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  • English  (1,117)
  • 1960-1964  (1,117)
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  • 1
    Series available for loan
    Series available for loan
    Praha : Nakladatelství Československé Akademie věd
    Call number: O 3037
    Type of Medium: Series available for loan
    Pages: 304 Seiten , Illustrationen, Karten , 9 Karten
    Language: Czech , German , Russian , English
    Note: 1961 , In tschechischer Sprache mit russischen, deutschen und englischen Zusammenfassungen
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: O 2075/1964 II
    Type of Medium: Journal available for loan
    ISSN: 0367-6684 , 0568-5249 , 0568-5249
    Former Title: Vorg. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Serija geografičeskaja i geofizičeskaja
    Subsequent Title: Forts. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Fizika zemli
    Subsequent Title: Forts. Akademija nauk SSSR Izvestija Akademii Nauk SSSR / Fizika atmosfery i okeana
    Language: Russian , English
    Note: Teils mit Jg.-Zählung , In kyrill. Schr
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
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  • 3
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 4
    Monograph available for loan
    Monograph available for loan
    New York, NY [u.a.] : Wiley
    Call number: MR 22.94938
    Type of Medium: Monograph available for loan
    Pages: X, 378 Seiten , Illustrationen, graphische Darstellungen, Karten
    ISBN: 0-471-16698-7
    Language: English
    Location: Upper compact magazine
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  • 5
    Call number: 5537
    Type of Medium: Monograph available for loan
    Pages: XIV, 497 Seiten , Illustrationen
    Series Statement: The SIAM series in applied mathematics
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 6
    Publication Date: 2022-07-13
    Language: German , English
    Type: info:eu-repo/semantics/conferenceObject
    Format: application/pdf
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  • 7
    Call number: 10.1144/GSL.SP.1964.001.01.31 (e-book)
    In: Special publications / the Geological Society, London, Volume [1]
    Type of Medium: 12
    Pages: 1 Online-Ressource (VIII, 458 Seiten) , Illustrationen , 1 Corrigenda
    Series Statement: The quarterly journal of the Geological Society of London : Supplement 120
    Language: English
    Note: Table of Contents Part 1: Introduction Arthur Holmes Frederick Henry Stewart Geological Society, London, Special Publications, 1, 1-11, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.03 The history of attempts to establish a quantitative time-scale L. R. Wager Geological Society, London, Special Publications, 1, 13-28, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.04 A review of recent Phanerozoic time-scales N. J. Snelling Geological Society, London, Special Publications, 1, 29-36, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.05 Sedimentation rates in relation to the Phanerozoic time-scale J. D. Hudson Geological Society, London, Special Publications, 1, 37-42, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.06 The relationship between radiometric ages obtained from plutonic complexes and stratigraphical time R. St J. Lambert Geological Society, London, Special Publications, 1, 43-54, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.07 The geological significance of radiometric age studies on volcanic and hypabyssal rocks F. J. Fitch and J. A. Miller Geological Society, London, Special Publications, 1, 55-69, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.08 Part 2: Radiometric Methods with Respect to the Time-Scale Uranium–thorium–lead age-determinations with respect to the phanerozoic time-scale A. G. Darnley Geological Society, London, Special Publications, 1, 73-86, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.09 The rubidium–strontium method Stephen Moorbath Geological Society, London, Special Publications, 1, 87-99, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.10 Potassium—argon methods with special reference to basic igneous rocks John Alfred Miller and Frank John Fitch Geological Society, London, Special Publications, 1, 101-117, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.11 Potassium—argon ages of sedimentary and pyroclastic rocks Halfdan Baadsgaard and Martin Henry Dodson Geological Society, London, Special Publications, 1, 119-127, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.12 Potassium—argon decay constants and age tables Alan Gilbert Smith Geological Society, London, Special Publications, 1, 129-141, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.13 Part 3: Original Data Glauconite dates from the Upper Jurassic and Lower Cretaceous Martin Henry Dodson, David Charles Rex, Raymond Casey and Percival Allen Geological Society, London, Special Publications, 1, 145-158, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.14 The age of the paroxysmal Variscan orogeny in England Frank Joseph Fitch and John Alfred Miller Geological Society, London, Special Publications, 1, 159-175, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.15 Part 4: Stratigraphical Review The Tertiary period Brian Michael Funnell Geological Society, London, Special Publications, 1, 179-191, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.16 The Cretaceous period Raymond Casey Geological Society, London, Special Publications, 1, 193-202, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.17 The Jurassic period Michael Kingsley Howarth Geological Society, London, Special Publications, 1, 203-205, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.18 The Triassic period Edward Timothy Tozer Geological Society, London, Special Publications, 1, 207-209, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.19 The Permian period Denys Barker Smith Geological Society, London, Special Publications, 1, 211-220, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.20 The Carboniferous period Edward Howel Francis and Austin William Woodland Geological Society, London, Special Publications, 1, 221-232, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.21 The Devonian period Peter Furneaux Friend and Michael Robert House Geological Society, London, Special Publications, 1, 233-236, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.22 The Silurian period I. Strachan Geological Society, London, Special Publications, 1, 237-240, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.23 The Ordovician period H. B. Whittington and A. Williams Geological Society, London, Special Publications, 1, 241-254, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.24 The Cambrian period J. W. Cowie Geological Society, London, Special Publications, 1, 255-258, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.25 GENERAL DISCUSSION OF PAPAERS IN PART 4S Geological Society, London, Special Publications, 1, 259, 1 January 1964, https://doi.org/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, 1 January 1964, https://doi.org/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, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.28 Items Geological Society, London, Special Publications, 1, 269-442, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.29 Erratum Errata Geological Society, London, Special Publications, 1, 443, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.01 Corrigenda Geological Society, London, Special Publications, 1, 444, 1 January 1964, https://doi.org/10.1144/GSL.SP.1964.001.01.30
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  • 8
    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
    Location: AWI Archive
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  • 9
    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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  • 10
    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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  • 11
    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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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-108
    In: Research report / Cold Regions Research and Engineering Laboratory, 108
    Description / Table of Contents: Summary: The theory of snow densification is further developed on the basis of an exponential relation between viscosity and density. A linear relation between load-stress and strain rate is not valid for high stresses, and is replaced by a hyperbolic sine function. An empirical function is given for the temperature cycle correction. Two equations are derived for calculating depth-density curves with computers, and a simplified one for use with desk calculators. Instructions are given for determination of function parameters from field data. Four depth-density curves for Greenland and Antarctic locations are computed and graphed to show that the theory is useful.
