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  • English  (1,920)
  • Russian  (121)
  • Portuguese  (6)
  • Italian  (1)
  • 1975-1979  (2,034)
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Years
Year
  • 1
    Series available for loan
    Series available for loan
    Stuttgart : Schweizerbart
    Associated volumes
    Call number: SR 90.0066(33)
    In: Geologisches Jahrbuch . Reihe A, Allgemeine und regionale Geologie Bundesrepublik Deutschland und Nachbargebiete, Tektonik, Stratigraphie, Paläontologie, 33
    Type of Medium: Series available for loan
    Pages: 159 S. , Ill., graph. Darst., Kt. , 2 Beil.
    Series Statement: Geologisches Jahrbuch / A Heft 33
    Language: German , English , French , Russian
    Note: Mit engl., franz. und russ. Zsfassungen
    Location: Lower compact magazine
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  • 2
    Call number: ZSP-SCAR-570-1
    In: Report to SCAR on Antarctic research activities of Germany (FRG), 1
    Type of Medium: Series available for loan
    Pages: 21 Seiten
    ISSN: 0179-0072
    Series Statement: Report to SCAR on Antarctic research activities of Germany (FRG) 1
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research of the Federal Republic of Germany. - Introduction. - Station. - Field Activities 1974-1979. - Planned Activities 1979/80. - References.
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  • 3
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: MOP 40046 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 113 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 4
    Call number: ZSP-201-76/33
    In: CRREL Report, 76-33
    In: Detecting structural heat losses with mobile infrared thermography / R.H. Munis, S.J. Marshall and M.A. Bush, Part IV
    Description / Table of Contents: During the winter of 1973-74 a mobile infrared thermography system was used to survey campus buildings at Dartmouth College, Hanover, New Hampshire. Both qualitative and quantitative data are presented regarding heat flow through a small area of a wall of one brick dormitory building before and after installation of aluminum reflectors between radiators and the wall. These data were used to estimate annual cost savings for 22 buildings of similar construction having aluminum reflectors installed behind 1100 radiators. The data were then compared with the actual savings which were calculated from condensate meter data. The discrepancy between estimated and actual annual cost savings is explained in detail along with all assumptions required for these calculations.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 76-33
    Language: English
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  • 5
    Call number: MOP 41424 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 31 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 6
    Monograph available for loan
    Monograph available for loan
    Stroudsburg : Dowden, Hutchinson & Ross
    Associated volumes
    Call number: G 8115
    In: Benchmark papers in geology
    Type of Medium: Monograph available for loan
    Pages: XV, 468 Seiten , Illustrationen
    ISBN: 0-471-13540-2
    Series Statement: Benchmark papers in geology 15
    Language: English
    Location: Upper compact magazine
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  • 7
    Monograph available for loan
    Monograph available for loan
    Sofija
    Call number: MOP 44702 / Mitte
    Type of Medium: Monograph available for loan
    Language: Russian
    Location: MOP - must be ordered
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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-201-79/13
    In: CRREL Report, 79-13
    Description / Table of Contents: Heat transfer in turbulent flow was measured in a rectangular channel with a width of 0.254 m and a flow depth of 0.0254 m. Correlations between the Nusselt and Reynolds numbers are given for a range of 3020 Re 22360. A Prandtl number range of 9.90 or = Pr or = 12.28 for water was used in the tests. The results are compared with those of other investigations and show that some well-known correlations underpredict the heat transfer by about 35%.
    Type of Medium: Series available for loan
    Pages: ii, 5 Seiten , Illustrationen
    Series Statement: CRREL Report 79-13
    Language: English
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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-201-79/10
    In: CRREL Report, 79-10
    Description / Table of Contents: Ice cores from Byrd Station and Little America V have been used to test an ultrasonic technique for evaluating crystal anisotropy in the Antarctic Ice Sheet. P-wave velocities measured parallel and perpendicular to the vertical axes of cores from the 2164-m-thick ice sheet at Byrd Station have yielded results in excellent agreement with the observed c-axis fabric profile and with the in-situ P-wave velocity profile measured parallel to the bore hole axis. Velocity differences in excess of 140 m/s for core samples from deeper than 1300 m attest to the strong single pole clustering of crystallographic c-axes about the vertical, especially in the zone from 1300-1800 m. Such oriented structure is compatible only with strong horizontal shearing in this zone. The existence in an ice sheet of widespread shearing several hundred meters above its bed raises serious questions as to the validity of current concepts of the flow of large ice masses that tend to gloss over or ignore crystal alignments of this magnitude.
    Type of Medium: Series available for loan
    Pages: IV, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 79-10
    Language: English
    Note: CONTENTS Abstract Preface Introduction Laboratory measurements Sample sources Ultrasonic velocity measurements Effects of inclined drilling at Byrd Station Results Byrd Station Little America V Summary and conclusions Literature cited
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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-201-78/11
    In: CRREL Report, 78-11
    In: Mechanics of cutting and boring, Part VIII
    Description / Table of Contents: The report deals with forces and power requirements for cutting machines of the belt type, as exemplified by large chain saws and ladder trenchers. The forces of single cutting tools are considered, and related to the overall forces on a cutter bar. Forces are related to power, and sources of loss are identified. Tractive thrust and normal reaction are analyzed and used to assess the traction, weight and balance.
    Type of Medium: Series available for loan
    Pages: vi, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 78-11
    Language: English
    Note: CONTENTS Abstract Preface Foreword Introduction Terminology Tool forces Number of active cutting teeth Tool force and chain force Chain power Tool turce and belt power Tractive thrust and normal reaction Traction of carrier vehicles Power/weight ratio Cutter bar moments Specific energy Performance index Power density Apparent belt pressure Acceleratin and transport of cuttings Examples
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  • 11
    Call number: ZSP-201-76/24
    In: CRREL Report, 76-24
    Description / Table of Contents: Chemical analysis of surface snows and deeper ice core samples from Milcent, Greenland, indicates a marine origin for Na and Cl and a terrestrial origin for Al, Mn and V. Pre-1900 enrichment factors, based on average crustal composition, are high for Zn and Hg and appear to be related to their volatility. A comparison of pre-1900 and 1971-1973 concentrations of V and Hg shows no decided increase from industrial production; however, the abundance of Zn (relative to Al) increased three-fold during this time period. The chemical composition of ancient ice is extremely useful in interpreting modern aerosols.
    Type of Medium: Series available for loan
    Pages: ii, 6 Seiten , Illustrationen
    Series Statement: CRREL Report 76-24
    Language: English
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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-201-76/25
    In: CRREL Report, 76-25
    Description / Table of Contents: The primary objective of this investigation was to compile baseline information pertaining to the ocean circulation, especially the extent and patterns of tidal currents and tidal flushing, in Cook Inlet, Alaska, utilizing aircraft and satellite imagery with corroborative ground truth data. LANDSAT-1 and NOAA-2 and -3 imagery provided repetitive, synoptic views of surface currents, water mass migration and sediment distribution during different seasons and tides. Color, color infrared and thermal infrared imagery acquired on 22 July 1972 with the NASA NP-3A aircraft were used to analyze currents, mixing patterns and sediment dispersion in selected areas. Temperature(C), salinity (0/00) and suspended sediment concentration (mg/l) data and hand-held photography were utilized as ground truth information in the interpretation of the aircraft and satellite imagery. Coriolis effect, semidiurnal tides and the Alaska current govern the estuary circulation. Clear, oceanic water enters the inlet on the southeast during flood tide, progresses northward along the east shore with minor lateral mixing, and remains a distinct water mass to the latitude of Kasilof-Ninilchik. South of the forelands, mixing with turbid inlet water becomes extensive. Turbid water moves south primarily along the north shore during ebb tide and a shear zone between the two water masses forms in mid-inlet south of Kalgin Island. Currents adjacent to and north of the forelands are complicated by tidal action, coastal configuration and bottom effects. Turbulence is greatest throughout the water column along the south shore and stratification is more pronounced in Kamishak and Kachemak Bays, especially when fresh water runoff is high.
    Type of Medium: Series available for loan
    Pages: ix, 92 Seiten , Illustrationen
    Series Statement: CRREL Report 76-25
    Language: English
    Note: CONTENTS Abstract Preface Summary Conversion factors: U.S. customary to metric (SI) units of measurement. Introduction Background Objectives Project history Approach Aircraft imagery LANDSAT-1 imagery NOAA-2 and -3 satellite imagery Ground truth data Imagery and ground truth data analysis Physical and cultural setting Geography Geology Climate Hydrology Local industry and population density Sources of estuarine pollution Results and discussion Coastal configuration Bathymetry Tides Asymmetry of tidal flow/duration across inlet Suspended sediment distribution and circulation Sea ice Tidal flushing characteristics Summary and conclusions Applications Recommendations Literature cited Appendix A. RS-14 infrared scanner imagery
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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-201-76/28
    In: CRREL Report, 76-28
    Description / Table of Contents: Fourier transforms of selected ground-motion time histories from five underground high-explosive and nuclear detonations are used to define the transmission properties (Transfer functions) of three rock types. Absorption, a measure of a rock's energy dissipating characteristics, is expressed for each of the tests as a function of the frequency of transmission. Dispersion results from a variation in transmission velocity with frequency and is described for each test by a phase velocity spectrum. The transmission properties from one of the sites are used to predict a ground-motion time history at that site from another nuclear event. The potential use of Fourier techniques to make ground-motion predictions and to measure in-situ material properties is discussed.
    Type of Medium: Series available for loan
    Pages: vi, 91 Seiten , Illustrationen
    Series Statement: CRREL Report 76-28
    Language: English
    Note: Contents Section I: Introduction Section II: Analytical procedures 1. Fourier transforms 2. Basic transform properties 3. Transform techniques 4. The transfer function Section II: Parameter studies and program evaluations 1. Analytical parameter study 2. I-TRAIN evaluation 3. S-TRAIN evaluation Section IV: Data 1. DATEX I 2. DATEX II 3. STARMET 4. MINERAL LODE 5. HARD HAT and PILEDRIVER Section V: Analysis of transformed data 1. Absorption 2. Dispersion 3. Transfer function Section VI: Fourier synthesis Section VII: Discussion Literature cited Appendix A: The Fourier integral and series Appendix B: Subroutine FOURT used in analysis Appendix C: I-TRAIN and S-TRAIN programs
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  • 14
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/32
    In: CRREL Report, 76-31
    Description / Table of Contents: Four large grounded multi-year shear ridge formations were found in the grounded ice subzone of the fast ice zone near the Harrison Bay/Prudhoe Bay area of Alaska. A 166-m-long cross section of one of these formations was obtained by leveling and sonar measurements. These measurements revealed that the maximum ridge height was 12.6 m and that the formation was grounded in 17-18 m of water. The salinity, temperature, brine volume and density of the ice were determined on samples obtained by coring. The physical characteristics of the formations as observed in satellite, SLAR and aerial imagery indicate that these formations have not moved between the time of their formation in the fall of 1974 and August of 1976. Evidence of significant aeolian debris discoloring the ice is discussed.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 76-32
    Language: English
    Note: Contents Abstract Preface Introduction Background Fast ice study area Results and discussion Literature cited
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  • 15
    Call number: ZSP-201-76/31
    In: CRREL Report, 76-31
    Description / Table of Contents: Sections in the Connecticut River where ice jam potential is high were identified through the use of low-altitude black and white photographs taken during low-flow, ice-free conditions. The hydraulics and mechanics of ice jam initiation were investigated in the river reach where these sections were identified. Certain areas were found in the river that had a high susceptibility to ice clogging, but this high potential decreased with increasing discharge because of the improved surface conveyance of the ice through the reach. The stability of ice floes was established along the channel, but the floes generally became unstable as the flow increased. This was calculated by using a Froude number criterion. Grounding locations for ice became evident when the critical Froude number was zero for a given thickness and water depth. No single factor was determined to be responsible for initiating the ice jams in the Connecticut River at Windsor. Apparently there existed a multitude of interacting conditions: surface constrictions, possible high backwater conditions from the Brattleboro Dam, a solid ice cover in the backwater of the Brattleboro Dam that prevented ice transport from the Windsor area, deep pools followed by shallow depth sections upstream of bridge piers, a greater ice thickness accumulation of fragmented floes than would result if a uniform cover could be established in the same reach, and the diurnal fluctuation of river stage casued by the release of water at Wilder Dam.
