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  • 1
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik bei der Akademie der Wissenschaften der Deutschen Demokratischen Republik
    Associated volumes
    Call number: MOP Per 581(2/22) ; ZSP-319/B-22 ; ZSP-319/B-22(2. Ex.)
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre, Heft 22
    Type of Medium: Series available for loan
    Pages: 56 Seiten , Illustrationen
    ISSN: 0533-7585
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre 22
    Language: German
    Note: INHALT: Vorwort. - 1. Das Arbeitsprogramm während der 21. SAE und die Bearbeitung des Beobachtungsmaterials. - 1.1. Das Arbeitsprogramm während der 21. SAE. - 1.2. Bearbeitung und Nutzung des Beobachtungsmaterials. - 2. Das ionosphärische Beobachtungsprogramm. - 2.1. Zielstellung für das ionosphärische Beobachtungsprogramm. - 2.2. Beobachtungsmethoden. - 2.2.1. A1-Absorptionsmessungen. - 2.2.2. A2-Absorptionsmessungen. - 2.2.3. A3-Absorptionsmessungen. - 2.2.4. Polarlichtbeobachtungen. - 2.3. Grundlagen für die Primärauswertung. - 3. Ionosphärische Bedingungen für A1-Messungen in subauroralen Breiten über der Station "Novolasarevskaja". - 3.1. Beobachtungsergebnisse anderer Stationen. - 3.2. Ionosphärische Reflexionsbedingungen über Novolasarevskja von Juni bis Dezember 1976. - 3.3. Einfluß der Reflexionsbedingungen auf das jahreszeitliche Absorptionsverhalten. - 3.3.1. Ermittlung von Absorptionswerten bei A1-Messungen in subauroralen Breiten. - 3.3.2. Absorption und scheinbare Reflexionshöhe im Jahresgang. - 3.3.2.1. Normalverhalten im Juli 1976. - 3.3.2.2. Normalverhalten im September 1976. - 3.3.2.3. Normalverhalten im Dezember 1976. - 3.4. Zusammenfassung. - 4. Frequenzabhängigkeit der Absorptionsmessungen. - 4.1. Vergleich zwischen A1- und A2-Messungen. - 4.2. Frequenzabhängigkeit der Meßverfahren. - 5. Einfluß der Winteranomalie auf die Ausbreitung von Langwellen. - 5.1. Ausbreitung der Langwellen über große Entfernungen (A3-Methode). - 5.2. Wirkungen der Winteranomalie auf die Langwellenausbreitung. - 6. Bemerkungen zur Umstellung des stratomesosphärischen Zirkulationssystems der Südhemisphäre. - 6.1. Beobachtungen über der Station Molodjoshnaja. - 6.2. "Break-down" der Winteranomalie auf der Nord- und der Südhemisphäre. - 6.3. Phänomenologische Zusammenstellung von Beobachtungen auf der Südhemisphäre für Juni 1976 bis Oktober 1976. - 6.3.1. Verfügbares Datenmaterial. - 6.3.2. Vergleichende Betrachtung der Meßreihen. - 7. Bemerkungen zum Tages- und Jahresgang der iono~phärischen Absorption in subauroralen Breiten. - 7.1. Tagesgänge der Absorption bei den A1- und A2-Messungen. - 7.2. Besonderheiten im Jahresgang der Absorption. - 8. Nächtliche Es -Schichten bei ruhigen oder schwach gestörten Bedingungen. - 8.1. Tagesgang der Reflexionsbedingungen. - 8.2. Einfluß des Polarlichtovals. - 9. Partikelpräzipitation in subauroralen südlichen Breiten. - 9.1. Perioden erhöhter Partikelpräzipitation von Juni bis Oktober 1976. - 9.2. Absorptionsverhalten der Mesopausenregion bei erhöhter Partikelpräzipitation. - 10. Komplexe Betrachtung eines Substorms am 29. 07. 1976 / (GERNANDT, H.; GRAFE, A.). - 10.1. Registrierung des Substormereignisses. - 10.2. Höhenvariationen der scheinbaren Reflexionshöhe und Absorptionsvariationen bei der A1-Messung. - 10.3. Komplexe Betrachtung des Substorms am 29. 07. 1976. - 11 . Bemerkungen zur Breitenabhängigkeit der ionosphärischen Absorption / (BREMER, J.; GERNANDT, H.). - 11.1. Absorptionsmessungen auf dem Expeditionsschiff "Kapitan Markow". - 11.2. Breitenabhängigkeit der ionosphärischen Absorption. - 11.3. Theoretische Breitenabhängigkeit der ionosphärischen Absorption. - 12. Zusammenfassung über die ionosphärischen Beobachtungen. - 13. Weitere Ergebnisse aus dem Arbeitsprogramm der DDR-Überwinterungsgruppe in Novolasarevskaja. - 13.1. Erprobung der Ozonradiosonde OSE 2 über der sowjetischen Antarktisstation Novolasarevskja während der 21. SAE. - 13.1.1. Einleitung. - 13.1.2. Einsatzbedingungen für die Ozonsonde in der