    Type of Medium: Series available for loan
    Pages: iv, 18, A3, B5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 108
    Language: English
    Note: CONTENTS Preface Summary Introduction Notation Stress analysis Analysis of densification process Non-Newtonian densification Equation for hyperbolic sine densification law Determination of parameters Discussion Glaciological engineering aspects References Appendix A: Example of calculation Appendix B: Snow density profiles
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  • 13
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-110
    In: Research report / Cold Regions Research and Engineering Laboratory, 110
    Description / Table of Contents: Summary: Nafe's (1957) presentation of reflection and transmission coefficients at a solid-solid interface was used to compute tables for the case of ice in contact with another solid at a plane interface. Energy ratios of all the combinations of reflected and refracted plane P and S waves were computed for 30 different cases of the second solid. A compressional velocity of 3.6 km/sec, a density of 0.9 g/cm^3, and a value of 1/3 for Poisson's ratio were assumed for the ice. For the other solid, the velocity ranged from 1.2 to 6.0 km/sec, the density from 1.5 to 3.0 g/cm^3, and Poisson's ratio from 0 to 1/3. The computations were carried out with an electronic computer, and the results are presented graphically.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 110
    Language: English
    Note: CONTENTS Preface Summary Introduction Definitions Computation Results
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  • 14
    Call number: ZSP-202-111,1
    In: Research report / Cold Regions Research and Engineering Laboratory, 111,1
    Description / Table of Contents: Summary: Optical scintillation, visual resolution, and wind and temperature profiles were measured over snow, ice and frozen ground. The data were analyzed to determine relationships between (1) scintillation and visual resolution and (2) scintillation and meteorological and surface conditions. The experimental results included (1) estimates of the limit of visual resolution, (2) telephotometer measurements of the apparent fluctuations in brightness (scintillation) of an artificial light source, and (3) measurements of wind direction and of the vertical distributions of wind speed and temperature. The optical path was 543 m long and 1.5 m above uniform horizontal surfaces. All scintillation and meteorological data are given in an appendix. The principal results of the analysis showed that for turbulent flow in stable stratification over snow (1) visual resolution deteriorated systematically as scintillation increased in intensity and (2) scintilliation intensity increased with increase in vertical temperature gradient. Scintilliation was at a minimum in the absence of thermal stratification and at a maximum (in very stable thermal stratification) during the sudden transition from laminar to turbulent flow. For a given temperature gradient, scintilliation increased with increase in wind speed. When wind and temperature gradients were combined in terms of the Richardson number and related to scintilliation, the data obtained over snow indicated a critical Richardson number of about 0.35. Scintilliation power spectra for eight periods revealed characteristics that could be related to visual resolution, the Richardson number and the mean wind speed component normal to the optical path. NOTE: This file is large. Allow your browser several minutes to download the file.
    Type of Medium: Series available for loan
    Pages: iii, 32, A17, B44 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 111,1
    Language: English
    Note: CONTENTS Preface Page Summary Introduction The problem Previous work Plan of the investigation Conclusions Visual resolution and scintillation Visual resolution and wind, temperature, and surface conditions Visual resolution and height and length of optical path Results Measurements Analysis and discussion Visual resolution and scintillation relationships Scintillation and micrometeorological parameters Index of refraction fluctuations Scintillation and the temperature profile Scintillation and average wind speed Combined effects of wind speed and temperature gradient Scintillation and surface roughness Scintillation power spectra Scintillation and path length References Appendix A: Equipment and procedures Appendix B: Micrometeorological and scintillation data
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  • 15
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-112
    In: Research report / Cold Regions Research and Engineering Laboratory, 112
    Description / Table of Contents: Summary: The age hardening of artificially and naturally compacted snow has been investigated at the South Pole. Results show that the age-hardening process is greatly retarded at low temperatures. Artificially compacted samples of density 0.55 g/cm^3 attained a compressive strength of less than 3.0 kg/cm^2 after one year's aging at -49°C. Exposure to solar radiation accelerated the age hardening. Irradiated samples attained a strength of 6.0 kg/cm^2 after 100 hr, increasing to a virtual maximum of 8.0 kg/cm^2 at 600 hr. Compressive strengths increased witha decrease in snow-particle size and with an increasing angularity of the particles. Below 3 m the strength of naturally compacted snow was found to increase rapidly with an increase in density. Naturally compacted snow of density 0.55 g/cm^3 possessed considerably greater strength than any of the age-hardened samples of artificially compacted snow of the same density. Thin-section studies show that age hardening can be correlated with the formation and growth of intergranular bonds, and that bond growth falls off rapidly with decreasing temperature. In view of the low strength found in both naturally and artificially compacted snow at the South Pole, "cut-and-cover" undersnow camp construction may not prove practical at the South Pole.
    Type of Medium: Series available for loan
    Pages: v, 19, A6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 112
    Language: English
    Note: CONTENTS Preface Summary Introduction Previous work Experimental methods Experimental results Series A Series B Series C Series D Series E Discussion Conclusions References Appendix A
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  • 16
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-101
    In: Research report / Cold Regions Research and Engineering Laboratory, 101
    Description / Table of Contents: Partial Summary: This paper is a pilot study of interrelations between structural features readily observed in horizontal thin sections of sea ice under low magnification. The core studied was 31.4 cm in length and was collected from Elson Lagoon at Point Barrow, Alaska on 26 October 1960.
    Type of Medium: Series available for loan
    Pages: iv, 11 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 101
    Language: English
    Note: CONTENTS Preface Summary Introduction Petrographic characteristics Intercrystalline features Intracrystalline features References
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  • 17
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-103
    In: Research report / Cold Regions Research and Engineering Laboratory, 103
    Description / Table of Contents: Summary: The effect of air flow on the thermal conductivity of snow was investigated. Steady-state temperature measurements were made along the edge and axis of a cylindrical bed of snow to determine the effective axial thermal conductivity of snow. Unconsolidated snow samples were used, with densities ranging from 0.376 to 0.472 g/cm^3 and corresponding snow particle sizes of 0.065 to 0.219 cm nominal diameter; the mass flow rates employed ranged from approximately 10-40 x 10^-4g/cm^2 sec. Snow density and sample size apparently have opposite effects on the effective thermal conductivity because of the flow of fluid in snow. The test apparatus is described in detail and is illustrated. The results of the experiments are tabulated, and a least square equation is given which represents the results well.
    Type of Medium: Series available for loan
    Pages: iv, 14, A2 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 103
    Language: English
    Note: CONTENTS Preface Summary Introduction Theory Apparatus and experimental procedure Results and discussion References Appendix A: Sample calculations of a and ke
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  • 18
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-105
    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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  • 19
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-107
    In: Research report / Cold Regions Research and Engineering Laboratory, 107
    Description / Table of Contents: Summary: The formation of lake ice was studied during the winter of 1956-57 at Post Pond, Lyme, N. H. Tabular, columnar, granular, and crenulate textures of 36 blocks of ice observed are discussed in terms of relative growth velocity and shown in a classification chart. Ice structures are characterized by Forel striations, Tyndall figures, bubbles and strain shadows. Average crystal areas increased with ice thickness, the rate of increase being greater toward lake center, and ceased to enlarge when in a continuous bubble layer. The lake-ice sheet grew both from top and bottom, .downward growth resulting from crystals in a favorable vertical orientation of a-axes and upward growth coming about by water flowing on the original upper ice surface and freezing. Exception to this type of growth was found in the lake area which froze first, where individual crystal areas were larger at the surface and there was no upper surface ice accretion. Fabric diagrams of ice outside the anomolous area show a change of optic axis orientation from a high percentage of c-axes vertical near the surface to a high percentage horizontal at the bottom.
    Type of Medium: Series available for loan
    Pages: iv, 22, A2, B1 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 107
    Language: English
    Note: CONTENTS Preface Summary Description of the lake Cli rna te of the lake Methods of study Ice textures Crystal size Ice structures Crystal fabric studies Growth of an ice sheet References Appendix A: Weather data Appendix B: Sample data
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-99
    In: Research report / Cold Regions Research and Engineering Laboratory, 99
    Description / Table of Contents: Summary: A study of how age hardening affects the various mechanical properties of processed snow was made. A description of how the age hardening process is affected by the variables of density, temperature, grain size, and shape is given. An empirical equation relating creep rate to stress, age, and density was obtained. The study also shows that the various mechanical properties are related to age by an exponential function.