    Type of Medium: Series available for loan
    Pages: vi, 39 Seiten , Illustrationen
    Series Statement: CRREL Report 76-31
    Language: English
    Note: CONTENTS Abstract Preface Summary Conversion factors: U.S. customary to metric units of measurement Introduction Testsite Aerial photography Channel morphology — Interpretation of aerial photographs Ground surveys Hydraulic analysis Analysis of ice jam locations Winter field observations Conclusions Literature cited Appendix: Locations and plots of cross sections from Sumner Falls to Chase Island, Connecticut River
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  • 16
    Call number: MOP 44631 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 80 Seiten , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 17
    Call number: MOP 44652 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 61 Seiten , Illustrationen , 20 cm
    Series Statement: Serija Meteorologija / VNII Gidrometeorologičeskoj Informacii - Mirovoj Centr dannych
    Language: Russian
    Note: In kyrillischer Schrift
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  • 18
    Call number: MOP 44808 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 152 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 19
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/41
    In: CRREL Report, 76-41
    Description / Table of Contents: Eight Geoceiver stations were established and suitably marked along or near the crestiline of the Greenland ice sheet during GISP field operations from 1971 to 1975. At one of these stations, DYE-3, repeated Geoceiver positions indicate an ice velocity of 12.7 m.yr on an azimuth of approximately 60 degrees. Data from the International Greenland Glaciological Expedition (EGIG) surveys show that ice flow in the vicinity of Crete is radiating outward from a dome to the south. Two independent calculations of the state of equilibrium at Crete indicate ice sheet thinning rates of 0.25 to 0.37 m/yr, while direct measurement of elevation change by EGIG indicates an ice sheet thickening rate of difference of 0.06 m/yr. Resolution of these differences must await further geophysical work and deep drilling in the ice sheet.
    Type of Medium: Series available for loan
    Pages: iii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 76-41
    Language: English
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  • 20
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/43
    In: CRREL Report, 76-43
    Description / Table of Contents: Ice fog generated at the Eielson AFB power plant cooling pond contributes heavily to the total ice fog problem on the base. Several methods for ice fog suppression were studied and two techniques were tested experimentally. Experiments were also conducted to determine the magnitude of the various modes of heat transfer within the pond's microclimate. Values of evaporative and radiative heat loss during ice fog are presented. Ice cover is shown to be an effective ice fog suppression technique. Monomolecular films are also shown to be effective and offer some unique advantages, such as ease of application and low overall cost. The heat normally lost to evaporation must be dissipated by other means during suppression. With the ice cover technique this is accomplished by melting the ice cover. During suppression with monomolecular films, the heat must be dissipated by increasing radiative and convective losses. The simplicity of application of monomolecular films, along with their lower cost, combine to make this technique attractive; however, the lower pond temperatures and increased suppression effectiveness weigh heavily in favor of the ice-cover technique.
    Type of Medium: Series available for loan
    Pages: viii, 86 Seiten , Illustrationen
    Series Statement: CRREL Report 76-43
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Conversion factors: U.S. customary to metric units of measurement Introduction Section I. Ice fog Section II. Evaporation Bowen's equation Evaporation equation Evaporation measurements during ice fog conditions Evaporation measurements at Eielson Power Plant cooling pond Data analysis Section Ill. Radiation during ice fog Brunt's equation Ångström equation Elsasser's equation Cloud cover Reflection Field experimental results Analysis of experimental results Radiation equations for ice fog Transmissivity of ice fog Radiation model Wind effect Summary Section IV. Convection Convective heat transfer theory Rotem and Claassen equation Kay's approach Russian approach Analysis Heat budget at the surface Conclusions Section V. Ice fog suppression techniques Fans Injection wells Latent heat storage Monomolecular films Use of heated water from the cooling pond Section VI. Latent heat storage experiments Freezing rates Cooling pond Ice building Ice growth rate -maximum system limitation Evaporation heat loss -maximum Realistic growth rate Ice building techniques Ice volume measurements Melting experiments Ice fog suppression considerations Experimental results Section VII. Recommendations and conclusions Hexadecanol studies Injection well suppression Latent heat storage suppression Comparison of approaches Measurements of evaporation Measurements of radiation loss Convective heat losses Ice fog suppression Selected bibliography Appendix A. Convective heat transfer coefficient from water to ice and from ice to air
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  • 21
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/3
    In: CRREL Report, 77-3
    Description / Table of Contents: Tests were conducted in uniaxial compression and tension to determine the effect of temperature on the strength of frozen Fairbanks silt. Test temperatures ranged from 0 C to -56.7 C. Two machine speeds, 4.23 cm/sec and 0.0423 cm/sec, were used for the constant displacement rate tests. From the highest to the lowest temperature, the compressive strength increased up to about one order of magnitude and the tensile strength increased one-half an order of magnitude. Equations are presented which correlate strength with temperature at the strain rates obtained. The initial tangent and 50% strength moduli and the specific energy are given for each test. The mode of fracture and the effects of unfrozen water content and ice matrix strengthening are discussed, and the test results are compared with the data of other investigations.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 77-3
    Language: English
    Note: CONTENTS Abstract Preface Introduction Sample preparation Apparatus and testing procedure Test results Discussion Compressive strength Tensile strength Initial tangent and 50% stress moduli Specific energy Mode of failure Strength as a function of unfrozen water Thermal activation Conclusions and recommendations Literature cited
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  • 22
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/6
    In: CRREL Report, 77-6
    Description / Table of Contents: It has been reported that small arms projectiles are inherently unstable in snow and that snow has an unexpectedly high ability to stop them and other fast-moving projectiles. Field tests showed that the typical subarctic snow of interior Alaska can be used effectively to provide protection from both rifle and machine gun fire. The undisturbed snow had an average density of 0.18 g/cu. cm., but simple processing, such as shoveling, increased the density to around 0.34 g/cu. cm. Further processing increased the density to above o.40 g/cm3 but densities much above that value were difficult to obtain with simple hand equipment. Tests of the M16 rifle and M60 and M2HB machine guns showed that bullet penetration was inversely related to density - the higher the density the lower the bullet penetration. Design values for the three weapons were determined. A number of types of snow trenches and structures were designed and tested. They were found to provide good protection, in part since bullets showed a strong tendency to ricochet from the snow surface when striking it at a low angle. Burlap bags were filled with snow to revet structures and worked very well. Several types of Russian defensive works of snow were tested but proved unsuitable in the light, weak subarctic snow. The times required for troops to build several types of structures using only shovels and scoops were recorded.
    Type of Medium: Series available for loan
    Pages: vi, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 77-6
    Language: English
    Note: CONTENTS Abstract Preface Summary Background Objectives Subarctic snow General Snow processing Construction productivity Shovel capacity Snow piles Bullet behavior and penetration in snow Test procedure M16 M60 ball M60 tracers .50 caliber Tumbling Bullet deformation and breakage Design penetration values Defensive works of snow Revetments Snow bags The snow trench The hardened snow trench Breastworks and bunkers Evaluation of foreign technology Russian expedient snow trenches Snow blocks and block structures The snow arch An expedient shelter Conclusions Recommendations Literature cited
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  • 23
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : McGraw-Hill Book Company
    Call number: MOP 44210 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XV, 523 Seiten , graphische Darstellungen
    ISBN: 978-0-070-56042-0
    Language: English
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  • 24
    Call number: MOP 45557 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 221 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 25
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/34
    In: CRREL Report, 76-34
    Description / Table of Contents: Some physical characteristics of two grounded floebergs (fragments of multi-year pressure ridges) near Prudhoe Bay, Alaska, are described. Cross-sectional profiles of the sails and keels of both floebergs were obtained. A sail to keel ratio of 1 to 3.38 obtained with one floeberg was found to be in good agreement with previous investigations. A survey of the sea floor for evidence of scoring induced during grounding yielded a maximum depth of gouging of 1.1m. Additional studies included investigations of the internal structure of the floebergs, and a brief examination of the organic and sedimentary debris found entrained within the floebergs. The grounding of ice on the continental shelves of the Arctic is of considerable interest to those concerned with the development and impact of development of these continental shelves. The field study reported here provides information useful in assessing the nature and characteristics of interactions between floebergs and the sea bed on which they are grounded.
    Type of Medium: Series available for loan
    Pages: iii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 76-34
    Language: English
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  • 26
    Call number: ZSP-201-76/35
    In: CRREL Report, 76-35
    Description / Table of Contents: Crystalline textures and fabrics of ice cores from the 2164-m-thick ice sheet at Byrd Station, Antarctica, reveal the existence of an anisotropic ice sheet. A gradual but persistent increase in the c-axis preferred orientation of the ice crystals was observed between the surface and 1200m. This progressive growth of an oriented crystal fabric is accompanied by a 20-fold increase in crystal sized between 56 and 600m, followed by virtually no change in crystal size between 6000 and 1200m. A broad vertical clustering of c-axes develops by 1200m. Between 1200 and 1300 m the structure transforms into a fine-grained mosaic of crystals with their basal glide planes now oriented substantially within the horizontal. This highly oriented fine-grained structure, which persists to 1800m, is compatible only with a strong horizontal shear deformation in this part of the ice sheet. Rapid transformation from single- to multiple-maximum fabrics occurs below 1800m. This transformation, accompanied by the growth of very large crystals, is attributed to the overriding effect of relatively high temperatures in the bottom layers of old ice at Byrd Station rather than to a significant decrease in stress. The zone of single-maximum fabrics between 1200 and 1800 m also contains numerous layers of volcanic dust. Fabrics of the very fine-grained ice associated with these dust bands indicate the bands are actively associated with shearing in the ice sheet. Some slipping of ice along the bedrock seems likely at Byrd Station, since the basal ice is at the pressure melting point and liquid water is known to exist at the ice/rock interface.
    Type of Medium: Series available for loan
    Pages: v, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 76-35
    Language: English
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  • 27
    Call number: MOP 44439 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 68 Seiten
    Language: English
    Location: MOP - must be ordered
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  • 28
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : [Verlag nicht ermittelbar]
    Call number: MOP 44941 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 24 Seiten
    Language: English
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  • 29
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/29
    In: CRREL Report, 79-29
    Description / Table of Contents: An analytical study of the propagation of shock waves in snow was carried out to evaluate the response of medium density snow to high rates of loading. One solution was developed for steady shock waves; this resulted in calculation of pressure jump, density jump and stress wave speed. Correlation with available experimental data was found to be good. Nonsteady shock waves were also considered in order to evaluate wave attenuation rates in snow. Very few data were available to compare with the analytical results, so no definite conclusions on the part of the study could be made. The results show, however, that shock waves that produce plastic deformation attenuate at extremely high rates and that differences in pressure between two waves are quickly eliminated within a short distance. Calculations were also made to evaluate the effect of wave frequency on attenuation rates. The results show that, for plastic waves, frequency is not a predominant factor for determining attenuation rates.
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    Pages: v, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-29
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature I. Introduction II. A constitutive law for snow and balance principles III. Compatibility laws and jump equations for stress waves IV. Steady shock waves in snow V. Comparison of steady-wave theory with experimental results VI. A numerical solution to the nonsteady wave problem VII. Jump equations for nonsteady shock waves VIII. Reduced jump equations Discussion and conclusions Literature cited
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  • 30
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-79/28
    In: CRREL Report, 79-28
    Description / Table of Contents: Transmission and scanning electron micrographs of Umiat bentonite revealed thin, mica-like grains with irregular shapes. Most of the bentonite showed electron diffraction ring patterns, but some showed hexagonal net patterns as well as ring patterns. The lengths of the unit cells were calculated to be 5.18 A along the a-axis and 8.97 A along the b-axis. Semiquantitative analyses were made using an energy dispersive spectrometer. Common elements such as Si, Ti, Al, Fe, Mg, Na and K were determined. The molecular ratio of SiO2:Al2O3 was calculated to be 492:100 for the bulk sample, indicating that Umiat bentonite is similar in most respects to Wyoming bentonite, and is classified as a mont-morillonite. The microstructure of frozen Umiat bentonite was observed at a specimen temperature of -100 C using a scanning electron microscope equipped with a cold stage. Frozen bentonite and segregated ice patterns formed from wet bentonite were examined using an X-ray map and Si X-ray line scan. Sublimation processes of ice in the frozen bentonite were observed at specimen temperatures of -60 and -80 C. After sublimation of the ice the bentonite displayed a honeycomb structure. It was concluded that the freezing-sublimation cycle in frozen soil increases the permeability of water vapor due to the three-dimensional structure of the coagulated clay formed by freezing.
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    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-28
    Language: English
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  • 31
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/25
    In: CRREL Report, 79-25
    In: Charged dislocation in ice, I.
    Description / Table of Contents: The motion of dislocations in single crystal ice under an electric field was observed by using X-ray topographic methods. Electric charge density on these dislocations was deduced from the amplitude and length of the dislocation segment under the known AC electrical field. The most likely linear charge density was about +5x10^-11 c/m, although considerable variation is possible depending on the effective field acting on the dislocation lines.
