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  • Books  (525)
  • 2015-2019  (252)
  • 1970-1974  (253)
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  • 1
    Call number: ZSP-592-3
    In: Memoirs of National Institute of Polar Research
    Type of Medium: Series available for loan
    Pages: 83 p. : Ill
    Series Statement: Memoirs of National Institute of Polar Research : Special issue 3
    Branch Library: AWI Library
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  • 2
    Series available for loan
    Series available for loan
    Tokyo : Polar Research Center, National Science Museum
    Associated volumes
    Call number: ZSP-592-2
    In: Japanese Antarctic Research Expedition
    Type of Medium: Series available for loan
    Pages: xii, 279 S. : Ill. + Kt.-Beil.
    Series Statement: Scientific reports / Japanese Antarctic Research Expedition : Special issue 2
    Branch Library: AWI Library
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  • 3
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    Unknown
    Associated volumes
    Call number: K-13-0027
    In: Zemlja ±Enderbi
    Pages: 1 Kt. in 7 Bl. : mehrfarb.
    Branch Library: AWI Library
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  • 4
    Call number: AWI G8-13-0050
    In: Trudy Gosudarstvennogo Astronomiceskogo Instituta Imeni P. K. Sternberga
    Description / Table of Contents: Contents: Les recherches gravimétriques dans la régione des stations antarctiques soviétiques Lasarev et Novolaserevscakaja / A. L. Kogan, P. A. Stroev. - An approximate method of determination of spectal density of geophysical fields / V. L. Panteleev. - Le dévelopment des anomalies de la force d'attraction dans la suite des fonctions ellipsoidals de Lamé / L. A. Savrov. - On the short periodic solar perturbations in the motion of planetary satellites / A. A. Orlov. - Application of von Zeipel's method to the stellar three-body problem / N. A. Solovaya. - The determination of a simmetrical intermediate of an artificial earth's satellite / E. P. Aksenov, L. M. Domozhilova. - The determination of an asimetrical intermediate of an artifical earth's satellite / E. P. Aksenov, L. M. Domozhilova. - The influence of solar radiation pressure on the motion of some non-spherical satellites / E. E. Mukin. - Phenomenon of QSS / N. E. Kurochkin.
    Type of Medium: Series available for loan
    Pages: 117 S. : graph. Darst.
    Branch Library: AWI Library
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  • 5
    Call number: AWI G7-90-0151
    In: Icefield ranges research project
    Description / Table of Contents: Contents: Editors' Preface. - The High Mountain Environment Project: Chitistone Pass Region, Alaska and Mt. Logan, Yukon. - CLIMATOLOGICAL AND METEOROLOGICAL STUDIES. - Investigations in alpine climatology: the St. Elias Mountains, 1963-1971. - Micro- and Topo-climatology: the case of an alpine pass, Chitistone Pass, Alaska. - The observation and simulation of diurnal surface thermal contrast in an Alaskan Alpine Pass. - The observation and simulation of diurnal evaporation contrast in an Alaskan Alpine Pass. - Comparison of estimated and observed solar radiation and counterradiation at Chitistone Pass, Alaska. - Energy-balance studies over glacier and tundra surfaces, Chitistone Pass, Alaska, Summer 1969. - A note on topoclimatic variation of air temperature, Chitistone Pass Region, Alaska. - Seasonal radiation balance trends over a broken subarctic spruce forest and clearing, Kluane Lake, 1970 - 1971. - The comparative energy balances over a broken spruce forest and clearing, Kluane Lake, 1970 - 1971. - Summer climatic observations at the 5360-Meter level, Mt. Logan, 1968 - 1969. - Solar radiation measurements at 5365 Meters, Mt. Logan, Yukon. - The development and application of a simple digital surface-climate simulator. - The effects of forest-fire smoke on insolation in the St. Elias Mountains. - Baric-Map-Patterns and mountain weather St. Elias Mountains, Yukon and Alaska. - WATER AND SNOW STUDIES. - Hydrological studies of the Slims River, Yukon, June - August 1970. - Sedimentation in Kluane Lake. - Variations in quality and quantity of Slims River water, Yukon Territory. - Water masses in Southern Kluane Lake. - Sublacustrine morphology and deposition, Kluane Lake, Yukon Territory. - Channel adjustments in supraglacial streams. - Snowmelt along the environmental transect at Chitistone Pass, Alaska