soils, independent of sample preparation and hydration time. A standard sample was prepared by dry-mixing commercial clay, "Grundite", with a pure silt. After the sample was hydrated for 3 weeks, five random samples were taken and five replicates performed on each sample. Analysis of variance (AOV) shows that there is no reason to doubt that the sample is homogeneous at the 0.05 level of significance. Random samples were then distributed to five zones of operators, where a zone is defined as a group of operators with similar backgrounds and engineering interests. Two operators from each group performed five replicates. The AOV model used in the analysis is mixed with the upper level fixed and the two lower levels random. The estimated "within" and "between" operator variances are 0. 45 and 4. 18 respectively. The estimated "between zones" contribution to the total sum of squares is negative. No correlation was found between an operator's internal variance and his deviation from the grand mean. On the basis of this experiment, no reason-exists to doubt that an "untrained" operator can obtain results comparable to those of professional operators. The major factor contributing to the total sample variance is the inconsistency between the individual operators who, although able to duplicate their own determinations, do not call the same end point. To minimize between operator variance, a readily prepared standard sample is suggested with which any operator can calibrate his plastic limit determinations against the expected national average.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 117
    Language: English
    Note: CONTENTS Preface Summary ­Introduction Sample preparation Sample homogeneity Distribution of samples Analysis Conclusions and suggested standardization References
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  • 25
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-118
    In: Research report / Cold Regions Research and Engineering Laboratory, 118
    Description / Table of Contents: Summary: The observation that newly frozen ice sheets, resulting from pools of -water freezing over,- support more than would be predicted by ordinary theory is assessed. A solution is presented for a circular plate on an elastic, sealed foundation. Graphical results are shown for supports at the circumference of the plate. Graphs to obtain moments in a circular plate on an elastic bearing surface, using a sealed or unsealed foundation, are compiled for fixed and simple supports. In reality the foundation may not be completely sealed, calling for discretion in selecting the actual moment. The ability of the refrozen ice sheet to support the extra load is explained by the fact that the water has been sealed between the surface and main sheet of ice and the volume occupied by the water cannot change.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 118
    Language: English
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  • 26
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-119
    In: Research report / Cold Regions Research and Engineering Laboratory, 119
    Description / Table of Contents: Summary: An experimental investigation of stress-wave propagation in snow and ice is described. Seven types of Greenland snow were investigated to determine the extent to which the variation in dynamic response of the snow is a function of snow types, and were compared with results of similar Michigan snow experiments. A low-density explosive charge was detonated, sending a steep-fronted shock wave through a metal transfer plate and into the snow sample, compressing the snow and setting it in motion. Measurements were made on shock waves with amplitudes of less than 200 atm. Density and pressure behind the wave fronts were determined by simultaneous measurement of wave-propagation and particle velocity as limited by the fast elastic wave and the slow plastic wave of the two-front structure. Values calculated by the Rankine-Hugoniot jump conditions determined the points at which the material behaves plastically or hydrodynamically. The maximum stable pressure-volume states that snow can reach under shock loading are also shown. Sources of scatter in the results from variations in snow type and errors in data reduction and geometry changes are pointed out.
    Type of Medium: Series available for loan
    Pages: v, 25, A11 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 119
    Language: English
    Note: CONTENTS Test area description Experimental techniques Explosive initiation system Grid lines on snow Grid lines on driving plates The streak camera Synchronization of camera and event Synchronization of flash bulb and event Timing-light generator High-speed framing camera
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  • 27
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-79
    In: Research report / Cold Regions Research and Engineering Laboratory, 79
    Description / Table of Contents: Summary: The theory of a plate on an elastic foundation will closely predict the radial cracks observed in loading tests on floating ice sheets. However, the plate theory does not predict accurately the circumferential crack which forms ultimately with increased loading. The wedge theory is developed in an attempt to better predict the location and magnitude of the stresses causing the circumferential crack. The results obtained can be applied to help predict the ultimate bearing capacity of an ice sheet, provided the modulus of elasticity and flexural strength of the ice are known.
    Type of Medium: Series available for loan
    Pages: Getrennte Zählung , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 79
    Language: English
    Note: CONTENTS Preface Summary Introduction Solution Applications Conclusions References Appendix A Computer program Graphs of nev functions, derivatives, and integrals Tables of nev functions, derivatives, and integrals
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  • 28
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-84
    In: Research report / Cold Regions Research and Engineering Laboratory, 84
    Description / Table of Contents: Summary: The law of sliding of ice over bedrock is generalized to include the effect of the presence of a longitudinal stress. The sliding velocity thus depends on both the shear stress acting at the bottom of an ice mass and the longitudinal stress. With this generalized law, it is still possible to make a one-dimensional analysis of the problem of calculating the profile of an ice cap or glacier, such as was carried out by Nye, and yet introduce the effect of large longitudinal stresses. As a result a profile can be calculated with two equations. One equation is applicable to the central region of an ice cap and the other equation (which was found by Nye) is valid elsewhere. By an appropriate joining of the profiles derived from these two equations, the complete profile of an ice cap can be obtained. From two sample calculations it is shown that, for a large ice cap, Nye's theory is valid practically everywhere, and there is no real need to bring in the modification. For a small ice cap, the modification to the profile is valid over an appreciable fraction of the total width of the ice cap. A very simple extension of the analysis of the ice cap profile allows for the effect of isostatic sinking of the bedrock surface under a large ice cap. (An initially flat bedrock surface was assumed. The analysis can be extended easily to allow for an arbitrarily shaped initial bedrock surface.)
