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  • English  (1,347)
  • Japanese  (12)
  • 2000-2004  (1,359)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Garmisch-Partenkirchen : Institut für atmosphärische Umweltforschung der Fraunhofer- Gesellschaft
    Call number: MOP 44829 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 25 S. , graph. Darst.
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    [Edgecumbe, N.Z.] : A. Muller
    Call number: M 15.89146
    Description / Table of Contents: An account of the results of the 2 March 1987 earthquake in the eastern Bay of Plenty and the aftermath's effects on the people and places on the Rangitaiki Plains
    Type of Medium: Monograph available for loan
    Pages: 223 S., , Ill.
    Language: English
    Branch Library: GFZ Library
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  • 3
  • 4
    Monograph available for loan
    Monograph available for loan
    Stuttgart : Schweizerbart Science Publishers ; Volume 1, number 1 (1978)-
    Call number: M 18.91571
    Type of Medium: Monograph available for loan
    Pages: 134 Seiten
    ISSN: 2363-7196
    Series Statement: Global tectonics and metallogeny : special issue Vol. 10/2-4
    Classification:
    Tectonics
    Parallel Title: Erscheint auch als Global tectonics and metallogeny
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 5
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 6
    Call number: ZSP-994
    Type of Medium: Series available for loan
    Pages: 21 x 21 cm
    ISSN: 1618-3703
    Former Title: Vorgänger: Zweijahresbericht / Stiftung Alfred-Wegener-Institut für Polar- und Meeresforschung
    Subsequent Title: Fortsetzung Zweijahresbericht ... / AWI, Alfred-Wegener-Institut für Polar- und Meeresforschung in der Helmholtz-Gemeinschaft
    Language: German , English
    Note: Erscheint alle 2 Jahre , Text in deutscher und englischer Sprache
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 7
    Publication Date: 2020-02-12
    Description: An energy-flux model (EFM) and a teleseismic fluctuation wavefield method (TFWM) have been applied to interpret the teleseismic P coda observed at three temporary and two permanent networks in northern and central Europe. The aim is to determine the small-scale random structure of the lithosphere below the receivers. Various subsets of these data have been exploited previously with one of the two methods. The main objectives here are: To compare the performance of both methods with synthetic data sets. To map the random structure of the lithosphere in terms of inverse scattering Q (Q−1s), correlation length a, RMS velocity fluctuation σ, thickness L of the scattering layer and autocorrelation function (ACF) using a combination of both methods. With TFWM, the product aσ2 can be reliably determined if L is known. L can be roughly estimated with EFM. Although EFM can, in principle, resolve a and σ separately, a is recovered with a rather large uncertainty. TFWM does not distinguish much between the ACF type, whereas with EFM determination of the ACF type is sometimes possible. By combining the results of both methods we determine improved random medium parameters of the lithosphere for eleven subregions in northern and central Europe. In the Baltic shield, Rhenohercynian belt, Ardenne and Brabant mountains, eastern Rhenish massif, Eifel, Hunsrück mountains, Lorraine, Frankonian Jura and massif Central scattering predominantly occurs in the crust. For the frequency range from 0.5 to 5 Hz correlation lengths of 1–7 km and rms velocity fluctuations of 3-7 per cent are obtained. For the Rhenohercynian belt (RH) and the N-German basin RMS velocity fluctuations and correlation lengths could not be resolved. The data from the N-German basin (NB) cannot be explained by scattering within the crust only. Smallest scattering Q was found in the N German basin (Qs≈ 100 at 1 Hz) and largest scattering Q in the Baltic shield (Qs≈ 450 at 2-3 Hz). For the Frankonian Jura only a Gaussian ACF can fit the Q−1s values. The data from the eastern Rhenish massif also indicate a random medium with Gaussian ACF. For all other subregions we cannot distinguish between exponential or Gaussian ACF for the random medium structure.
    Language: English
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  • 8
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    In:  The Climate in Historical Times : Towards a Synthesis of Holocene Proxy Data and Climate Models | GKSS School of Environmental Research
    Publication Date: 2020-02-12
    Description: Trees, as long living plants, are governed by environmental and/or climate changes within their habitat. Their growth rings record to a large extent the temporal dynamics of these changes either directly or through tree physiological reactions. They render the highest time resolution thus far possible for environmental or climate reconstructions of the past 10,000 years (exactly dated, annually resolved, see: [828], [994]). Trees are a substantial part of the human environment with a high socio-economic value. Their large geographical extension over various regions of the world, including those with greatest population densities but also marginal areas allows to gain unique informations about local and regional consequences of global climate change.
    Keywords: 550 - Earth sciences
    Language: English
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  • 9
    Publication Date: 2020-02-12
    Description: Signals from 11 shots and 8 earthquakes, and numerous teleseismic events were recorded along the 400-km seismic line INDEPTH III in centralTibet and interpreted together with previous seismic and tectonic data. The abnormal behavior of various mantle phases reveals a complex Moho-transition zone, especially in the northern part of the line, in the Changtang Block, where the lower crust and the mantle show unusually low velocities, a shingled appearance of Pn and no low-velocity layer in the upper crust. The strong east–west anisotropy in the Changtang Block is related to an easterly escape movement of the whole lithosphere, facilitated by the warm and weak layers in the lower crust and the upper mantle, bounded apparently by two prominent west–east running fault zones.
    Language: English
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  • 10
    Publication Date: 2020-02-12
    Description: The final report contains a description of the results obtained within a research contract between IRE RAS and GFZ Potsdam during the period April-November 2004. The objectives of investigation included (1) the radio-holographic methods for obtaining vertical profiles of the vertical gradients of physical parameters in the atmosphere, (2) radio holographic methods for atmospheric, ionospheric and stratospheric waves, and (3) validation of the software with GPS/MET (GPS/METeorology, e.g., Rocken et al. 1997) and CHAMP (CHAllenging Minisatellite Payload, e.g., Reigber et al. 2005) data and final report with recommendations.
    Language: English
    Type: info:eu-repo/semantics/report
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  • 11
    Publication Date: 2020-04-17
    Language: English
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  • 12
    Publication Date: 2021-02-26
    Description: This letter proposes a building characterization tech-nique for L-band polarimetric interferometric synthetic apertureradar (SAR) data. This characterization consists of building iden-tification and height estimation. Initially, a polarimetric interfer-ometric segmentation is performed to isolate buildings from theirsurroundings. This classification identifies three basic categories:single bounce, double bounce, and volume diffusion. In order tocompensate for the misclassifications among the volume and thedouble-bounce classes, interferometric phases given by the high-resolution Estimation of Signal Parameters via Rotational Invari-ance Techniques (ESPRIT) method are analyzed. Once buildingsare localized, a phase-to-height procedure is applied to retrievebuilding height information. The method is validated using E-SAR,German Aerospace Center (DLR) fully polarimetric SAR data, atL-band, repeat-pass mode, over the Oberpfaffenhofen, Germany,test site, with a spatial resolution of 1.5 m in range and azimuth.More than 80% of buildings are retrieved with acceptably accu-rate height estimates
    Language: English
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  • 13
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2020-02-12
    Description: Late Miocene to Quaternary volcanic rocks from the frontal arc to the back-arc region of the Central Volcanic Zone in the Andes show a wide range of delta 11B values (+4 to -7 ‰) and boron concentrations (6 to 60 ppm). Positive delta 11B values of samples from the volcanic front indicate involvement of a 11B-enriched slab component, most likely derived from altered oceanic crust, despite the thick Andean continental lithosphere, and rule out a pure crust-mantle origin for these lavas. The delta 11B values and B concentrations in the lavas decrease systematically with increasing depth of the Wadati-Benioff Zone. This across-arc variation in delta 11B values and decreasing B/Nb ratios from the arc to the back-arc samples are attributed to the combined effects of B-isotope fractionation during progressive dehydration in the slab and a steady decrease in slab-fluid flux towards the back arc, coupled with a relatively constant degree of crustal contamination as indicated by similar Sr, Nd and Pb isotope ratios in all samples. Modelling of fluid-mineral B-isotope fractionation as a function of temperature fits the across-arc variation in delta 11B and we conclude that the B-isotope composition of arc volcanics is dominated by changing delta 11B composition of B-rich slab-fluids during progressive dehydration. Crustal contamination becomes more important towards the back-arc due to the decrease in slab-derived fluid flux. Because of this isotope fractionation effect, high delta 11B signatures in volcanic arcs need not necessarily reflect differences in the initial composition of the subducting slab. Three-component mixing calculations for slab-derived fluid, the mantle wedge and the continental crust based on B, Sr and Nd isotope data indicate that the slab-fluid component dominates the B composition of the fertile mantle and that the primary arc magmas were contaminated by an average addition of 15 to 30 % crustal material.
    Language: English
    Type: info:eu-repo/semantics/doctoralThesis
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  • 14
    Publication Date: 2020-02-12
    Description: An active-source seismic experiment at the KTB deep drill hole in southeast Germany reveals seismic P wave anisotropy to exist within a tectono-metamorphic sub-terrane of the crystalline Bohemian massif. The experiment used multi-azimuth vertical seismic profiling whereby downhole sensors recorded surface seismic Vibroseis sources located along six 7.5-km radial profiles emanating from the borehole location. Representative bulk anisotropic P wave velocities of the upper crust were derived from this seismic data and compared with predictions of velocity and anisotropy based on petrophysical laboratory measurements and geological information. We show that azimuth and inclination behavior of the observed anisotropy is consistent with characterization of the geology surrounding the borehole as a coherent regional block containing pervasive highly tilted foliation. This seismic anisotropy can be explained by “intrinsic” material properties associated with the well-developed foliation fabrics.
    Language: English
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  • 15
    Publication Date: 2020-02-12
    Language: German , English
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  • 16
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    In:  Geophysical Research Letters
    Publication Date: 2020-02-12
    Description: The Atacama basin is a prominent morphological anomaly in the Central Andean forearc. 3D seismic structure beneath the depression and its surroundings has been determined from local earthquake tomography. Depth maps of P-wave velocity and attenuation (1/Q p ) through the lithosphere reveal a rheologically strong (high Q p and v p ) lithospheric block beneath the basin, surrounded by weak regions (low Q p and v p ) beneath Pre- and Western Cordilleras. The anomalous lithospheric structure appears to bar hot asthenospheric mantle from penetrating trenchward, and hence causes the volcanic front to be deflected by the Salar de Atacama basin. The cold block may also influence the thermal structure of the subducted slab causing reduced Benioff seismicity and less hydration of mantle rocks evident from reduced v p /v s ratios. Seismic data are hard to reconcile with extension and lithospheric thinning as a mechanism for subsidence of the basin. Instead, high strength of the Atacama lithospheric block may contribute to basin formation by focussing deformation and uplift along the block's weak edges.
    Language: English
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  • 17
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado
    In:  IUGG Publications
    Publication Date: 2021-04-16
    Language: French , English
    Type: info:eu-repo/semantics/report
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  • 18
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2021-07-25
    Description: This manual outlines the characteristics and structure of the software and describes how to use the software. The principles and new features are outlined systematically and referred partly to existing references. Numerical examples of multi-functions and internal tests as well as external comparisons are given.
    Language: English
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  • 19
    Publication Date: 2021-07-28
    Description: We review the historical, geological, tide-gauge, GPS and gravimetric evidence advanced in favour of or against continuing land uplift around Hudson Bay, Canada. After this, we reanalyse the tide-gauge and GPS data for Churchill using longer time series than those available to previous investigators. The dependence of the mean rate of relative sea-level change obtained on the length and mid-epoch of the observation interval considered is investigated by means of the newly developed linear-trend analysis diagram. For studying the shorter-period variability of the tide-gauge record, the continuous-wavelet transform is used. The mean rate of land uplift obtained from GPS is based on a new analysis using IGS solutions of GFZ. Furthermore, sea-level indicators from the Churchill region representing the relative sea-level history during the past 8000 a are included. Finally, the four types of observable are jointly inverted in terms of mantle viscosity. The optimum values are 3×10^20 Pa s and 1.6 × 10^22 Pa s for the upper- and lower-mantle viscosities, respectively.
    Language: English
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  • 20
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2021-07-25
    Description: This report is also published as Scientific Report No. 04-9 of the Danish Meteorological Institute.
    Language: English
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  • 21
    Publication Date: 2020-02-12
    Description: A schematic model for hadronic states, based on constituent quarks and antiquarks and gluon pairs, is discussed. The phenomenological interaction between quarks and gluons is QCD motivated. The obtained hadronic spectrum leads to the identification of nucleon and Δ resonances and to pentaquark and heptaquark states. The predicted lowest pentaquark state ( J π = 1 2 − ) lies at the energy of 1.5 GeV and it is associated to the observed Θ + ( 1540 ) state. For heptaquarks ( J π = 1 2 + , 3 2 + ) the model predicts the lowest state at 2.5 GeV .
    Language: English
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  • 22
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2020-02-12
    Description: As observed on the Earth's surface, the magnetic field can be separated into three components: The "Main Field", the "Crustal Field" and the "External Magnetic Field". This work concentrates on the magnetospheric current systems, in order to correct the effect of large-scale magnetospheric current systems. Their exact knowledge is vital to improve the main field and secular variation models. Spherical harmonic analysis (SHA) is commonly used to describe the magnetic field. In SHA it is possible to distinguish between internal and external contributions to the Earth's magnetic field. The spherical harmonic coefficients describe dipolar, quadrupolar and higher parts in spherical coordinates. Here, CHAMP (CHAllenging Minisatellite Payload) measurements are used. Due to the inclination CHAMP is changing the orbit in local time. From time to time CHAMP is flying in resonance with the Earth's rotation, i.e. the satellite is flying over the same ground track after a couple of days. To model changes during a period of a few days these so called "repeat tracks" are very helpful for an improved main field/external field model. On the Earth's surface the magnetic effect of magnetospheric currents is often characterised by the DST-indix. In this study, it is explained how a possible constitution of the external sources of the geomagnetic field can look like and how the effect of these magnetospheric currents can be corrected in main field modelling.
    Language: English
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  • 23
    Publication Date: 2020-02-12
    Description: A 39-km-long deepseismic reflection profile recorded during two field campaigns in 1996 and 2002 provides a first detailed image of the deepcrust at the eastern margin of the Eastern Alps (Austria). The ESE–WNW-trending, low-fold seismic line crosses Austroalpine basement units and extends approximately from 20 km west of the Penninic window group of Rechnitz to 60 km SSE of the Alpine thrust front. The explosive-source seismic data reveals a transparent shallow crust down to 5 km depth, a complexly reflective upper crust and a highly reflective lowermost crust. The upper crust is dominated by three prominent west-dipping packages of high-amplitude subparallel reflections. The upper two of these prominent packages commence at the eastern end of the profile at about 5 and 10 km depth and are interpreted as low-angle normal shear zones related to the Miocene exhumation of the Rechnitz metamorphic core complex. In the western portion of the upper crust, east-dipping and less significant reflections prevail. The lowermost package of these reflections is suggested to represent the overall top of the European crystalline basement. Along the western portion of the line, the lower crust is characterised by a 6-8-km-thick band of high-amplitude reflection lamellae, typically observed in extensional provinces. The Moho can be clearly defined at the base of this band, at approximately 32.5 km depth. Due to insufficient signal penetration, outstanding reflections are missing in the central and eastern portion of the lower crust. We speculate that the result of accompanying gravity measurements and lower crustal sporadic reflections can be interpreted as an indication for a shallower Moho in the east, preferable at about 30.5 km depth. The high reflectivity of the lowermost part of the lower crust and prominent reflection packages in the upper crust, the latter interpreted to represent broad extensional mylonite zones, emphasises the latest extensional processes in accordance with eastward extrusion.