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    Pages: iv, 12 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 99
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental facilities Experimental in-place measurements Density and homogeneity of processed snow Ram hardness Temperature measurements Mechanical properties Unconfined compressive strength Stress-strain relationships in unconfined compress ion Creep in unconfined compression Tensile strength Discussion of results References
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  • 21
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-100
    In: Research report / Cold Regions Research and Engineering Laboratory, 100
    Description / Table of Contents: From the Summary: During the summer of 1960, observations were made of ground fog on the Greenland Ice Cap and of sea fog in the Thule area in northwestern Greenland. A microscope-stage-fog impactor was designed, and its collection efficiency determined both empirically and by computation from the theoretical work of Langmuir and Blodgett (1946). The empirical efficiency was found to be considerably greater than the theoretical efficiency.
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    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 100
    Language: English
    Note: CONTENTS Preface Summary Introduction Method Design and operation of the impactor Collection efficiency Computation from theoretical values of Langmuir and Blodgett Empirical values Observations and results Fog on the ice cap Sea fog near Thule Discussion Conclusions References
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  • 22
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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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  • 23
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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.
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    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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  • 24
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    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.
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    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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    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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    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.
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    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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    Call number: ZSP-202-78
    In: Research report / Cold Regions Research and Engineering Laboratory, 78
    Description / Table of Contents: Summary: This climatological study makes use of the temperature, wind, and precipitation records from 12 stations on the Greenland Ice Sheet. Many of these stations were not in operation for concurrent periods and records for a year or more were available from only a few of them. The mean, mean maximum, mean minimum, absolute maximum, and absolute minimum temperatures were computed from the records. The highest absolute maximum temperature reported was 44°F at Mint Julep in southwestern Greenland. The lowest absolute minimum was -94°F at Northice in northern Greenland. This study shows that the prevailing wind usually was from the direction of the high central area of the ice sheet. Stations on the west slope had prevailing winds with an easterly component whereas stations on the east slope had prevailing winds with a westerly component. The wind speed varied from 0 to approximately 60 kt, but was predominantly in the 0 to 20 kt range. At some of the stations on the ice sheet, precipitation was measured in precipitation gages, at others it was measured as surface accumulation. At many locations the annual accumulation was determined from stratigraphic studies of the snow profile. The number of days on which snow occurred, expressed as percent of total days of observation, was used as an index to the amount of snowfall. The mean annual accumulation shows precipitation to be heavier on the west slope of the ice sheet than in other areas. The precipitation records at Northice indicate that the annual precipitation in that part of northern Greenland may be very light. The means for the various climatological parameters covered in this study are presented in tables and on a climatological map which presents a cartographic picture of the overall climatology of the Greenland Ice Sheet.
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    Pages: iv, 13, A5, B4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 78
    Language: English
    Note: CONTENTS Preface Summary Introduction Air temperature Wind direction and speed Precipitation and accumulation Climatological map for the Greenland Ice Sheet Appendix A: Temperature data Appendix B: Precipitation data
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    Call number: ZSP-202-74
    In: Research report / Cold Regions Research and Engineering Laboratory, 74
    Description / Table of Contents: Summary: The heat exchange of a snow cover was studied with respect to the effects of heat transfer processes on metamorphic action within the snow cover and the prediction of heat fluxes and the resulting changes in snow cover characteristics from standard meteorological information. Data collected at the USA SIPRE Keweenaw Field Station, Houghton, Michigan, were used to determine heat transfer by thermal radiation, convection, and conduction. The percent of daily incident solar radiation at the outer limits of the earth's atmosphere which reaches the snow surface ranged from 94 with clear skies to less than 20 with an overcast less than 1000 ft high and precipitation. Average diurnal patterns of total solar radiation may be estimated for various cloudiness. Total solar radiation with overcast clouds less than 5000 ft high averaged about 70% of the clear-sky radiation. Atmospheric radiation related to temperatures during clear nights gave a curve paralleling the black body radiation curve, although about 7 ly/hr lower in absolute values. Atmospheric radiation during clear skies was about 9 ly/hr less than that with low overcast conditions with no snow falling. In the presence of falling snow, total hemispherical radiation was about 5 ly/hr greater than with no snow falling but with' similar low overcast cloudiness. With low overcast cloudiness, the net long-wave exchange averaged about -17 ly/day in January and -8 ly/day in February. With clear skies the net long-wave exchange averaged about -128 ly/day in January and -120 ly/day in February. The net radiation exchange with clear skies during midday remained slightly negative in January and became increasingly positive through February. The highest positive values of net radiation occurred during the day with low overcast or broken cloudiness and precipitation. The largest net radiational loss of 9 ly/hr occurred at night with clear skies and nearly calm winds. The average magnitude of surface temperature inversions over snow was related to observations of cloudiness and wind speeds for both day and night. With winds of 12 knots or greater, the temperature difference in the first 10m was usually near adiabatic even with clear skies at night. During the day inversions seldom exceeded 1-2°C, and a slight lapse commonly occurred during low overcast conditions and moderate winds. The Liljequist method for computing turbulent heat transfer and conductive heat transfer in snow was used. Average air temperature is shown to exert a pronounced effect upon snow heat conduction, cold content and temperature profile. Average temperature differences through the snow, responsible for metamorphic action leading to the formation of depth hoar, can be estimated by a knowledge of the previous 20-hr average temperature. Snow hardness distributions, indicators of supporting capacity of snow, can be estimated graphically from snow density and depth observations.
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    Pages: v, 73 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 74
    Language: English
    Note: CONTENTS Preface Summary Part 1. Data analysis Introduction Estimating snow temperature distributions from meteorological information Radiative heat transfer Short-wave radiation Long-wave radiation Net radiation exchange Convective heat transfer Liljequist method Monin-Obukhov method Conductive heat transfer Heat transfer in soil Heat transfer in snow Direct relationships Measurement of snow properties Cold content of snow Vertical temperature gradient in snow and its effects Snow hardness Summary of the analysis Thermal radiative heat transfer Convective heat transfer Heat transfer processes in soil and snow Part II. Tabulated data for Keweenaw Field Station Description of data Location and periods of measurement Instrumentation Data processing Explanation of tables Thermal radiation data, Keweenaw Field Station References
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-80
    In: Research report / Cold Regions Research and Engineering Laboratory, 80
    Description / Table of Contents: From the Introduction: During the last few years, there has been an increased interest in developing a rational explanation for the rather considerable variation in such bulk properties of sea ice as its strength, density, thermal conductivity, latent heat of melting, and coefficient of thermal expansion. Of these properties, sea-ice strength has received by far the most attention for practical reasons.
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    Pages: iv, 30, A6, B10, C2, D5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 80
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimentation Method of growing salt ice Strength test procedures Bulk properties of salt ice Phase relations Density and air content Strength results Strength of fresh-water ice Strength of NaCl ice as a function of brine volume Strength of NaCl· 2H2O ice as a function of the relative volume of solid salt Effect of thermal history on salt-ice strength Phase hysteresis Geometric hysteresis Effect of short-term cooling on the strength of fresh-water and NaCl·2H2O ice Effect of the volume of inclosed air on the strength of salt ice Conclusions NaCl ice Sea ice References Appendix A: Volume of brine and NaCl· 2H2O in NaCl ice as a function of salinity and temperature Appendix B: Ring test results Normal test sequences Appendix C: Ring test results Hysteresis test sequences Appendix .b: Ring test results Thermal history test sequences
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-85,1
    In: Research report / Cold Regions Research and Engineering Laboratory, 85,1
    In: The frost behavior of soils : laboratory and field data for a new concept, Part I
    Description / Table of Contents: Partial summary: Laboratory experiments have been performed with special cabinets in which soil samples, under complete saturation and without surcharges, were subjected to alternate freezing and thawing cycles. Tests included series with both freezing and thawing from the top and with freezing from the bottom and thawing from the top. The soil materials used were well-graded, sandy gravels, the finest one with 14% finer than no. 200 mesh (0. 074 mm).