    Type of Medium: Series available for loan
    Pages: iv, 12 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 84
    Language: English
    Note: CONTENTS Preface Summary Introduction Theory Effective sliding velocity Estimate of stresses Surface profilecalculations Effect of the weight of ice on the bedrock base Sample calculations References
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  • 29
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-85,2
    In: Research report / Cold Regions Research and Engineering Laboratory, 85,2
    In: The frost behavior of soils : laboratory and field data for a new concept, Part II
    Description / Table of Contents: Laboratory experiments were performed with a specil closed-system side-freezing cabinet in which completely saturated soil samples were subjected to alternate freeze-thaw cycles without surcharge. A vertical or nearly vertical freezethaw plane was obtained in the side-freezing cabinet. The soil used was a straight graded noncohesive material with 14 finer than the No. 200 0.074 mm mesh sieve. According to frost criterion based only on gradation, the soil would be classified as a never frost-heaving moraine soil or non-frost-susceptible. All experiments were run for 20 and 22 cycles. Freezing rates used were as follows 30.0 mmhr 33.0 mmhr and 4 .0 mmhr. The initial dry density was approximately constant for each test at 1.8 gcm3 or 112.4 lbft3, and complete saturation was maintained in the tests.
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    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 85,2
    Language: English
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  • 30
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-90
    In: Research report / Cold Regions Research and Engineering Laboratory, 90
    Description / Table of Contents: Summary: A new method is presented for extracting more meaningful information from snow profile data which will simplify the study of the permeability of snow. Earlier analyses normally employed statistical methods to determine property variations with depth, with the line of mean values established by the method of least squares. The mean curves derived in this manner may not represent properly the true nature of the snow pack, or aid in understanding the dynamic processes which are in action. The new graphical methods described distinguish the separate effects of densification and thermal metamorphism on permeability, permitting future advances in the analysis. Profile data obtained in 1954 and 1960 are reanalyzed using the new techniques. For a natural polar pack under conditions when no melting occurs and the accumulation is assumed continuous, the following conclusions may be made: permeability for a given density of snow increases with depth and time except possibly near the surface or at depths below 30 m; the rate of permeability change with depth for given densities decreases in a calculable way relative to the density; and, mean permeability changes with depth in a complex manner.
    Type of Medium: Series available for loan
    Pages: iv, 14, A3, B2, C2 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 90
    Language: English
    Note: CONTENTS Preface Summary Introduction Standard methods of data presentation- A class interval method of data presentation Interpretation of the numerical data Interpretation of thin sections Conclusions References Appendix A Appendix B Appendix C
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  • 31
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-88
    In: Research report / Cold Regions Research and Engineering Laboratory, 88
    Description / Table of Contents: Summary: Four ground patterns were investigated by means of trenches cut in the outwash near Thule, Greenland: circular and linear depressions in unsorted material, polygonal troughs in unsorted material, sorted circles, and irregular mounds and depressions of low relief formed in unsorted finer grained material. Correlation is made between surface pattern, grain size and structure of the active layer, and type and distribution of ground ice for the patterns investigated. Classification of the active layer as disturbed, slightly disturbed, and undisturbed is based on the condition of primary depositional bedding and the presence or absence of vertical sorting. Other features of the active layer, depending upon its type, are an accumulation of fines at the bottom of the active layer and on top of stones, and a siliceous calcareous evaporite on the under surface and clean washed coarser particles beneath the larger stones. Fabric analysis of four kinds of ground ice is presented: ice wedge, relict ice, ice mass, and ice lens, as well as analysis of the contact of ice wedges with relict and mass ice. Practical applications, based on the conclusions, are given for the selection of foundation sites and the location of non-frost-susceptible building materials. NOTE: This is a very large file. Please give your browser several minutes to download the file.