    Type of Medium: Series available for loan
    Pages: iii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-25
    Language: English
    Note: CONTENTS Abstract Preface Introduction Theory Experimental apparatus and procedure Results Discussion Concluding remarks Selected bibliography Appendix A. Mosotti type field on core of cylindrical cavity
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  • 32
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/24
    In: CRREL Report, 79-24
    Description / Table of Contents: By using a new thermocoring technique, a hole was successfully drilled through the 416-m thickness of the Ross Ice Shelf at J-9 Camp. This report provides a description of the drill and an account of this drilling project. A provisional examination of the core shows the ice shelf to consist of 410 m of snow and glacial ice underlain by 6 m of sea ice formed by direct freezing of sea water to the bottom of the Ross Ice Shelf.
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    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-24
    Language: English
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  • 33
    Call number: ZSP-201-79/23
    In: CRREL Report, 79-23
    Description / Table of Contents: The performance of surface impedance and magnetic induction electromagnetic subsurface exploration techniques was studied seasonally at various sites in Alaska where permafrost and massive ground ice occurred. The surface impedance method, which uses radiowaves in the LF and VLF bands, and the magnetic induction method, which uses low-frequency magnetic induction fields, distinguish subsurface materials by the electrical resistivity of the materials. The methods used have greatest sensitivity within about 20 m of the surface and are, therefore, most applicable for shallow subsurface investigations. The selection of study sites was based on anticipated contrasts in electrical resistivity between ground ice and adjacent earth materials. A magnetic induction instrument, using a separation of 3.66-m between the transmitter and receiver antennas, in general was able to detect near-surface zones of massive ice and to provide data regarding permafrost distribution in both the Fairbanks and Prudhoe Bay areas. At this antenna separation, the depth of magnetic field penetration was sufficient to include mainly the zone containing maximum contrasts in resistivity between ground ice and other earth materials. In the Fairbanks area, contrasts, in this zone were greatest in late winter when the seasonally thawed surface layer was completely frozen. When thawed, this layer usually becomes more conductive and often masks the deeper resistivity contrasts. In the Prudhoe Bay area, maximum ground resistivity contrasts were detected in late summer when shallow subsurface temperatures had risen sufficiently to permit resistivity contrasts between the massive ice and the ice-rich ground to appear.
    Type of Medium: Series available for loan
    Pages: v, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 79-23
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Obiectives and procedures Ground electrical resistivity in permafrost regions Electromagnetic techniques General Magnetic induction method Surface impedance fradiowave method Direct current method General description of field sites Results Site 1 CRREL permafrost station, Fairbanks, Alaska Site 2 Planned road cut for Steese Highway near Fox, Alaska Site 3 Relic floodplain near Fairbanks, Alaska Site 4 Pingos, Prudhoe Bay, Alaska Site 5 Ice wedges, Prudhoe Bay, Alaska Comparisons between the surface impedance and magnetic induction methods Conclusions and recommendations Literature cited Appendix A. Discussion of the depth of sensitivity of the magnetic induction method using two- and three-layer apparent resistivity curves
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  • 34
    Call number: MOP 46654 / Mitte
    In: World weather program : plan for fiscal year, 1980 and 1981
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    Language: English
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  • 35
    Call number: MOP 42980 / Mitte
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  • 36
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/27
    In: CRREL Report, 79-27
    Description / Table of Contents: Some Bessel function identities found by solving problems of the deflection of a floating ice plate by two different methods are rigorously proved. The master formulas from which all the identities are derived are in a Fourier reciprocal relationship, connecting a Hankel function to an exponential function. Many new formulas can be derived from the master formulas. The analytical method presented here now opens the way to study a hitherto impossible type of problem--the deflection of floating elastic plates of various shapes and boundary conditions.
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    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 79-27
    Language: English
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  • 37
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/26
    In: CRREL Report, 79-26
    Description / Table of Contents: A 19-year record of the annual closing and opening dates of operation of the Lake Champlain ferry at Grand Isle, Vermont, which are controlled by the lake's ice cover, was made available to CRREL. These navigation records accurately approximated the freeze-over and breakup dates for the ferry crossing area between Gordon Landing, Vermont, and Cumberland Head, New York. When compared statistically with water temperature and climatological data for the same years at nearby Lake Champlain locations, the dates allowed accurate predictions of ice formation. From nearby air temperature records, cumulative freezing degree-day (deg C) curves were plotted for each year of record, and ice formation dates and standard deviations were predicted with considerable accuracy. Several methods of predicting ice formation on Lake Champlain were attempted. The most accurate approach used a combination of water temperatures and freezing degree-days. The influence of wind speed on ice cover formation and prediction are also discussed in the report.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Data tabulation and collection Air temperatures 11-reezing degree-days Water temperatures Closing and opening dates Results Air temperature Freezing degree-days Water temperatures Analysis: Attempted methods of predicting ice formation Predicting air temperatures 8Summer water temperatures Fall water temperatures and freezing degree-days Wind speed influence on closing of the lake Water temperature vs surface air temperature analysis Prediction of ice-out dates Conclusions Literature cited Appendix A. Freezing degree-day curves with ice notations and watertemperature notations Appendix B. Summary
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  • 38
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    Monograph available for loan
    New York [u.a.] : Plenum Press
    Call number: 9790
    Type of Medium: Monograph available for loan
    Pages: XV, 508 Seiten , Illustrationen
    ISBN: 0306307391
    Language: English
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  • 39
    Call number: MOP 44044 / Mitte
    Type of Medium: Monograph available for loan
    Pages: vi, 126 Seiten , Illustrationen , 28 cm
    Language: English
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  • 40
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    Monograph available for loan
    Hanover, NH : US Army Cold Regions Research and Engineering Laboratory
    Call number: AWI G7-19-92301
    Description / Table of Contents: The pulse radiosounding technique was used in studying Antarctic land and sea ice, their internal structures, volumes, movements, and physical properties. Electromagnetic properties of different ice types and their measurement are discussed.
    Type of Medium: Monograph available for loan
    Pages: 83 Seiten , Illustrationen
    Series Statement: Draft translation / Cold Regions Research and Engineering Laboratory, Corps of Engineers, U.S. Army 614
    Uniform Title: Radiozondirovanie lʺda 〈rus.〉
    Language: English
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  • 41
    Call number: AWI G6-19-92215
    Type of Medium: Monograph available for loan
    Pages: 182 Seiten , Illustrationen
    Edition: Izd. 2., pererabot. i dop.
    Language: Russian
    Note: In kyrillischer Schrift
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  • 42
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/29
    In: CRREL Report, 76-29
    Description / Table of Contents: In order to verify current theoretical equations on ice bearing capacity, a heavily loaded truck was used to make successive passes over two ice bridges. Equipment, weather and the normal problems associated with field work resulted in only one complete breakthrough test. Breakthrough occurred on one bridge with a vehicle weight of 53,630 lb (24,327 kg) and an ice thickness of 17.5 in. (44.5 cm). Since only one test was completed, the conclusions drawn cannot be unequivocal. However, the results do indicate that Nevel's equation for ultimate failure of a floating ice sheet is a good working tool.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 76-29
    Language: English
    Note: Contents Abstract Preface Summary Introduction Location Test procedure Loading Site preparation and bridge construction Deflection measurements Conclusions Literature cited Appendix, Test data
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  • 43
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-76/44
    In: CRREL Report, 76-44
    Description / Table of Contents: The deformation of wet snow is explained in terms of the thermodynamics of the three phases of water. When deformation by particle rearrangement is fully developed, deformation can occur most rapidly by melting at the particle contacts. The rate of deformation is highly sensitive to the liquid water content, ionic impurity content, particle contact area, and stress level. A model of the hydrostatic deformation of wet snow is constructed, and examples of the deformation of wet snow are given for a variety of conditions. These results are in agreement with existing experimental evidence. The model accurately simulates the transient nature of the deformation and the effect of water content on the quasi-stable density of wet snow subjected to a constant stress.
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    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 76-44
    Language: English
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  • 44
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-76/47
    In: CRREL Report, 76-47
    Description / Table of Contents: This report describes two mechanical ice-cutting systems for the removal of ice collars at the high pool level on the Poe Lock of the St. Marys Falls Canal at Sault Ste. Marie, Michigan. One system was a narrow-kerf (3.25-in.-wide) coal-cutting chain saw mounted on a bar, driven by a 65-hp wheeled trencher. The other system was a lumber-cutting chain saw mounted on a bar, driven by a 30-hp wheeled soil trencher which cut a 0.56-in.-wide kerf. The lumber-cutting saw's bar was too flexible and the desired cutting traverse speed was not met. The coal-cutting saw cut 6-ft-deep ice collars at traverse speeds of up to 10 ft/min and is acceptable. With a few modifications, the coal-cutting saw would be operational.
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    Pages: iii, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 76-47
    Language: English
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  • 45
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/1
    In: CRREL Report, 77-1
    Description / Table of Contents: Studies of the growth history and structural characteristics of winter ice covers on two New Hampshire lakes are described. These investigations included measurements of ice cover thickness, characterization of the stratigraphic and crystalline structure of the ice, identification and classification of major ice types and measurements of electrolytic conductivity. The formation of cracks and flaws in the ice and their effects on the mechanical properties of the ice were also investigated. A method of correlating ice growth with surface wind and temperature measurement is described and the interrelationships of the various physical and mechanical properties of temperate lake ice covers are discussed.
    Type of Medium: Series available for loan
    Pages: v, 29 Seiten , Illustrationen
    Series Statement: CRREL Report 77-1
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Study areas Study methods Winter freeze-up Composition of ice cover Freezing degree day records and applications Evaluation of ice growth coefficient α Growth history and entrapped bubble stratigraphy Mechanical properties Electrolytic conductivity Literature cited
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  • 46
    Call number: MOP 44818 / Mitte
    Type of Medium: Monograph available for loan
    Pages: vii, 50 Seiten , 28 cm
    Language: English
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  • 47
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/9
    In: CRREL Report, 79-9
    Description / Table of Contents: Sedimentation at the terminus of the Matanuska Glacier has been found to be primarily subaerial in a 100- to 300-m wide, ice-cored zone paralleling the edge of the active ice. Certain physical and chemical characteristics of the ice and debris of the superglacial, englacial and basal zones of the glacier indicate the debris of the basal zone, the primary source of sediment, is entrained during freeze-on of meltwater, probably surficially derived, to the glacier sole. Till formation results from the melting of buried ice of the basal zone. Melt-out till inherits the texture and particle orientations of basal ice debris; other properties are not as well preserved. Most deposits result from resedimentation of till and debris by sediment gravity flows, meltwater sheet and rill flow, slump, spall, and ice ablation. Depositional processes are interrelated in the process of backwasting of ice-cored slopes. Sediment flows are the primary process of resedimentation. Their physical characteristics, multiple mechanisms of flow and deposition, and characteristics of their deposits vary with the water content of the flow mass. Deposits of each process are distinguished from one another by detailed analysis of their internal organization, geometry and dimensions, and the presence of other internal and related external features. Genetic facies are defined by these characteristics. The interrelationship of processes develops a composite depositional sequence defined in terms of genetic facies associations; an upper, resedimented facies association, a middile, till facies association, and a lower, subglacial-resedimental facies association. The lateral and vertical distribution of genetic facies within the associations is mainly nonrepetitive.