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    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 85,1
    Language: English
    Note: CONTENTS Preface Summary Introduction to the problem Laboratory data Preliminary experiments Vertical sorting and volume changes produced by cyclic freeze -thaw Volume increase by sorting in straight graded samples without freezing and thawing Field data Vertical sorting of the active layer Correlation between laboratory and field data Conclusion and recommendations References
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    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.)
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    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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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-71
    In: Research report / Cold Regions Research and Engineering Laboratory, 71
    Description / Table of Contents: Summary: The depth-density relationship of the surface snow to 30-ft depth at three locations on the Greenland Ice Cap east of Thule is presented. Rates of accumulation and densification deduced from the pit studies are used in elementary mathematical expressions developed in this report. These expressions describe a densification process applicable to continuously accumulating polar snow, between the depths of 10 and 40 ft. Loads, densities, and rates of densification are presented in relation to depth and time and applied to problems of undersnow military construction.
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    Pages: iv, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 71
    Language: English
    Note: CONTENTS Preface Summary Introduction Field investigations Application of profile data Densification theory Engineering applications References
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    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.
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    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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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-60
    In: Research report / Cold Regions Research and Engineering Laboratory, 60
    Description / Table of Contents: Summary: This report presents numerical results on the feasibility study of the use of in-ice cooling for a power plant. As a result of this type of arrangement, a water pond under ice is formed. The pond size as a function of time for various operating conditions has been computed. The associated problems such as water temperature, power consumption, etc., are also studied.
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    Pages: iv, 17, A6 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 60
    Language: English
    Note: CONTENTS Preface Summary Introduction Open-loop system Method of analysis Time dependence of pond size Temperature of water in the pond Effect of inlet water temperature Effect of convection duct Power consumption for circulation of cooling water Condlusions Closed-loop system Method of analysis Time dependence of pond size Flow conditions of glycol solutions inside coil Discussion and conclusions References Appendix: Examples of calculations
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-62
    In: Research report / Cold Regions Research and Engineering Laboratory, 62
    Description / Table of Contents: Summary: Adhesive strength of ice for the systems ice/stainless steel and ice/optically flat fused quartz has been investigated as a function of surface roughness of steel surfaces and rates of shear for steel and quartz. The adhesive strength decreases with decreasing roughness of steel surfaces and the force vs time curves for smooth steel plates resemble those of two solids sliding over each other with a liquid layer sandwiched between them. This is particularly so in the case of quartz. The adhesive strength as a function of rate of shear is linear both for ice/stainless steel and ice/quartz; however, there are indications of yield values. The experimental results are in agreement with the assumption of a liquidlike layer on ice. Ratios of viscosity coefficient to the thickness of the layer have been evaluated for both systems and viscosity coefficients are estimated. The importance of interfacial free energy considerations is pointed out.
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    Pages: iii, 10 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 62
    Language: English
    Note: CONTENTS Preface Summary Introduction Experimental Materials Apparatus Experimental results Ice/metal interface Ice/quartz interface Discussion References
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-67
    In: Research report / Cold Regions Research and Engineering Laboratory, 67
    Description / Table of Contents: Summary: The temperature distribution in snow subjected to gamma radiation from an operating nuclear reactor is analyzed mathematically, assuming that the effect of radiation is equivalent to a continuous heat source, the intensity of which is a function of the radial distance from the reactor. Steady-state solutions are derived for two cases: when the radial distance is 13 ft and when it is 19.1 ft. The results indicate that the temperature of the snow in certain regions in the several feet immediately below the foundation will exceed the design limit of 20°F. Increasing the shielding of the reactor will reduce the intensity of the radiation and snow temperature. Other possible ways to reduce the snow temperature include the use of refrigeration coils and the forcing of the atmospheric air through the snow.
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    Pages: iii, 4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 67
    Language: English
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
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    Call number: ZSP-202-61
    In: Research report / Cold Regions Research and Engineering Laboratory, 61
    Description / Table of Contents: Summary: The results of experiments on the bonding of polished and microtomed surfaces of bubble-free ice samples at -5°C with various loads are reported. Only a small part of the available surface area appeared to be bonded, this area increasing with the bonding load. Surfaces apposed immediately after preparation showed an appreciably higher force of separation than those joined after a time interval. The force of separation for surfaces placed together at 0% relative humidity was higher than that at 100% relative humidity. A simplified theory of bonding of irregular ice surfaces is formulated in the appendix. The calculations are based on the assumption of a distribution of small ice cylinders of equal cross sections but different heights located on a non-deformable plate. The cylinders are deformed by a constant force which is applied by another completely non-deformable flat plate. The deformation as a function of force and time and the force of separation as a function of load are derived, assuming that the distribution of heights is given by a box distribution (i.e., frequency of heights is constant).
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    Pages: iv, 6, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 61
    Language: English
    Note: CONTENTS Preface Summary Introduction Materials Apparatus and procedure Results Discussion References Appendix: Compression of an assembly of cylinders
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    Wilmette, Ill. : Snow Ice and Permafrost Research Establishment, Corps of Engineers, U.S. Army
    Associated volumes
    Call number: ZSP-202-63
    In: Research report / Cold Regions Research and Engineering Laboratory, 63
    Description / Table of Contents: Summary: Experiments have been carried out on the plastic deformation of thick-walled snow-ice cylinders under hydrostatic pressure as a function of pressure and temperature. At constant circumferential stress and temperature the natural strain rate of closure is a constant. This constant varies with the circumferential stress according to a sine function and is exponentially dependent on temperature with an energy of activation of 14.1 kcal/mole at an average circumferential stress of 3.1 kg/cm^2. The mechanism of the plastic flow is in agreement with a mechanism proposed previously, that is, flow between grain boundaries takes place.
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    Pages: iv, 7 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 63
    Language: English
    Note: CONTENTS Preface Summary Experimental Materials Apparatus Experimental results Deformation under constant hydrostatic pressure Deformation as a function of hydrostatic pressure Deformation as a function of temperature at constant pressure Discussion References
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  • 39
    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-202-69
    In: Research report / Cold Regions Research and Engineering Laboratory, 69
    Description / Table of Contents: Summary: The relations between rate of snow accumulation, snow density, snow age, and depth below the surface are formulated in terms of a compactive viscosity factor, which is assumed to be a function of only density and temperature, with parameters which will vary with the snow-type sequences of different climatic areas of high polar glaciers. The theory could be useful in an analysis of the data obtained from the large number of snow pits in Greenland, Ellesmere Island,and Antarctica.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 69
    Language: English
    Note: CONTENTS Preface Summary Introduction The Sorge depth-density curve Generalization for time-variable rate of accumulation Path of a particle on the surface y=B(h,t) Effect of temperature Computational procedure Densification under high loads References
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  • 40
    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-202-64
    In: Research report / Cold Regions Research and Engineering Laboratory, 64
    Description / Table of Contents: Summary: The distribution of temperature throughout an idealized ice cap is studied. The idealized ice cap is considered as one with a constant growth rate, without internal movement, subject to a linear climatic change and to a constant geothermal influx. The problem is treated as a Stefan-type problem and the solution is obtained by the principle of superposition. The results indicate that the temperature at the base of the ice cap rises with time and eventually would reach the melting point of the ice. Under such conditions, it is concluded that the ice cap is not resting on a permafrost base as suggested by previous investigation.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 64
    Language: English
    Note: CONTENTS Preface Summary Introduction Mathematical development Method of solution Discussion of results Base temperature Minimum temperature Effect of rate of growth Effect of geothermal influx Comparison with observed results References
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  • 41
    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-202-66
    In: Research report / Cold Regions Research and Engineering Laboratory, 66
    Description / Table of Contents: Summary: A simple theory is proposed for crack formation and development by soil desiccation on the basis of laboratory experiments utilizing soil samples (Bloomington till) with max particle size of 1 mm diam. held in flat wooden containers. The crack pattern is more dependent on the thickness of the soil sample than on temperature or humidity. Some effect is caused also by differences in the bottom material of the containers. The area of cells made by crack patterns has a log normal size distribution. Total length of cracks decreases with increase in sample thickness. The number of sides of cells also depends on the thickness. Cracking was found to begin from the center of the soil layer and to propagate to the surface or bottom with non-uniform speed.