    Language: English
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  • 24
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Language: English
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  • 25
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    International Association of Geomagnetism and Aeronomy (IAGA)
    In:  IAGA Annual Report
    Publication Date: 2020-02-12
    Language: English
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  • 26
    Publication Date: 2020-02-12
    Description: The volcanism responsible for creating the chain of the Hawaiian islands and seamounts is believed to mark the passage of the oceanic lithosphere over a mantle plume1,2. In this picture hot material rises from great depth within a fixed narrow conduit to the surface, penetrating the moving lithosphere3. Although a number of models describe possible plume–lithosphere interactions4, seismic imaging techniques have not had sufficient resolution to distinguish between them. Here we apply the S-wave ‘receiver function’ technique to data of three permanent seismic broadband stations on the Hawaiian islands, to map the thickness of the underlying lithosphere. We find that under Big Island the lithosphere is 100–110 km thick, as expected for an oceanic plate 90–100 million years old that is not modified by a plume. But the lithosphere thins gradually along the island chain to about 50–60 km below Kauai. The width of the thinning is about 300 km. In this zone, well within the larger-scale topographic swell, we infer that the rejuvenation model5 (where the plume thins the lithosphere) is operative; however, the largerscale topographic swell is probably supported dynamically.
    Keywords: 550 - Earth sciences
    Language: English
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  • 27
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    In:  XXIX ESC General Assembly, Sept. 12-17, 2004
    Publication Date: 2020-02-12
    Language: English
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  • 28
    Publication Date: 2020-02-12
    Description: Continuous recordings of 17 broadband and short-period digital seismic stations from a newly established seismological network in Saudi Arabia, along with digital recordings from the broadband stations of the GSN, MEDNET, GEOFON, a temporary array in Saudi Arabia, and temporary short period stations in Oman, were analysed to study the lithospheric structure of the Arabian Plate and surrounding regions. The Arabian Plate is surrounded by a variety of types of plate boundaries: continental collision (Zagros Belt and Bitlis Suture), continental transform (Dead Sea fault system), young seafloor spreading (Red Sea and the Gulf of Aden) and oceanic transform (Owen fracture zone). Also, there are many intraplate Cenozoic processes such as volcanic eruptions, faulting and folding that are taking place. We used this massive waveform database of more than 6200 regional seismograms to map zones of blockage, inefficient and efficient propagation of the Lg and Sn phases in the Middle East and East Africa. We observed Lg blockage across the Bitlis Suture and the Zagros fold and thrust belt, corresponding to the boundary between the Arabian and Eurasian plates. This is probably due to a major lateral change in the Lg crustal waveguide. We also observed inefficient Lg propagation along the Oman mountains. Blockage and inefficient Sn propagation is observed along and for a considerable distance to the east of the Dead Sea fault system and in the northern portion of the Arabian Plate (south of the Bitlis Suture). These mapped zones of high Sn attenuation, moreover, closely coincide with extensive Neogene and Quaternary volcanic activity. We have also carefully mapped the boundaries of the Sn blockage within the Turkish and Iranian plateaus. Furthermore, we observed Sn blockage across the Owen fracture zone and across some segments of the Red Sea. These regions of high Sn attenuation most probably have anomalously hot and possibly thin lithospheric mantle (i.e. mantle lid). A surprising result is the efficient propagation of Sn across a segment of the Red Sea, an indication that active seafloor spreading is not continuous along the axis of the Red Sea. We also investigated the attenuation of Pn phase (QPn) for 1–2 Hz along the Red Sea, the Dead Sea fault system, within the Arabian Shield and in the Arabian Platform. Consistent with the Sn attenuation, we observed low QPn values of 22 and 15 along the western coast of the Arabian Plate and along the Dead Sea fault system, respectively, for a frequency of 1.5 Hz. Higher QPn values of the order of 400 were observed within the Arabian Shield and Platform for the same frequency. Our results based on Sn and Pn observations along the western and northern portions of the Arabian Plate imply the presence of a major anomalously hot and thinned lithosphere in these regions that may be caused by the extensive upper mantle anomaly that appears to span most of East Africa and western Arabia.
    Language: English
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  • 29
    Publication Date: 2020-02-12
    Description: The TRANSALP Group, comprising of partner institutions from Italy, Austria and Germany, acquired data on a 340 km long deep seismic reflection line crossing the Eastern Alps between Munich and Venice. Although the field work was split into four campaigns, between fall 1998 and summer 2001, the project gathered for the first time a continuous profile across the Alps using consistent field acquisition and data processing parameters. These sections span the orogen itself, at its broadest width, as well as the editor Fred Davey and the two adjacent basins. Vibroseis and explosion data, complementary in their depth penetration and resolution characteristics, were obtained along with wide-angle and teleseismic data. The profile shows a bi-vergent asymmetric structure of the crust beneath the Alpine axis which reaches a maximum thickness of 55 km, and 80–100 km long transcrustal ramps, the southward dipping ‘Sub-Tauern-Ramp’ and the northward-dipping ‘Sub-Dolomites-Ramp’. Strongly reflective patterns of these ramps can be traced towards the north to the Inn Valley and towards the south to the Valsugana thrust belt, both of which show enhanced seismicity in the brittle upper crust. The seismic sections do not reveal any direct evidence for the presence of the Periadriatic Fault system, the presumed equivalent to the Insubric Line in the Western Alps. According to our new evolutionary model, the Sub-Tauern-Ramp is linked at depth with remnants of the subducted Penninic Ocean. The ‘crocodile’-type model describes an upper/lower crustal decoupling and wedging of both the European and the Adriatic–African continents.
    Language: English
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  • 30
    Publication Date: 2020-02-12
    Description: The hadronic spectrum obtained in the framework of a QCD-inspired schematic model is presented. The model is the extension of a previous version, whose basic degrees of freedom are constituent quarks, antiquarks, and gluons. The interaction between quarks and gluons is a phenomenological interaction and its parameters are fixed from data. The classification of the states, in terms of quark and antiquark and gluon configurations is based on symmetry considerations, and it is independent of the chosen interaction. Following this procedure, nucleon and Δ resonances are identified, as well as various penta- and hepta-quarks states. The lowest pentaquarks state is predicted at 1.5 GeV and it has negative parity, while the lowest hepta-quarks state has positive parity and its energy is of the order of 2.5 GeV .
    Language: English
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  • 31
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Language: English
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  • 32
    Publication Date: 2020-02-12
    Description: Quantum mechanics in dissipative systems with a magnetic field is discussed. For strong magnetic fields the system exhibits an oscillatory behavior around the classical trajectory of the electron which should generate emissions in the millimeter range of the electromagnetic spectrum.
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  • 33
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    International Association of Meteorology and Atmospheric Sciences (IAMAS)
    In:  IAMAS Annual Report
    Publication Date: 2020-02-12
    Language: English
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  • 34
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2021-08-20
    Description: The Dead Sea Transform (DST) is a prominent shear zone in the Middle East. It separates the Arabian plate from the Sinai microplate and stretches from the Red Sea rift in the south via the Dead Sea to the Taurus-Zagros collision zone in the north. Formed in the Miocene »17 Ma ago and related to the breakup of the Afro-Arabian continent, the DST accommodates the left-lateral movement between the two plates. The study area is located in the Arava Valley between the Dead Sea and the Red Sea, centered across the Arava Fault (AF), which constitutes the major branch of the transform in this region. A set of seismic experiments comprising controlled sources, linear profiles across the fault, and specifically designed receiver arrays reveals the subsurface structure in the vicinity of the AF and of the fault zone itself down to about 3–4 km depth. A tomographically determined seismic P velocity model shows a pronounced velocity contrast near the fault with lower velocities on the western side than east of it. Additionally, S waves from local earthquakes provide an average P -to-S velocity ratio in the study area, and there are indications for a variations across the fault. High-resolution tomographic velocity sections and seismic reflection profiles confirm the surface trace of the AF, and observed features correlate well with fault-related geological observations. Coincident electrical resistivity sections from magnetotelluric measurements across the AF show a conductive layer west of the fault, resistive regions east of it, and a marked contrast near the trace of the AF, which seems to act as an impermeable barrier for fluid flow. The correlation of seismic velocities and electrical resistivities lead to a characterisation of subsurface lithologies from their physical properties. Whereas the western side of the fault is characterised by a layered structure, the eastern side is rather uniform. The vertical boundary between the western and the eastern units seems to be offset to the east of the AF surface trace. A modelling of fault-zone reflected waves indicates that the boundary between low and high velocities is possibly rather sharp but exhibits a rough surface on the length scale a few hundreds of metres. This gives rise to scattering of seismic waves at this boundary. The imaging (migration) method used is based on array beamforming and coherency analysis of P -to-P scattered seismic phases. Careful assessment of the resolution ensures reliable imaging results. The western low velocities correspond to the young sedimentary fill in the Arava Valley, and the high velocities in the east reflect mainly Precambrian igneous rocks. A 7 km long subvertical scattering zone (reflector) is offset about 1 km east of the AF surface trace and can be imaged from 1 km to about 4 km depth. The reflector marks the boundary between two lithological blocks juxtaposed most probably by displacement along the DST. This interpretation as a lithological boundary is supported by the combined seismic and magnetotelluric analysis. The boundary may be a strand of the AF, which is offset from the current, recently active surface trace. The total slip of the DST may be distributed spatially and in time over these two strands and possibly other faults in the area.
    Description: Ein transversales Störungssystem im Nahen Osten, die Dead Sea Transform (DST), trennt die Arabische Platte von der Sinai-Mikroplatte und erstreckt sich von Süden nach Norden vom Extensionsgebiet im Roten Meer über das Tote Meer bis zur Taurus-Zagros Kollisionszone. Die sinistrale DST bildete sich im Miozän vor »17 Ma und steht mit dem Aufbrechen des Afro-Arabischen Kontinents in Verbindung. Das Untersuchungsgebiet liegt im Arava Tal zwischen Totem und Rotem Meer, mittig über der Arava Störung (Arava Fault, AF), die hier den Hauptast der DST bildet. Eine Reihe seismischer Experimente, aufgebaut aus künstlichen Quellen, linearen Profilen über die Störung und entsprechend entworfenen Empfänger-Arrays, zeigt die Untergrundstruktur in der Umgebung der AF und der Verwerfungszone selbst bis in eine Tiefe von 3–4 km. Ein tomographisch bestimmtes Modell der seismischen Geschwindigkeiten von P-Wellen zeigt einen starken Kontrast nahe der AF mit niedrigeren Geschwindigkeiten auf der westlichen Seite als im Osten. Scherwellen lokaler Erdbeben liefern ein mittleres P -zu-S Geschwindigkeitsverhältnis und es gibt Anzeichen für Änderungen über die Störung hinweg. Hoch aufgelöste tomographische Geschwindigkeitsmodelle bestätigen der Verlauf der AF und stimmen gut mit der Oberflächengeologie überein. Modelle des elektrischen Widerstands aus magnetotellurischen Messungen im selben Gebiet zeigen eine leitfähige Schicht westlich der AF, schlecht leitendes Material östlich davon und einen starken Kontrast nahe der AF, die den Fluss von Fluiden von einer Seite zur anderen zu verhindern scheint. Die Korrelation seismischer Geschwindigkeiten und elektrischer Widerstände erlaubt eine Charakterisierung verschiedener Lithologien im Untergrund aus deren physikalischen Eigenschaften. Die westliche Seite lässt sich durch eine geschichtete Struktur beschreiben, wogegen die östliche Seite eher einheitlich erscheint. Die senkrechte Grenze zwischen den westlichen Einheiten und der östlichen scheint gegenüber der Oberflächenausprägung der AF nach Osten verschoben zu sein. Eine Modellierung von seismischen Reflexionen an einer Störung deutet an, dass die Grenze zwischen niedrigen und hohen Geschwindigkeiten eher scharf ist, sich aber durch eine raue Oberfläche auf der Längenskala einiger hundert Meter auszeichnen kann, was die Streuung seismischer Wellen begünstigte. Das verwendete Abbildungsverfahren (Migrationsverfahren) für seismische Streukörper basiert auf Array Beamforming und der Kohärenzanalyse P -zu-P gestreuter seismischer Phasen. Eine sorgfältige Bestimmung der Auflösung sichert zuverlässige Abbildungsergebnisse. Die niedrigen Geschwindigkeiten im Westen entsprechen der jungen sedimentären Füllung im Arava Tal, und die hohen Geschwindigkeiten stehen mit den dortigen präkambrischen Magmatiten in Verbindung. Eine 7 km lange Zone seismischer Streuung (Reflektor) ist gegenüber der an der Oberfläche sichtbaren AF um 1 km nach Osten verschoben und lässt sich im Tiefenbereich von 1 km bis 4 km abbilden. Dieser Reflektor markiert die Grenze zwischen zwei lithologischen Blöcken, die vermutlich wegen des horizontalen Versatzes entlang der DST nebeneinander zu liegen kamen. Diese Interpretation als lithologische Grenze wird durch die gemeinsame Auswertung der seismischen und magnetotellurischen Modelle gestützt. Die Grenze ist möglicherweise ein Ast der AF, der versetzt gegenüber des heutigen, aktiven Asts verläuft. Der Gesamtversatz der DST könnte räumlich und zeitlich auf diese beiden Äste und möglicherweise auch auf andere Störungen in dem Gebiet verteilt sein.