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    Pages: X, 112 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 79-9
    Language: English
    Note: CONTENTS Abstract Preface Summary Chapter 1. Introduction Field site Historical background Chapter 2. Characteristics of the debris and ice Characteristics of the facies and subfacies Basal zone Characteristics of the debris Discussion Chapter 3. Oxygen isotope analysis Sampling and analysis Results Discussion Chapter 4. Depositional processes—till formation Methods of analysis Environmental setting Till formation Chapter 5. Depositional processes—resedimentation Sediment flows Other resedimentation processes Resedimentation process relationships Chapter 6. Process distribution, sediment dispersal and depositional patterns Physical characteristics Sediment dispersal Sedimentary facies Patterns of terminus sedimentation Chapter 7. Conclusions Literature cited
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  • 48
    Call number: MOP 45476 / Mitte
    Type of Medium: Monograph available for loan
    Pages: [400] Seiten , Illustrationen , 28 cm
    Language: English
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  • 49
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/21
    In: CRREL Report, 79-21
    Description / Table of Contents: The report studies the question of whether Great Lakes freighters could move effectively through ice-clogged channels with the aid of tows provided by warping or kedging systems. Ten operational concepts are outlined, and their advantages and disadvantages are noted. The crushing resistance of floating brash ice is then analyzed. The neutral, active and passive states of stress for laterally confined brash ice are considered, and the resistance to horizontal thrusting by a smooth vertical wall is calculated for cohesionless brash ice, and for ice in which there is finite cohesion between the ice fragments. The thickening of the ice cover in the vicinity of a "pusher", and the formation of pressure ridges, are analyzed in order to estimate the amount of pile-up that can occur against a ship hull. The analysis then moves on to consideration of ship resistance by brash ice, taking into account crushing resistance at the bow, tangential friction at the bow, and hull friction aft of the bow section. Comparisons are made between thrust from the ship’s screws and the calculated ice resistance. The next section of the report estimates the force requirements for a warping or kedging system in terms of thrust augmentation for existing vessels. Tow cable requirements are given, and estimates are made for cable anchors and for anchorage of underwater structures. The force and power requirements for winches and windlasses are given, the practical problems involved in the pickup or transfer of cables are mentioned, and the report concludes with a brief appraisal. The conclusion is that a simple warping tug system is appropriate for a full scale experiment, a chain ferry with auxiliary barge seems attractive for an operational system, and a chain ferry plow may be an efficient way to clear ice from channels.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Operational concepts A. Warping tug system B. Chain ferry system C. Chain ferry with auxiliary barge D. Ski tow system E. Dual winch warping system F. Simple kedging G. Trailing-line system H. Above-surface dual winch system I. Pulley systems J. Chain ferry plow Crushing resistance of fragmented ice covers Resistance to ship passage by broken ice Crushing resistance at the bow Tangential friction at the bow Hull friction aft of the bow section Total ship resistance from brash ice Comparison of ship thrust and ice resistance Force requirements for a warping or kedging system Tow cable requirements Anchors and anchorages Force and power requirements for winches and windlasses Pickup or transfer of cable General appraisal Literature cited
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  • 50
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/26
    In: CRREL Report, 76-26
    Description / Table of Contents: Debris over a 44-mile stretch of the Chena River was studied. The study area extended from the first bridge on the Chena Hot Springs Road to the Chena River Flood Control damsite. The purpose of the study was to assess the potential danger to the Chena River Flood Control Dam outlet structure. Debris was catalogued, log jams were measured, and sources of debris were studied. The average size of logs was determined, as well as the number of logs present on the river. The authors concluded that a serious debris problem existed and would remain serious for the foreseeable future. Recommendations for debris handling were made.
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    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 76-26
    Language: English
    Note: Contents Abstract Preface Summary Introduction Origin of debris Volume, magnitude Types of debris Hazards of the debris Recommended measures to counteract log jamming Conclusions and recommendations Future work Epilogue Selected bibliography Appendix: Additional photographs of Chena River debris
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  • 51
    Call number: MOP 40847 / Mitte
    Type of Medium: Monograph available for loan
    Pages: x, 424 Seiten
    Language: English
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  • 52
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 40419 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 302 Seiten , Illustrationen
    Language: Russian
    Note: Zsfassung in englischer Sprache , In kyrillischer Schrift
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  • 53
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    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45175 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 181 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
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  • 54
    Call number: MOP 44237 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 93 Seiten , Illustrationen , 20 cm
    Series Statement: Serija Meteorologija / VNII Gidrometeorologičeskoj Informacii - Mirovoj Centr dannych
    Language: Russian
    Note: In kyrillischer Schrift
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  • 55
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45690 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 263 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 56
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    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45688 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 119 Seiten
    Language: Russian
    Note: In kyrillischer Schrift
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  • 57
    Call number: MOP 45353 / MItte
    In: Developments in atmospheric science, 9
    Type of Medium: Monograph available for loan
    Pages: 327 Seiten , Illustrationen
    ISBN: 0444417486
    Series Statement: Developments in atmospheric science 9
    Language: English
    Note: CONTENTS Preface CONFERENCE SUMMARY / A. L. Fymat TEMPERATURE SOUNDING INVERSION METHODS AND THE OBSOLESCENCE OF DIFFERENTIAL EQUATIONS FOR SPECIFYING PHYSICAL OBSERVABLES / J. I. F. King SOME EXPERIMENTS ON THE EFFECT OF REMOTE SOUNDING TEMPERATURES UPON WEATHER FORECASTING / M. Halem, M. Ghil and R. Atlas NONLINEAR INVERSION: THEORY AND PRAXIS / J. I. F. King A NEW TREATMENT OF THE BOUNDARY TERM IN THE INVERSION OF THE RADIATIVE TRANSFER EQUATION / H. E. Fleming and D. S. Crosby EVALUATION OF ERRORS IN DERIVED CLEAR COLUMN RADIANCES / L. McMillin RECURSIVE FILTERING OF RADIANCE DATA FROM NIMBUS-E SATELLITE / I. A. Ismail DEPENDENCE OF THE TEMPERATURE DEVIATION OF THE OCEAN SURFACE AS MEASURED BY SATELLITE ON THE SIZE DISTRIBUTION OF AEROSOLS / T. Takashima THE DETERMINATION OF ATMOSPHERIC TEMPERATURE PROFILES FROM INFRARED INTERFEROMETER MEASUREMENTS ON BOARD OF METEOR-25 / V. A. Golovko and D. Spänkuch COMPOSITION SOUNDING GLOBAL TOTAL OZONE DETERMINATION FROM NIMBUS 4 BUV SPACECRAFT DATA / A. J. Fleig, R. S. Fraser, B. W. Guenther, D. F. Heath, E. Hilsenrath, L. V. Novak, V. G. Kaveeshwar, R. D. McPeters, C. L. Mateer and A. G. Miller INFORMATION CONTENT AND RESULTS OF NON-LINEAR INVERSION OF NIMBUS 6 LIMB RADIANCE INVERSION RADIOMETER DATA / J. C. Gille and P. L. Bailey AN APPROXIMATE METHOD FOR NONLINEAR INVERSION OF LIMB RADIANCE OBSERVATIONS / P. L. Bailey and J. C. Gille A NONLINEAR TECHNIQUE FOR INVERTING LIMB ABSORPTION PROFILES / J. D. Mill and S. R. Drayson SENSITIVITY OF THE INVERSION OF LIMB RADIANCE MEASUREMENTS IN THE 6.3μm WATER VAPOR BAND / H. Fischer AN ANALYSIS OF NIMBUS-V THIR 6-7 μm OBSERVATIONS OVER THE MEDITERRANEAN SEA / M. Roulleau MICROWAVE GROUND-BASED DETERMINATION OF ATMOSPHERIC TOTAL WATER CONTENT / G. G. Shchukin and L. P. Bobylev A SOLAR HETERODYNE RADIOMETER FOR THE DETERMINATION OF THE ALTITUDINAL PROFILES OF ATMOSPHERIC GASES / V. I. Astakhov, N. V. Vanin, V. V. Galaktionov, V. M. Dorokhov, V. M. Zakharovand V. U. Khattatov PASSIVE REMOTE SENSING IN THE PRESENCE OF MULTIPLE SCATTERING: A NUMERICAL INVERSION METHOD / B. R. Barkstrom PARTICULATE SOUNDING RECONSTRUCTING THE SIZE DISTRIBUTION OF SPHERICAL PARTICLES FROM ANGULAR FORWARD SCATTERING DATA / A. L. Fymat and K. D. Mease COMPLEX REFRACTIVE INDEX OF ATMOSPHERIC AEROSOLS: A SIZE DISTRIBUTION INDEPENDENT RETRIEVAL APPROACH USING MULTISPECTRAL TRANSMISSION RATIOS / A. L. Fymat and K. D. Mease THE METHOD OF MULTIFREQUENCY LASER SOUNDING OF ATMOSPHERIC AEROSOL MICROSTRUCTURE / V. E. Zuev and I. E. Naats LASER SOUNDING OF THE ATMOSPHERE USING AEROSOL SCATTERING / V. E. Zuev STRATOSPHERIC AEROSOL LAYERS MONITORED BY LIDAR / R. Reiter, H. Jaeger, W. Carnuth and M. Littfass LIDAR DETECTION OF ATMOSPHERIC CONTAMINANTS BY RAMAN SCATTERING AND FLUORESCENCE SPECTRA / V. M. Zakharov and V. A. Torgovichev REMOTE SENSING OF CLOUD PROPERTIES FROM NIMBUS 5 / D. J. McCleese THE ATMOSPHERIC BLURRING EFFECT OF REMOTELY SENSED EARTH IMAGERY / S. Ueno, Y. Haba, Y. Kawata, T. Kusaka and Y. Terashita Author Index Subject Index
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  • 58
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Physikalisch-Bioklimatische Forschungsstelle der Fraunhofer-Gesellschaft zur Förderung der angewandten Forschung
    Call number: MOP 40082 / Mitte
    Type of Medium: Monograph available for loan
    Pages: ca. 100 Seiten
    Series Statement: AEC Document Number NYO - 3425 - 10
    Language: English
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  • 59
    Monograph available for loan
    Monograph available for loan
    Wellington : New Zealand Meteorological Service
    Call number: MOP 44877 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 127 Seiten
    Language: English
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  • 60
    Call number: MOP 40801 / Mitte
    Type of Medium: Monograph available for loan
    Pages: II, 170 Seiten , Illustrationen
    Language: English
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  • 61
    Call number: MOP 44705 / Mitte
    Type of Medium: Monograph available for loan
    Pages: iii, 78 Seiten , 24 cm
    Language: English
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  • 62
    Monograph available for loan
    Monograph available for loan
    Oak Ridge, Tenn. : U.S. Department of Energy
    Call number: MOP 44436 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 15, 3, 5 Seiten
    Language: English
    Note: The field experiments were continued to estimate convective storm particulate scavenging efficiency in proximity to the St. Louis, Missouri urban-industrial complex. Complementary studies of the urban aerosol characterization, source strength, and removal processes were also studied. The 1975 field effort shifted emphasis from the immediate St. Louis area to the Alton-Wood River industrial complex. Along with the change in size and configuration of the network, there were increases in the numbers of most types of samplers. The new network yielded the following types of samples for analysis and interpretation: 1065 total rain samples from 85 sites; 68 sequential rainwater samples from 2 locations; 272 wet/dry samples from 7 locations; 216 air filter samples from 7 locations; 36 air filter samples from aircraft; and raindrop spectrometer data from 11 sites for the period 17 June-18 August. The analysis procedures require that all water samples undergo filtering for separate analyses of soluble and insoluble fractions of the elemental concentrations. This data collection effort provided a record number of samples for chemical analysis. Approximately 4000 pibals and over 370 radiosondes were released in the operational period, providing wind and thermodynamic data on 33 days. Aircraft missions were flown on 24 days, with one air tracer release of cesium on 19 July 1975. The status of the analysis of all types of data is described.
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  • 63
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/14
    In: CRREL Report, 79-14
    Description / Table of Contents: Solid ice growth rates due to the presence of frazil slush beneath the ice cover have been shown to be greater than the so-called static growth. The frazil slush reduces the effective heat of ice solidification and the frazil particles freeze into the interstitial water. Numerical schemes are presented which clearly show the effect of frazil ice porosity on ice cover growth rates and the numerical model using air temperature as the major input is compared with field data on ice thickness in a small river laden with frazil ice beneath its cover.
    Type of Medium: Series available for loan
    Pages: ii, 4 Seiten , Illustrationen
    Series Statement: CRREL Report 79-14
    Language: English
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  • 64
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/22
    In: CRREL Report, 79-22
    Description / Table of Contents: Field observations at 60 Sites located in the fast or near-fast ice along a 1200-km stretch of the north coast of Alaska between Bering Strait and Barter Island have shown that the great majority of the ice samples (95%) exhibit striking c-axis alignments within the horizontal plane. Such alignments were usually well developed by the time the ice was 50 cm thick and in some cases when the ice was 20 cm thick. In all cases the degree of preferred orientation increased with depth in the ice. Representative standard deviations around a mean direction in the horizontal plane are commonly less than ± 10° for samples collected near the bottom of the ice. The general patterns of the alignments support a correlation between the preferred c-axis direction and the current direction at the ice/water interface. A comparison between c-axis alignments and spot current measurements made at 42 locations shows that the most frequent current direction coincides with the mean c-axis direction. Such alignments are believed to be the result of geometric selection with the most favored orientation being that in which the current flows normal to the (0001) plates of ice that compose the dendritic sea ice/sea water interface.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-22
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Techniques and sampling Observations Crystal alignments “Odd” sites Causes Conclusions Literature cited Appendix A: Current observations
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  • 65
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/19
    In: CRREL Report, 79-19
    Description / Table of Contents: The critical velocities of loads moving over floating ice plates have been determined by several authors. In all these analyses it was assumed that the in-plane force field in the ice cover is zero. However, due to constrained thermal strains, in-plane forces do occur in the field. The purpose of the present paper is to determine their effect upon the critical velocities of the moving loads. It is shown that a uniform compression force field reduces the critical velocity, whereas a tension force field has the opposite effect.