    Type of Medium: Series available for loan
    Pages: vi, 48, A4 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 66
    Language: English
    Note: CONTENTS Preface Summary Introduction Soil material Soil Preparation of the soil material Containers Temperature and humidity of the air Moisture content and dry density of the soil Experimental procedures and results General procedures Definition of the characteristics of cracking of soil Cracking moisture content Size of cells made by cracking of the soil Length of cracks Number of sides of cells Development of cracks Additional experiments Interfacial fracture markings Method of auxilliary tests on physical properties of the soil Elastic constants of the soil Shrinkage of soil due to desiccation Tests of the adhesion between the soil and the bottom material Results of auxiliary tests Elastic constants of the soil Free shrinkage process of the soil due to desiccation Adhesion between the soil and glass or wood Mechanism of crack formation due to the desiccation of soil Geometric interpretation Mechanical interpretation Conclusions References Appendix: Table of experiments
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  • 42
    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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  • 43
    Call number: MOP 46980 / Mitte
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    Language: English
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  • 44
    Monograph available for loan
    Monograph available for loan
    New York : MacMillan
    Call number: MOP 43086 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XIV, 170 Seiten
    Language: English
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  • 45
    facet.materialart.
    Unknown
    Akademie-Verlag
    In:  Veröffentlichungen des Instituts für Bodendynamik und Erdbebenforschung in Jena | ESC-Proceedings
    Publication Date: 2020-02-12
    Language: German , English , French , Russian
    Type: info:eu-repo/semantics/conferenceObject
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  • 46
    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
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  • 47
    Series available for loan
    Series available for loan
    Hanover, New Hampshire : U.S. Army Material Command, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-145
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 145
    Description / Table of Contents: An analysis is made of the time required to build up an ice-age ice sheet and of the time required to destroy such an ice sheet. The calculations are based on the approximation that the theory of perfect plasticity is valid. It is concluded that the time required to eliminate it. If it is assumed that the accumulation rate of an ice-age ice sheet lies of a large ic sheet is of the order of 15.000 to 30.00 years. Ablation rates of 1 to 2 meters/year lead to shrinkage times of the order of 2000 to 4000 years, provided ablation occurs over an appreciable area of the ice sheet.
    Type of Medium: Series available for loan
    Pages: 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 145
    Language: English
    Note: Contents: Preface. - Summary. - Introduction. - Basis of theory. - Basic equations. - Ice sheets with only accumulation or ablation. - Growing ice sheets which contain only an accumulation zone. - Shrinking ice sheets which contain only an ablation zone. - Comments. - Ice sheet with both accumulation and ablation zones. - Growing ice sheets. - Shrinking ice sheets. - Conclusions. - References.
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  • 48
    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-202-70
    In: Research report / Cold Regions Research and Engineering Laboratory, 70
    Type of Medium: Series available for loan
    Pages: 93 Seiten , Karten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 70
    Language: English
    Note: CONTENTS: Preface. - Summary. - Chapter I. Introduction. - Operations and logistics. - Chapter II. Methods of investigation. - Region of investigation. - Pit studies. - Elevation measurements. - Chapter Ill. Stratigraphy and accumulation. - Introduction. - Diagenesis without melt. - Diagenesis with melt. - Diagenetic facies defined on glaciers. - Grain size. - Description of three stratigraphic features. - Principles of stratigraphic interpretation. - Selection of a reference datum in the annual stratigraphic sequence. - Stratigraphic correlation. - Distribution of annual accumulation. - Independent checks on the stratigraphic interpretations. - Chapter IV. Temperature distribution. - Seasonal temperature variation on the snow surface. - Seasonal temperature variation below the snow surface. - Distribution of mean annual temperature on the ice sheet. - Chapter V. Diagenetic facies- a classification of glaciers. - Temperature. - Hardness. - Density. - Glacier facies - a classification of glaciers. - Chapter VI. Densification of snow and firn. - Load-volume relationship. - Depth-density relationship. - Chapter VII. Climatological implications. - Introduction. - Katabatic winds and accumulation. - Annual heat exchange. - The balance of the Greenland Ice Sheet. - References. - Appendix A: Stratigraphy, meteorology and glaciology. - Appendix B: Mean annual temperature. - Appendix C: The data sheets.
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  • 49
    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
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  • 50
    Call number: MOP 28519/4
    In: Detailed analyses of selected Pacific storms based on continuous radar records and short-interval serial ascents, Nr. 4
    In: Technical report / University of Washington, Department of Meteorology and Climatology, Nr. 6
    In: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, 62-448
    Type of Medium: Series available for loan
    Pages: VII, 72 S , graph. Darst., Kt
    Series Statement: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force 62-448
    Language: English
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  • 51
    Call number: MOP 28519/2
    In: Detailed analyses of selected Pacific storms based on continuous radar records and short-interval serial ascents, Vol. 2
    In: Technical report / University of Washington, Department of Meteorology and Climatology, Nr. 4
    In: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, 62-243
    Type of Medium: Series available for loan
    Pages: VII, 46 S , graph. Darst., Kt
    Series Statement: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force 62-243
    Language: English
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  • 52
    Call number: MOP 28519/3
    In: Detailed analyses of selected Pacific storms based on continuous radar records and short-interval serial ascents, Vol. 3
    In: Technical report / University of Washington, Department of Meteorology and Climatology, Nr. 5
    In: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, 62-447
    Type of Medium: Series available for loan
    Pages: VII, 64 S , graph. Darst., Kt
    Series Statement: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force 62-447
    Language: English
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  • 53
    Call number: MOP 28519/5
    In: Detailed analyses of selected Pacific storms based on continuous radar records and short-interval serial ascents, Vol. 5
    In: Technical report / University of Washington, Department of Meteorology and Climatology, Nr. 7
    In: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, 62-469
    Type of Medium: Series available for loan
    Pages: VII, 55 S , graph. Darst., Kt
    Series Statement: AFCRL / Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force 62-469
    Language: English
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  • 54
    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Translations
    Call number: AWI A7-98-0092 ; PIK N 456-99-0205 ; MOP 35101
    Type of Medium: Monograph available for loan
    Pages: 200 S. : graph. Darst.