    Language: English
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  • 35
    Publication Date: 2022-03-09
    Description: The oil play of the Permo-Carboniferous Cooper and Jurassic-Cretaceous Eromanga Basins in South Australia is complicated to unravel due to the presence of multiple source rocks that bear similar geochemical characteristics and has consequently been subject to intense debate. The underlying Warburton Basin, although initially regarded an exploration target, subsequently has never been seriously considered to having participated in the oil play. The Cooper/Eromanga couplet is Australia's largest onshore petroleum province and still bears potential for undiscovered commodities, making a profound understanding of origin and migration of petroleum a prerequisite for efficient future exploration. Being a typical example of structurally trapped oils in stacked fluvial sandstone reservoirs, the Gidgealpa Ridge was chosen as subject for this study. A suite of 13 sandstone cores, 11 source rocks and 24 drill stem test (DST) oils were processed at the University of Cologne by extraction, sequential extraction of sandstone cores to yield residual oils, preparative liquid chromatography and solid phase extraction to yield fractions of saturated hydrocarbons, aromatic hydrocarbons, maltene resins and a carbazole enriched fractions. While biomarker analyses on saturates and aromatics were performed by Dr. Khaled Arouri at the University of Adelaide, molecular characterisation of carbazoles and bulk geochemical characterisation was also done at the University of Cologne. Sequentially extracted residual oils are particularly useful because they allow a temporal resolution of petroleum reservoir filling histories. While hydrocarbon compositions are quickly equilibrated over a few tens of metres in oil columns, there is substantial evidence that the same is not true for polar species such as e.g. carbazoles and for lateral variations in hydrocarbon composition. Carbazoles were initially regarded as molecular markers indicating relative migration distances. However, counterevidence soon appeared, showing the dependency of carbazole distributions on other factors. The results of this study show that, while the distribution of benzocarbazoles seems to depend only on fractionation processes during primary and secondary migration, alkylated carbazole distribution patterns are governed by source rock facies. This new finding allowed the recognition of a Warburton Basin contribution in certain residual oil fractions, yielding the first conclusive evidence that Warburton Basin rocks bear a source potential and have actively participated in the oil play of the Cooper and Eromanga Basins. The application of carbazole facies parameters, benzocarbazole migration parameters and aromatic maturity data on oils and residual oils from the Gidgealpa Field has allowed the reconstruction of its charging history. Generally, Cooper Basin oils exhibit large maturity variations but a uniformly short migration distance, indicating their origin from a nearby deep trough (eastern source kitchen). Eromanga Basin oils are characterized by similarly low maturity values but highly varying migration distances, suggesting that they were sourced by an extensive and shallow source kitchen. More precise consideration of the carbazole distribution in Eromanga Basin oils shows that the Gidgealpa Field has received two discrete Birkhead charges: a Late Cretaceous pulse from an eastern source kitchen, which migrated a short distance, and became locally displaced by a Tertiary charge from a western source kitchen, which had to migrate further before reaching the Gidgealpa Field. Residual oil fractions from the sandy intervals of the Toolachee and Patchawarra Formations indicate that while the former is a source for Cooper Basin Family 2 oils, the latter can unambiguously be tied to the production of Cooper Basin Family 1 oils. After petroleum generation in the Patchawarra Formation, this petroleum was probably retained by the coaly Patchawarra source rock, and underwent further maturation before it was expelled as condensate-like light oil in gaseous solution. The analysis of sequentially extracted residual oils promises to become a powerful tool in reservoir geochemical studies by adding a temporal resolution to otherwise time-integrated samples, thereby allowing a relatively precise reconstruction of an oil field's charging history. The finding of facies dependent markers in the polar fraction of oils is a constructive motivation for further research into the facies and maturity dependency of NSO compounds. As many residual oils are characterized by minimum extracts yields and a high percentage of NSO compounds, conventional biomarker analyses are complicated and polar markers are necessary for a more precise evaluation.
    Language: English
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  • 36
    Publication Date: 2020-02-12
    Description: The Irish Seismological Lithospheric Experiment (ISLE 2002) has been designed to investigate the deep lithospheric and asthenospheric structure across the late-Caledonian Iapetus Suture Zone in southern Ireland. The project is a collaboration between the Dublin Institute for Advanced Studies (DIAS), Ireland, and the Geophysical Institute (GPI) of the University of Karlsruhe, Germany. This is the first passive teleseismic experiment conducted in Ireland, building upon a large body of earlier work on the crustal structure offshore and onshore Ireland, based on controlled source seismics and potential field studies.
    Language: English
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  • 37
    Publication Date: 2020-02-12
    Description: On a SW–NE profile from the Libyan coast towards central Turkey phase velocity curves of the fundamental Rayleigh mode were measured using a two-station method. The inversion of phase velocity curves yields 1-D models of shear wave velocity down to approximately 200 km depths that may be interpreted as estimates of average models between neighbouring stations on the profile. Strong lateral variations in the shear wave velocity structure are imaged along the profile. The subducted oceanic African mantle lithosphere is indicated in 1-D models for the region around Crete by significantly enlarged shear wave velocities. It is also imaged by an average model of the structure between stations on Crete and Santorini. On a path crossing the Libyan Sea south of Crete the resulting model is slower than a model expected for 110 Myr old oceanic lithosphere. The passive African margin is thus assumed to extend northwards beneath the Libyan Sea. Anomalous low shear wave velocities are found for the uppermost mantle beneath central Turkey down to a depth of approximately 130 km. Using two stations on Crete the average depth of the oceanic Moho within the subducting slab is estimated to be at approximately 50 km beneath Crete. For this arc-parallel path, an enlarged standard deviation of the measured phase velocities of approximately 0.2 km s−1 between 10 and 30 mHz is observed that is probably caused by strong lateral heterogeneity related to the subducting slab. In addition, in this frequency range an anomalous propagation of the fundamental Rayleigh mode is detected that is indicated by measured phase velocities that are approximately one standard deviation faster than phase velocities expected from a great-circle approximation. An average shear wave velocity of approximately 3.5 km s−1 is observed above the oceanic Moho. In order to explain the recent lithospheric structure of the Hellenic subduction zone a tectonic model is assumed for the NE–SW striking profile considered. It is based on the calculated 1-D models, tectonic reconstructions and on a model derived from the metamorphic history of rocks exposed on Crete. The suggested model summarizes the tectonic development at a lithospheric scale starting in the Late Cretaceous. Accretion of crustal material of two microcontinents to Eurasia is assumed, while continuous subduction of the oceanic lithosphere of different ocean basins and possibly of the mantle lithosphere of the microcontinents resulted in a single slab. The length of the oceanic lithosphere that was subducted south of Crete is estimated to be not greater than approximately 550 km.
    Language: English
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  • 38
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado
    Publication Date: 2020-02-12
    Language: English
    Type: info:eu-repo/semantics/other
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  • 39
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    International Association of Hydrological Sciences (IAHS)
    In:  IAHS Annual Report
    Publication Date: 2020-02-12
    Language: English
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  • 40
    Publication Date: 2020-02-12
    Description: We present a case study of lithospheric structure in the forearc of a retreating subduction zone for the Hellenic Arc. Lateral structural variations along the arc beneath the island of Crete are jointly investigated by receiver functions and Rayleigh phase velocities. Data from temporary short-period networks amend previous results from broad-band stations by broadening the frequency range available for phase-velocity determination and increasing the spatial coverage of receiver function profiles. Both receiver functions and dispersion analysis reveal distinct structural differences between western and central Crete. Western Crete is characterized by nearly constant S-velocities of 3.72–3.75 km s−1 from 10 km depth down to a depth of 50 km and no distinct continental Moho signal. Meanwhile, central Crete shows lower S-velocities equal to 3.3 km s−1 in the crust between 10 and 20 km depth which are followed by the Aegean Moho in about 30 km depth and a mantle wedge with an S-velocity of 4.35 km s−1. Both methods lead to an average depth of 55 km for the subducted oceanic African Moho beneath Crete. This means that the slab is separated from the Aegean crust by a mantle wedge beneath central Crete, while beneath western Crete the corresponding depth region is characterized by crustal velocities. This thickened crust in the forearc might be formed by crustal material of the Aegean Plate dragged down with the subducting African lithosphere. Furthermore, rocks extruded from a melange circulating in a subduction channel might accumulate between a depth of 20 and 50 km and contain low-velocity material, e.g. in the form of serpentinized Aegean mantle. In addition, the lateral extent of a prominent negative phase observed around 4 s differential time in receiver functions from western Crete is mapped. This phase might point to low-velocity material around 30 km depth which could be extruded from a subduction channel. An important property of the forearc found in this study is its strong lateral heterogeneity.
    Language: English
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  • 41
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    International Association of Seismology and Physics of the Earth's Interior (IASPEI)
    In:  IASPEI Annual Report
    Publication Date: 2020-02-12
    Language: English
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  • 42
    Publication Date: 2021-07-28
    Description: Recently released global gravity field models generated solely from CHAMP and GRACE satellite observations allow with an unprecedented accuracy and resolution the recovery of the mean sea surface topography from the difference between an altimetry-based mean sea surface height model and the gravity model's derived geoid. Here the CHAMP EIGEN-2 gravity field model, and the first GFZ GRACE gravity model, EIGEN-GRACE01S, are used. The mean sea surface height model has been compiled from four years'; worth of TOPEX altimeter data. To evaluate the accuracy and resolution limits of the CHAMP and GRACE geoids for the envisaged application, a low pass filter in the spatial domain with different cut-off wavelengths has been applied to the geoid and sea surface data before subtraction. The minimum wavelength, where noisy and erroneous features in the recovered sea surface topography are minimised, can be interpreted as an indicator for the best suited common spatial resolution. The EIGEN-2 model's geoid has been tested to have a resolution of 1800 km, which corresponds to a truncation degree of l = 22 in terms of spherical harmonics. Using the EIGEN-GRACE01S model, the resolution could be extended to 1000 km (l = 40). These boundaries can be attributed to the geoid's error, exceeding 2 cm in case of the CHAMP model, and in case of the GRACE model to spurious systematic signals increasing with increasing spherical harmonic degree. The calculated sea surface topography models have been used to derive absolute geostrophic sea surface velocities. An error propagation shows that the requirement of 1 cm/s for geoid induced velocity errors is fulfilled at the given resolutions for all latitudes excluding a narrow equatorial band. Maximum geostrophic velocities are derived in the 1000 km-resolution model for the Kuroshio region with 40 cm/s, and for the Gulf Stream east off Cape Hatteras with 25 cm/s.
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  • 43
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    Deutsches GeoForschungsZentrum GFZ
    In:  Scientific Technical Report STR
    Publication Date: 2021-07-25
    Language: English
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  • 44
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences, University of Colorado
    In:  IUGG Annual Report
    Publication Date: 2023-03-02
    Language: English
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  • 45
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: AWI G8-08-0028
    Type of Medium: Monograph available for loan
    Pages: XLVI, 486 S. : Ill., graph. Darst., Kt.
    ISBN: 354042640X
    Series Statement: Springer-Praxis books in geophysical sciences
    Language: English
    Branch Library: AWI Library
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  • 46
    Monograph available for loan
    Monograph available for loan
    Joensuu : European Forest Institute
    Call number: PIK W 510-16-89952
    Type of Medium: Monograph available for loan
    Pages: 150 S. , graph. Darst.
    Series Statement: EFI proceedings 50
    Language: English
    Branch Library: PIK Library
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  • 47
    Call number: PIK W 510-16-89951
    Type of Medium: Monograph available for loan
    Pages: 322 S. , Ill., Darst., Kt.
    ISBN: 9525453006
    Series Statement: EFI proceedings 49
    Language: English
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  • 48
    Monograph available for loan
    Monograph available for loan
    Joensuu : European Forest Institute
    Call number: PIK W 510-16-89954
    Type of Medium: Monograph available for loan
    Pages: 216 S. , graph. Darst.