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    Pages: viii, 79 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 88
    Language: English
    Note: CONTENTS Preface Summary Introduction Glossary Part 1 : Surface pattern, structure of the active layer, and type and distribution of ground ice in the permafrost Pattern type 1: Circular and linear depressions in unsorted outwash Circular depressions, area 1 Structure of the active layer Ground ice and its relation to surface morphology Linear depressions, area 5 Structure of the active layer Ground ice and its relation to surface morphology Pattern t ype 2 and 3: Polygonal troughs in unsorted outwash and sorted circles or centers of fines Area 3 Structure of the active layer Ground ice and its relation to surface morphology Area 4 Structure of the active layer Ground ice and its relat ion to surface morphology Pattern type 4: Mounds and depressions of low relief in unsorted outwash Area 4a Structure of the active layer Ground ice and its relatiop. to surface morphology Part 2: Ground ice studies Area 1 Lens ice History Appearance of the ice Fabric analysis Wedge ice History Appearance of the ice Fabric analysis Relict ice History Appearance of the ice Fabric analysis Contact between ice wedge and relict ice Ice sockets Area 5 Wedge ice Fabric analysis Relict ice Fabric analysis Area 3 Ice mass History Appearance of the ice Fabric analysis Ice wedge Fabric analysis Contact between ice mass and wedge Appearance of the ice Fabric analysis Summary and conclusions Pattern type 1: Linear and circular depressions in. unsorted outwash Pattern type 2: Polygonal troughs formed in unsorted outwash Pattern type 3: Sorted circles or centers of fines Pattern type 4: Mounds and depressions of low relief in fine-grained unsorted outwash Engineering applications References Appendix A: Associated studies Appendix B : Recommendations for further field and laboratory work Appendix C: Recommendations for field and laboratory techniques
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  • 32
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-94
    In: Research report / Cold Regions Research and Engineering Laboratory, 94
    Description / Table of Contents: Summary: A new mechanism is described which explains the formation of moraines in the ablation areas of cold ice caps. The mechanism involves the freezing of water onto the bottom surface of an ice cap. This water comes from regions of the bottom surface where the combination of the geothermal heat and the heat produced by sliding of ice over the bed is sufficient to melt ice. A number of criticisms are made of the shear hypothesis, which has been advanced to explain moraines occurring on Baffin Island and near Thule, Greenland. It is concluded that this older hypothesis may be inadequate to account for these moraines. Although in theory the mechanism proposed here undoubtedly would lead to the formation of moraines, the existing field data are insufficient to prove conclusively that actual moraines have originated in this way.
    Type of Medium: Series available for loan
    Pages: iv, 12 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 94
    Language: English
    Note: CONTENTS Preface Summary Introduction Comments on the shear hypothesis Appearance of the debris layers The possibility of cold ice scraping up debris The shear across a debris layer The geometry of the debris layers Freezing model Theory Discussion Conclusion References
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  • 33
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-95
    In: Research report / Cold Regions Research and Engineering Laboratory, 95
    Description / Table of Contents: Summary: An investigation was conducted at Camp Century, Greenland, to study the feasibility of using air wells to cool undersnow structures in the arctic during the summer months. From results obtained during the summers of 1959,and 1960 and late November, 1960, it was found that the air well is a practical and effective means of providing a -20°C air supply at volumetric flow rates of 1200 to 1700 ft^3/min. The extent and rate of warming of the snow beneath the trench floor by heat exchange between the air and the snow foundation was found to depend upon trench air temperature, fan capacity, fan arrangement, and casing length. For example, in a well cased to a depth of 17. 5 ft and equipped with a 5 hp fan drawing in air at a rate of 1700 ft^3/min, the maximum warming was found to be 12.5°C during a 42-day period. Snow temperature differences of about 7°C were found between similar trenches with and without a fan installation. The minimum permissible distance between two adjacent fans to eliminate, overlap in warming up the snow foundation is approximately 80 ft.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 95
    Language: English
    Note: CONTENTS Preface Summary Theoretical background Test method and equipment Test operations Effectiveness of the air well Estimation of fan capacity Natural cooling in winter Change of trench foundation temperature Trench wall warm-up Conclusions and recommendations
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  • 34
    Call number: MOP 28519/1
    In: Detailed analyses of selected Pacific storms based on continuous radar records and short-interval serial ascents, Vol. 1
    In: Technical report / University of Washington, Department of Meteorology and Climatology, Nr. 3
    In: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, 62-242
    Type of Medium: Series available for loan
    Pages: IV, 44 S. , graph. Darst., Kt.
    Series Statement: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force 62-242
    Language: English
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  • 35
    Series available for loan
    Series available for loan
    Washington : Smithsonian Institution
    Call number: MOP Sü Sonderdruck
    Type of Medium: Series available for loan
    Pages: S. 173-176
    Series Statement: Publication / Smithsonian Institution 3922
    Language: English
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  • 36
    Monograph available for loan
    Monograph available for loan
    Washington, DC : Off. of Tech. Services, U.S. Dep. of Commerce
    Associated volumes
    Call number: MOP 29627
    In: AFCRL Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, 63-22
    Type of Medium: Monograph available for loan
    Pages: VIII, 82 S. , graph. Darst., Kt.
    Series Statement: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force 63-22
    Language: English
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  • 37
    Call number: PIK N 456-16-90113
    Type of Medium: Monograph available for loan
    Pages: X, 270 S.
    Language: English
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  • 38
    Monograph available for loan
    Monograph available for loan
    Oxford : Clarendon Press
    Call number: MOP 16750
    Description / Table of Contents: Professor Frenkel's book on the theory of liquids deals with a wider subject than that of liquids alone. Liquids are in his view much more closely akin to solids than to gases, but have a structure in which the long-range order of the solid has been lost. The book therefore includes a discussion of all types of disorder in solids, of the purely thermal displacements of the atoma, of the motion of interstitial atoms and ions, and of many types of transition from an ordered to a disordered state. The theory of these transitions, which has been developed fully, is discussed at length in this book and forms an introduction to the problems as yet unsolved of the transition to the liquid phase. There are also sections dealing with the specific heats of liquids, diffusion in liquids, and similar subjects.