    Type of Medium: Series available for loan
    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-19
    Language: English
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  • 66
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/17
    In: CRREL Report, 79-17
    Description / Table of Contents: Six test roofs of two different slopes — 16.3° and 39.8°, and three different roof coverings — asphalt shingles, cedar shingles, and corrugated aluminum sheeting, were constructed at USACRREL, Hanover, New Hampshire, and were instrumented with thermocouples, heat flow meters, and calibrated gutters. Measurements were recorded for the winters of 1971-72 and 1972-73. The degree of icing and the chronological changes in the snow cover were recorded on 35-mm Kodachrome slides. It was found that eave icing is a sensitive function of the slope, roof covering composi­tion, and solar radiation. The effects of wind were not investigated; the data were screened to remove all informa­tion corresponding to windspeeds over 8 km/h. In order of increasing tendency to form ice dams on the eaves, the roofs were high-slope asphalt, high-slope cedar, high-slope aluminum, low-slope asphalt, low-slope cedar, and low- slope aluminum.
    Type of Medium: Series available for loan
    Pages: vi, 40 Seiten , Illustrationen
    Series Statement: CRREL Report 79-17
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Experimental procedure Description of roofs Meteorological data Procedure Analysis General Temperature profiles Temperature rankings Heat flow Snow depths and meltwater volumes Degree of icing Results and conclusions General Temperature profiles of the roofs Comparative temperatures of roofs by section — rankings Heat flow and accumulation Snow depth, coverage, and meltwater Degree of icing Discussion of the icing problem Literature cited
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  • 67
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/16
    In: CRREL Report, 79-16
    Description / Table of Contents: In 1973 two membrane encapsulated soil layer (MESL) test sections were constructed into existing gravel surfaced roads at Elmendorf A FB and at Ft. Wainwright in Anchorage and Fairbanks, Alaska, respectively. The Elmendorf AFB MESL contains a silty clay soil and the Ft. Wainwright MESL contains a nonplastic silt. Both sections were constructed at soil moisture contents of approximately 2% to 3% below optimum for the CE-12 compactive effort. There were no indica­tions of soil moisture migration during freezing in either test section and after-thaw field California Bearing Ratio values were nearly equal to values measured before freezing. There is growing evidence of a slight increase in the overall soil moisture content in the Elmendorf AFB MESL possibly from moisture entering through the single layer polyethylene sidewalls which were not treated with asphalt emulsion. There is good evidence that the membrane of the same section might have received damage during a soil sampling operation which allowed localized moisture infiltration. A two-layer polyethylene membrane used in the Ft. Wainwright MESL is considered a more positive moisture barrier than the single sheet and a justifiable added cost for permanent construction.
    Type of Medium: Series available for loan
    Pages: v, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 79-16
    Language: English
    Note: CONTENTS Preface Introduction Laboratory studies General Elmendorf AFB silty clay Fairbanks silt Field studies Elmendorf AFB MESL Ft. Wainwright MESL Traffic use Elmendorf AFB MESL Ft. Wainwright MESL Performance observations Elmendorf AFB MESL Ft. Wainwright MESL Conclusions Elmendorf AFB MESL Ft. Wainwright MESL General Literature cited Appendix A. The MESL concept Appendix B. Classification, compaction, freezing and CBR test results for Fairbanks silt
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  • 68
    Call number: MOP 44440 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 105 Seiten , Illustrationen , 27 cm
    Language: English
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  • 69
    Monograph available for loan
    Monograph available for loan
    Wageningen : Centre for Agricultural Publ.and Documentation
    Call number: MOP 44708 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 141 Seiten , Illustrationen
    ISBN: 9022006018
    Series Statement: Simulation monographs
    Language: English
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  • 70
    Call number: MOP 40015 / Mitte
    Type of Medium: Monograph available for loan
    Pages: Seite 307-713 , Illustrationen, Diagramme
    Series Statement: Seminars of scientific foundation of medium range weather forecasts 2
    Language: English
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  • 71
    Call number: MOP 44126/2 / Mitte
    In: Proceedings of the tenth international symposium on remote sensing of environment, Volume 2
    Type of Medium: Monograph available for loan
    Pages: Seiten XLIX, 671-1456
    Series Statement: Proceedings of the tenth international symposium on remote sensing of environment 2
    Language: English
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  • 72
    Call number: MOP 40704 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VI, 35 Seiten
    Language: English
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  • 73
    Monograph available for loan
    Monograph available for loan
    Washington : Special Committee for Solar-Terrestrial Physics (SCOSTEP), National Academy of Sciences
    Call number: MOP 43858/1 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 142 Seiten , Illustrationen , 28 cm
    Language: English
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  • 74
    Call number: AWI G3-23-95343
    In: Trudy Instituta Geologii i Geofiziki, Vypusk 297
    Description / Table of Contents: According to the fossils study of 44 borings the stratigraphy of Paleozoic of the West-Siberian lowland is considered. The first stratigraphical scheme from Devonian to Lower Permian is given for this region. The paper gives the formational analysis as well as notions concerning the tectonic nature of the region, which are based both on this analysis and geophysical data. There are some data on paleozoic geological history of the region. The monography may be of great interest for geologists - specialists in oil geology, stratigraphists, paleontologists, lecturers and students of higher colleges.
    Description / Table of Contents: На основании анализа органических остатков, встреченных в разрезах 44 скважин, рассматривается стратиграфия палеозоя Западно-Сибирской равнины. Для девона и карбона нижней nерми приводятся первые для этой области стратиграфические схемы. Дается информационный анализ и основанные на нем и геофизических данных представления о тектонической природе области в палеозое. Работа представляет интерес для широкого круга геолоrовстратиграфов, палеонтологов, преподавателей и студентов вузов.
    Type of Medium: Monograph available for loan
    Pages: 43 Seiten , Illustrationen
    Series Statement: Trudy Instituta Geologii i Geofiziki Vypusk 297
    Language: Russian
    Note: Contents Introduction / V. S. Bochkarev Stratigraphy of palaeozoic deposits of the West-Siberian lowland / O. I. Bogush, V. S. Bochkarev, O. V. Yuferev Tectonics of the Palaeozoic of the West-Siberian lowland / V. S. Bochkarev Prinicpal features of the Palaeozoic history of the West-Siberian lowland / O. I. Bogush, V. S. Bochkarev, O. V. Yuferev References Appendix Palaeontological tables I-III , In kyrillischer Schrift , Mit englischer Zusammenfassung und Inhaltsverzeichnis
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  • 75
    Call number: AWI G3-23-95356
    In: Trudy Instituta geologii i geofiziki : Serija "Ėndogennye rudnye formacii Sibiri", vypusk 319
    Description / Table of Contents: В монографии на базе детального анализа производных субвулканического магматизма, сопровождающего эксплозивного брекчирования, метасоматизма и рудообразования рассматриваются генетические и физико-химические особенности эндогенного процесса на месторожденнях медно-молибденовой формации Сибири и сопредельных областей. Анализ ведется на формационнои основе, что позволяет рассмотреть вопрос о границах и объеме медно-молибденовой рудной формации, о формационной принадлежности метасоматитов, наметить круг типоморфных признаков и высказать рекомендации по использованию их при экономической оценке медно-молибденовых проявлений и проведении прогнозно-металлогенических исследований. Книга представляет интерес для минералогов, геохимиков и для широкого круга геологов, занимающихся изучением месторождений полезных ископаемыхю
    Description / Table of Contents: Translation of the abstract: Based on a detailed analysis of the derivatives of subvolcanic magmatism accompanying explosive brecciation, metasomatism and ore formation, the monograph examines the genetic and physicochemical features of the endogenous process in deposits of the copper-molybdenum formation of Siberia and adjacent areas. The analysis is carried out on a formational basis, which allows us to consider the issue of the boundaries and volume of the copper-molybdenum ore formation, the formational affiliation of metasomatites, outline a range of typomorphic features and make recommendations for their use in the economic assessment of copper-molybdenum occurrences and conducting predictive metallogenic studies. The book is of interest to mineralogists, geochemists and a wide range of geologists involved in the study of mineral deposits.
    Type of Medium: Monograph available for loan
    Pages: 422 Seiten, [2] gefaltete Blätter , Illustrationen
    Series Statement: Trudy Instituta geologii i geofiziki : Serija "Ėndogennye rudnye formacii Sibiri" vypusk 319
    Language: Russian
    Note: In kyrillischer Schrift
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  • 76
    Call number: AWI G3-24-95571-7
    In: Tektonika Sibiri, Tom 7
    Description / Table of Contents: Сборник включает доклады участников юбилейной Х сессии Научного совета по тектонике Сибири и Дальнего Востока, посвященной 50-летию образования Бурятской АССР и состоявшейся в г. Улан-Удэ. Тематика сборника многопланова. В обобщающих докладах рассмотрены главнейшие итоги развития научных и практических геологических исследований в Бурятской АССР. В других докладах результаты изучения разновозрастных тектонических структур Забайкалья и Прибайкалья (докембрийских, палеозойских и мезозойских), обсуждены особенности Байкальской рифтовой зоны и ее аналогов, большое внимание уделено разломам и связанным с ними магматизму и металлогении. В ряде докладов проведен сравнительный анализ тектоники Забайкалья и других регионов Азии, в частности северо - востока СССР, Монгольской Народной Республики и других территорий. Авторами использованы различные геологические и геофизические методы, включая экспериментальные. Сборник логически продолжает серию крупных работ по тектонике Сибири и Дальнего Востока, в которой уже издано шесть томов.
    Description / Table of Contents: Translation of the abstract: The collection includes reports from participants in the tenth anniversary session of the Scientific Council on Tectonics of Siberia and the Far East, dedicated to the 50th anniversary of the formation of the Buryat Autonomous Soviet Socialist Republic and held in Ulan-Ude. The collection's themes are multifaceted. The summary reports examine the most important results of the development of scientific and practical geological research in the Buryat Autonomous Soviet Socialist Republic. In other reports, the results of studying tectonic structures of Transbaikalia and Cisbaikalia of different ages (Precambrian, Paleozoic and Mesozoic), the features of the Baikal rift zone and its analogues were discussed, much attention was paid to faults and associated magmatism and metallogeny. A number of reports carried out a comparative analysis of the tectonics of Transbaikalia and other regions of Asia, in particular the northeast of the USSR, the Mongolian People's Republic and other territories. The authors used various geological and geophysical methods, including experimental ones. The collection logically continues the series of major works on the tectonics of Siberia and the Far East, in which six volumes have already been published.