    ISBN: 9525453065
    Series Statement: EFI proceedings 52
    Language: English
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  • 49
    Call number: AWI G7-18-91807
    Type of Medium: Monograph available for loan
    Pages: 150 Seiten
    ISBN: 5-286-01500-X
    Language: Russian , English
    Note: Beiträge teilweise englisch, teilweise russisch , Überwiegend kyrillische Schrift
    Location: AWI Reading room
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  • 50
    Monograph available for loan
    Monograph available for loan
    New York : Cambridge University Press
    Call number: PIK B 160-04-0288
    Type of Medium: Monograph available for loan
    Pages: XV, 355 S
    ISBN: 0521472830
    Uniform Title: Prix, reproduction, rareté
    Language: English
    Location: A 18 - must be ordered
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  • 51
    Call number: AWI G10-04-0095
    Type of Medium: Monograph available for loan
    Pages: XVI, 364 Seiten , Illustrationen , 1 CD-ROM (12 cm) , 28 cm
    ISBN: 3540434577
    Language: English
    Note: Contents (I) Motivation and Methods (A) The Antarctic Ice Sheet and its Role in the Global System (A.1) Main Geographic and Glaciologic Provinces of Antarctica (A.2) Climatic Change, Sea-Level Rise,and Changes in the Cryosphere (A.3) Modeling Versus Measuring B) Satellite Remote Sensing (B.1) An Overview of Ice Sheet Observations by Satellite (B.2) Satellite Radar Altimetry (B.2.1) Satellite Missions with Radar Altimeter Observations (B.2.1.1) SEASAT (B.2.1.2) GEOSAT (B.2.1.3) ERS-1 and ERS-2 (B.2.1.4) Other Missions with Altimeters, and Related Missions (B.2.2) Mission Types: Exact Repeat Missions and Geodetic Missions (B.2.3) Radar Measurement Principles (B.3) Analysis of Satellite Radar Altimeter Data over Ice Sheets and Glaciers (B.3.1) Problems and Methods of Mapping Ice Surface Elevation (B.3.2) Derivation of Ice Surface Roughness and Morphology (C) Data Analysis Methods Applied in the Antarctic Atlas (C.0) Introduction (C.1) Corrections of Radar Altimeter Data (C.1.1) Corrections Applied to Satellite Radar Altimeter Data for Ice Surface Mapping (C.1.2) The Bad-Track Problem (C.1.3) The Need for Interpolation of Geophysical Line Survey Data (C.2) Map Projection and Atlas Mapping (C.2.1) The UTM Projection (C.2.2) The Atlas Mapping Problem (C.2.3) The Solution: The Antarctic Atlas Mapping Scheme (C.2.4) Map Sheet Calculation with TRANSVIEW (C.3) Geostatistical Estimation (C.3.1) Concept of the Regionalized Variable and Principles of Variography (C.3.2) Kriging (C.3.3) Variography for Satellite Radar Altimeter Data over Antarctic Ice Surfaces (C.3.4) Application: Search Algorithm and Kriging Parameters for Antarctic Atlas DTMs. Mapping Parameters (C.3.4.1) Search Routine for Geophysical Line Survey Data and Software (C.3.4.2) Grid Spacing (C.3.4.3) Mapping Parameters: Contouring and Coloring Scheme (C.3.5) Error Analysis (C.3.6) Influence of the Radar Altimeter Sensor Compared to Influence of the Variogramin Kriging for GEOSAT and ERS-1 Data (C.4) The Role of the Geodetic Reference Surface (C.4.1) Ellipsoid and Geoid Concepts (C.4.2) Mapping of Ice Surfaces with Reference to Geoid Models (II) The Atlas (D) Atlas Maps (D.0) Map Organization and Description Principles (D.1) Latitude Row 63-68°S: Maps from GEOSAT and ERS-1 Radar Altimeter Data Map m45e37-53n63-68 Casey Bay Map m57e49-65n63-68 Napier Mountains Map m69e61-77n63-68 Mawson Coast East Map m81e73-89n63-68 Leopold and Astrid Coast Map m93e85-101n63-68 Queen Mary Coast Map m105e97-113n63-68 Knox Coast Map m117e109-125n63-68 Sabrina Coast Map m129e121-137n63-68 Clarie Coast Map m141e133-149n63-68 Adélie Coast Map m153e145-161n63-68 Ninnis Glacier Tongue Map m297e289-305n63-68 Antarctic Peninsula (Graham Land) (D.2) Latitude Row 67-72.1°S: Maps from GEOSAT and ERS-1 Radar Altimeter Data Map m15we23W-7Wn67-721 Ekström Ice Shelf Map m3we11w-5n67-721 Fimbul Ice Shelf Map m9e1-17n67-721 Princess Astrid Coast Map m21e13-29n67-721 Erskine Iceport Map m33e25-41n67-721 Riiser-Larsen Peninsula Map m45e37-53n67-721 Prince Olav Coast Map m57e49-65n67-721 Kemp Coast Map m69e61-77n67-721 Lambert Glacier Map m81e73-89n67-721 Ingrid Christensen Coast Map m93e85-101n67-721 Wilkes Land (e85-101n67-721) Map m105e97-113n67-721 Wilkes Land (e97-113n67-721) Map m117e109-125n67-721 Wilkes Land (e109-125n67-721) Map m129e121-137n67-721 Wilkes Land (e121-137n67-721) Map m141e133-149n67-721 Wilkes Land (e133-149n67-721) Map m153e145-161n67-721 Cook Ice Shelf Map m165e157-173n67-721 Pennell Coast Map m292e284-300n67-721 Antarctic Peninsula (Palmer Land) (D.3) Latitude Row 71-77°S: Maps from ERS-1 Radar Altimeter Data Map m333e315-351n71-77 Riiser-Larsen Ice Shelf Map m357e339-15n71-77 New Schwabenland Map m21e3-39n71-77 Sør Rondane Mountains Map m45e27-63n71-77 Belgica Mountains Map m69e51-87n71-77 Upper Lambert Glacier Map m93e75-111n71-77 American Highland Map m117e99-135n71-77 Dome Charlie Map m141e123-159n71-77 Southern Wilkes Land (e123-159) Map m165e147-183n71-77 Victoria Land Map m213e195-231n71-77 Ruppert Coast Map m237e219-255n71-77 Bakutis Coast Map m261e243-279n71-77 Walgreen Coast Map m285e267-303n71-77 Ellsworth Land Map m309e291-327n71-77 Black Coast (D.4) Latitude Row 75-80°S: Maps from ERS-1 Radar Altimeter Data Map m333e315-351n75-80 Coats Land Map m357e339-15n75-80 Western Queen Maud Land (North) Map m21e3-39n75-80 Central Queen Maud Land (North) Map m45e27-63n75-80 Valkyrie Dome Map m69e51-87n75-80 South of Lambert Glacier Map m93e75-111n75-80 East Antarctica (Sovetskaya) Map m117e99-135n75-80 East Antarctica (Vostok) Map m141e123-159n75-80 East Antarctica (Mt. Longhurst) Map m165e147-183n75-80 Scott Coast Map m189e171-207n75-80 Roosevelt Island Map m213e195-231n75-80 Saunders Coast Map m237e219-255n75-80 Northern Marie Byrd Land Map m261e243-279n75-80 Northern Hollick-Kenyon Plateau Map m285e267-303n75-80 Zumberge Coast Map m309e291-327n75-80 Ronne Ice Shelf (D.5) Latitude Row 78-81.5°S: Maps from ERS-1 Radar Altimeter Data Map m333e315-351n78-815 Filchner Ice Shelf Map m357e339-15n78-815 Western Queen Maud Land (South) Map m21e3-39n78-815 Central Queen Maud Land (South) Map m45e27-63n78-815 Eastern Queen Maud Land (South) Map m69e51-87n78-815 Dome Argus Map m93e75-111n78-815 East Antarctica (e75-111n78-815) Map m117e99-135n78-815 EastAntarctica (e99-135n78-815) Map m141e123-159n78-815 Byrd Glacier Map m165e147-183n78-815 Hillary Coast Map m189e171-207n78-815 Ross Ice Shelf Map m213e195-231n78-815 Shirase Coast Map m237e219-255n78-815 Southern Marie Byrd Land Map m261e243-279n78-815 Southern Hollick-Kenyon Plateau Map m285e267-303n78-815 Ellsworth Mountains Map m309e291-327n78-815 Berkner Island (III) Applications (E) Monitoring Changes in Antarctic Ice SurfaceTopography: The Example of the Lambert Glacier/Amery Ice Shelf System (E.1) The Problem of Monitoring Changes (E.2) Time Series of Digital Terrain Models and Maps (E.3) Altimeter Data: Acquisition and Corrections (E.4) Visual Comparison - Quantitative Comparison (E.5) Calculation of Elevation Changes (E.6) Discussion of Results on Elevation Changes (E.6.1) Results of the Monitoring Study (E.6.2) Comparison with Other Maps of Lambert Glacier/Amery Ice Shelf (E.7) On the Potential Existence of Surge Glaciers in the Lambert Glacier/Amery Ice Shelf System (E.7.1) Introduction to the Surge Phenomenon and Relationship to Results of the Monitoring Study (E.7.2) Discussion of the Surge Hypothesis in the Glaciologic Literature (F) Detailed Studies of Selected Antarctic Outlet Glaciers and Ice Shelves (F.0) Introduction (F.1) Detail Map 1: Slessor Glacier (ERS-1 Data 1995) (F.2) Detail Map 2: Stancomb-Wills Glacier (ERS-1 Data 1995) (F.3) Detail Map 3: Jutulstraumen Glacier (ERS-1 Data 1995) (F.4) Detail Map 4: Shirase Glacier (ERS-1 Data 1995) (F.5) Detail Map 5: Lambert Glacier (ERS-1 Data 1995) (F.6) Detail Map 6: West Ice Shelf (ERS-1 Data 1995) (F.7) Detail Map 7: Denman Glacier (ERS-1 Data 1995) (F.8) Detail Map 8: Vanderford Glacier (ERS-1 Data 1995) (F.9) Detail Map 9: Totten Glacier (ERS-1 Data 1995) (F.10) Detail Maps 10: Mertz Glacier,11: Ninnis Glacier, and 12: Mertz and Ninnis Glaciers (GEOSAT Data 1985-86) (F.11) Detail Map 13: Rennick Glacier (ERS-1 Data 1995) (F.12) Detail Map 14: David Glacier/Drygalski Ice Tongue (ERS-1 Data 1995) (F.13) Detail Map15: Thwaites Glacier (ERS-1 Data 1995) (F.14) Detail Map 16: PineIsland Glacier (ERS-1 Data 1995) (G) Combination of SAR and Radar Altimeter Data: Lambert Glacier/Amery Ice Shelf (IV) References and Appendix (H) References (I) Appendix (I.1)Glaciological Glossary (I.2) Index of Place Names (I.3) Antarctic Expeditions (I.3.1) Early Seagoing Expeditions (I.3.2) Expeditions to the Antarctic Continent (I.3.3) Antarctic Expeditions after the International Geophysical Year
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  • 52
    Call number: AWI G2-05-0017
    Type of Medium: Monograph available for loan
    Pages: 162 S.
    Language: English
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  • 53
    Monograph available for loan
    Monograph available for loan
    Oldendorf/Luhe : International Ecology Inst.
    Call number: PIK N 531-16-89771
    Type of Medium: Monograph available for loan
    Pages: XXIX, 235 S. , graph. Darst.
    Series Statement: Excellence in ecology 16
    Language: English
    Location: A 18 - must be ordered
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  • 54
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: PIK A 130-04-0179
    In: Biennial report
    Type of Medium: Monograph available for loan
    Pages: 162 S.
    Language: English
    Location: A 18 - must be ordered
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  • 55
    Call number: AWI G2-05-0084 ; AWI G2-06-0213
    Description / Table of Contents: To understand the global oceanic carbon budget and related climate change, exact measurements of organic carbon flux in all oceans environments, especially the continental margins, are crucial. In fact, data have been available for some time on organic carbon sources, pathways, and burial for most of the world's oceans, with the notable exception of the Arctic. With this book, the editors remedy this gap in knowledge, presenting an overview of organic-carbon sources, pathways, and burial of the circum-Arctic continental margin and deep-sea areas. Data from each Arctic shelf and basin are collates, presented in common and parallel formats, and related to the global carbon cycle. The book is suitable for lecturers, graduate students as well as scientists interested in the organic-carbon-cycle and Arctic Ocean (paleo-)environment.
    Type of Medium: Monograph available for loan
    Pages: XIX, 363 Seiten , Illustrationen
    ISBN: 3-540-01153-6
    Language: English
    Note: Contents: 1 The Arctic Ocean: Boundary Conditions and Background Information. - 1.1 Physiography and Bathymetry of the Arctic Ocean. - 1.2 The Arctic Ocean: Modern Status and Recent Climate Change. - 1.3 The Tectonic Evolution of the Arctic Ocean: Overview and Perspectives. - 1.4 Geochemical Proxies Used for Organic Carbon Source Identification in Arctic Ocean Sediments. - 2 Modern Terrigenous Organic Carbon Input to the Arctic Ocean. - 2.1General Introduction. - 2.2 River Input. - 2.3 Organic Carbon Input to the Artic Seas Through Coastal Erosion. - 2.4 The Role of Arctic Sea Ice in Transporting and Cycling Terrestrial Organic Matter. - 2.5 Aeolian Input. - 2.6 Summary and Concluding Remarks. - 3 Primary and Secondary Production in the Arctic Seas. - 3.1 Introduction. - 3.2 Major Algal Groups and Their Distribution. - 3.3 Limitation and Control of Primary Production 3.4 Primary Production and Growth Rate. - 3.5 Seasonality. - 3.6 Distribution of Primary Production. - 3.7 Mesozooplankton . - 3.8 Primary Production - Impact of Climate Change. - 3.9 Summary and Concluding Remarks . - 4 The Role of Dissolved Organic Matter for the Organic Carbon Cycle in the Arctic Ocean. - 4.1 Introduction. - 4.2 Riverine DOM on Arctic Shelves and Beyond. - 4.3 Distribution, Chemical Composition, and Fluxes of Marine DOM in the Central Arctic Ocean. - 4.4 Summary and Concluding Remarks. - 5 Particulate Organic Carbon Flux to the Arctic Ocean Sea Floor. - 5.1 Introduction 5.2 What do we Know About Vertical Carbon Flux from the Arctic Ocean?. - 5.3 Case Studies. - 5.4 Regional Variability in POC Export Flux in the Arctic Ocean Determined Using 234Th as a Tracer. - 5.5 Particulate Organic Carbon Flux to the Sea floor of the Arctic Ocean: Quantity, Seasonality and Processes. - 5.6 Summary and Concluding Remarks. - 6 The Benthos of Arctic Seas and its Role for the Organic Carbon Cycle at the Seafloor. - 6.1 Introduction. - 6.2 Origin and Evolution of Arctic Habitats and Species. - 6.3 Food Supply of the Arctic Benthos: Sources and Pathways. - 6.4 Benthic Communities of the Arctic Seas. - 6.5 Organic Carbon Utilization by the Arctic Benthos. - 6.6 Summary and Concluding Remarks. - 7 Organic Carbon in Arctic Ocean Sediments: Sources, Variability, Burial, and Paleoenvironmental Significance. - 7.1 Organic Carbon in Arctic Ocean Sediments: A General Introduction. - 7.2 The Beaufort Sea: Distribution, Sources, Fluxes, and Burial Rates of Organic Carbon. - 7.3 The Continental Margin of the North Bering - Chukchi Sea: Distribution, Sources, Fluxes, and Burial Rates of Organic Carbon. - 7.4 The East Siberian Sea: Distribution, Sources, and Burial of Organic Carbon. - 7.5 The Laptev Sea: Distribution, Sources, Variability and Burial of Organic Carbon. - 7.6 The Kara Sea: Distribution, Sources, Variability and Burial of Organic Carbon. - 7.7 The Barents Sea: Distribution, Sources, Variability and Burial of Organic Carbon. - 7.8 Northern Fram Strait und Yermak Plateau: Distribution, Variability and Burial of Organic Carbon and Paleoenvironmental Implications. - 7.9 The Central Arctic Ocean: Distribution, Sources, Variability and Burial of Organic Carbon. - 8 Organic Carbon Budget: Arctic Ocean vs. Global Ocean. - 8.1 Introduction. - 8.2 Global Organic Carbon Fluxes: Sources and Sinks. - 8.3 Arctic Ocean Organic Carbon Fluxes: Sources and Sinks. - 8.4 Summary and Concluding Remarks. - 9 References.
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  • 56
    Monograph available for loan
    Monograph available for loan
    Hoboken, N.J. : Wiley-Interscience
    Call number: AWI A14-06-0535
    Description / Table of Contents: Over the forty years since the invention of the laser, optical and electronic technology has made great strides, enabling the practical use of lidar in many fields. As lidar technology moves from being an object of research to providing data for other types of researchers to use, it becomes increasingly important to have a resource that explains the topic simply, yet thoroughly. Intended as a handbook for researchers, graduate students, and lidar users, Elastic lidar : theory, practice, and analysis methods bridges a twenty-year gap in the lidar literature and brings its subject into the twenty-first century. Focusing on elastic lidars, the most common type of lidars in use today, the authors, both researchers in the field, provide a comprehensive discussion of practical elastic lidar methodology and inversion techniques, data analysis methods, and the construction of elastic lidars. The book provides lidar professionals and students alike with clear and simple explanations of how lidars work, data inversion techniques, construction of elastic lidars, how to extract information from the data lidars provide. Based on their own professional experience, the authors provide readers with a straightforward explanation of what lidar technology can and cannot do with the methods currently available, while providing alternate viewpoints so that readers can draw their own conclusions.