    Type of Medium: Monograph available for loan
    Pages: XI, 488 Seiten , Diagramme
    Series Statement: The international series of monographs on physics
    Uniform Title: Kinetičeskaja teorija židkostej
    Language: English
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  • 39
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Pergamon Press
    Call number: MOP 31672
    Type of Medium: Monograph available for loan
    Pages: XIII, 408 S. , graph. Darst.
    Edition: Rev. and enlarged ed.
    Uniform Title: Mechanika aerozolej
    Language: English
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  • 40
    Call number: MOP 27221
    Type of Medium: Monograph available for loan
    Pages: 255 S. , Ill.
    Language: English
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  • 41
    Monograph available for loan
    Monograph available for loan
    [Tucson, Ariz.] : The University of Arizona
    Call number: PIK N 456-17-90924
    Type of Medium: Monograph available for loan
    Pages: ix, 132 Seiten , Karten, Tabellen , 28 cm
    Edition: [Prelim. ed.]
    Series Statement: University of Arizona, Institute of Atmospheric Physics. Technical reports on the meteorology and climatology of arid regions, 14
    Language: English
    Note: With : Distribution of rainfall in Arizona / Christine R. Green. -- Climatological data for Sonora and Northern Sinaloa / James Rodney Hastings. -- Probabilities of precipitation at selected points in Arizona / Paul C. Kangieser and Christine R. Green. Tucson, 1964-1965. Bound together subsequent to publication.
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  • 42
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : McGraw-Hill
    Call number: 6295
    Type of Medium: Monograph available for loan
    Pages: xiii, 408 S. : graph. Darst.
    Series Statement: McGraw-Hill Electronic Sciences Series
    Language: English
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  • 43
    Monograph available for loan
    Monograph available for loan
    Nairobi [u.a.] : Buchanan
    Call number: PIK N 630-15-89531
    Type of Medium: Monograph available for loan
    Pages: XXVII, 654 S. , zahlr. Ill. , 1 Kt.
    Language: English
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  • 44
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : American Geophysical Union
    Call number: MOP S 12842
    Description / Table of Contents: The penetration of radiation into snow is assumed to follow Fick's second law of diffusion with a term for simultaneous absorption. From this, the distribution of radiant energy in a deep homogeneous snow cover, a laminated snow cover, and a snow cover with an absorbing surface beneath is deduced. An equation for albedo is also derived. The penetration phenomenon is then analyzed in terms of the physical processes occurring and formulated as a random walk process. After a correction is made for a certain amount of nondiffuse radiation in the snow, more accurate equations for energy distribution and albedo are obtained. These results are applied to the theory of radiation measurement in snow. After experimental procedures were established on the Blue Glacier summer firn, field data were collected from winter snow at Alta, Utah, and used to check the theoretical equations for albedo and transmission to a black surface. The agreement of theory and experiment is very satisfactory.
    Type of Medium: Monograph available for loan
    Pages: pages 181-189
    ISSN: 0022-1406
    Series Statement: Journal of Geophysical Research JGR Vol. 66, Iss. 1, January 1961
    Language: English
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  • 45
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    Monograph available for loan
    [Edgecumbe, N.Z.] : A. Muller
    Call number: M 15.89146
    Description / Table of Contents: An account of the results of the 2 March 1987 earthquake in the eastern Bay of Plenty and the aftermath's effects on the people and places on the Rangitaiki Plains
    Type of Medium: Monograph available for loan
    Pages: 223 S., , Ill.
    Language: English
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  • 46
    Call number: ZSP-553-165,2
    In: Meddelelser om Grønland
    Type of Medium: Series available for loan
    Pages: 120 S. : Ill., graph. Darst. , 4
    Series Statement: Meddelelser om Grønland 165,2
    Language: English
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  • 47
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : McGraw-Hill
    Call number: 6294
    Type of Medium: Monograph available for loan
    Pages: xiii,304 S. : graph. Darst.
    Series Statement: McGraw-Hill Series in Missile and Space Technology
    Language: English
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  • 48
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    Monograph available for loan
    Lahaina, Hawaii : Ross-Hargreaves
    Call number: PIK N 630-15-89562
    Type of Medium: Monograph available for loan
    Pages: 62 S. , zahlr. Ill.
    Language: English
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  • 49
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Interscience
    Associated volumes
    Call number: M 93.0136/7
    In: Interscience monographs and texts in physics and astronomy
    Type of Medium: Monograph available for loan
    Pages: XI, 283 S.