    Series Statement: IPST 1031
    Uniform Title: Fizika pogranichonogo sloya atmosfery 〈engl.〉
    Language: English
    Note: Contents: Preface. - Introduction. - I. THE EQUATIONS OF HYDROTHERMODYNAMICS OF THE BOUNDARY LAYERS; ANALYSIS OF THESE EQUATIONS. - § 1. Derivation of the Equations for the Averaged Quantities. - § 2. The Relation Between Fluctuations of the Meteorological Elements and the Averaged Characteristics. Currents of Various Substances Due to Turbulence. - § 3. Some Problems of Turbulence Dynamics. The Reynolds Number. The Richardson Number § 4. Classification of Motions. Estimation of the Thickness of the Planetary Boundary Layer. The Surface Sublayer. - II. THE BOUNDARY LAYER OF THE ATMOSPHERE IN STATIONARY CONDITIONS. - § 1. Some Information on the Distribution of the Meteorological Elements in the Boundary Layer. - § 2. External Factors Determining the Structure of the Boundary Layer of the Atmosphere. - § 3. A Boundary Layer Model with Height-Independent Turbulence Coefficient (One-Parameter Model). - § 4. The Structure of the Surface Sublayer. - § 5. Calculation of the Basic Characteristics of the Surface Sublayer. - § 6. Two-Parameter Model of the Boundary Layer of the Atmosphere. - § 7. Some Information on the Processes at the Active Surface and in the Upper Layers of the Ground Influencing the Boundary Layer. - III. DAILY VARIATION OF THE METEOROLOGICAL ELEMENTS. - § 1. The Simplest Model for the Daily Temperature Variation. Features of the Daily Temperature Variation Over Water. - § 2. Daily Temperature Variations for Turbulent Mixing Intensity Growing with Height. - § 3. An Account of the Time Variations of the Eddy Exchange in the Theory of the Daily Temperature Variations. - § 4. The Influence of the Radiative Heat Influx on the Daily Temperature Variation. - § 5. Nocturnal Lowering of the Temperature. Forecasting of Radiation Frosts. - § 6. Daily Humidity Variations. Radiation Fogs. - § 7. Daily Variations of Wind Velocity. - IV. VARIATIONS OF METEOROLOGICAL FIELDS DUE TO THE INHOMOGENEITY OF THE ACTIVE SURFACE. - § 1. Qualitative Analysis of the Transformation Process. - § 2. Variations of the Temperature and Humidity Fields Over an Inhomogeneous Underlying Surface. - § 3. Formation of Advection Fogs. - § 4. Variations of the Micrometeorological Regime in Irrigation, Irrigation Standards for Various Meteorological Conditions. - § 5. Influence of Small Reservoirs on the Structure of the Lower Layers of the Atmosphere. - § 6. Nonstationary Processes Over An Inhomogeneous Underlying Surface. - § 7. Local Winds. - V. PHENOMENA AND PROCESSES OF A SPECIAL NATURE RELATED TO THE METEOROLOGICAL REGIME OF THE BOUNDARY LAYER. - §1. Wind Drift of Ice Floes. - § 2. Applications of the Laws of the Boundary Layer of the Atmosphere to Problems of Construction and Power Engineering. - § 3. Freezing of the Upper Layer of the Ground. - § 4. Pollution of the Lower Layers of the Atmosphere by Smoke From Factory Chimneys. - § 5. Some Features of the Electrostatic Field in the Surface Layer of the Atmosphere. , Transl. from Russian
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  • 55
    Call number: MR 17.91138
    Type of Medium: Monograph available for loan
    Pages: [167 S.]
    Language: English
    Note: 1. Deutscher Landesbericht (DDR) für die XIII. Generalversammlung der IUGG in Berkeley/Cal. 1963, Fachgruppe Geomagnetismus und Aeronomie 2. Bericht über die Sitzung des Europäischen Seismologischen Kommission (ESC), Assoziation für Seismologie und Physik des Erdinnern der IUGG 3. IQSY-Beauftragter: Übersicht über die bisher (Stand vom 1.2.65) von DDR-Instituten im Rahmen der IQSY-Verpflichtungen des NKGG an die Weltdatenzentren versandten Beobachtungsmaterialien und Sonderdrucke wissenschaftlicher Veröffentlichungen 4. Nr. I/3: Final Report on IQSY Activities in the German Democratic Republic 1964-1965 (Presented by G. Cumme and E. A. Lauter) 5. IQSY-Activities in the GDR: Report to the IV Assembly of the Special Committee for the IQSY, London 1967 (Compiled by Cumme, G. und Wagner, C.-U.) , 1. Deutscher Landesbericht (DDR) für die XIII. Generalversammlung der IUGG in Berkeley/Cal. 1963, Fachgruppe Geomagnetismus und Aeronomie 2. Bericht über die Sitzung des Europäischen Seismologischen Kommission (ESC), Assoziation für Seismologie und Physik des Erdinnern der IUGG 3. IQSY-Beauftragter: Übersicht über die bisher (Stand vom 1.2.65) von DDR-Instituten im Rahmen der IQSY-Verpflichtungen des NKGG an die Weltdatenzentren versandten Beobachtungsmaterialien und Sonderdrucke wissenschaftlicher Veröffentlichungen 4. Nr. I/3: Final Report on IQSY Activities in the German Democratic Republic 1964-1965 (Presented by G. Cumme and E. A. Lauter) 5. IQSY-Activities in the GDR: Report to the IV Assembly of the Special Committee for the IQSY, London 1967 (Compiled by Cumme, G. und Wagner, C.-U.)
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  • 56
    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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  • 57
    Monograph available for loan
    Monograph available for loan
    Washington : U. S. Dept. of Commerce, Weather Bureau
    Call number: PIK N 456-17-90921
    Type of Medium: Monograph available for loan
    Pages: 71 Seiten , Diagramme, Karten , 26 cm
    Edition: Rev.
    Series Statement: U. S. Department of Comerce / Weather Bureau : Technical Paper 20
    Language: English
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  • 58
    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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  • 59
    Monograph available for loan
    Monograph available for loan
    [Tucson, Ariz.] : The University of Arizona, Institute of Atmospheric Physics
    Call number: PIK N 456-17-90925
    Type of Medium: Monograph available for loan
    Pages: iv, 96 Seiten , Karten, Tabellen , 28 cm
    Series Statement: University of Arizona, Institute of Atmospheric Physics. Technical reports on the meteorology and climatology of arid regions 18
    Language: English
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  • 60
    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Translations; [available from the Office of Technical Services, U.S. Dept. of Commerce, Washington]
    Call number: PIK N 456-16-90134
    Type of Medium: Monograph available for loan
    Pages: iv, 355 S. , Ill., graph Darst. , 24 cm
    Uniform Title: Meteorologičeskij i radiacionnyj režim antarktiky [Meteorologicheskiĭ i radiat︠s︡ionnyĭ rezhim Antarktidy] 〈engl.〉
    Language: English
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  • 61
    Call number: PIK N 456-16-90113
    Type of Medium: Monograph available for loan
    Pages: X, 270 S.
    Language: English
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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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    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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    Call number: G 5517 2.Ex. ; AWI G2-96-0028
    In: The sea ; 3, Vol. 3
    Type of Medium: Monograph available for loan
    Pages: XVI, 963 S. : Ill., graph. Darst., Kt.
    Edition: 1. publ.