    Type of Medium: Monograph available for loan
    Pages: XVI, 615 Seiten , Illustrationen
    ISBN: 0471201715
    Language: English
    Note: CONTENTS: Preface. - Definitions. - 1 Atmospheric Properties. - 1.1. Atmospheric Structure. - 1.1.1. Atmospheric Layers. - 1.1.2. Convective and Stable Boundary Layers. - 1.1.3. Boundary Layer Theory. - 1.2. Atmospheric Properties. - 1.2.1. Vertical Profiles of Temperature, Pressure and Number Density. - 1.2.2. Tropospheric and Stratospheric Aerosols. - 1.2.3. Particulate Sizes and Distributions. - 1.2.4. Atmospheric Data Sets. - 2 Light Propagation in the Atmosphere. - 2.1. Light Extinction and Transmittance. - 2.2. Total and Directional Elastic Scattering of the Light Beam. - 2.3. Light Scattering by Molecules and Particulates: Inelastic Scattering. - 2.3.1. Index of Refraction. - 2.3.2. Light Scattering by Molecules (Rayleigh Scattering). - 2.3.3. Light Scattering by Particulates (Mie Scattering). - 2.3.4. Monodisperse Scattering Approximation. - 2.3.5. Polydisperse Scattering Systems. - 2.3.6. Inelastic Scattering. - 2.4. Light Absorption by Molecules and Particulates. - 3 Fundamentals of the Lidar Technique. - 3.1. Introduction to the Lidar Technique. - 3.2. Lidar Equation and lts Constituents. - 3.2.1. The Single-Scattering Lidar Equation. - 3.2.2. The Multiple-Scattering Lidar Equation. - 3.3. Elastic Lidar Hardware. - 3.3.1 Typical Lidar Hardware. - 3.4. Practical Lidar lssues. - 3.4.1. Determination of the Overlap Function. - 3.4.2. Optical Filtering. - 3.4.3. Optical Alignment and Scanning. - 3.4.4. The Range Resolution of a Lidar. - 3.5. Eye Safety Issues and Hardware. - 3.5.1. Lidar-Radar Combination. - 3.5.2. Micropulse Lidar. - 3.5.3. Lidars Using Eye-Safe Laser Wavelengths. - 4 Detectors, Digitizers, Electronics. - 4.1. Detectors. - 4.1.1. General Types of Detectors. - 4.1.2. Specific Detector Devices. - 4.1.3. Detector Performance. - 4.1.4. Noise. - 4.1.5. Time Response. - 4.2. Electric Circuits for Optical Detectors. - 4.3. A-D Converters/Digitizers. - 4.3.1. Digitizing the Detector Signal. - 4.3.2. Digitizer Errors. - 4.3.3. Digitizer Use. - 4.4. General. - 4.4.1. Impedance Matching. - 4.4.2. Energy Monitaring Hardware. - 4.4.3. Photon Counting. - 4.4.4. Variable Amplification. - 5 Analytical Solutions of the Lidar Equation. - 5.1. Simple Lidar-Equation Solution for a Homogeneaus Atmosphere: Slope Method. - 5.2. BasicTransformation of the Elastic Lidar Equation. - 5.3. Lidar Equation Solution for a Single-Component Heterogeneaus Atmosphere. - 5.3.1. Boundary Point Solution. - 5.3.2. Optical Depth Solution. - 5.3.3. Solution Based on a Power-Law Relationship Between Backscatter and Extinction. - 5.4. Lidar Equation Solution for a Two-Component Atmosphere. - 5.5. Which Solution is Best?. - 6 Uncertainty Estimation for Lidar Measurements. - 6.1. Uncertainty for the Slope Method. - 6.2. Lidar Measurement Uncertainty in a Two-Component Atmosphere. - 6.2.1. General Formula. - 6.2.2. Boundary Point Solution: Influence of Uncertainty and Location of the Specified Boundary Value on the Uncertainty δkw(r). - 6.2.3. Boundary-Point Solution: lnfl.uence of the Particulate Backscatter-to-Extinction Ratio and the Ratio Between Kp(r) and Km(r) on Measurement Accuracy. - 6.3. Background Constituent in the Original Lidar Signal and Lidar Signal Averaging. - 7 Backscatter-to-Extinction Ratio. - 7.1. Exploration of the Backscatter-to-Extinction Ratios: Brief Review. - 7.2. lnfluence of Uncertainty in the Backscatter-to-Extinction Ratio on the Inversion Result. - 7.3. Problem of a Range-Dependent Backscatter-to-Extinction Ratio. - 7.3.1. Application of the Power-Law Relationship Between Backscattering and Total Scattering in Real Atmospheres: Overview. - 7.3.2. Application of a Range-Dependent Backscatter-to-Extinction Ratio in Two-Layer Atmospheres. - 7.3.3. Lidar Signal Inversion with an Iterative Procedure. - 8 Lidar Examination of Clear and Moderately Turbid Atmospheres. - 8.1. One-Directional Lidar Measurements: Methods and Problems. - 8.1.1. Application of a Particulate-Free Zone Approach. - 8.1.2. Iterative Method to Determine the Location of Clear Zones. - 8.1.3. Two-Boundary-Point and Optical Depth Solutions. - 8.1.4. Combination of the Boundary Point and Optical Depth Solutions. - 8.2. Inversion Techniques for a "Spotted" Atmosphere. - 8.2.1. General Principles of Localization of Atmospheric "Spots". - 8.2.2. Lidar-Inversion Techniques for Monitaring and Mapping Particulate Plumes and Thin Clouds. - 9 Multiangle Methods for Extinction Coefficient Determination. - 9.1. Angle-Dependent Lidar Equation and Its Basic Solution. - 9.2. Solution for the Layer-Integrated Form of the Anglenependent Lidar Equation. - 9.3. Solution for the Two-Angle Layer-Integrated Form of the Lidar Equation. - 9.4. Two-Angle Solution for the Angle-Independent Lidar Equation. - 9.5. High-Altitude Tropospheric Measurements with Lidar. - 9.6. Which Method Is the Best?. - 10 Differential Absorption Lidar Technique (DIAL). - 10.1. DIAL Processing Technique: Fundamentals. - 10.1.1. General Theory. - 10.1.2. Uncertainty of the Backscatter Corrections in Atmospheres with Large Gradients of Aerosol Backscattering. - 10.1.3. Dependence of the DIAL Equation Correction Terms on the Spectral Range Interval Between the On and Off Wavelengths. - 10.2. DIAL Processing Technique: Problems. - 10.2.1. Uncertainty of the DIAL Solution for Column Content of the Ozone Concentration. - 10.2.2. Transition from Integrated to Range-Resolved Ozone Concentration: Problems of Numerical Differentiation and Data Smoothing. - 10.3. Other Techniques for DIAL Data Processing. - 10.3.1. DIAL Nonlinear Approximation Technique for Determining Ozone Concentration Profiles. - 10.3.2. Compensational Three-Wavelength DIAL Technique. - 11 Hardware Solutions to the Inversion Problem. - 11.1. Use of N2 Raman Scattering for Extinction Measurement. - 11.1.1. Method. - 11.1.2. Limitations of the Method. - 11.1.3. Uncertainty. - 11.1.4. Altemate Methods. - 11.1.5. Determination of Water Content in Clouds. - 11.2. Resolution of Particulate and Molecular Scattering by Filtration. - 11.2.1. Background. - 11.2.2. Method. - 11.2.3. Hardware. - 11.2.4. Atomic Absorption Filters. - 11.2.5. Sources of Uncertainty. - 11.3. Multiple-Wavelength Lidars. - 11.3.1. Application of Multiple-Wavelength Lidars for the Extraction of Particulate Optical Parameters. - 11.3.2. Investigation of Particulate Microphysical Parameters with Multiple-Wavelength Lidars. - 11.3.3. Limitations of the Method. - 12 Atmospheric Parameters from Elastic Lidar Data. - 12.1. Visual Range in Horizontal Directions. - 12.1.1. Definition of Terms. - 12.1.2. Standard Instrumentation and Measurement Uncertainties. - 12.1.3. Methods of the Horizontal Visibility Measurement with Lidar. - 12.2. Visual Range in Slant Directions. - 12.2.1. Definition of Terms and the Concept of the Measurement. - 12.2.2. Asymptotic Method in Slant Visibility Measurement. - 12.3. Temperature Measurements. - 12.3.1. Rayleigh Scattering Temperature Technique. - 12.3.2. Metal Ion Differential Absorption. - 12.3.3. Differential Absorption Methods. - 12.3.4. Doppler Broadening of the Rayleigh Spectrum. - 12.3.5. Rotational Raman Scattering. - 12.4. Boundary Layer Height Determination. - 12.4.1. Profile Methods. - 12.4.2. Multidimensional Methods. - 12.5. Cloud Boundary Determination. - 13 Wind Measurement Methods from Elastic Lidar Data. - 13.1. Correlation Methods to Determine Wind Speed and Direction. - 13.1.1. Point Correlation Methods. - 13.1.2. Two-Dimensional Correlation Method. - 13.1.3. Fourier Cerrelation Analysis. - 13.1.4. Three-Dimensional Correlation Method. - 13.1.5. Multiple-Beam Technique. - 13.1.6. Uncertainty in Correlation Methods. - 13.2. Edge Technique. - 13.3. Fringe Imaging Technique. - 13.4. Kinetic Energy, Dissipation Rate, and Divergence. - Bibliography. - Index.
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  • 57
    Series available for loan
    Series available for loan
    Terra Antarctica Publications : Siena
    Associated volumes
    Call number: ZSP-760/A-10
    In: Terra Antartica reports
    Type of Medium: Series available for loan
    Pages: 49 S. + Kt.
    ISBN: 8888395075
    Series Statement: Terra Antartica reports 10
    Language: English
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  • 58
    Journal available for loan
    Journal available for loan
    Associated volumes
    In: Economic Geology
    Type of Medium: Journal available for loan
    Pages: 842 S.
    Language: English
    Location: Lower compact magazine
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  • 59
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI Bio-06-0035-1
    In: Molecular microbial ecology manual
    Type of Medium: Monograph available for loan
    Pages: XVI, 848 S.
    Edition: 2nd ed.
    Language: English
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  • 60
    Monograph available for loan
    Monograph available for loan
    [Jakarta] : Ministry of Research and Technology 〈Jakarta〉
    Call number: M 06.0033
    Type of Medium: Monograph available for loan
    Pages: 199 S. : überw. Ill.
    ISBN: 9796300184
    Uniform Title: Membangun IPTEK untuk Peradaban dan Kesejahteraan Bangsa
    Classification:
    E.7.
    Language: English
    Location: Upper compact magazine
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  • 61
    Call number: ILP/M 06.0353
    In: Publication of the International Lithosphere Programme
    In: Tectonophysics
    Type of Medium: Monograph available for loan
    Pages: vi, 271 S. : Ill., graph. Darst.
    Series Statement: [Publication of the International Lithosphere Programme] 381,1-4 : special issue
    Language: English
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  • 62
    Monograph available for loan
    Monograph available for loan
    Copenhagen : Geological Survey of Denmark and Greenland
    Call number: AWI P8-04-0125
    Description / Table of Contents: Contents: Preface. - llulissat Icefjord - a unique natural phenomenon. - llulissat - a modern town. - 4400 years of history. - The Inland Ice and the icefjord . - Sermeq Kujalleq - the fast glacier. - A rich fauna. - ln the spotlight of the world and science. - Protection and management. - Science born at the Inland Ice and the icefjord. - The period of discovery: 1700-1845. - Observations and theories: 1845-1950. - Modern glaciology from 1950. - Glacier surges. - The Inland Ice and glaciology. - Earlier glaciations. - Glaciation history in the llulissat area. - The Inland Ice from top to margin. - Portrait of Sermeq Kujalleq. - Calving. - Dynamics of Sermeq Kujalleq. - Dramatic break-up in 2002. - The icefjord. - The iceberg bank. - The land below and around the ice. -Drainage channels, troughs and fjords. - Moraine ridges, kame terraces and marginal deltas . - Land uplift. - Climate, darkness and light . - The nutrient-rich icefjord - and the profusion of life. - Marine plankton. - Fish and larger crustaceans. - Marine mammals. - Birds at the icefjord. - Land mammals. - Plants on rocky ground. - Traditional use of plants. - The land of the 'icefjord people'. - Palaeo-Eskimo settlements. - Thule people at the icefjord. - Rich archaeological finds. - Eqi - a settlement at the mouth of the icefjord . - Colonisation and the Napoleonic Wars (1800-1830). - Recovery, whale oil and edueation (1830-1850). - The exodus from Sermermiut and the tuberculosis epidemic (1850-1890). - Halibut for export (1890-1930). - World war, reform and centralisation (1930-1960). - 96 Shrimp bonanza, population explosion and tourism (1960-2000). -Hunting mammals, fish and birds. - Recreational hunting. - Professional hunting. - Fishing methods, tackle and localities. - llulissat today. - Supplementary reading. - Epilogue. - Box 1: The Earth and the ice. - Box 2: 150 years of exploration. - Box 3a: Climate archives in the Inland Ice. - Box 3b: The unstable ice age. - Box 3c: Close-up of the Icefjord. - Box 4: Kaneling. -Box 5: Bubbles and glacier ice. - Box 6: Icebergs. - Box 7: When the ice advances and retreats. - Box 8: Fish species in the area. - Box 9: Lichens in the llulissat area. - Box 10: Faith and story-telling tradition. - Box 11: Halibut, hunger and survival. - Box 12: Knud Rasmussen's great expeditions.
    Description / Table of Contents: At the 28th session of the World Heritage Committee in the summer of 2004, Ilulissat Icefjord was included on UNESCO's World Heritage List. The icefjord is one of the first natural phenomena in the Arctic to find its place on this prestigious list, which includes numerous world famous localities. The icefjord has been accpeted because of its unique glaciological characteristics and its magnificient scenic beauty.
    Type of Medium: Monograph available for loan
    Pages: 116 S.
    ISBN: 8778711363
    Language: English
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    Call number: 11/N 05.0570
    In: International tables for crystallography
    Type of Medium: Monograph available for loan
    Pages: XXII, 731 S. : graph. Darst.
    Edition: 1. ed
    ISBN: 1402023553
    Classification:
    Mineralogy
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Goa : National Centre for Antarctic and Ocean Research
    Call number: AWI A4-06-0015
    Type of Medium: Monograph available for loan
    Pages: 33, XXVIII S. : graph. Darst.
    Edition: 1. ed.