Station Novolasarevskaja. - 13.1.3. Durchführung der Aufstiege. - 13.1.4. Ergebnisse der Primärauswertung. - 13.2. Satellitenbeobachtung der Seeisgrenze im Küstengebiet Königin-Maud-Land bis Filchner-Schelfeis. - 13.2.1. Einleitung. - 13.2.2. Bearbeitung des Bildmaterials. - 13.2.3. Die Eisverhältnisse im November 1976. - 13.2.4. Die Eisverhältnisse im Dezember 1976. - 13.2.5. Die Eisverhältnisse im Januar 1977. - 13.3. Unterwasseraufnahmen der Bodenvegetation in Seen der Schirmacher-Oase / (KAUP, E.; PROBST, W.; GERNANDT, H.). - 13.3.1. Bemerkungen zur Unterwasservegetation in antarktischen Frischwasserseen. - 13.3.2. Physikalische Bedingungen in den Oasenseen und deren Umgebung für die Unterwasserfotografie. - 13.3.3. Technik der Unterwasserfotografie. - 13.3.4. Zusammenfassung. - 14. Literaturverzeichnis.
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  • 2
    Call number: MOP Per 581(1/6) ; ZSP-319/A-6
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 1, Nr. 6
    Type of Medium: Monograph available for loan
    Pages: 42 Seiten , Illustrationen
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 1 6
    Language: German
    Note: Inhalt: Vorwort. - Begrüßungsrede / H. Werner. - Laudatio / W. Rüger. - Grußadressen. - Neue Aspekte der Hochschulausbildung in der Geodäsie / K. Rinner. - Fehlertheoretische Interpretationen der zweidimensionalen Verianzanalyse / J. Böhm. - Ergebnisse und Probleme bei der Erforschungs des Erdkörpers / H. Stiller. - Neue Aspekte der globalen Geodäsie / L. Stange. - Schlußwort / H. Peschel.
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  • 3
    Call number: ZSP-201-79/1
    In: CRREL Report, 79-1
    Description / Table of Contents: Experiments were conducted to study the flow of water through columns of homogeneous, repacked snow. The gravity flow theory of water flow through snow was verified, although possibly there is some dependence of the relative permeability on the state of metamorphism of the snow. Also, at very large values of saturation there may be some additional flow in saturated channels.
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 79-1
    Language: English
    Note: CONTENTS Preface Symbols Introduction Test procedure Theory Evaluation of the experimental results Example evaluation Results and discussion Literature cited Appendix A. Measured and computed discharge
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  • 4
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/20
    In: CRREL Report, 78-20
    Description / Table of Contents: Abstract: Measurements of the concentrations of Aitken nuclei in maritime air were made near Barrow, Alaska, in June 1975 with a modified Nolan-Pollack small-particle detector. The concentrations varied from 50 to 300 particles cm^-3 depending upon meteorological conditions. The mean Aitken nuclei count was 100 particles cm^-3 for diameters greater than 2 x 10^-3 μm. Transmission electron micrographs of aerosols in maritime air near Barrow were taken. The size range was measured to be 0.01 to 2.5 μm in diameter with the most frequently observed diameter being 0.04 μm. The volume of the maritime air and the collection efficiency of aerosol particles on filmed grids for electron microscopy were measured. The aerosol concentrations were found to be 76 to 101 particles cm^-3 ; the mean concentration was calculated to be 87 particles cm^-3. The aerosol particles in the maritime air were identified by electron microscopy and selected area electron diffraction analysis. About 20% of the aerosol particles were identified, and 80% of the particles were too small for electron diffraction analysis. Sea salt particles constituted 2% of the total, and clay minerals 3%; these particles were considered to be of natural origin. Solid combustion by-products such as coagulated carbon particles and fly ash particles constituted 16%. Despite the comparative remoteness of the sampling site, the measurements indicate that many anthropogenic aerosols were found using an electron microscope.