    Series Statement: Interscience monographs and texts in physics and astronomy 7
    Language: English
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  • 50
    Monograph available for loan
    Monograph available for loan
    London : Allen & Unwin
    Associated volumes
    Call number: M 93.0088/2 ; G 5377
    In: Sedimentary petrography
    Type of Medium: Monograph available for loan
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 51
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Pergamon Pr
    Call number: MOP 31629
    Type of Medium: Monograph available for loan
    Pages: XIII, 383 S.
    Uniform Title: Vvedenie v gidrodinamičeskie metody kratkosročnogo prognoza pogody
    Language: English
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  • 52
    Call number: ZSP-553-164,5
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 66 S., 7 Taf. : Ill., graph. Darst., Kt.
    Series Statement: Meddelelser om Grønland 164,5
    Language: English
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  • 53
    Monograph available for loan
    Monograph available for loan
    København : Reitzel
    Associated volumes
    Call number: ZSP-553-171,1
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 77 S. : Ill., graph. Darst., Kt.
    Series Statement: Meddelelser om Grønland 171,1
    Language: English
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  • 54
    Call number: ZSP-553-159,10
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 45 S. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 159,10
    Language: English
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  • 55
    Monograph available for loan
    Monograph available for loan
    København : Reitzel
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    Call number: ZSP-553-159,11
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 74 S., XXI Taf. : zahlr. Ill.
    Series Statement: Meddelelser om Grønland 159,11
    Language: English
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  • 56
    Call number: ZSP-553-159,9
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 40 S., II Taf. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 159,9
    Language: English
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  • 57
    Call number: ZSP-553-163,6
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 64 S., V Taf. : Ill.
    Series Statement: Meddelelser om Grønland 163,6
    Language: English
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  • 58
    Call number: ZSP-553-164,6 ; AWI P8-88-0281
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 105 S., 4 Taf. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 164,6
    Language: English
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  • 59
    Call number: ZSP-553-170,1
    In: Meddelelser om Grønland
    Type of Medium: Monograph available for loan
    Pages: 40 S. : Ill., Kt.
    Series Statement: Meddelelser om Grønland 170,1
    Language: English
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  • 60
    Monograph available for loan
    Monograph available for loan
    London : Allen & Unwin
    Associated volumes
    Call number: G 5376/1 ; M 93.0088/1
    In: Sedimentary petrography
    Type of Medium: Monograph available for loan
    Pages: 643 S.
    Edition: 4th., rev. edition
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
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  • 61
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 93.0087/1 ; AWI G2-96-0026 ; MOP 34194
    In: The sea ; 1, Vol. 1
    Type of Medium: Monograph available for loan
    Pages: xv, 864 S. , Ill., graph. Darst., Kt.
    Edition: 1. publ.
    Language: English
    Note: CONTENTS: PHYSICAL OCEANOGRAPHY. - SECTION I. FUNDAMENTALS. - 1. PHYSICAL PROPERTIES OF SEA-WATER / BY N. P. FOFONOFF. - 1. The equilibrium thermodynamic state. - 2. Equation of state for sea-water. - 3. Entropy. - 4. Chemical potential difference. - 5. The non-equilibrium state. - 6. Other physical properties of sea-water. - 2. THE EQUATIONS OF MOTION OF SEA-WATER / BY CARL ECKART. - 1. Introduction. - 2. Thermodynamics. - 3. Hydrodynamics. - 4. The irreversible processes. - 5. Transformation of the equation. - 6. The zeroth approximation. - 7. The first approximation. - 8. Definitions related to convective motion. - 9. The field equations. - SECTION II. INTERCHANGE OF PROPERTIES BETWEEN SEA AND AIR. - 3. SMALL-SCALE INTERACTIONS / BY E. L. DEACON AND E. K. WEBB. - 1. General considerations of transfer. - 2. Momentum transfer and the wind-profile. - 3. Drag coefficients of the sea surface. - 4. Transfer of heat and water vapour. - 4. LARGE-SCALE INTERACTIONS / BY JOANNE S. MALKUS. - 1. Introduction. - 2. How the whole system works. - 3. Determination of air-sea fluxes. - 4. Climatology of energy exchange and the global heat and water budgets. - 5. Heat and water exchange and its role in tropical circulations. - 6. Large-scale momentum relations. - 7. Exchange mechanisms and fluctuations. - 8. Exchange fluctuations in mid-latitudes and long-period interaction anomalies. - 9. Concluding remarks. - 5. INSOLUBLES / BY R. W. REX AND E. D. GOLDBERG. - 1. Meteorology of transport. - 2. Eolian materials in marine sediments. - 6. SOLUBLES / BY A. H. WOODCOCK. - 7. GASES / BY R. REVELLE AND H. E. SUESS. - 1. Introduction. - 2. Oxygen and nitrogen. - 3. Rare gases. - 4. Carbon dioxide. - SECTION III. DYNAMICS OF OCEAN CURRENTS / BY N. P. FOFONOFF. - 