during the summers of 1967, 1968, and 1969. - Snow studies at high elevations, Mt. Logan, Yukon. - A note on snow accumulation and climatic trends in the Icefield Ranges, 1969 - 1970. - Sampling of glacial snow for pesticide analysis: the High Plateau Glacier of Mt. Logan. - GEOLOGICAL AND GEOMORPHOLOGICAL STUDIES. - A petrographic study of Mt. Logan, Yukon. - Miocene-Pliocene glaciations in Southern Alaska. - A possible advanced hypsithermal position of the Donjek Glacier. - The morphological effects of surges of the Donjek Glacier, St. Elias Mountains. - Survey of the Rusty Glacier Area, Yukon Territory, 1967 - 1970. - Mt. Logan survey, 1968. - A suggested revision in the height of Mt. Logan. - BIOLOGICAL STUDIES. - Soils and patterned ground in the Chitistone Pass Region of Alaska. - Alpine plant communities of the Southeastern Wrangell Mountains, Alaska. - The effect of snow duration on alpine plant community composition and distribution. - Successional patterns on Moraines and outwash of the Frederika Glacier, Alaska. - The vegetation of Chitistone, Skolai, and Frederika Valleys, Alaska. - Floristic and ecological phytogeography of the Southeastern Wrangell Mountains, Alaska. - Vegetation-snow cover relations in an Alpine Pass, Alaska. - Notes on eight species of Coprinus of the Yukon Territory and adjacent Alaska. - Arctic and alpine agarics from Alaska and Canada. - Blood chemistry of the Brown Bear (Ursus arctos) from the Southwestern Yukon Territory. - Hermatology of the Brown Bear (Ursus arctos) from the Southwestern Yukon Territory. - Appendix. - Map of landforms of the Chitistone Pass and Skolai Pass Area, Alaska.
    Type of Medium: Series available for loan
    Pages: XI, 385 S. : Ill., graph. Darst., Kt. + Kt.-Beil.
    Branch Library: AWI Library
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  • 6
    Call number: AWI E4-13-0145-3
    In: Werke
    Type of Medium: Monograph available for loan
    Pages: 915 S. : Ill.
    Branch Library: AWI Library
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  • 7
    Call number: AWI A6-94-0331
    In: Annual review of fluid mechanics
    Type of Medium: Series available for loan
    Pages: viii, 371 S. : Ill., graph. Darst., Kt.
    ISBN: 0824307062
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  • 8
    Call number: ZSP-594/C-7
    In: Japanese Antarctic Research Expedition
    Description / Table of Contents: Glaciological studies of the upper 10m of the ice sheet in East Antarctica were made during the JARE South Pole Traverse 1968-1969. The glaciological studies consisted of studies of surface snow and subsurface snow by means of pits as well as analyses of snow cores. Conditions of surface snow such as accumulation, roughness, density and hardness are described in this paper. It is found that the conditions are distinctly different in four regions along the route from Syowa Station to the South Pole, and that they have a close connection with the slope inclination. Relationship between the snow conditions and the slope inclination is discussed in terms of the dependence of wind speed on the slope inclination. Thus, it is concluded that the conditions of surface snow are mainly controlled by wind speed. Measurements of annual snow accumulations disclose that local variations in accumulations take place in a strong wind region, and coincide with local topography of the region. Also, distinct regional differences in accumulations during the summer season are discussed from the differences between cyclonic and anticyclonic precipitations. Studies of subsurface snow in 2m deep pits indicate that regions located in the north and south of 73°S are characterized respectively by compact fine-grained snow and well-developed depth hoar. Analyses of snow cores from the surface to a depth of 10m revealed the distribution of snow density in the upper 10m of the ice sheet along the route from Syowa Station to the South Pole. Regional profiles of snow density at the depths of 5 and 9m were different from those at the surface. This is due to the differences in the mean annual air temperature.
    Type of Medium: Series available for loan
    Pages: 27 S.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series C, Earth sciences 7
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  • 9
    Series available for loan
    Series available for loan
    København : Reitzel
    Associated volumes
    Call number: AWI K-93-0076(Erl-H.)