    Series Statement: SAC-NCAOR-01-2004
    Language: English
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  • 65
    Call number: ZS-090(489) ; ZSP-168-489
    In: Berichte zur Polar- und Meeresforschung, 489
    Type of Medium: Series available for loan
    Pages: 231 Seiten , Illustrationen
    ISSN: 1618-3193
    Series Statement: Berichte zur Polar- und Meeresforschung 489
    Language: English
    Note: Enthaltener Beitrag: Russian-German cooperation System Laptev Sea : the expedition Lena-Anabar 2003 / edited by Lutz Schirrmeister, Mikhail N. Grigoriev, Lars Kutzbach, Dirk Wagner and Dmitry Yu. Bolshiyanov , Enthaltener Beitrag: The Russian-German TRANSDRIFT IX Expedition of RV "Ivan Kireyev" 2003 / edited by Carolyn Wegner, Jens Hölemann and Vladimir Churun , Contents for "Russian-German cooperation System Laptev Sea : the expedition Lena-Anabar 2003" 1 Introduction 2 Expedition itinerary and general logistics 3 Ecological studies on permafrost soils and landscapes of the central Lena Delta6 3.1 Aims and study area 3.2 Energy and water budget of permafrost soils – long time soil survey station on Samoylov Island 3.3 Micrometeorological measurements of energy, water, and carbon exchange between Arctic tundra and the atmosphere 3.3.1 Introduction 3.3.2 Experimental set-up 3.3.3 The observation period 2003 3.3.3.1 Wind characteristics 3.3.3.2 Meteorological conditions 3.3.3.3 Turbulent fluxes 3.4 Microbial process studies on methane fluxes from permafrost environments 3.4.1 Introduction 3.4.2 Methane emission and microbial methane production 3.4.2.1 Methods and field experiments 3.4.2.2 Preliminary results 3.4.3 Process studies on methane oxidation 3.4.3.1 Introduction and objectives 3.4.3.2 Methods and field experiments 3.4.3.3 Preliminary results 3.4.4 Further investigations 3.5 Studies on recent cryogenesis 3.6 Seasonal progression of active-layer thickness dependent on microrelief 3.6.1 Introduction 3.6.2 Methods 3.6.3 First results 3.7 Air photography and surface classification of Samoylov Island 3.8 Hydrobiological investigations in the Lena Delta in summer 2003 3.8.1 Objectives 3.8.2 Research tasks 3.8.3 Material and methods 3.8.4 Preliminary results 3.9 Appendices Appendix 3-1 Collected variables determined by direct measurements within the micrometeorological campaign Samoylov, 2003 Appendix 3-2 Variables derived from calculations within the micrometeorological campaign Samoylov, 2003 Appendix 3-3 Constants required in calculations Appendix 3-4 List of samples for methane emission and microbial methane production studies Appendix 3-5 List of soil samples for methane oxidation studies 3.10 References 4 Periglacial studies around Cape Mamontov Klyk 4.1 Introduction 4.2 Geological and geographical background 4.3 Geomorphologic route along the Urasalakh River 4.3.1 Structure of Quaternary deposits along the Urasalakh River valley 4.3.2 Geomorphologic structure of the valley 4.3.3 Studies of lakes 4.4 Multi-sensor optical remote sensing of periglacial tundra landscapes 4.4.1 Research aim 4.4.2 Satellite data 4.4.3 General geomorphology in the Lena-Anabar interfluve 4.4.4 Geomorphology in the investigation area near Cape Mamontov Klyk 4.4.5 Field data 4.4.6 Tachymetric survey of periglacial surface features 4.4.7 Characterisation in situ surface properties with a soil probe at a typical elevated Edoma plain 4.5 Methane-related studies on recent tundra soils 4.5.1 Introduction and objectives 4.5.2 Methods 4.5.3 First results 4.6 The coastal section of Cape Mamontov Klyk 4.6.1 General profile 4.6.2 Cryolithological studies of permafrost deposits 4.6.2.1 The first composite profile 4.6.2.2 The second composite profile 4.6.2.3 Additional sampled subprofiles 4.6.3 Ice wedges of Cape Mamontov Klyk 4.6.3.1 Introduction 4.6.3.2 The ice wedges in the lower sands (Unit A) and in the sand-peat-complex (Unit B) 4.6.3.3 Ice wedges of the Late Pleistocene Ice Complex (Unit C) and of Holocene deposits (Unit D) 4.6.3.4 Ground ice of unknown origin 4.6.3.5 Ice wedge section west of the Nuchcha Dzhiele River mouth 4.6.3.6 General interpretation of the sampled profile 4.6.4 Geomicrobiological studies 4.6.4.1Introduction and objectives 4.6.4.2 Methods 4.6.4.3 First results: Methane content of permafrost samples 4.6.5 Paleontological studies 4.7 Studies of coastal dynamics and sub sea permafrost 4.7.1 Preliminary results of sub-sea permafrost drilling in the near-shore zone (spring 2003) 4.7.1.1 Introduction and background 4.7.1.2 Methods and preliminary results 4.7.1.3 Further investigations 4.7.2 Measurements of the coast relief in the area of Cape Mamontov Klyk and ice and sediment sampling 4.7.2.1 Introduction 4.7.2.2 Methods 4.7.2.3 Preliminary results 4.7.2.4 Further investigations 4.7.3 Shore face profiles in the area of Cape Mamontov Klyk: echo sounding, seawater and sea bottom deposits sampling 4.7.3.1 Introduction 4.7.3.2 Methods 4.7.3.3 Preliminary results 4.7.3.4 Further investigations 4.8 References 4.9 Appendices Appendix 4-1. Surface parameters for the studied geolocated sites around Cape Mamontov Klyk Appendix 4-2. Active layer data of the geo-located sites Appendix 4-3. List of soil samples (active layer); collected in the coastal lowland Appendix 4-4. List of permafrost sediment and paleosol samples for microbiological, molecular biological and biochemical analyses Appendix 4-5. List of sediment samples Appendix 4-6. List of ice and water samples Appendix 4-7. Collection of bone samples , Content for "The Russian-German TRANSDRIFT IX Expedition of RV "Ivan Kireyev" 2003" 1. Process Studies on Permafrost Dynamics in the Laptev Sea – An Introduction 2. The TRANSDRIFT IX Expedition: Process studies on submarine permafrost dynamics in the Laptev Sea 3. Motivation: Deployment of two seafloor observatories 4. Recent stability factors of submarine permafrost 4.1 Working program 4.2 Preliminary results 5. Hydrochemical structure of the water column 5.1 Working program 6. Diversity of nitrifying bacteria in submarine permafrost 6.1 Working program 6.2 Preliminary Results 7. Appendix: Station list of the TRANSDRIFT IX (IK03) expedition 8. References
    Location: Lower compact magazine
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    Monograph available for loan
    Monograph available for loan
    Cambridge Univ. Press : Cambridge [u.a.]
    Call number: AWI A13-04-0126
    Description / Table of Contents: This comprehensive text and reference work on numerical weather prediction covers for the first time, not only methods for numerical modeling, but also the important related areas of data assimilation and predictability. It incorporates all aspects of environmental computer modeling including an historical overview of the subject, equations of motion and their approximations, a modern and clear description of numerical methods, and the determination of initial conditions using weather observations (an important new science known as data assimilation). Finally, this book provides a clear discussion of the problems of predictability and chaos in dynamical systems and how they can be applied to atmospheric and oceanic systems. Professors and students in meteorology, atmospheric science, oceanography, hydrology and environmental science will find much to interest them in this book, which can also form the basis of one or more graduate-level courses.
    Type of Medium: Monograph available for loan
    Pages: XXII, 341 S. : graph. Darst., Kt.
    Edition: 1st publ. 2003,Reprint. 2004
    ISBN: 0521796296
    Language: English
    Note: Contents: Foreword. - Acknowledgements. - List of abbreviations. - List of variables. - 1 Historical overview of numerical weather prediction. - 1.1 Introduction. - 1.2 Early developments. - 1.3 Primitive equations, global and regional models, and nonhydrostatic models. - 1.4 Data assimilation: determination of the initial conditions for the computer forecasts. - 1.5 Operational NWP and the evolution of forecast skill. - 1.6 Nonhydrostatic mesoscale models. - 1.7 Weather predictability, ensemble forecasting, and seasonal to interannual prediction. - 1.8 The future. - 2 The continuous equations. - 2.1 Governing equations. - 2.2 Atmospheric equations of motion on spherical coordinates. - 2.3 Basic wave oscillations in the atmosphere. - 2.4 Filtering approximations. - 2.5 Shallow water equations, quasi-geostrophic filtering, and filtering of inertia-gravity waves. - 2.6 Primitive equations and vertical coordinates. - 3. Numerical discretization of the equations of motion. - 3.1 Classification of partial differential equations (PDEs). - 3.2 Initial value problems: numerical solution. - 3.3 Space discretization methods. - 3.4 Boundary value problems. - 3.5 Lateral boundary conditions for regional models. - 4 Introduction to the parameterization of subgrid-scale physical processes. - 4.1 Introduction. - 4.2 Subgrid-scale processes and Reynolds averaging. - 4.3 Overview of model parameterizations. - 5 Data assimilation. - 5.1 Introduction. - 5.2 Empirical analysis schemes. - 5.3 Introduction to least squares methods. - 5.4 Multivariate statistical data assimilation methods. - 5.5 3D-Var, the physical space analysis scheme (PSAS), and their relation to OI. - 5.6 Advanced data assimilation methods with evolving forecast error covariance. - 5.7 Dynamical and physical balance in the initial conditions. - 5.8 Quality control of observations. - 6 Atmospheric predictability and ensemble forecasting. - 6.1 Introduction to atmospheric predictability. - 6.2 Brief review of fundamental concepts about chaotic systems. - 6.3 Tangent linear model, ad joint model, singular vectors, and Lyapunov vectors. - 6.4 Ensemble forecasting: early studies. - 6.5 Operational ensemble forecasting methods. - 6.6 Growth rate errors and the limit of predictability in mid-latitudes and in the tropics. - 6.7 The role of the oceans and land in monthly, seasonal, and interannual predictability. - 6.8 Decadal variability and climate change. - Appendix A The early history of NWP. - Appcndix B Coding and checking the tangent linear and the adjoint models. - Appendix C Post-processing of numerical model output to obtain station weather forecasts. - References. - Index.
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    Boulder, Colo. : Geol. Soc. of America
    Call number: 2006/5
    Language: English
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    Series available for loan
    Series available for loan
    [Tokyo] : Japan Aerospace Exploration Agency
    Associated volumes
    Call number: ZSP-405-06-0030
    In: JAXA Research and Development Report
    Type of Medium: Series available for loan
    Pages: 13 S.
    Series Statement: JAXA Research and development report RR-04-005E
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI Bio-06-0035-2
    In: Molecular microbial ecology manual
    Type of Medium: Monograph available for loan
    Pages: S. 853 - 1774
    Edition: 2nd ed.
    Language: English
    Branch Library: AWI Library
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    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: 5/M 14.0137
    Description / Table of Contents: This book on the terrestrial space environment is directed at a broad group of students and scientists, who seek knowledge of the methods and results of space research. The only prerequisites are fundamental physics and mathematics as usually acquired in introductory college courses in science or engineering curricula. Stressing physical insight rather than mathematical precision, "Physics of the Earth's Space Environment" derives further knowledge on selected topics as each phenomenon is considered and strives to present experimental results in conjunction with basic reasoning about the underlying physics. The content's breadth and introductory nature make this an ideal reader for students in geophysics, meteorology, space sciences and astronomy
    Type of Medium: Monograph available for loan
    Pages: XV, 513 S. , Ill., graph. Darst.
    ISBN: 3540214267 , 978-3-540-21426-7
    Uniform Title: Physik des erdnahen Weltraums
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: AWI G4-04-0085
    Type of Medium: Monograph available for loan
    Pages: X, 331 Seiten , Illustrationen
    ISBN: 3-540-21477-1
    Language: English
    Note: Contents 1 Introduction 2 Features of the Arctic Seas of Russia and Their Ecosystems 2.1 Brief History of the Studies 2.2 Physical Geography 2.3 Features of Geological Structure and Sedimentation 2.4 Hydrology 2.5 Hydrochemistry 2.5.1 Oxygen 2.5.2 pH 2.5.3 Alkalinity 2.5.4 Nutrients (P, N, and Si) 3 Biological Production of the Arctic Seas of Russia 3.1 Introduction 3.2 Barents Sea 3.3 White Sea 3.4. Kara Sea 3.5. Seas of the East Arctic 4 Particulate Matter and Vertical Carbon Fluxes in the Water–Bottom System 4.1 Introduction 4.2 Barents Sea 4.3 White Sea 4.4 Kara Sea 4.5 Laptev, East Siberian, and Chukchi Seas 4.6 Carbon Fluxes from the Photic Zone to the Seafloor 4.7 Conclusion 5 Horizontal Carbon Fluxes in the Land–Sea System 5.1 Riverine Runoff and Carbon Fluxes 5.1.1 Water Runoff and Particulate Matter Supply 5.1.2 Carbon runoff 5.2 Coastal Abrasion and Carbon Fluxes 5.3 Aerosols and Eolian Carbon Fluxes 5.4 Underground and Glacial Runoff 5.4.1 Underground Runoff 5.4.2 Ice and Glacial Discharge 5.4.3 Interstitial Waters 6 Carbon in the Bottom Sediments 6.1 Introduction 6.2 Brief History of the Studies of Carbon and Organic Matter Composition 6.3 Selected Features of the Polar Lithogenesis 6.4 Organo-Chemical Composition of the Sediments 6.5 Distribution and Accumulation Rate of Carbon in the Bottom Sediments 6.5.1 Contents of TOC and Ccarb in Different Types of the Sediments 6.5.2 Distribution of TOC and its Accumulation Rate in the Bottom Sediments 6.5.3 Distribution of Ccarb and its Accumulation Rates in the Bottom Sediments 7 Elements of Carbon Balance and Cycling in the Arctic Seas of Russia 7.1 Fluxes and Balance of Masses 7.2 Ecological Features of the Arctic Seas and their Influence on Carbon Cycling References Index
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    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Earthscan
    Call number: IASS 16.89900
    Type of Medium: Monograph available for loan
    Pages: XIV, 296 S , graph. Darst
    Edition: Second edition
    ISBN: 978-1-138-80262-9
    Language: English
    Branch Library: RIFS Library
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    Monograph available for loan
    Monograph available for loan
    Enfield, NH [u.a.] : Science Publishers
    Associated volumes
    Call number: AWI Bio-07-0011
    In: Flora of Siberia / ser. ed.: I. M. Krasnoborov, Vol. 7
    Type of Medium: Monograph available for loan
    Pages: VIII, 318 S. : graph. Darst., Kt.
    ISBN: 1578081068
    Uniform Title: Flora Sibiri 〈engl.〉
    Language: English
    Note: Contents: Preface. - Family Berberidaceae. - Family Menispermaceae. - Family Papaveraceae. - Family Hypecoaceae. - Family Fumariaceae. - Family Brassicaceae, or Cruciferae: Key to Genera. - Genera Macropodium R.Br.--Gorodkovia Botsch. et Karav. - Genera Erysimum L.--Goldbachia DC. - Genera Hesperis L.--Neuroloma Andrz. - Genera Strigosella Boiss.--Microstigma Trautv. - Genera Dontostemon Andrz. ex C.A. Meyer--Dimorphostemon Kitag. - Genera Chorispora R.Br. ex DC.--Galitzkya V. Boczantzeva. - Genera Alyssum L.--Ptilotrichum C.A. Meyer. - Genus Lesquerella S. Watson. - Genera Draba L.--Subularia L. - Family Droseraceae. - Family Crassulaceae. - Family Saxifragaceae. - Family Parnassiaceae. - Family Grossulariaceae. - Maps of Plant Distribution. - Index of Latin Names of Plants.
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    Call number: PIK W 510-16-89882
    Type of Medium: Monograph available for loan
    Pages: XIV, 459 Seiten , graph. Darst., Kt.