    Type of Medium: Monograph available for loan
    Pages: 262 Seiten , Illustrationen
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 7
    Language: Russian
    Note: CONTENTS INTRODUCTION TECTONICS OF TRANSBAIKAL AND ADJACENT TERRITORIES The main results and tasks of geological service of Buryat ASSR / A.S. Filko, P.Ch. Shobogorov, V.A. Lbov The state and perspectives of development of the Earth's sciences in Buryat ASSR / G.V. Andreev, V.V. Zolotukhin, Ts.O. Ochirov. The main problems of tectonics of Transbaikalje / l.V. Luchitsky The pecularities of the tectonics evolucion's style of Sayan-Baikal mountain folded belt (on territory of Buryat ASSR) / V.P. Arsentyev, P.M. Khrenov. On structural position of Transhaikal in the Middle-Asian transcontinental mobile belt / Ts.O. Ochirov On nature of mosaic structure of Transbaikal / E.N. Altukhov The continental Mesosoic structures of Transbaikal / Ts.O. Ochirov, K.B. Bulnaev, V.I. Turunkhaev, Ts.Ts. Tsyrendorzhiev Some regularities of development of Earth crust's structure of south territory of Eastern Siberia in Pre-Cambrian and Lower Paleozoic / S.M.Zamaraev, A.M. Mazukabzov, E.P. Vasilyev, A. T. Sezko The main features of evolution of tectonic magmatic stages of North Prebaikal / V. V. Balkhanov Tectonic structure and development of North territory of Baikal mountains in Late Pre-Cambrian and Early Paleozoic / S.A. Gurulev Influence of Pre-Cambrien North Muja block on sedimentation in Early and Middle Cambrian / B.A. Dalmatov, M.M.Yazmir On distinguishing of subzones in Gida Early Paleozoic structural-formation zone / M.M. Yazmir Tectonic structures of Khilok structural-formation zone (Western Transbaikal) / V.l. Sizykh Middle and Upper Paleozoic outgeosyncline magmatism of Sayan-Baikal mountain region / I. V. Gordienko Role of granitoids in reconstruction of paleotectonic condition (examplified by Transbaikal) / V.A. Dvorkin-Samarsky Principles of systematics and study of deep faults of south part of Siberian platform's frame / V.G. Gladkov, V.A. Naumov, V.l. Sizykh Magmatism of boundary sutures of Siberian platform in Middle Proterozoic / A.A. Bukharov Faults of Sayan-Baikal mountain region and some problems of its study / Ts.O. Ochirov, S.I. Sherman, V.F. Erkhov Structural-formation complexes of deep faults and rumple zones (Baikal mountain region) / M.P. Lobanov, I.A. Okhotnikov The deep faults of Transbaikal and its reflections in geophysical fields / Ts. Ts. Tsyrendorzhiev Faults of Baikal-Patom Upland according to geological-geophysical data / Yu.I. Egorov. Tectonics and metallogeny of Buryat ASSR / P.Ch. Shobogorov, A.S. Filko, V.V. Levitsky The deep faults are the main ore-controling structures of Western Baikalian rare-mecall province / E.E. Baturina Sayan-Transbaikalian poligonal system of ore-belts / V. V. Levitsky GENERAL QUESTIONS OF DEVELOPMENT OF GEOLOGICAL STRUCTURES Problems of postgeosyncline tectonic development of Central Asian folded belt / A.L. Yanshin Geosyncline folded structures of the Mongolian People's Republic / N.S. Zaitsev, The main features of tectonics of central zone of Eastern Mongolia as region of Mesozoic Tectonic-magmatic stirring up / V. T. Grigorov Pre-Cambrian tectonics of Ural-Mongolian belt and the problem of paleooceans / L.M. Parfyonov, V.A. Popeko Problem of "foundation" of Baikalian folded region / K.A. Klitin Orogenic stage of baikalids and time of its formation / A.N. Bulgatov The main features of tectonics of caledonides of South Siberia / A.L. Dodin Outgeosyncline collapse depressions of South Siberia and methodological aspects of its study / V.S. Bochkarev Minor structural forms of metamorphic strata of Eastern Transbaikal and of South Ural / V.I. Gromin The main features of structure and development of orogenic regions of North-Eastern Asia / K.B. Mokshantsev Some physical regularities of formation of Earth crust's faults / S.I. Sherman Recent Earth crust's movements in south part of Baikalian rift zone and in adjacent regions / P.P. Kolmogorova, B.G. Kolmogorov The peculiarities of structure of recent and ancient rift zones / V.V. Fedynsky, A.G. Gainanov, B.A. Sokolov, N.A. Strakhova Role of wave movements in formation of tectonic structures of South Siberian boundary system / V.G. Gladkov , СОДЕРЖАНИЕ ПРЕДИСЛОВИЕ ТЕКТОНИКА ЗАБАЙКАЛЬЯ И СМЕЖНЫХ ТЕРРИТОРИЙ Основные итоги и задачи геологоразведочной службы Бурятской АССР / А. С. Филько, П. Ч. Шобогоров, В. А. Лбов, Состояние и перспективы развития наук о Земле в Бурятской АССР / Г. В. Андреев, В. В. Золотухин, Ц. О. Очиров Основные проблемы тектоники Забайкалья / И. В. Лучицкий Особенности стиля тектонической эволюции Саяно-Байкальского горно-складчатого пояса (в пределах Бурятской АССР) / В. П. Арсентьев, П. М. Хренов О структурном положении Забайкалья в Срединно-Азиатском трансконтинентальном подвижном поясе / Ц. О. Очиров О природе мозаичности структурного плана Забайкалья / Е. Н. Алтухов Континентальные структуры мезозоя Забайкалья / Ц. О. Очиров, К. Б. Булнаев, В. И. Турунхаев, Ц. Ц. Цырендоржиев Некоторые закономерности развития структуры земной коры юга Восточной Сибири в докембрии и нижнем палеозое / С. М. Замараев, А. М. Мазукабзов, Е. П. Васильев, А. И. Сезько Основные черты эволюции тектоно-магматических этапов Северного Прибайкалья / В. В. Балханов Тектоническое строение и развитие северной части Байкальской горной области в позднем докембрии и раннем палеозое / С. А. Гурулев Влияние докембрийской Северо-Муйской глыбы на осадконакопление в раннем и среднем кембрии / Б. А. Далматов, М. М. Язмир К выделению подзон в Джидинской раннепалеозойской структурно-формационной зоне / М. М. Язмир Тектонические структуры Хилокской структурно-формационной зоны (Западное Забайкалье) / В. И. Сизых Средне- и верхнепалеозойский внегеосинклинальный магматизм Саяно-Байкальской горной области / И. В. Гордиенко Роль гранитоидов в восстановлении палеотектонической обстановки (на примере Забайкалья) / В. А. Дворкин- Самарский Принципы, систематики и изучения глубинных разломов южного обрамления Сибирской платформы / В. Г. Гладков, В. А. Наумов, В. И. Сизых Магматизм краевых швов Сибирской платформы в среднем протерозое / А. А. Бухаров Разломная тектоника Саяно-Байкальской горной области и некоторые проблемы ее изучения / Ц. О. Очиров, С. И. Шерман, В. Ф. Ерхов Структурно-формационные комплексы глубинных разломов и зон смятий (Байкальская горная область) / М. П. Лобанов, И. А. Охотников Глубинные разломы Забайкалья и их отражение в геофизических полях / Ц. Ц. Цырендоржиев Разрывная тектоника Байкало-Патомского нагорья в свете геолого-геофизических данных / Ю. И. Егоров Тектоника и металлогения Бурятской АССР / П. Ч. Шобогоров, А . С. Филько, В. В. Левицкий Глубинные разломы - главные рудоконтролирующие структуры Западно-Забайкальской редкометальной провинции / Е. Е. Батypина Саяно-Забайкальская решетчатая система рудных поясов / В. В. Левицкий ОБЩИЕ ВОПРОСЫ РАЗВИТИЯ ГЕОЛОГИЧЕСКИХ СТРУКТУР Проблемы постгеосинклинальноrо тектонического развития Центрально-Азиатского складчатого пояса / А. Л Яншин Геосииклинальные складчатые структуры МНР / Н. С. Зайцев Основные черты тектоники Центральной зоны Восточной Монголии как области мезозойской тектоно-маrматической активизации / В. Т. Григоров Докембрийская тектоника Урало-Монгольского пояса и проблема палеоокеанов / Л. М. Парфенов, В. А. Попеко Проблема "фундамента" Байкальской складчатой области / К. А . Клитин Орогенный ярус байкалид и время его формирования / А. Н. Булгатов Основные черты тектонического строения каледонид юга Сибири / А. Л. Додин Внегеосинклинальные впадины обрушения юга Сибири и методологическне аспекты их изучения / В. С. Бочкарев Малые структурные формы метаморфических толщ Восточного Забайкалья и Южного Урала / В. И. Громин Основные черты строения и развития орогенных областей северо-востока Азии / К. Б. Мокшанцев Некоторые физические закономерности формирования сети разломов земной коры / С. И. Шерман Современные движения земной коры в южной части Байкальской рифтовой зоны и в сопредельных областях / П. П. Колмогорова, В. Г. Колмогоров Особенности строения современных и древних рифтовых зон / В. В. Федынский, А. Г. Гайнанов , Б. А . Соколов, Н. А. Страхова Роль волновых движений в формировании тектонических структур Южно-Сибирской краевой системы / В. Г. Гладков , In kyrillischer Schrift
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  • 77
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: AWI G3-24-95699
    Description / Table of Contents: Translation of abstract: The book summarizes and analyzes information about the mechanical properties of snow. Particular attention is paid to describing the patterns of deformation and destruction of snow and assessing the parameters characterizing its compaction, creep and resistance to destruction. The book is intended for a wide range of researchers of the Earth's cryosphere and engineers involved in forecasting avalanches and protecting against them, using snow for engineering purposes and combating the harmful effects of snow on human economic activity.
    Description / Table of Contents: В книге обобщены и проанализированы сведения о механических свойствах снега. Особое внимание уделено описанию закономерностей деформирования и разрушения снега и оценке параметров, характеризующих его уплотнение, ползучесть и сопротивление разрушению. Книга предназначена для широкого круга исследователей криосферы Земли и инженеров, занимающихся прогнозированием снежных лавин и защитой от них, использованием снега в инженерных целях и борьбой с вредным влиянием снега на хозяйственную деятельность человека.
    Type of Medium: Monograph available for loan
    Pages: 125 Seiten , Illustrationen
    Language: Russian
    Note: Translation of TABLE OF CONTENTS Preface Chapter 1. Some physical properties of snow Formation of ice crystals in the atmosphere Formation of snow cover Density and Porosity Breathability Water holding capacity and water permeability Heat capacity Latent heat of fusion and sublimation of ice Water vapor diffusion Thermal conductivity Metamorphism Chapter 2. Patterns of deformation and destruction of snow Deformation of ice crystals Interaction of snow grains Basic patterns of deformation and destruction of snow Chapter 3. Elastic properties of snow Propagation of elastic waves in snow Elastic deformations under static and dynamic loads Chapter 4. Snow compaction Compression seal. Snow compaction during compaction Snow compaction under short-term and vibration loads Techniques for artificial snow compaction Chapter 5. Snow Creep Shear creep Creep under uniaxial compression Tensile creep Creep under complex stress conditions Stress relaxation Creep under variable loads Chapter 6. Strength characteristics of snow Snow destruction Shear Strength Tensile strength Uniaxial compressive strength Snow hardness Bearing capacity of snow cover Chapter 7. Surface friction and snow adhesion Sliding friction Static friction and adhesion Chapter 8, Stability of snow cover on mountain slopes Compaction and flow of snow cover Limit equilibrium of snow cover on a flat slope Interaction of snow cover on a slope with obstacles Limit equilibrium of snow cover on a slope with complex orography Violation of the stability of snow cover and the occurrence of pavements Artificial retention of snow cover on mountain slopes Conclusion Literature , ОГЛАВЛЕНИЕ Предисповие Гпава 1. Некоторые физические свойства снега Образование кристаплов льда в атмосфере Формирование снежного покрова Плотность и пористость Воздухопроницаемость Водоудерживающая способность и водопроницаемость Теплоемкость Скрытая теплота плавления и возгонки льда Диффузия водяного пара Теплопроводность Метаморфизм Глава 2. Закономерности деформирования и разрушения снега Деформирование кристаплов льда Взаимодействие зерен снега Основные закономерности деформирования и разрушения снега Глава 3. Упругие свойства снега Распространение упругих волн в снеге Упругие деформации при статических и динамических нагрузках Глава 4. Уплотнение снега Компрессионное уплотнение. Уплотнение снега в процессе попзучести Уплотнение снега под действием кратковременных и вибрационных нагрузок Приемы искусственного уплотнения снега Глава 5. Ползучесть снега Ползучесть при сдвиге Ползучесть при одноосном сжатии Ползучесть при растяжении Ползучесть в условиях сложного напряженного состояния Релаксация напряжений Ползучесть при переменных нагрузках Глава 6. Прочностные характеристики снега Разрушение снега Прочность при сдвиге Прочность при растяжении Прочность при одноосном сжатии Твердость снега Несущая способность снежного покрова Глава 7. Поверхностное трение и адгезия снега Трение скольжения Статическое трение и адгезия Глава 8, Устойчивость снежного покрова на склонах гор Уплотнение и течение снежного покрова Предельное равновесие снежного покрова на ровном склоне Взаимодействие снежного покрова на склоне с препятствиями Предельное равновесие снежного покрова на склоне со сложной орографией Нарушение устойчивости снежного покрова и возникновение павин Искусственное удержание снежного покрова на склонах гор Заключение Литературе , In kyrillischer Schrift
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  • 78
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: AWI G2-24-95716
    Description / Table of Contents: Сборник включает материалы симпозиума "Поздиечетвертичная история и седиментогенез окраинных и внутренних морей", проведенного Океанографической комиссией АН СССР в 1977 г. На симпозиуме были рассмотрены результаты исследований последних лет в области стратиграфии и литологии четвертичных осадков морей СССР и шельфовой зоны Мирового океана, поздиечетвертичная история южных и дальневосточных морей СССР и некоторых морей европейского Севера. Сборник представляет интерес для геологов-четвертичников, географов, литологов, океанологов, морских геоморфологов и геологов.
    Description / Table of Contents: Translation of abstract: The collection includes materials from the symposium “Late Quaternary history and sedimentogenesis of marginal and inland seas”, held by the Oceanographic Commission of the USSR Academy of Sciences in 1977. The symposium examined the results of recent research in the field of stratigraphy and lithology of Quaternary sediments of the seas of the USSR and the shelf zone of the World Ocean, the late Quaternary history of the southern and the Far Eastern seas of the USSR and some seas of the European North. The collection is of interest to Quaternary geologists, geographers, lithologists, oceanologists, marine geomorphologists and geologists.