1. Conservation equations for momentum and mass. - 2. Separation into steady and time-dependent motion. - 3. Magnitude of forces. - 4. Steady-state circulation. - 5. Steady inertial circulation. - 6. Convective circulation. - 7. Time-dependent motion. - SECTION IV. TRANSMISSION OF ENERGY WITHIN THE SEA. - 8. LIGHT / BY J. E. TYLER AND R. W. PREISENDORFER. - 1. Physical constructs. - 2. Instrumentation for the measurement of the underwater light field and the determination of the optical properties of the sea. - 3. Radiance distribution. - 4. Attenuation coefficient. - 5. Volume scattering functions and total scattering coefficient. - 6. Irradiance. - 7. Diffuse attenuation function and reflectance function. - 8. Scalar irradiance (spherical irradiance). - 9. Absorption coefficient. - 10. Path function. - 11. Data. - 12. Applications. - 13. List of symbols. - 9. UNDERWATER VISIBILITY / BY S. Q. DUNTLEY. - 1. Image transmission. - 2. Inherent contrast. - 3. Sighting range. - 10. LIGHT AND ANIMAL LIFE / BY G. L. CLARKE AND E. J. DENTON. - 11. OTHER ELECTROMAGNETIC RADIATION / BY L. N. LIEBERMANN. - 1. Introduction. - 2. Electromagnetic properties of sea-water. - 3. Propagation through sea-water. - 4. The effect of the sea-surface on electromagnetic propagation. - 5. Natural electromagnetic radiation or "noise" in the sea. - 12. SOUND IN THE SEA / BY P. VIGOUREUX and J. B. HERSEY. - 1. The nature of sound. - 2. Propagation of sound in water. - 3. Noise. - 4. Instruments and applications of sound to oceanography. - 13. SOUND SCATTERING BY MARINE ORGANISMS / BY J. B. HERSEY AND R. H. BACKUS. - 1. Introduction. - 2. Occurrence and description of scattering layers. - 3. Identification of sound scatterers. - 4. Sound-scattering theory. - 5. Sound-scattering observations. - 6. What is "the deep scattering layer"?. - 7. Ideas and miscellaneous observations. - 14. SOUND PRODUCTION BY MARINE ANIMALS / BY W. E. SCHEVILL, R. H. BACKUS, AND J. B. HERSEY. - 1. Introduction. - 2. History. - 3. Instrumentation. - 4. Identification of source. - 5. Purposeful and adventitious sounds. - 6. Sound-producing mechanisms. - 7. Spectra of sounds. - 8. Functions of sound. - 9. Hearing as related to sound production. - 10. Eliciting and suppressing marine animal sounds. - 11. Exploitation of marine animal sounds by the oceanographer. - SECTION V. WAVES. - 15. ANALYSIS AND STATISTICS / BY D. E. CARTWRIGHT. - 1. Introduction. - 2. Fundamental equations of wave motion. - 3. Statistical formulation. - 4. Properties of a wave system in terms of its directional energy spectrum. - 5. Estimating the directional energy spectrum. - 6. Waves recorded by a single detector. - 7. Spectral measurement. - 8. Second-order approximations to energy spectra. - 16. LONG-TERM VARIATIONS IN SEA-LEVEL / BY J. R. ROSSITER. - 1. Introduction. - 2. The determination of mean sea-level. - 3. Causes of variations in sea-level. - 4. The analysis of observations. - 5. Some geophysical implications of long-term variations in sea-level. - 6. Conclusion. - 17. SURGES / BY P. GROEN AND G. W. GROVES. - 1. Introduction. - 2. Description. - 3. Dynamics and forecasting. - 18. LONG OCEAN WAVES / BY W. H. MUNK. - 1. Introduction. - 2. The instruments. - 3. The spectrum. - 4. Surf beat. - 5. Shelf waves. - 6. Tsunamis. - 19. WIND WAVES / BY N. F. BARBER AND M. J. TUCKER. - 1. Kinematics of waves. - 2. The description of a complicated wave pattern: the wave spectrum. - 3. Theories of wave generation by wind. - 4. Wave prediction. - 5. Waves from distant storms. - 6. Waves approaching the shore. - 7. The surf zone. - 8. Ships and waves. - 9. Methods of observation and analysis-methods taking no account of direction of travel. - 10. Methods of observation and analysis - the directional power spectrum. - 20. MICROSEISMS / BY J. DARBYSHIRE. - 1. Relation between sea waves and microseisms. - 2. The nature of microseisms. - 3. Refraction of microseisms. - 4. Storm tracking and estimation of the direction of approach of microseisms. - 5. Estimation of direction from the nature of microseisms. - 6. Instruments. - 7. Other work. - 21. RIPPLES / BY C. S. COX. - 1. Spectrum and mean square slope. - 2. Effect of slicks. - 3. Shape of a rippled water surface. - 4. Growth of ripples. - 22. INTERNAL WAVES : Part I / BY E. C. LAFOND. - 1. Introduction. - 2. Measurements. - 3. Observed relations. - 22. INTERNAL WAVES : Part II / BY C. S. COX. - 4. Differential equations. - 5. Spectrum. - 6. Internal waves and turbulence. - 23. TIDES / BY W. HANSEN. - 1. Introduction. - 2. The hydrodynamic equations and their application to tidal problems. - 3. Tidal observation. - 4. Tidal charts. - 5. Classical theory. - 6. Numerical methods for ascef!.aining the tides and tidal currents. Boundary-value problems. - 7. The application of difference methods to initial-boundary problems. - 8. Numerical solutions of initial-boundary-value problems of tides in one and two dimensions. - 9. Internal tides. - SECTION VI. TURBULENCE / BY K. F. BOWDEN. - 1. General properties of turbulence. - 2. Turbulence in the sea. - 3. Turbulent fluctuations and turbulent transports. - 4. Vertical turbulence. - 5. Horizontal turbulence. - SECTION VII. THE PHYSICS OF SEA-ICE / BY E. R. POUNDER. - 1. Introduction. - 2. Mechanical properties. - 3. Thermal properties. - 4. Electrical properties. - 5. Growth and disintegration of an ice cover. - 6. Theory of sea-ice structure and properties. - AUTHOR INDEX. - SUBJECT INDEX.