    ISBN: 9280880241
    Series Statement: Forests in transition 2
    Language: English
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    Call number: AWI G7-19-92029
    Type of Medium: Monograph available for loan
    Pages: 37 ungezählte Blätter
    Language: English
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    Washington, D.C. : George Washington University
    Description / Table of Contents: This handbook is for any educator teaching a topic that includes data analysis or computation in order to support learning. It is not just for educators teaching courses in engineering or science, but also data journalism, business and quantitative economics, data-based decision sciences and policy, quantitative health sciences, and digital humanities. It aims to provide an entry point, and a broad overview of Jupyter in education. Whether you are already using Jupyter to teach, you have found learning materials built on Jupyter that piqued your curiosity, or have never heard of Jupyter, the material in this open book can empower you to use this technology in your teaching. Project Jupyter is a broad collaboration that develops open-source tools for interactive and exploratory computing. The tools include: over 100 computer languages (with a focus on Python), the Jupyter Notebook, JupyterHub, and an ecosystem of extensions contributed by a large community. The Jupyter Notebook has exploded in popularity since late 2014, fueled by its adoption as the favorite environment for doing data science. It has also grown as a platform to use in the classroom, to develop teaching materials, to share lessons and tutorials, and to create computational stories. Notebooks are documents containing text narratives with images and math, combined with executable code (many languages are supported) and the output of that code. This marriage of content and code makes for a powerful new form of data-based communication. Educators everywhere are adopting Jupyter for teaching. Educators newly adopting Jupyter can be overwhelmed by having to navigate the ecosystem of tools and content. They could study many examples, or consume a myriad of blog posts and videos of talks to distill the patterns of good practices and technical solutions to serve their students best. Several early adopters, having much experience to share, decided to begin collecting this know-how, and share open documentation about using Jupyter for teaching and learning. The result is this open book: a living document that captures the experiences of community members using Jupyter in education. The Jupyter Community Workshop in Washington, DC (November 2018) began that process, with a book sprint aimed at producing the first version of this handbook. The collaboratively written book consolidates explanations and examples covering key topics, including: what is Jupyter, how to try Jupyter, sharing notebooks with students, locally installing Jupyter, cloud offerings, finding example notebooks, writing lessons in Jupyter, making collections for a course, exporting to other formats with nbconvert, writing textbooks with Jupyter, using Binder and JupyterHub, making assignments and auto-grading, making online courses, teaching with Jupyter in the classroom, active learning and flipped learning pedagogies with Jupyter, and guiding learners to create their own content in Jupyter. This open handbook will grow to encompass all you need to know about Jupyter in teaching and learning.
    Type of Medium: 12
    Pages: Online-Ressource
    Language: English
    Note: 1 Introduction Acknowledgments 2 Why we use Jupyter notebooks 2.1 Why do we use Jupyter? 2.2 But first, what is Jupyter Notebook? 2.3 Course benefits & anecdotes 2.4 Student benefits 2.5 Instructor benefits 2.6 Conclusions 3 Notebooks in teaching and learning 3.1 Oh the places your notebooks will go! 3.2 Before You Begin… 4 A catalogue of pedagogical patterns 4.1 Introduction 4.2 Shift-Enter for the win 4.3 Fill in the blanks 4.4 Target Practice 4.5 Twiddle, tweak, and frob 4.6 Notebook as an app 4.7 Win-day-one 4.8 Top-down sequence 4.9 Two bites at every apple 4.10 Coding as translation 4.11 Symbolic math over pencil + paper 4.12 Replace analysis with numerical methods 4.13 The API is the lesson 4.14 Proof by example, disproof by counterexample 4.15 The world is your dataset 4.16 Now you try (with different data or process) 4.17 Connect to external audiences 4.18 There can be only one 4.19 Hello, world! 4.20 Test driven development 4.21 Code reviews 4.22 Bug hunt 4.23 Adversarial programming 5 Jupyter Notebook ecosystem 5.1 Language support: kernels 5.2 Using Jupyter notebooks 5.3 Authoring Jupyter notebooks 5.4 Tips and tricks 5.5 Gotchas 6 Getting your class going with Jupyter 6.1 Local installation on students’ or lab computers 6.2 Jupyter on remote servers 6.3 Distribution and collection of materials 6.4 Assessing student learning with Jupyter notebooks 6.5 How do you create Jupyter notebooks for reuse and sharing? 6.6 Jupyter: a 21st Century genre of Open Educational Resources and practices 7 Usage case studies 7.1 Jupyter notebooks in support of scaling for large enrollments 7.2 The “CFD Python” story: guiding learners at their own pace 7.3 Analyzing music with music21 7.4 Interactivity in computer science (high school and middle school) 7.5 Interactive geophysics with Jupyter 7.6 Investigating hurricanes 8 About the authors 8.1 Project lead 8.2 Authors at the sprint 9 Glossary References
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    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. : MIT Press
    Call number: PIK V 102-19-92226
    Type of Medium: Monograph available for loan
    Pages: viii, 477 Seiten , Illustrationen, Diagramme , 23 cm
    Edition: Third edition
    ISBN: 0262232375 (alk. paper) , 9780262232371 (alk. paper) , 0262731541 (pbk.) , 9780262731546 (pbk.)
    Language: English
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    Series available for loan
    Series available for loan
    Zurich : Cryospheric Commission of the Swiss Academy of Sciences (SCNAT)
    Associated volumes
    Call number: AWI G3-19-92381
    In: Permafrost in Switzerland, 2004/2005 and 2005/2006
    Type of Medium: Series available for loan
    Pages: XIV, 100 Seiten , Illustrationen
    Series Statement: Glaciological Report (Permafrost) / Permafrost Monitoring Switzerland 6/7
    Language: English
    Note: Contents: Imprint Published Reports Preface Summary Zusammenfassung Résumé Riassunto Resumaziun 1 Introduction 2 Weather and Climate 2.1 Weather and Climate in 2004/2005 2.2 Weather and Climate in 2005/2006 2.3 Climate Deviation from the Mean Value 1961–1990 2.4 Duration of the Snow Cover 3 Borehole Measurements 3.1 Active Layer Thickness 3.2 Permafrost Temperatures 3.2 ERT Monitoring Network 3.4 Conclusions Boreholes 4 Surface Temperatures 4.1 Surface Temperatures in Unconsolidated Sediments 4.2 Rock Surface Temperatures 4.3 Conclusions Surface Temperatures 5 Air Photos 5.1 Air Photos in 2004/2005 and 2005/2006 6 Conclusion 7 Selected Aspects of Permafrost Monitoring 7.1 Short-term Variations in Rock Glacier Kinematics 7.2 Destabilized Rock Glaciers 7.3 Conclusions Rock Glacier Dynamics Acknowledgements References Appendix
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    Monograph available for loan
    Monograph available for loan
    Cambridge, UK : Polity
    Call number: PIK B 130-19-93058
    Type of Medium: Monograph available for loan
    Pages: IX, 254 Seiten
    ISBN: 0745609961 , 074560997X (pbk.) , 9780745609973 (pbk.)
    Language: English
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    Monograph available for loan
    Monograph available for loan
    Wallingford : IAHS Press, Centre for Ecology and Hydrology
    Associated volumes
    Call number: AWI G4-22-95045
    In: IAHS publication, 290
    Type of Medium: Monograph available for loan
    Pages: VIII, 271 Seiten , Illustrationen
    ISBN: 1901502821
    Series Statement: IAHS publication 290
    Language: English
    Note: Contents Preface / by Douglas L. Kane & Daqing Yang Overview of water balance determinations for high latitude watersheds / Douglas L. Kane & Daqing Yang Water balance of a snowy watershed in Hokkaido, Japan / Yoshiyuki Ishii, Yuji Kodama, Ryo Nakamura & Nobuyoshi Ishikawa Features of water balance for small mountainous watersheds in East Siberia: Kolyma Water Balance Station case study / Sergei A. Zhuravin Estimation of annual water balance in Siberian tundra using a new land surface model / Hiroyuki Hiroshima, Tetsuo Ohata, Yuji Kodama & Hironori Yabuki Summer water balance in an Arctic tundra basin, eastern Siberia / Yoshiyuki Ishii, Yuji Kodama, Norifumi Sato & Hironori Yabuki Water balance of small Russian catchments in the southern mountainous Taiga Zone: "Mogot" case study / Ninel G. Vasilenko Features of forest-steppe small basins water balance: the Nizhnedevitsk Water Balance Station case study / Sergei A. Zhuravin Water balances of experimental watersheds in the Valdai Branch of the State Hydrological Institute (SHI), Russia / J. A. Balonishnikova, O. I. Krestovsky & V. A. Shutov Extensive studies in boreal wetland watersheds in northwestern Russia / Vladimir A. Shutov Water balances of the northern catchments of Finland Pertti Seuna & Jarmo Linjama Water balance studies in two catchments on Spitsbergen, Svalbard / Ånund Killingtveit Estimation of water balance in and around the Mittivakkat Glacier basin, Ammassalik Island, southeast Greenland / Bent Hasholt & Sebastian H. Mernild Water balance in a west Greenlandic watershed Christian Helweg Queen Elizabeth Islands: water balance investigations / Kathy L. Young & Ming-Ko Woo Hydrological processes and water balance for the Dead Creek Watershed of southeastern Manitoba, 1982—1995 / Garry Thome & Janice Hawkins Evaporation studies in small NWT watersheds / Bob Reid & Derek Faria The water balance of wetland-dominated permafrost basins / W.L. Quinton, M. Hayashi, K. E. Blais, N. Wright & A. Peitroniro Wolf Creek Research Basin water balance studies / J. Richard Janowicz, Newell Hedstrom, John Pomeroy, Raoul Granger & Sean Carey A multi-year hydrological data set for two research basins in the Mackenzie Delta region, NW Canada / Philip Marsh, Cuyler Onclin & Mark Russell Water balance dynamics of three small catchments in a Sub-Arctic boreal forest / W. Robert Bolton, Larry Hinzman & Kenji Yoshikawa Hydrological cycle on the north slope of Alaska / Douglas L. Kane,Robert E. Gieck, Danielle C. Kitover, Larry D. Hinzman, James P. McNamara & Daqing Yang Queen Elizabeth Islands: problems associated with water balance research / Kathy L. Young & Ming-Ko Woo Winter streamflow as a source of uncertainty in water balance calculations / Stuart Hamilton Diagnostic model analysis of spatial mass, energy and melt distribution in a catchment in northeast Greenland / Carl Egede Boggild Key word index Author index
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  • 81
    facet.materialart.12
    Amsterdam : Elsevier Science/Butterworth-Heinemann
    Call number: 0750674571 (e-book)
    Description / Table of Contents: 'The Diversity Scorecard' is designed to provide step-by-step instructions, worksheets and examples to help diversity executives and managers analyze and track the impact of their diversity initiatives to mobilize the organization for strategic culture change. Diversity is not a program; it is a systemic process of organizational change that requires measurement for organizational improvement and success. Measuring the progress and results of diversity initiatives is a key strategic requirement to demonstrate its contribution to organizational performance. Diversity executives, professionals and managers know they must begin to show how diversity is linked to the bottom-line in hard numbers or they will have difficulty maintaining funds, gaining support, and obtaining resources to generate progress. Many organizations collect some type of diversity-related data today, even if it focuses only on Affirmative Action statistics. "The Diversity Scorecard" focuses on tools and techniques to make sure diversity professionals are collecting and measuring the right type of data that will help ensure the organization"s success both now and in the future. This book helps the reader spend some time thinking about what they currently measure and adding new measures to a database to track progress towards their diversity vision. The basic premises of this book are that it is important to develop measures that focus on the past, present, and future; and that measures need to consider the needs of the organization"s diverse workforce, its work climate, diverse customers, the community, and shareholders. Part I of "The Diversity Scorecard" identifies the need for diversity measurement highlighting a business case for diversity and providing an introduction to diversity measurement. Part II of the book outlines the diversity return on investment (DROI) process taking you through step-by-step processes and techniques. Part III teaches you how to use measures in six key categories - Diversity Leadership Commitment, Workforce Profile Representation, Workplace Climate, Learning & Growth, Diverse Customer / Community Partnerships, and Financial Impact - to build a diversity scorecard that is aligned and linked with the business strategy of the organization. Finally, in Part IV, Dr. Hubbard discusses implementation issues involving strategic change procedures and techniques to avoid the pitfalls inherent in a diversity-based cultural transition process.
    Type of Medium: 12
    Pages: xviii, 348 Seiten , Illustrationen
    Edition: Electronic reproduction. Ann Arbor, MI : ProQuest, 2015. Available via World Wide Web. Access may be limited to ProQuest affiliated libraries.
    ISBN: 1-4175-0785-3 , 978-1-4175-0785-6 , 0-7506-7457-1 , 978-0-7506-7457-7
    Series Statement: Improving human performance series
    Language: English
    Note: Contents Foreword Preface Acknowledgments Part I: The Need for Diversity Management Chapter 1 - The Business Case for Diversity Chapter 2 - Introduction to Diversity Measurement Part II: The Diversity Return-on-Investment (DROI) Process Chapter 3 - Introduction to the Diversity ROI Process Chapter 4 - Planning and Collecting Data Chapter 5 - Evaluating Diversity's Contribution Chapter 6 - Track and Assess Progress Part III: Building a Diversity Scorecard Chapter 7 - Basic Diversity Scorecard Components Chapter 8 - Diversity Leadership Commitment Perspective Chapter 9 - Workforce Profile Perspective Chapter 10 - Workplace Culture/Climate Perspective Chapter 11 - Learning and Growth Perspective Chapter 12 - Diverse Customer/Community Partnership Perspective Chapter 13 - Financial Impact Perspective Chapter 14 - Building Your Diversity Scorecard Part IV: Implementation Issues Chapter 15 - Achieving Strategic Alignment from Top to Bottom Chapter 16 - Implementing the Diversity Scorecard Process Appendix A - Hubbard Diversity Measurement and Productivity (DM&P) Institute: Creating Applied Sciences for Measuring Diversity Performance and Results Index About the Author
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  • 82
    Monograph available for loan
    Monograph available for loan
    River Edge, NJ : World Scientific
    Call number: 8/M 17.90372
    Description / Table of Contents: "Earthquakes and Animals places in front of the reader the simple laboratory evidence of the behavior of animals, plants and objects when they are subjected to intense electromagnetic pulses - of the kind created by rocks under stress before an earthquake. In many cases they behave in ways that have been recorded for centuries - and are still reported today - as earthquake-related." "Written for both the general public and scientists, Earthquakes and Animals demonstrates, using many experiments, that the old earthquake legends are probably rare natural phenomena. It also adds tantalisingly to the science of earthquake forecasting and cautiously suggests a legitimate new field of study - Electromagnetic Seismology."--BOOK JACKET
    Type of Medium: Monograph available for loan
    Pages: xix, 295 Seiten , Illustratione, Karten
    ISBN: 9812385916 (print) , 9789812385918 (print)
    Classification:
    Natural Disasters, Disaster Management
    Language: English
    Note: 1. Legends of unusual phenomena before earthquakeswisdom or superstition? -- 2. Precursors before recent earthquakes -- Kobe, Izmit, Taiwan and India -- 3. Earth sciences and electromagnetism -- 4. Unusual animal behavior : I -- what do they detect? -- electric field effects -- 5. Unusual animal behavior : II -- rock compression and increased animal activity -- 6. Unusual plant responses before earthquakes -- 7. Atmospheric precursors -- earthquake light, clouds, sun, moon, stars and rainbows -- 8. Precursor phenomena -- on land, sea and elsewhere -- 9. Mysteries before earthquakes : the behavior of electric appliances -- 10. Forecasting using animal monitoring -- 11. Monitoring seismo-electromagnetic signals (SEMS) -- a general survey -- 12. Summary..