    Type of Medium: Monograph available for loan
    Pages: 211 Seiten , Illustrationen , 2 Kartenbeilagen
    Language: Russian
    Note: СОДЕРЖАНИЕ Особенности седиментогенеза на континентальных окраинах океанов и во внутренних морях / Ф. А. Щербаков Строение плиоцен-четвертичной толщи дна Баренцева моря на разрезе полуостров Рыбачий - острова Земля Франца-Иосифа / А. И. Блажчишин, Т. И. Линькова, О. В. Кириллов, Е. П. Шкатов К палеогеографии Баренцева моря в позднеледниковье и голоцене / Б. Н. Котенев Эволюция осадконакопления в прибрежных районах Баренцева и Белого морей в поздне- и послеледниковое время / В. Я. Евзеров Стратиграфия верхнечетвертичных отложений северной части Белого моря / Р. Н. Джиноридзе, Е. А. Кириенко, Л. В. Калугина, А. Е. Рыбалко, М. А. Спиридонов, Е. А. Спиридонова Палинологический и диатомовый анализ донных отложений Балтийского моря / Г. И. Клейменова, В. И. Хомутова, Е. М. Вишневская Стратиграфия позднечетвертичных отложений Черного моря / Ф. А. Щербаков, Е. В. Коренева, Э. К. Забелина Палеогеография Черноморского бассейна в позднечетвертичное время по данным палинологического анализа глубоководных отложений / А. В. Комаров Особенности седиментогенеза в морских подводных каньонах кавказского шельфа Черного моря / К. И. Джанджгава Об изменении биопродуктивности вод Черного моря в голоцене / Н. М. Андреева, Б. Н. Котенев, Л. Н. Розов Закономерности формирования и распределения водно-физических свойств глубоководных осадков Черного моря / В. А. Емельянов, А. Ю. Митропольский Геологическая история Керченского пролива в позднечетвертичное время / Е. Ф. Шнюков, В. М. Аленкин, А. В. Григорьев, А. Л. Путь, Н. А. Ломаев Отражение глубинных структур в морских четвертичных отложениях центральной части Азовского моря / В. Н. Семененко, О. Г. Сиденко Марганцеворудный процесс в позднем антропогене Азово-Черноморского бассейна / Г. Н. Орловский Палеоклиматы, водный баланс и уровни Черного и Каспийского морей в позднем плейстоцене-голоцене / И. Г. Авенариус Гипотетическая климатическая кривая основных этапов осадконакопления Каспийского моря в позднем плейстоцене / В.К Шкатова Процессы седиментогенеза в море Леванта / А. А. Мусса, А. Ю. Митропольский Петрографо-минералогическая характеристика современных отложений Бенгальского залива и Андаманского моря / Д. Е. Гершанович, А. И. Конюхов, И. А.Назаревич Терригенно-минералогические провинции прибрежно-шельфовой зоны Западного Индостана / О. К. Тареева Морфотектоника материкового побережья юга Дальнего Востока и морские трансгрессии позднего плейстоцена-голоцена / А. П. Кулаков Последние этапы голоценовой трансгрессии в бассейнах Японского и Охотского морей / А. М. Короткий, П. Ф. Бровко, И. И. Задкова, В. С. Пушкарь, И. Г. Шахгельдян Основные черты геологического строения шельфа и материкового склона Японского моря у побережья СССР / И. И. Берсенев, И. К. Пущин Четвертичные отложения шельфа Южного приморья на примере залива Петра Великого (Японское море) / Ю. Д. Марков Позднеnлейстоценовые бассейны Юго-Западной Камчатки и их связь с неотектоническими движениями / Р. Б. Крапивнер Криолитозона арктического шельфа Азии / З. Н. Антипина, Ф. Э. Арэ, В. В. Войченко, E. H. Молочушкин Опыт количественной оценки голоценовых тектонических движений в области шельфа / Н. Н. Дунаев Об использовании метода измерения магнитной восприимчивости морских осадков для восстановления условий их формирования на шельфе / Ю. В. Кочемасов , Translation of Table of Contents Features of sedimentogenesis on the continental margins of the oceans and in inland seas / F. A. Shcherbakov Structure of the Pliocene-Quaternary strata of the Barents Sea bottom in the section of the Rybachy Peninsula - Franz Josef Land Islands / A. I. Blazhchishin, T. I. Linkova, O. V. Kirillov, E. P. Shkatov On the paleogeography of the Barents Sea in the Late Glacial and Holocene / B. N. Kotenev Evolution of sedimentation in the coastal areas of the Barents and White Seas in late and post-glacial times / V. Ya. Evzerov Stratigraphy of Upper Quaternary sediments of the northern part of the White Sea / R. N. Dzhinoridze, E. A. Kiriyenko, L. V. Kalugina, A. E. Rybalko, M. A. Spiridonov, E. A. Spiridonova Palynological and diatom analysis of bottom sediments of the Baltic Sea / G. I. Kleimenova, V. I. Khomutova, E. M. Vishnevskaya Stratigraphy of Late Quaternary sediments of the Black Sea / F. A. Shcherbakov, E. V. Koreneva, E. K. Zabelina Paleogeography of the Black Sea basin in the late Quaternary according to palynological analysis of deep-sea sediments / A. V. Komarov Features of sedimentogenesis in marine underwater canyons of the Caucasian shelf of the Black Sea / K. I. Dzhandzhgava On changes in the bioproductivity of the Black Sea waters in the Holocene / N. M. Andreeva, B. N. Kotenev, L. N. Rozov Regularities of formation and distribution of water-physical properties of deep-sea sediments of the Black Sea / V. A. Emelyanov, A. Yu. Mitropolsky Geological history of the Kerch Strait in the late Quaternary / E. F. Shnyukov, V. M. Alenkin, A. V. Grigoriev, A. L. Put, N. A. Lomaev Reflection of deep structures in marine Quaternary sediments of the central part of the Azov Sea / V. N. Semenenko, O. G. Sidenko Manganese ore process in the late Anthropogene of the Azov-Black Sea basin / G. N. Orlovsky Paleoclimates, water balance and levels of the Black and Caspian Seas in the Late Pleistocene-Holocene / I. G. Avenarius Hypothetical climate curve of the main stages of sedimentation of the Caspian Sea in the Late Pleistocene / V.K Shkatova Processes of sedimentogenesis in the Levant Sea / A. A. Mussa, A. Yu. Mitropolsky Petrographic-mineralogical characteristics of modern sediments of the Bay of Bengal and the Andaman Sea / D. E. Gershanovich, A. I. Konyukhov, I. A. Nazarevich Terrigenous-mineralogical provinces of the coastal-shelf zone of Western Hindustan / O. K. Tareeva Morphotectonics of the continental coast of the south of the Far East and marine transgressions of the late Pleistocene-Holocene / A. P. Kulakov The last stages of the Holocene transgression in the basins of the Sea of Japan and the Sea of Okhotsk / A. M. Korotkiy, P. F. Brovko, I. I. Zadkova, V. S. Pushkar, I. G. Shakhgeldyan Main features of the geological structure of the shelf and continental slope of the Sea of Japan off the coast of the USSR / I. I. Bersenev, I. K. Pushchin Quaternary sediments of the Southern Primorye shelf using the example of Peter the Great Bay (Sea of Japan) / Yu. D. Markov Late Leistocene basins of Southwestern Kamchatka and their connection with neotectonic movements / R. B. Krapivner Cryolithozone of the Arctic shelf of Asia / Z. N. Antipina, F. E. Are, V. V. Voichenko, E. H. Molochushkin Experience in quantitative assessment of Holocene tectonic movements in the shelf area / N. N. Dunaev On the use of the method of measuring the magnetic susceptibility of marine sediments to restore the conditions of their formation on the shelf / Yu. V. Kochemasov , In kyrillischer Schrift
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  • 79
    Call number: MOP Per 607(216)
    In: Trudy
    Type of Medium: Monograph available for loan
    Pages: 130 S.
    Series Statement: Trudy / Gidrometeorologičeskij Naučno-Issledovatel'skij Centr SSSR 216
    Language: Russian
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  • 80
    Monograph available for loan
    Monograph available for loan
    Warszawa : Polish Scient. Publ.
    Call number: PIK N 456-11-0194
    Description / Table of Contents: Contents: 1. Climatology as a science ; 2. Climate-forming factors ; 3. Geographical distribution and variation of major meteorological elements ; 4. A brief survey of major types of climate ; 5. Changes and fluctuations of climates
    Type of Medium: Monograph available for loan
    Pages: XIV, 422 S. : graph. Darst., 1 Kt.
    Uniform Title: Klimatologia ogólna
    Language: English
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  • 81
    Call number: MOP 44357 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 227 S.
    Series Statement: Problemy Konstruktivnoj Geografii
    Language: Russian
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  • 82
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-345
    In: Research report / Cold Regions Research and Engineering Laboratory, 345
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - List of symbols. - Introduction. - Previous work. - Experimental design. - The radioisotope 22Na. - Description of apparatus. - Experimental procedure. - Correction of profiles. - Assumptions. - Decay correction. - Boundary correction. - Error analysis. - Results. - Salinity data. - Temperature data. - Growth velocity. - Discussion. - Brine and ice properties. - Brine salinity. - Brine density. - Brine volume. - Brine latent heat of freezing. - Brine viscosity, specific heat, and thermal conductivity. - Ice properties. - Theoretical brine expulsion model. - Continuity equations. - Thermal energy equation. - Simplified brine expulsion equations. - Brine expulsion in NaCl ice. - Results. - Discussion. - Gravity drainage in NaCl ice. - Application of results to natural sea ice. - Effective distribution coefficient. - Previous work. - Experimental procedure and results. - Conclusions. - Literature cited. - Appendix A: Profile correction data. - Appendix B: Program "correct" and sample output. - Appendix C: Tabulation of salinity data. - Appendix D: Tabulation of profile data. - Appendix E: Time-ice thickness equations (Runs 2 and 3). - Appendix F: Tabulation of distribution coefficient data.
    Description / Table of Contents: To obtain a better understanding of the desalination of natural sea ice, an experimental technique was developed to measure sequential salinity profiles of a growing sodium chloride ice sheet. Using radioactive 22Na as a tracer, it was possible to determine both the concentration and movement of the brine within the ice without destroying the sample. A detailed temperature and growth history of the ice was also maintained so that the variation of the salinity profiles could be properly interpreted. Since the experimental salinity profile represented a smoothed, rather than a true salinity distribution, a deconvolution method was devised to restore the true salinity profile. This was achieved without any significant loss of end points. In all respects, the salinity profiles are similar to those of natural sea ice. They have a characteristic C-shape, and clearly exhibit the effects of brine drainage. Not knowing the rates of brine expulsion or gravity drainage, the variation of the salinity profiles during the period of ice growth could be explained by either process. To determine the relative importance of the desalination mechanisms, a theoretical brine expulsion model was derived and compared to the experimental data. As input for the model, equations describing the variation of some properties of NaCl brine with temperature were derived. These included the brine salinity, viscosity, specific heat, thermal conductivity, and latent heat of freezing. The theoretical brine expulsion model was derived by performing mass and energy balances over a control volume of NaCl ice. A simplified form of the model, when compared to the experimental results, indicated that brine expulsion was only important during the first several hours of ice growth, and later became a minor desalination process relative to gravity drainage which continued to be the dominant mechanism for the remainder of the study period (up to 6 weeks). The rate of gravity drainage was found to be dependent on the brine volume and the temperature gradient of the ice. As either the brine volume or temperature gradient was increased, the rate of change of salinity due to gravity drainage increased. The equation commonly used to calculate the effective distribution coefficient (Weeks and Lofgren 1967) was modified and improved by taking brine drainage into account. An expression was also derived to give the distribution coefficient at very low growth velocities.