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  • 62
    Call number: M 93.0087/2 ; AWI G2-96-0027
    In: The sea ; 2, Vol. 2
    Type of Medium: Monograph available for loan
    Pages: xv, 554 S. , Ill., graph. Darst.
    Language: English
    Note: CONTENTS: THE COMPOSITION OF SEA-WATER. - SECTION I. CHEMISTRY. - 1. THE OCEANS AS A CHEMICAL SYSTEM / BY E. D. GOLDBERG. - 1. The composition of sea-water. - 2. Reactivities of the elements. - 3. Chemical reaction in the oceans and the compositions of the end-products. - 4. Space and time distributions of the elements. - 2. THE INFLUENCE OF ORGANISMS ON THE COMPOSITION OF SEAWATER / BY A. C. REDFIELD, B. H. KETCHUM AND F. A. RICHARDS. - 1. Introduction. - 2. The biochemical cycle. - 3. The biochemical circulation. - 3. ARTIFICIAL RADIOACTIVITY IN THE SEA / BY Y. MIYAKE. - 1. Artificial radioactivity in oceanic waters. - 2. Enrichment of radioactive substances in marine products. - 3. Artificial radioactivity as a tracer of water movements in the ocean. - 4. Disposal of radioactive waste in the ocean. - 4. RADIOISOTOPES AND LARGE-SCALE OCEANIC MIXING / W. BROECKER. - 1. Introduction. - 2. Useful isotopes. - 3. Steady-state distribution of 14C. - 4. Ocean-atmosphere CO2 exchange rates. - 5. Oceanic mixing models. - 6. Industrial CO2 effect. - 7. 226Ra distribution. - 8. 90Sr distribution. - 9. Non-steady-state conditions. - 10. Conclusion. - 5. CHEMICAL INSTRUMENTATION / BY D. E. CARRITT. - 1. Introduction. - 2. Chlorinity, salinity, density and related properties. - 3. Water tagging and tracer techniques. - 4. Measurement of dissolved gases. - 6. WATER SAMPLING AND THERMOMETERS / BY H. F. P. HERDMAN. - 1. Sampling. - 2. Thermometry. - SECTION II. FERTILITY OF THE OCEANS. - 7. PRODUCTIVITY, DEFINITION AND MEASUREMENT / BY E. STEEMANN NIELSEN. - 1. Introduction. - 2. Definitions. - 3. Methods for measuring primary production. - 4. The relation between the rate of gross production and net production below a surface unit. - 5. Transparency of the water versus organic production. - 6. The significance of single individual measurements of primary production. - 7. The influence of weather conditions. - 8. ORGANIC REGULATION OF PHYTOPLANKTON FERTILITY / BY L. PROVASOLI. - 1. Introduction. - 2. Data from chemical analysis. - 3. Organic products of algae and bacteria. - 4. Nutritional requirements of marine algae. - 5. Crustacea and organic solutes. - 6. Data from biological analysis of sea-water. - 7. Prospects. - 8. Addendum. - 9. BIOASSAY OF TRACE SUBSTANCES / BY W. L. BELSER. - 1. Introduction. - 2. Vitamins. - 3. Amino acids. - 4. Purines and pyrimidines. - 5. Perspectives. - COMPARATIVE AND DESCRIPTIVE OCEANOGRAPHY. - SECTION III. CURRENTS. - 10. EQUATORIAL CURRENT SYSTEMS / BY J. A. KNAUSS. - 1. Methods of study of ocean currents. - 2. Gross circulation pattern. - 3. A two-layer ocean - the thermocline. - 4. Zonal fiow-geostrophic currents. - 5. Meridional flow-upwelling. - 6. Conclusions and speculations. - 11. EASTERN BOUNDARY CURRENTS / BY W. S. WOOSTER AND J. L. REID, JR. - 1. Introduction. - 2. Common features of eastern boundary currents. - 3. Coastal upwelling. -4. Poleward eastern boundary currents. - 5. Biological implications. - 12. THE SOUTHERN OCEAN / BY G. E. R. DEACON. - 1. Topography. - 2. Oceanographic data. - 3. Wind zones. - 4. The water-masses. - 5. Climatology and zoogeography. - 6. Nutrient salts. - 7. Future needs. - 13. DEEP-CURRENT MEASUREMENTS USING NEUTRALLY BUOYANT FLOATS / BY G. H. VOLKMANN. - 1. Introduction. - 2. The pinger. - 3. Measurements. - 14. DROGUES AND NEUTRAL-BUOYANT FLOATS / BY J. A. KNAUSS. - 15. ESTUARIES / BY W. M. CAMERON AND D. W. PRITCHARD. - 1. Definition of estuaries. - 2. General considerations. - 3. Estuarine circulation patterns. - 4. Some variations on the estuarine sequence. - 5. Flushing in estuaries. - 6. Dynamics of estuaries. - 7. Kinematic description of the distribution of properties in an estuary. - 16. APPLICATIONS OF THE GYROPENDULUM / BY W. S. VON ARX. - 