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  • 83
    Monograph available for loan
    Monograph available for loan
    Ithaca [u.a.] : Cornell Univ. Press
    Call number: IASS 16.90576
    Type of Medium: Monograph available for loan
    Pages: XI, 226 S.
    ISBN: 0801488230 (pbk.) , 9780801488238 (pbk.) , 0801440904 (cloth)
    Language: English
    Branch Library: RIFS Library
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  • 84
    Monograph available for loan
    Monograph available for loan
    Dordrecht : Springer
    Call number: AWI A1-18-91447
    Type of Medium: Monograph available for loan
    Pages: XIII, 161 S , Ill., graph. Darst., Kt , 25 cm
    ISBN: 1402029403
    Uniform Title: Chikyū-ondanka-kenkyū-no-saizensen 〈engl.〉
    Language: English
    Note: Translated from the Japanese
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  • 85
    Call number: AWI E3-19-92148
    Description / Table of Contents: In this publication for the first time the scientific activities of the Russian researchers of Antarctica are reviewed and summarized, from the very first landing to the ice continent until the present time (1956-2004). Dozens of monographs and hundreds of articles regarding the climate of Antarctica, its geology, geophysics, biology, oceanology, glaciology, medicine, etc. disciplines are used and generalized. For use by the specialists working in the field of earth sciences and by the readers interested in polar research.
    Type of Medium: Monograph available for loan
    Pages: 303 Seiten , Illustrationen
    ISBN: 5-9584-0108-4
    Language: Russian , English
    Note: CONTENTS: From the author. - Foreword (V. M. Kotlyakov, the academician of Russian Academy of Science). - Introduction. - 1. A legal status of research in Antarctic. - 2. The Russian (Soviet) Antarctic expeditions. - 3. The first stage of the Russian Antarctic research (1956-1965). - 3.1. General characteristic of the first stage. - 3.2. Types of observations and research at the first stage of Soviet Antarctic expedition (SAE). - 3.3. Main scientific results of the first stage of SAE operation. - 4. The second stage of the Russian Antarctic Research (1966-1973). - 4.1. General characteristic of the second stage of SAE operation. - 4.2. Types of observations and research at the second stage of SAE operation. - 4.3. Main scientific results of the second stage of SAE operation. - 5. The third stage of the Russian Antarctic Research (1974-1990). - 5.1. General characteristic of the third stage of SAE operation. - 5.2. Types of observations and research at the third stage of SAE operation. - 5.3. Main basic scientific results ofthe third stage of SAE operation. - 6. The fourth stage of the Russian Antarctic Research (1991-2005). - 6.1. General characteristic of the fourth stage of Russian Antarctic expedition (RAE) operation. - 6.2. Types of observations and research at the fourth stage of RAE operation. - 6.3. Main scientific results of the fourth stage of RAE operation. - Conclusion. - References. - Appendices (1-8): Appendix 1. Chronology of RAE (SAE) operation. - Appendix 2. Number of native publications on various disciplines. - Appendix 3. Members of the Russian Antarctic expeditions. - Appendix 4. Number of RAE (SAE) wintering stations. - Appendix 5. Number of vessels operated in RAE (SAE). - Appendix 6. Volume of the cargo delivered by RAE (SAE) vessels. - Appendix 7. Wintering RAE (SAE) members. - Appendix 8. Photo portraits of the Russian Antarctic researchers. , In kyrillischer Schrift , Zusammenfassung in englischer Sprache
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  • 86
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Routledge
    Call number: PIK N 071-18-91872
    Type of Medium: Monograph available for loan
    Pages: XXIII, 216 Seiten
    ISBN: 0415302765 , 9780415302760
    Series Statement: Routledge research in environmental politics 5
    Language: English
    Location: A 18 - must be ordered
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  • 87
    Monograph available for loan
    Monograph available for loan
    Moskva : Institut Geografii RAN
    Call number: AWI G6-18-92021
    Type of Medium: Monograph available for loan
    Pages: 167 Seiten , Illustrationen
    ISBN: 5-89658-024-X
    Language: Russian , English
    Note: Contents: Introduction / V. I. Nikolaev. - Oxygen isotope composition of the bone phosphate of reindeer: potential as a palaeoenvironmental recorder / Vladimir Nikolaev, Silvana Davanzo, Antonio Longinelli, Paola Iacumin. - Carbon isotope studies of mammoth's food and fossil remains / Vladimir Nikolaev, Silvana Davanzo, Ludmila Kuznetsova, Paola Iacumin. - A fresh approach to palaeogeography of northern regions of West Siberia in sartan time (Late Pleistocene) / Dimitri Bolshiyanov, Vladimir Nikolaev, Alexander Sosnovskiy. - Relief and sediments forming of the Eastern Khibiny Mountains in the end of Late Pleistocene and Holocene / F. A. Romanenko, A. A. Lukashov, E. D. Sheremetskaya, Yu. R. Belyaev, N. E. Zaretskaya, D. K. Kuznetsov, O. S. Olyunina, A. M. Tarbeeva. , In kyrillischer Schrift
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  • 88
    Type of Medium: Non-book medium
    Pages: Online-Ressource
    Language: English
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  • 89
    Call number: PIK N 162-18-91347
    Type of Medium: Monograph available for loan
    Pages: XIII, 461 Seiten , Diagramme
    Edition: Reprinted
    ISBN: 9971501155 , 9971501163 , 9789971501167
    Series Statement: World scientific lecture notes in physics 9
    Language: English
    Note: Contents: Introduction ; Part 1 - Spin Glasses ; 1. The Replica Approach ; 2 The Tap Approach ; 3 Breaking the Replica Symmetry ; 4 The Nature of the Spin Glass Phase ; 5 The Cavity Method ; 6 Dynamics ; Part 2 - Optimization ; 7 Combinatorial Optimization Problems ; 8 Simulated Annealing ; 9 Analytical Results ; Part 3 - Biological Application ; 10 Introduction ; 11 Prebiotic Evolution and Spin ; 12 Brain Modelling ; 13 The Hopfield Model and its Variations
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  • 90
    Call number: M 19.92943
    Type of Medium: Dissertations
    Pages: ix, 192 Seiten , Illustrationen
    ISBN: 90-9018106-7
    Language: English
    Branch Library: GFZ Library
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  • 91
    Call number: M 19.92945
    Type of Medium: Dissertations
    Pages: xix, 152 Seiten , Illustrationen
    ISBN: 90-9018395-7
    Language: English
    Branch Library: GFZ Library
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  • 92
    Monograph available for loan
    Monograph available for loan
    Cambridge, Mass. [u.a.] : Harvard Univ. Press
    Call number: PIK B 100-20-94186
    Type of Medium: Monograph available for loan
    Pages: IX, 442 Seiten , Diagramme , 26 cm
    ISBN: 0674010736 (alk. paper)
    Language: English
    Location: A 18 - must be ordered
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  • 93
    Series available for loan
    Series available for loan
    Warszawa : Inst. Geofizyki Polskiej Akad. Nauk
    Associated volumes
    Call number: S 91.0236(B-34) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 207 S.
    ISBN: 8388765396
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 34 = 367 : monograph volume
    Classification:
    Seismology
    Language: English
    Location: Magazine - must be ordered
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  • 94
    Monograph available for loan
    Monograph available for loan
    Hoboken, NJ : Wiley
    Call number: AWI G3-04-0027
    Type of Medium: Monograph available for loan
    Pages: XII, 363 S. , Ill., graph. Darst., Kt.
    Edition: 2nd ed.
    ISBN: 0471615498
    Language: English
    Note: Contents: Preface. - Preface to the First Edition. - 1. Frozen Ground. - 1.1 Frozen Ground Support Systems. - 1.2 Seasonally and Perennially Frozen Ground. - 1.3 Terrain Features in Permafrost Areas. - 1.4 Engineering Considerations. - Problems. - 2. Physical and Thermal Properties. - 2.1 Composition and Structure of Frozen Ground. - 2.2 Soil Classification. - 2.3 Water-Ice Phase Relationships. - 2.4 Soil Frost Action. - 2.5 Thermal Properties. - Problems. - 3. Heat Flow in Soils. - 3.1 Heat Transfer at the Ground Surface. - 3.2 Seasonal Ground Freezing (or Thawing). - 3.3 Frost Protection and Thermal Insulation. - 3.4 Temperature Below Cooled (or Heated) Areas. - 3.5 Thermal Analysis: Frozen Ground Support Systems. - Problems. - 4. Thaw Behavior of Frozen Ground. - 4.1 Thaw Settlement. - 4.2 Consolidation of Thawing Soils. - 4.3 Thaw Consolidation in Some Layered Systems. - Problems. - 5. Mechanical Properties of Frozen Soils. - 5.1 Stress-Strain-Time and Strength Behavior. - 5.2 Factors Influencing Creep and Strength. - 5.3 Analytical Representation of Creep and Strength Data. - 5.4 Frozen Soil Behavior in Uniaxial Tension. - 5.5 Deformability of Frozen Soils. - 5.6 Compressibility of Frozen Soils. - 5.7 Frozen Ground sensitivity to Climate Change. - 5.8 Frozen Soil Creep and Strength: Generalization of Test Data. - Problems. - 6. Construction Ground Freezing. - 6.1 Design Considerations. - 6.2 Freezing Methods and System Installation. - 6.3 Structural Design of Frozen Earth Walls. - 6.4 Monitoring Requirements. - 6.5 Other Construction Considerations. - Problems. - 7. Foundations in Frozen Soils. - 7.1 General Considerations. - 7.2 Shallow Foundations. - 7.3 Pile Foundations. - 7.4 Frost Heave Forces on Foundations. - 7.5 Frost Protection of Foundations Using Ground Insulation. - Problems. - 8. Stability of Soil Masses in Cold Regions. - 8.1 Landslides in Permafrost: Classification. - 8.2 Slopes in Thawing Permafrost. - 8.3 Slopes in Frozen Soils. - 8.4 Monitoring Creep in Frozen Slopes. - 8.5 Slope Stabilization Methods. - Problems. - 9. Earthwork in Cold Regions. - 9.1 Site Considerations. - 9.2 Excavation and Transport. - 9.3 Field Placement. - 9.4 Water-Retaining Embankments on Permafrost. - 9.5 Embankment Performance. - 10. Field Investigations. - 10.1 Sampling Frozen Ground. - 10.2 Ground-Temperature Measurement. - 10.3 Field Testing of Frozen Soils. - 10.4 Geophysical Methods. - 11. Pavement Structures. - 11.1 Seasonal Frost Areas. - 11.2 Permafrost Areas. - 11.3 Highway Insulation. - 11.4 Load Restrictions. - 11.5 Special Problems. - Problems. - Appendix A. Notation. - Symbols. - Greek Symbols. - Subscripts. - Appendix B. SI Units. - SI Base Units. - SI Prefixes. - SI Derived Units. - Conversion Factors. - Appendix C. Laboratory and Field Tests on Frozen Soils. - C.1 Handling, Storage, and Machining of Specimens Prior to Testing. - C.2 Uniaxial Compression Test. - C.3 Uniaxial Tensile Test. - C.4 Salinity of Soil Pore Water. - C.5 Thermosiphon. - C.6 Pile Load Test in Permafrost. - C.7 Hydraulic Conductivity of Frozen Soils. - References. - Author Index. - Subject Index.
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  • 95
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 11/M 04.0178
    In: Rock-forming minerals
    Type of Medium: Monograph available for loan
    Pages: XX, 758 S.
    Edition: 2nd ed.
    ISBN: 1862391424
    Classification:
    Mineralogy
    Language: English
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  • 96
    Call number: AWI G4-04-0032
    In: The lakes handbook, Volume 1
    Type of Medium: Monograph available for loan
    Pages: VI, 699 Seiten , Illustrationen
    Edition: first published
    ISBN: 0632047976
    Language: English
    Note: Contents: List of contributors. - 1. Lakes, limnology and limnetic ecology: towards a new synthesis. - 2. The origin of lake basins. - 3. The hydrology of lakes. - 4. Chemical processes regulating the composition of lake waters. - 5. Physical properties of water relevant to limnology and limnetic ecology. - 6. The motion of lake waters. - 7. Regulatory impacts of humic substances in lakes. - 8. Sedimentation and lake sediment formation. - 9. Organisation and energetic partitioning of limnetic communities. - 10. Phytoplankton. - 11 Aquatic plants and lake ecosystems. - 12. Benthic invertebrates. - 13. Pelagic microbes - protozoa and the microbial food web. - 14. Zooplankton. - 15. Fish population ecology. - 16. Fish community ecology. - 17. Self-regulation of limnetic ecosystems. - 18. Palaeolimnology. - Index.
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  • 97
    Keywords: DDC 512/.22 ; LC QC20.7.S54 ; Biology - Mathematical models ; Chaotic behavior in systems ; Dynamics - Mathematical models ; Singularities (Mathematics) ; Stochastic systems
    Pages: Online-Ressource (xiv, 237 pages)
    Edition: 1st ed
    ISBN: 9780444516138
    Language: English
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  • 98
    Keywords: DDC 519.6 ; LC QA402.5 ; Mathematical optimization ; Nonlinear programming
    Pages: Online-Ressource (xv, 598 pages)
    ISBN: 9781435687080
    Language: English
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  • 99
    Unknown
    Amsterdam ; Boston : Elsevier
    Keywords: DDC 006.3 ; LC Q339.2 ; Algebraic logic ; Modality (Logic) ; Nonmonotonic reasoning ; Semantics - Mathematical models
    Pages: Online-Ressource (xx, 447 pages)
    ISBN: 9780444517890
    Language: English
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  • 100
    Description / Table of Contents: District heating can make a substantial contribution to a sustainable energy future in Central Europe and the former Soviet Union. It is a critical energy source for countries in transition, covering 60 percent of heating and hot water needs. These systems can save energy and boost energy security, but a stronger policy framework is needed to encourage wise management and investment. With such a framework, district heating systems in former Socialist countries could save the equivalent of 80 billion cubic meters of natural gas a year through generation improvements alone. This is roughly the annual natural gas consumption in Germany. Reforming district heating is also essential for social reasons in cold countries in transition. District heating companies need to become more customer-oriented. Policy makers can help propel them in this direction either through new market mechanisms or an improved regulatory framework. Coming in from the Cold: Improving District Heating Policy in Transition Economies provides policymakers with a guide to key district heating issues. Countries need a clear policy on district heating, given the significant economic, social and environmental implications of this sector. This is true for IEA member and non-member countries alike if they are to improve their heat supply.
    Pages: Online-Ressource (262 Seiten)
    ISBN: 926410819X
    Language: English
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