    Type of Medium: Series available for loan
    Pages: vii, 85 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 345
    Language: English
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  • 83
    Monograph available for loan
    Monograph available for loan
    Boulder, Colo. : Environmental Research Laboratories
    Call number: MOP 41125 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VIII, 499 Seiten
    Language: English
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  • 84
    Call number: ZSP-799-326
    In: Trudy Ordena Lenina Arktičeskogo i Antarktičeskogo Naučno-Issledovatel'skogo Instituta, Tom 326
    Type of Medium: Series available for loan
    Pages: 228 Seiten , Illustrationen , 23 cm
    Series Statement: Trudy Ordena Lenina Arktičeskogo i Antarktičeskogo Naučno-Issledovatel'skogo Instituta 326
    Language: Russian
    Note: CONTENTS: Foreword. - Radio physical methods of ice and snow studies / V. V. Bogorodsky. - Radar frequency-modulated signals reflected from ice surfaces and the possibility of their modelling / A. B. Babayev, V. P. Logachev, V. N. Parfentyev, V. A. Fedorov, G. P. Shelomanova. - Ice structure and its effect on ice SHF emissivity / A. Ye. Basharinov, A. A. Kurskaya. - Radio wave propagation in glaciers / V. V. Bogorodsky, G. V. Trepov, B. A. Fedorov. - Radio echo sounding of sea ice / V. V. Bogorodsky, V. P. Tripolnikov. - Emissivity of ice, land and sea surfaces modelled by layered heterogeneous structures / V. V. Bogorodsky, A. I. Kozlov, L. T. Tuchkov. . - Radio sounding wide angle reflection measurements / J. W. Clough. - Depolarization of radio echo returns / J. W. Clough. - Remote radar measurements of sea ice thicknesses / M. I. Finkelshtein, V. A. Kutev, V. G. Glushnev, E. I. Lazarev. - Electrical properties of the vacuum-formed ice and their dependence on structure / A. K. Zhebrovsky, G. M. Strakhovsky, V. N. Nedostayev, V. I. Stebin. - Ice forces on separate supporting structures by laboratory and field tests / S. A. Vershinin, Ye. M. Kopaygorodsky, V. V. Panov, Z. I. Shvaishtein. - Correlation between the salinity of sea ice and extinction coefficient at 6328 Å / H. Davis, R. Munis. - Optical characteristics of some vanehes of natural ice / B. Ya. Gaitskhoki. - Instruments for the investigation of spectral reflection of liquid water on 1-50 Mm wave lengths / M. A. Kropotkin. - On the study of the process of charge generation at the phase interface of 10-3 molar solution of natrium chlorirde, freezing oriented / V. Petera. - The behavior of ice in rapidly variable electromagnetic fields of high intensity / L. B. Nekrasov. - Magnetic survey of ice wedges / B. V. Volodko, V. S. Yakupov, E. N. Akhmedzyanov, V. M. Kalinin, V. O. Papitashvili, G. A. Sereda. - Low frequency polarization of ice and frozen coarse-disperse formations / V. P. Melnikov, A. M. Snegiryev. - Coastal ice dynamics by SLAR observations / S. M. Losev, Yu. A. Gorbunov. - Surface water temperature observations by airborne radiation thermometer / A. I. Paramonov, Yu. A. Gorbunov, S. M. Losev. - Acoustic techniques in snow and ice studies / V. P. Gavrilo, A. V. Gusev. - Attenuation and scattering of sound waves by sea ice / V. V. Bogorodsky, G. E. Smirnov, S. A. Smirnov. - A study of sound attenuation in natural ice / N. A. Grubnik, O. V. Kudryavtsev. - Ice cover studies by seismic and tiltmeter methods / V. N. Smirnov, Ye. M. Linkov. - Glacier dynamics studies by laser deformograph / I. M. Belousova, I. P. Ivanov, N. G. Firsov. - An expenmental study of ice adhesion by laboratory and field tests / V. V. Panov, A. V. Panyushkin, Yu. D. Sinochkin, Z. I. Shvaishtein. - A study of ice layer destruction process / N. A. Grubnik, V. I. Fomin, A. B. Shemyakin. - Mechanical propterties of snow related to its use as a construction material / A. F. Wuori. - Arctic snow cover / I. M. Dolgin, N. N. Bryazgin, L. S. Petrov. - A technique to measure large moisture content in the snow by cosmic radiation / S. I. Avdyushin, Y. F. Barabantshchikov, R. M. Kogan, Y. M. Kulagin, I. M. Nazarov, Sh. D. Fridman, I. S. Yudkevich. - Techniques for measuring the strength characteristics of natural and processed snow / G. Abele. - Statistic evaluation of spatial distribution of the main parameters of the ice cover / A. Ya. Buzuyev. - Study of mechanical properties of fresh-water ice with slowly variable load / K. N. Korzhavin, A. B. Ivchenko. - On the short-term ice creep and micro crack kinetics of new formations / Yu. K. Zaretsky, A. M. Fish, V. P. Gavrilo, A. V. Gusev. - Field tests of physical and mechanical properties of the ice cover / A. Ya. Ryvlin. - Determination of specific failure energy and impact pressure values of ice / D. Ye. Kheisin, V. A. Likhomanov, V. A. Kurdyumov. - Radio hydro/acoustical method to study meso-scale characteristics of sea ice dynamics / V. V. Bogorodsky, V. P. Gavrilo, A. P. Polyakov. , In kyrillischer Schrift , Mit englischem Inhaltsverzeichnis
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  • 85
    Call number: MOP 40135/1 / Mitte
    In: Issledovanija statističeskoj struktury meteorologičeskich polej, Tom I
    Type of Medium: Monograph available for loan
    Series Statement: Issledovanija statističeskoj struktury meteorologičeskich polej 1
    Language: Russian
    Note: In kyrillischer Schrift
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  • 86
    Series available for loan
    Series available for loan
    Columbus, Ohio : Institute of Polar Studies, The Ohio State University
    Associated volumes
    Call number: AWI G7-19-92159
    In: Report / Institute of Polar Studies, No. 64
    Type of Medium: Series available for loan
    Pages: XVII, 148 Seiten , Illustrationen
    Series Statement: Report / Institute of Polar Studies 64
    Language: English
    Note: TABLE OF CONTENTS: Abstract. - Acknowledgments. - List of Figures. - List of Plates. - List of Tables. - Value of Microparticle Studies. - Reasons for Variations in Particle Concentration. - Laboratory Techniques. - Particle Concentration and Size Distribution. - Sample Preparation. - Contamination. - Particle Counters. - Laboratory Procedures. - Particle Composition. - Sample Preparation. - Types of Particles and Their Seasonal Variation. - Particle Types. - Variations of Particle Concentrations. - Antarctic Peninsula. - Marie Byrd Land. - Quelccaya Ice Cap, Peru. - Annual Layers in Deep Ice Cores. - Chronologies for the Byrd and Camp Century Deep Ice Cores. - The Byrd Station Deep Ice Core. - Age Calculation. - Discussion. - The Camp Century Deep Ice Core. - Vertical Strain Rates. - Age Calculation. - Discussion. - Morphology and Elemental Composition of Microparticles. - Data Analysis. - Results. - Discussion. - The Relationships Among Dust, Oxygen Isotopes and Climate. - Microparticle Variations Over Millennial Time Invervals. - Dust, Oxygen Isotopes and Climate. - Discussion. - Is There A Relationship Between Volcanic Activity and Climatic Change?. - General. - Theory. - Supportive Evidence. - Cycles. - Discussion. - Suggestions for Future Work. - Conclusions. - References. - Appendix A. - Appendix B. - Appendix C. - Appendix D.
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  • 87
    Monograph available for loan
    Monograph available for loan
    Urbana : Illinois State Water Survey
    Call number: MOP 45166
    Type of Medium: Monograph available for loan
    Pages: 57 Seiten
    Language: English
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  • 88
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45541 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 422 Seiten
    Uniform Title: Principles of applied climatology
    Language: Russian
    Note: In kyrillischer Schrift
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  • 89
    Call number: MOP 45693 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 238 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 90
    Call number: MOP 45268 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 302 Seiten , graphische Darstellungen, Karten
    Language: English
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  • 91
    Call number: MOP 45568 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 171 Seiten , Illustrationen , 20 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 92
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45558 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 231 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 93
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/12
    In: CRREL Report, 79-12
    Description / Table of Contents: An analysis of a point source bubbler system used to induce local melting of an ice cover is presented. The analysis leads to a numerical simulation programmed in FORTRAN which may be used to predict the effectiveness of such systems. An example application is presented using a typical record of average daily air temperatures. The FORTRAN program for the point source simulation as well as a FORTRAN program for line source systems are included in the Appendix.
    Type of Medium: Series available for loan
    Pages: iii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-12
    Language: English
    Note: CONTENTS Abstract Preface Introduction Outline of analysis Plume analysis Heat transfer analysis Temperature of impinging plume Heat transfer coefficient Melting of the ice cover Simulation example Thermal reserve analysis Literature cited Appendix
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  • 94
    Series available for loan
    Series available for loan
    Hanover, NH : U. S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-85/21
    In: CRREL Report, 85-21
    Description / Table of Contents: The development of lightweight coring augers for ice is reviewed. Emphasis is on equipment designed by the Cold Regions Research and Engineering Laboratory and its predecessor organizations for sampling to depths less than 20 m or so. Design and operation of the ACFEL/SIPRE/CRREL 3-in. -ID corer is discussed, and modifications of the basic design for powered operation and for drilling in frozen soil are outlined. Recent replacements for the traditional coring auger are described, and details are given for the construction and operation of the new 4 1/4-in-ID coring equipment. A powered 12-in.-ID drill for shallow-depth coring is also described.
    Type of Medium: Series available for loan
    Pages: iii, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 85-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction The 3-inch ice corer The Rand auger Parallel development of comparable drills The Big John 12-inch corer Power drives A simple Russian ice-corer Conclusions Literature cited
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  • 95
    Monograph available for loan
    Monograph available for loan
    Bochum : Studienverlag Brockmeyer
    Call number: MOP 44382 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 85 Seiten , 5 graphische Darstellungen
    Language: English
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  • 96
    Call number: MOP 40348/1 / Mitte
    In: Spravočnik po klimatu SSSR, Tom 1
    Type of Medium: Monograph available for loan
    Series Statement: Spravočnik po klimatu SSSR : Ustojčivostʹ i točnostʹ klimatičeskich charakteristik / Pod. red. O. A. Drozdova i I. D. Kopaneva 1
    Language: Russian
    Note: In kyrillischer Schrift
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  • 97
    Call number: MOP 40348/3 / Mitte
    In: Spravočnik po klimatu SSSR, Tom 3
    Type of Medium: Monograph available for loan
    Series Statement: Spravočnik po klimatu SSSR : Ustojčivostʹ i točnostʹ klimatičeskich charakteristik / Pod. red. O. A. Drozdova i I. D. Kopaneva 3
    Language: Russian
    Note: In kyrillischer Schrift
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  • 98
    Call number: MOP 44943 / Mitte
    Type of Medium: Monograph available for loan
    Language: English
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  • 99
    Monograph available for loan
    Monograph available for loan
    Obninsk : Informacionnyj Centr
    Call number: MOP 44752 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 42 Seiten , Illustrationen , 20 cm
    Series Statement: Serija Meteorologija / VNII Gidrometeorologičeskoj Informacii - Mirovoj Centr dannych
    Language: Russian
    Note: In kyrillischer Schrift
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  • 100
    Monograph available for loan
    Monograph available for loan
    Geneva : World Meteorological Organization
    Call number: MOP 44781/1 / Mitte ; MOP 44781/2 / Mitte
    Description / Table of Contents: Content: Provisional Programme Introduction: Climate and society: lessons from recent events / Robert R. Kates Overview Paper 1: Climatic change and human strategy / E. K. Fedorov Overview Paper 2: Global ecology and man / Bert Bolin Overview Paper 3: Climatic variation and variability: empirical evidence from meteorological and other sources / F. Kenneth Hare Overview Paper 4: Climates of past geological epochs / I. P. Gerasimov Overview Paper 5: The physical basis of climate / W. Lawrence Gates Overview Paper 6:Modelling of climatic changes and the problem of long-range weather forecasting / G. I. Marchuk Overview Paper 7: Climate monitoring and climatic data collection services for determining climatic changes and variations / Ju. A. Izrael Overview Paper 8: Human activities that affect climate / R. E. Munn and L. Machta Overview Paper 9: Some results of climate experiments with numerical models / B. J. Mason Overview Paper 10: A scenario of possible future climates - natural and man-made / H. Flohn Overview Paper 11: missing Overview Paper 12: Climate variability and the design and operation of water resource systems Overview Paper 13: Climate, health and disease / Wolf H. Weihe Overview Paper 14: Global aspects of food production / M. S. Swaminathan Overview Paper 15: Climatic variability and agriculture in the temperate regions / James D. McQuigg Overview Paper 16: Climatic variability and agriculture in tropical moist regions / Hayao Fukui Overview Paper 17: Climatic variability and agriculture in the semi-arid tropics / Francesco Mattei Overview Paper 18: Climatic change and the exploitation of climatic resources in china / Chang Chia-cheng, Wang Shao-wu, Cheng Szu-chung Overview Paper 19 (2x): Climatic variability and land use : an african perspective / Julius S. Oguntoyinbo and Richard S. Odingo Overview Paper 20: Renewable resources and agriculture in Latin America in relation to the stability of climate / Juan J. Burgos Overview Paper 21: Climatic variability and forestry / A. Baumgartner Overview Paper 22: Climatic variation and marine fisheries / D. H. Cushing Overview Paper 23: Climatic variability, marine resources and offshore development / T. F. Gaskell Overview Paper 24: Climate and economic activity / Ralph C. d'Arge
    Type of Medium: Monograph available for loan
    Pages: 2 Ordner
    Language: English
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