    Type of Medium: Series available for loan
    Pages: iv, 48 Seiten , Illustrationen
    Series Statement: CRREL Report 78-20
    Language: English
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  • 5
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/13
    In: CRREL Report, 78-13
    Description / Table of Contents: Field observations of the growth fabrics of the fast and near-fast ice along the coasts of the Beaufort and Chukchi Seas show that, at depths of more than 60 cm below the upper ice surface, the sea ice crystals show striking alignments within the horizontal plane. At one site this alignment was well developed at a depth of 15 cm and in all cases the degree of preferred orientation increased with depth, with the strongest orientations occurring at the bottom of the ice sheet. In general the c-axes of the crystals were aligned roughly E-W parallel to the coast. In the vicinity of islands the alignment roughly paralleled the outlines of the islands and in narrow passes between islands the alignment paralleled the channel. Our observations, as well as similar observations made in the Kara Sea by Cherepanov, can be explained if it is assumed that the c-axes of the crystals are aligned parallel to the 'long-term' current direction at the sea ice/sea water interface. The alignments are believed to be the result of geometric selection among the growing crystals, with the most favored orientation being that in which the current flows normal to the (0001) plates of ice that make up the dendritic ice/water interface characteristics of sea ice. It is hypothesized that current flow in this direction reduces the thickness of the solute boundary layer as well as the salinity in the liquid at the interface. This lowered salinity allows crystals in the favored orientation to extend farther into the melt than neighboring crystals with less favored orientations. In addition the current tends to induce a continuous flux of supercooled seawater against the sides of the crystals that extend ahead of the interface.
    Type of Medium: Series available for loan
    Pages: v, 29 Seiten , Illustrationen
    Series Statement: CRREL Report 78-13
    Language: English
    Note: CONTENTS Abstract Preface Introduction Locale and techniques Observations Vertical variations in crystal orientation Regional variations in crystal orientation Summary of observations Causes Initial ice skim Earth’s magnetic field Currents Conclusions and consequences Literature cited
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  • 6
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/10
    In: CRREL Report, 78-10
    Description / Table of Contents: The compressibility of wet snow is described in terms of pressure melting and nonlinear viscous deformation at grain contacts. The results of experiments with different salinities and liquid water contents are compared with computed densities. The decreasing compressibility of wet snow with increasing salinity and decreasing liquid content is quantified and explained. Simultaneous particle growth and the doubly charged layer at phase boundaries are included in the model. The results show that the density of wet snow increases approximately as a power of time but is highly dependent on the stress, initial particle size, liquid water content, and ionic impurity content of the snow.
    Type of Medium: Series available for loan
    Pages: vi, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 78-10
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Experimental procedure Grain growth Stressed particle contacts Fluid pressure Packing geometry Temperature distribution and heat flow Fluid and impurity flows Results The liquid film Conclusions Literature cited
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  • 7
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/18
    In: CRREL Report, 78-18
    Description / Table of Contents: The primary objective of this project was to demonstrate the utility of remote sensing techniques as an operational tool in the acquisition of data required by the U.S. Army Corps of Engineers, Seattle District, in the Grays Harbor dredging effects project, and related projects. Aerial imagery was used to map surface circulation and suspended sediment patterns near the hopper dredge pump site at the harbor entrance and near pulpmill outfalls in Aberdeen, and to map the areal distribution and extent of intertidal habitats. The surface circulation maps prepared from the aerial photographs and thermal imagery compared favorably with the large-scale circulation patterns observed in the Grays Harbor hydraulic model at the U.S. Army Engineer Waterways Experiment Station. Of the imagery provided by NASA, the thermal imagery was more useful than the color or color infrared (CIR) photographs for mapping circula­tion, while the CIR photographs were more useful than the thermal imagery or the color photographs for mapping intertidal habitats. Current velocities estimated from dye dispersion patterns and drifting dye drogues were comparable at some locations to velocities measured by in situ current meters and in the hydraulic model. Based on a cursory evaluation of LANDSAT-1 imagery acquired in January, February, and October 1973, it had limited utility in providing data on surface circulation patterns in Grays Harbor. The areal distribution and extent of nine wetland vegetation types, dune vegetation, and three types of eelgrass were mapped using primarily aerial C IR photographs and ground sur­veys. Color photographs were also used for areas not covered by the C IR photographs. Wetland vegetation types mapped were: low silty marsh, low sandy marsh, sedge marsh, high immature marsh, high mature marsh, salt marsh, diked pasture, freshwater marsh, and wooded swamp. Undiked salt marsh (first five types) covered 5540 acres (22.3 km2) in Grays Harbor.