1. Introduction. - 2. The gyropendulum. - 3. The problem of time variations. - SECTION IV. BIOLOGICAL OCEANOGRAPHY. - 17. GEOGRAPHIC VARIATIONS IN.PRODUCTIVITY / BY J. H. RYTHER. - 1. Introduction. - 2. Incident radiation. - 3. Transparency. - 4. Nutrients. - 5. Latitudinal variations in the stability of surface water. - 6. Productivity of the major oceanic regions. - 7. Hydrodynamic features which influence productivity. - 8. Plankton production in coastal and inshore waters. - 9. Production of benthic plant communities. - 18. BIOLOGICAL SPECIES, WATER-MASSES AND CRRRENTS / BY M. W. JOHNSON AND E. BRINTON. - 1. Introduction. - 2. Water-masses and biological species. - 3. Water currents and biological species. - 19. COMMUNITIES OF ORGANISMS / BY E. W. FAGER. - 1. Introduction. - 2. Definition of community. - 3. Identification of communities. - 4. Community structure. - 5. Community function. - 6. Community theory. - 20. THEORY OF FOOD-CHAIN RELATIONS IN THE OCEAN / BY G. A. RILEY. - 1. Introduction. - 2. Mathematical models of plankton populations. - 3. Complex versus simple models. - 4. Prognosis for mathematical models. - 5. Higher elements of the food chain. - 21. FISHERY DYNAMICS - THEIR ANALYSIS AND INTERPRETATION / BY M. B. SCHAEFER AND R. J. H. BEVERTON. - 1. Introduction. - 2. The Beverton-Holt approach. - 3. The Schaefer approach. - 4. Concluding remarks. - SECTION V. OCEANOGRAPHICAL MISCELLANEA. - 22. SEASONAL CHANGES IN SEA-LEVEL / BY JUNE G. PATTULLO. - 1. Introduction. - 2. The observed seasonal variations. - 3. Factors influencing variations in sea-level. - 4. Summary. - 5. Conclusions. - 23. BATHYSCAPHS AND OTHER DEEP SUBMERSIBLES FOR OCEANOGRAPHIC RESEARCH / BY R. S. DIETZ. - 1. Introduction. - 2. Diving chambers. - 3. Bathyscaphs. - 4. Diving saucer. - 5. Buoyant-hulled deep ships or bathynauts. - 6. Deep-research vessel (D.R.V.). - 7. Remote underwater manipulator (RUM). - 8. Concluding remarks. - 24. DEEP-SEA ANCHORING AND MOORING / BY JOHN D. ISAACS. - 1. Introduction. - 2. Historical background. - 3. Problems of taut-mooring. - 4. Remarks on components of moorings. - 5. Mooring cables. - 6. The anchors. - 7. Fittings. - 8. Performance. - AUTHOR INDEX. - SUBJECT INDEX.
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  • 63
    Call number: M 93.0202
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  • 64
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    Call number: ZSP-553-170,2
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    Call number: SR 90.0009(320)
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    Call number: M 91.0891 ; MR 90.0968 ; 5539/1
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    In: Italian expeditions to the Karakorum (K) and Hindu Kush : scientific reports
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  • 97
    Call number: SR 93.0768(501)
    In: Sveriges Geologiska Undersökning
    Type of Medium: Series available for loan
    Pages: 15 S.
    Series Statement: Sveriges geologiska undersökning : Ser. C, Avhandlingar och uppsatser 501
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 98
    Call number: SR 93.0764(55)
    In: Isogonic map of Australia and New Guinea showing predicted values for the epoch 1960.5.
    In: Report
    Type of Medium: Series available for loan
    Pages: 7 S.
    Series Statement: 55
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 99
    Call number: SR 90.0083(2,1)
    In: Publications on geodesy
    Type of Medium: Series available for loan
    Pages: 28 S.
    Series Statement: Publications on geodesy / Netherlands Geodetic Commission N.S., 2,1
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
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  • 100
    Call number: SR 90.0095(70)
    In: Special paper
    Type of Medium: Series available for loan
    Pages: 69 S.
    Series Statement: Geological Society of America special papers 70
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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