    Language: English
    Note: CONTENTS: SECTION I. GEOPHYSICAL EXPLORATION. - 1. ELEMENTARY THEORY OF SEISMIC REFRACTION AND REFLECTION MEASUREMENTS / BY J. I. EWING. - 1. Introduction. - 2. Reflected waves. - 3. Refracted waves. - 4. Computation of layer velocities and thicknesses. - 5. Shear waves and complex refracted waves. - 6. Some complications and deviations from simple theory. - 2. REFRACTION AND REFLECTION TECHNIQUES AND PROCEDURE / BY G.G. SHOR, JR. - 1. Introduction. - 2. Shooting techniques. - 3. Receiving techniques. - 4. Plan of operations. - 5. Miscellaneous variations. - 6. Reflection methods. - 3. SINGLE-SHIP SEISMIC REFRACTION SHOOTING / BY M. N. HILL. - 1. Introduction. - 2 . Instrumentation. - 3. Operation. - 4 . CONTINUOUS REFLECTION PROFILING / BY J. B. HERSEY. - 1. Introduction. - 2. Design. - 3. Operations at sea. - 4. Results. - 5. Interpretations. - 6. Geophysical measurements. - 7. Concluding remarks. - 5. THE UNCONSOLIDATED SEDIMENTS / BY J. I. EWING AND J. E. NAFE. - 1. Introduction. - 2. Evidence for gradients and low-velocity sediments. - 3. Variable angle reflections. - 4. Normal-incidence reflections. - 5. Summary. - 6. THE CRUSTAL ROCKS / BY R. W. RAITT. - 1. Introduction. - 2. Layer 2. - 3. Layer 3. - 4. Average oceanic crust. - 7. THE MANTLE ROCKS / BY J. I. EWING. - 1. Introduction. - 2. Compressional-wave measurements. - 3. Shear-wave measurements. - 4. Summary. - 8. EXPLORATION OF SUB-OCEANIC STRUCTURE BY THE USE OF SEISMIC SURFACE WAVES / BY J. OLIVER AND J. DORMAN. - 1. Introduction. - 2. The general nature of seismic surface waves. - 3. Evidence from mantle surface waves. - 4. Evidence from crustal surface waves. - 5. Evidence from short-period surface waves. - 9. GRAVITY AT SEA / BY J. LAMAR WORZEL AND J. C. HARRISON. - 1. Introduction. - 2. Methods and theory. - 3. Gravity observations and geological interpretations. - 10. THE MAGNETIC FIELD OVER THE OCEANS / BY E. C. BULLARD AND R. G. MASON. - 1. Historical. - 2. Measurement of the magnetic field at sea. - 3. General features of the field. - 4. Reduction of magnetic observations. - 5. The magnetic properties of submarine rocks. - 6. The magnetic surveys of the north-east Pacific. - 7. The continental shelves. - 8. Seamounts and mid-ocean ridges. - 9. The deep trenches. - 11 . THE FLOW OF HEAT THROUGH THE FLOOR OF THE OCEAN / BY E. C. BULLARD. - 1. Method. - 2. The temperature probe. - 3. The thermal properties of sediments. - 4. The results of heat-flow measurements. - 5. Future work. - SECTION II . TOPOGRAPHY AND STRUCTURE. - 12. TOPOGRAPHY OF THE DEEP-SEA FLOOR / BY BRUCE C. HEEZEN AND H. W. MENARD. - 1 . Introduction. - 2 . Outline of submarine topography. - 3. Summary of submarine topographic forms. - 13. CONTINENTAL SHELF AND SLOPE (CONTINENTAL MARGIN) / BY A. GUILCHER. - 1. Definitions. - 2. Topography of the continental shelf. - 3. Topography of the continental slope. - 4. Structure and origins of the continental margins. - 5. Conclusion. - 14. ABYSSAL PLAINS / BY BRUCE C. HEEZEN AND A. S. LAUGHTON. - 1. Introduction. - 2. Regional description. - 3. Trench abyssal plains. - 4. Archipelagic plains. - 5. Abyssal gaps, interplain channels, mid-ocean canyons and deep-sea channels. - 6. Sediments on the abyssal plains. - 7. Geophysical characteristics. - 8. Theories of the origin of the abyssal plains. - 15. OCEANIC ISLANDS, SEAMOUNTS, GUYOTS AND ATOLLS / BY H. W. MENARD AND H. S. LADD. - 1. Introduction. - 2. Oceanic islands. - 3. Seamounts. - 4. Guyots. - 5. Atolls. - 6. Submerged atolls. - 7. Oceanic volcanoes in geological time. - 8. Importance of islands and seamounts. - 16. THE MID-OCEANIC RIDGE / BY BRUCE C. HEEZEN AND MAURICE EWING. - 1. Introduction. - 2. North Atlantic. - 3. South Atlantic. - 4. Indian Ocean. - 5. Indian and South Pacific Oceans. - 6. Iceland and the Norwegian Sea. - 7. Arctic Basin. - 8. Crustal structure. - 9. Origin. - 17. TRENCHES / BY R. L. FISHER AND H. H. HESS. - 1. Previous work. - 2. Topography of trenches. - 3. Structure of trenches. - 18. MICROTOPOGRAPHY / BY A. S. LAUGHTON. - 1. Introduction. - 2. Classification of microtopographic features. - 19. UNDERWATER PHOTOGRAPHY / BY H. E. EDGERTON. - 1. Introduction. - 2. Camera details. - 3. Cables and winches for cameras. - 20. SUBMARINE CANYONS / BY F. P. SHEPARD. - 1. Introduction. - 2. Classification of submarine valleys. - 3. Canyon descriptions. - 4. East coast U.S. (New England type) canyons. - 5. Trough-shaped valleys. - 6. Delta foreset-slope gullies. - 7. Shallow straight-walled valleys of submarine escarpments. - 8. Origin of submarine canyons. - 9. Subaerial erosion. - 10. Pleistocene canyon cutting by turbidity currents. - SECTION III. SEDIMENTATION. - 21. BEACH AND NEARSHORE PROCESSES. - PART I. MECHANICS OF MARINE SEDIMENTATION / BY R. A. BAGNOLD. - 1. Definition, origin and relevant physical properties. - 2. Transport during fall through the sea. - 3. Transport of sediment over the sea bed. - 4. Transport rate and fluid "power". - 5. Auto-suspension of sediment: turbidity currents , etc. - 6. Wave drift. - 7. Threshold of bed disturbance by fluid action. - PART II. LITTORAL PROCESSES / BY D. L. INMAN AND R. A. BAGNOLD. - 8. Introduction. - 9. Littoral profile: two-dimensional case. - 10. Migration of sand grains by wave action. - 11. Littoral processes: three-dimensional case. - 12. Discussion. - 22. SHALLOW-WATER CARBONATE SEDIMENTS / BY R. N. GINSBURG, R. MICHAEL LLOYD, K. W. STOCKMAN AND J. S. MCCALLUM. - 1. Introduction. - 2. Types of skeletal particles. - 3. Skeletal particles in sediments. - 4. Distribution of skeletal particles. - 5. Discussion of the distribution of skeletal particles. - 6. Non-skeletal particles. - 7. Distribution of non-skeletal particles. - 23. BASIN SEDIMENTATION AND DIAGENESIS / BY I. R. KAPLAN AND S. C. RITTENBERG. - 1. Introduction. - 2. Physical aspects of sedimentation. - 3. Diagenesis in sediments. - 4. Isotopic studies related to biological processes in sediments. - 5. Special problems. - 24. ESTUARIES, DELTAS, SHELF, SLOPE / BY A. GUILCHER. - 1. Estuaries, tidal marshes and flats, and deltas. - 2. Continental shelf. - 3. Continental slope. - 25. PELAGIC SEDIMENTS / BY G. ARRHENIUS. - 1. Concept of pelagic sedimentation. - 2. Composition. - 3. Productivity control of pelagic sedimentation. - 4. Physical stratification. - 5. Topographic and tectonic control of sedimentation. - 26. CLAY-MINERAL DISTRIBUTIONS IN THE PACIFIC OCEAN / BY J. J. GRIFFIN AND E. D. GOLDBERG. - 1. Introduction. - 2. The clay minerals. - 3. Surface distribution of clay minerals. - 4. Vertical distribution. - 5. Summary. - 27. TURBIDITY CURRENTS / BY BRUCE C. HEEZEN. - 1. Early views. - 2. Full-scale experiment. - 3. Alternative explanations. - 4. Physiographic evidence. - 5. Sediments. - 6. Requirements of turbidity currents. - 7. Tectonic significance of turbidity currents. - 8. Biological significance of turbidity currents. - 9. Other processes of deep-sea erosion and transportation. - 10. Conclusion. - 28. ORGANIC TRANSPORTATION OF MARINE SEDIMENTS / BY K. O. EMERY. - 1. Introduction. - 2. Kelp. - 3. Driftwood . - 4. Sea mammals. - 5. Fishes. - 6. Birds. - 7. Invertebrates. - 8. Comparison with inorganic transporting agents. - 9. Criteria for recognition of rafting agent. - 29. PHYSICAL PROPERTIES OF MARINE SEDIMENTS / BY J. E. NAFE AND C. L. DRAKE. - 1. Introduction. - 2. Relationships among observables. - 3. Methods of measurement. - 4. Summary of results. - 5. Conclusions. - 30. AGE DETERMINATION IN SEDIMENTS BY NATURAL RADIOACTIVITY / BY F. F. KOCZY. - 1. Introduction. - 2. Theoretical considerations. - 3. Geochemical considerations. - 4. Practical methods of age determination. - 5. Rate of sedimentation. - 31. CROSS-CORRELATION OF DEEP-SEA SEDIMENT CORES AND DETERMINATION OF RELATIVE RATES OF SEDIMENTATION BY MICRO-PALEONTOLOGICAL TECHNIQUES / BY D. B. ERICSON. - 1. Introduction. - 2. Methods of correlation. - 3. Time-equivalence of the faunal zones. - 4. Some example
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    In: Detailed analyses of selected Pacific storms based on continuous radar records and short-interval serial ascents, Vol. 1
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    In: Scientific report / Department of Meteorology and Climatology, University of Washington, Nr. 1
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    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
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    Uniform Title: Issledovanie znachitel'nykh mesyachnykh anomalii temperatury vozdukha na Evropeikoi territorii SSSR
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    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Transl.