    In: Meddelelser om Grønland
    Description / Table of Contents: The Geological Map of East Greenland, 72°-76° N lat. (1 : 250 000), is the culminating result of Lauge Koch's expeditions from 1926 to 1958. A representative segment of the East Greenland Caledonides dominates the map area. Orogenic activity climaxed in the late Silurian, waned through the Devonian and terminated in the Permian. Deposition of post-Caledonian shelf sediments began with the transgression of the Upper Permian and continued with a few breaks into the Upper Cretaceous. During this period tensional tectonics gradually broke up the shelf into a series of antithetically rotated fault blocks. Regional uplift and erosion initiated the early Tertiary history of East Greenland which was swiftly followed by the eruption of plateau basalts, the intrusion of dykes and sills, and the emplacement of plutonic centres.
    Type of Medium: Series available for loan
    Pages: 26 S.
    ISBN: 8742100453
    Series Statement: Meddelelser om Grønland 183
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  • 10
    Call number: ZSP-594/A-11
    In: Japanese Antarctic Research Expedition
    Description / Table of Contents: A meridian scanning photometric system was designed for the simultaneous observation of the dynamic behavior of the proton and electron auroras with high time resolution. The hydrogen Balmer-beta (H_β) was selected as a typical emission line from proton auroras, whereas N_2+ 4278 Å, OI 5577 Å and OI 6300 Å emissions were selected for electron auroras. The H_β photometer has a so-called tilting filter to measure rapid space-time variations of faint proton auroras free from the contamination of strong electron auroras. The observations were carried out from March to October 1970 at Syowa Station (corrected geomagnetic lat. -66.7°, long. 72.5°) in Antarctica. From the records of the meridian scanning photometers, spatial distributitions of auroral luminosity along the geomagnetic meridian were displayed as a function of local time, and the iso-intensity contour lines were drawn. These space-time diagrams of auroral luminosity were shown to be very useful for the quantitative study of the dynamic behavior of auroras. Using auroral space-time diagrams, the constitution of the proton and electron aurora substorms was described in detail. During the growth phase of a magnetospheric substorm, the emission zone of the proton aurora moves equatorward with a speed of 100-200m/sec, accompanying the development of the asymmetric ring current and the positive H bay in the evening region. The equatorward movement and the growth of the asymmetric ring current were explained by an earthward movement of the ring current protons due to the intensification of the magnetospheric convection and the subsequent energization of protons through the betatron and Fermi acceleration processes. At the onset of the expansion phase, the quiet arcs suddenly brighten in the pre-midnight region, and the electron aurora bulge rapidly expands poleward and westward, whereas in the post-midnight region, the emission zone of proton auroras rapidly expands poleward and eastward with a large increase in luminosity. Proton auroras are absent in the leading edge of the expanding electron aurora bulge, while breakup-type electron auroras (arcs or bands) are not observed in the expanding proton aurora bulge. Therefore, it is suggested that there is a mechanism which accelerates electrons along the geomagnetic field lines from the magnetosphere down to the ionosphere in the pre-midnight region and protons in the postmidnight region. After the onset of the expansion phase, the luminosity of the proton aurora greatly increases, and simultaneously the emission zone expands equatorward in the evening region, accompanying the development of the asymmetric partial ring current and the positive bay. These features can be interpreted by means of the proton injection into the trapping region due to the magnetic collapse in the tail, and the subsequent westward and earthward drift. From the relationship between the movement of the proton auroras and the geomagnetic variation, it is suggested that the positive bay in the evening hours is induced by the eastward current concentrated along the emission zone of proton auroras. The enhancement of the ionospheric conductivity due to the precipitating protons required to excite the observed proton aurora luminosity is estimated to be sufficient for the concentration of the eastward current. A close relationship between the proton aurora and the IPDP event was also observed, indicating proton pitch-angle diffusion due to the ion cyclotron waves.
    Type of Medium: Series available for loan
    Pages: 78 S. : überw. graph. Darst.
    Series Statement: Japanese Antarctic Research Expedition : Scientific reports : Series A, Aeronomy 11
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