    Type of Medium: Series available for loan
    Pages: vi, 85 Seiten , Illustrationen
    Series Statement: CRREL Report 78-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Site description Background and objectives Project history Approach General Aircraft imagery and sensor data LANDSAT imagery Ground truth data Results and discussion Remote sensing techniques Conventional techniques Comparison of results Conclusions Advantages and disadvantages Applications Recommendations Literature cited
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  • 8
    Call number: ZSP-201-78/9
    In: CRREL Report, 78-9
    Description / Table of Contents: Large, simply supported beams of temperate lake ice were found, generally, to yield significantly higher flexural strengths than the same beams tested in the cantilever mode. Data support the view that a significant stress concentration may exist at the fixed corners of the cantilever beams. Maximum effects are experienced with beams of cold, brittle ice substantially free of structural imperfections; for this kind of ice the strength difference factor, here attributed to the effect of stress concentrations, may exceed 2.0; that is, simply supported beams test a factor of 2 or more stronger than the same beams tested in the cantilever mode. In ice that has undergone extensive thermal degradation, the stress concentration effect may be eliminated entirely. Simply supported beams generally yield higher strengths when the top surfaces are placed in tension. This behavior is attributed to differences in ice type; the fine-grained, crack-free top layer of snow-ice which constituted up to 50% of the ice cover in the current series of tests usually reacted more strongly in tension than the coarse-grained crack-prone bottom lake ice.
    Type of Medium: Series available for loan
    Pages: iv, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 78-9
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test sites and ice cover properties Beam testing Results Discussion Conclusions Literature cited
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  • 9
    Series available for loan
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/25
    In: CRREL Report, 78-25
    Description / Table of Contents: The objectives of this investigation were to describe channel characteristics and geographic settings of ice jam sites from aerial photographic interpretation, to indicate which characteristics may be important in causing ice jams, and to suggest additional uses of aerial photographs. Aerial photographs were taken of 19 sites with a Zeiss RMK 15/23 aerial camera on 17, 19, and 21 April 1976. Uncontrolled photomosaics of each site were assembled and major river characteristics were delineated on the photomosaics. Characteristics described include: manmade structures, falls, rapids, changes in channel depths, channel islands, mid-channel shoals or bars, river bed material, river sinuosity, meanders, floodplain width, riparian vegetation, and types of development on the floodplain. River channel widths were measured from the photographs along rivers where ground truth data were available for comparison. Lengths of channel riffles and pools were measured along the rivers where variations in river depths were evident on the photographs. Seventy-nine percent of the sites have some form of flow control structure which causes a pool with a backwater condition of low velocity. The low flow condition in the pool allows a solid ice cover to form which impedes ice movement and initiates ice jams. Aerial photographs provide a regional perspective for evaluating channel characteristics at an ice jam site and for analyzing the geographic setting at each site during ice-free conditions. Photographs taken after ice jams have formed are useful in monitoring ice jam formation, in analyzing ice characteristics, and in documenting ice jam breakup and movement.
    Type of Medium: Series available for loan
    Pages: iii, 60 Seiten , Illustrationen
    Series Statement: CRREL Report 78-25
    Language: English
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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-201-78/24
    In: CRREL Report, 78-24
    Type of Medium: Series available for loan
    Pages: v, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 78-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Comparison of winters Ship effects Measured forces Sequential breaking of the structure Discussion Conclusions Recommendations Literature cited Appendix A. Force level fluctuations in west ice boom, 20 January 1977
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