    Call number: MOP 35099
    Type of Medium: Monograph available for loan
    Pages: 209 S. : Ill., graph. Darst.
    Uniform Title: Gazovyj Sostav atmosfery zemli i metody ego analiza
    Language: English
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  • 76
    facet.materialart.
    Unknown
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1122-G)
    In: U.S. Geological Survey bulletin
    Pages: IV, G-69 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1122-G
    Language: English
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  • 77
    Monograph available for loan
    Monograph available for loan
    New York
    Call number: MOP 43569
    Type of Medium: Monograph available for loan
    Pages: 101 S. : Ill.
    Series Statement: Transactions of the Institute of Atmospheric Physics
    Uniform Title: Rascet jarkosti sveta v atmosfere pri anizotropnom rassejanii
    Language: English
    Location: MOP - must be ordered
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  • 78
    Monograph available for loan
    Monograph available for loan
    New York : American Geophysical Union
    Call number: MOP 28041
    Type of Medium: Monograph available for loan
    Pages: 181 S.
    Series Statement: Soviet research in geophysics 1
    Uniform Title: Sbornik statej po dinamiceskoj meteorologij
    Language: English
    Location: MOP - must be ordered
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  • 79
    Call number: MOP Per 434(3)
    In: Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam
    Type of Medium: Monograph available for loan
    Pages: IX, 286 S.
    Series Statement: Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam : Meteorologiceskie issledovanija 3
    Uniform Title: Atmosfernye processy v vysokich sirotach juznogo polusarija
    Language: English
    Location: MOP - must be ordered
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  • 80
    Monograph available for loan
    Monograph available for loan
    New York : Consultants bureau
    Call number: MOP 43569 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 103 S. : graph. Darst..
    Series Statement: Transactions of the Institute of Atmospheric Physics 1
    Uniform Title: Rascet jarkosti sveta v atmosfere pri anizotropnom rassejanii
    Language: English
    Location: MOP - must be ordered
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  • 81
    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
    Location: MOP - must be ordered
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  • 82
    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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  • 83
    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Translations
    Call number: MOP 35100
    Type of Medium: Monograph available for loan
    Pages: VIII, 392 S. , graph. Darst.
    Uniform Title: Fizika oblakov
    Language: English
    Note: Aus dem Russ. übers.
    Location: MOP - must be ordered
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  • 84
    Monograph available for loan
    Monograph available for loan
    Jerusalem : Israel Program for Scientific Transl
    Call number: MOP 35102
    Type of Medium: Monograph available for loan
    Pages: 202 S.
    Uniform Title: Metodika sostavlenija prognozov pogody na 3-7 dnej
    Language: English
    Location: MOP - must be ordered
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  • 85
    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
    Location: MOP - must be ordered
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  • 86
    facet.materialart.
    Unknown
    Leiden : Brill
    Associated volumes
    Call number: 91.0801
    In: Italian expeditions to the Karakorum (K) and Hindu Kush : scientific reports
    Pages: XVII, 242 S.
    Series Statement: Italian expeditions to the Karakorum (K) and Hindu Kush : scientific reports Vol. 1
    Language: English
    Branch Library: GFZ Library
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  • 87
    Call number: SR 90.0008(63-49)
    In: Field and laboratory methods used by the Geological Survey of Canada in geochemical surveys
    In: Paper
    Pages: 9 S.
    Series Statement: 63-49
    Language: English
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  • 88
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    Unknown
    Amsterdam [u.a.] : Elsevier
    Call number: G 5475
    Pages: XV, 377 S. : Ill., graph. Darst., Kt.
    Language: English
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  • 89
    Series available for loan
    Series available for loan
    Seattle, Wash.
    Associated volumes
    Call number: MOP 28673
    In: Occasional report / Department of Meteorology and Climatology, University of Washington, No. 13
    Type of Medium: Series available for loan
    Pages: VIII, 79 S. , Ill.
    Series Statement: Occasional report / Department of Meteorology and Climatology, University of Washington 13
    Language: English
    Location: MOP - must be ordered
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  • 90
    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
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 91
    Monograph available for loan
    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
    Location: A 18 - must be ordered
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  • 92
    Series available for loan
    Series available for loan
    Washinton, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1181-M,N)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: Getr. Zählung + 3 pl.
    Series Statement: U.S. Geological Survey bulletin 1181-M,N
    Language: English
    Location: Lower compact magazine
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  • 93
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1028-Q)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 555-562 + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1028-Q
    Language: English
    Location: Lower compact magazine
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  • 94
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1063-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 127-190 + 5 pl.
    Series Statement: U.S. Geological Survey bulletin 1063-E
    Language: English
    Location: Lower compact magazine
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  • 95
    Call number: SR 90.0001(1082-L)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V S., S. 835-891 + 7 pl.
    Series Statement: U.S. Geological Survey bulletin 1082-L
    Language: English
    Location: Lower compact magazine
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  • 96
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1071-I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 341-396, III S. + 3 pl.
    Series Statement: U.S. Geological Survey bulletin 1071-I
    Language: English
    Location: Lower compact magazine
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  • 97
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1081-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III S., S. 91-116 + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1081-C
    Language: English
    Location: Lower compact magazine
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  • 98
    Monograph available for loan
    Monograph available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1081-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Monograph available for loan
    Pages: III S., S. 117-158 + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1081-D
    Language: English
    Location: Lower compact magazine
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  • 99
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1081-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 189-260 + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1081-F
    Language: English
    Location: Lower compact magazine
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  • 100
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0001(1081-G)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 261-280 + 2. pl.
    Series Statement: U.S. Geological Survey bulletin 1081-G
    Language: English
    Location: Lower compact magazine
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