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  • 1
    Call number: 9/M 07.0421(380)
    In: Geological Society special publication
    Description / Table of Contents: Volcanoes have played a profound role in shaping our planet, and volcanic activity is a major hazard locally, regionally and globally. Many volcanoes are, however, poorly accessible and sparsely monitored. Consequently, remote sensing is playing an increasingly important role in tracking volcano behaviour, while synoptic remote sensing techniques have begun to make major contributions to volcanological science. Volcanology is driven in part by the operational concerns of volcano monitoring and hazard management, but the goal of volcanological science is to understand the processes that underlie volcanic activity. This volume shows how we may reach a deeper understanding by integrating remote sensing measurements with modelling approaches and, if available, ground-based observations. It includes reviews and papers that report technical advances and document key case studies. They span a range of remote sensing applications to volcanoes, from volcano deformation, thermal anomalies and gas fluxes, to the tracking of eruptive ash and gas plumes. The result is a state-of-the-art overview of the ever-growing importance of remote sensing to volcanology.
    Type of Medium: Monograph available for loan
    Pages: 362 S. : z.T. farb. Ill., graph. Darst.
    ISBN: 9781862393622
    Series Statement: Geological Society special publication 380
    Classification:
    Photogrammetry, Remote Sensing
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 03.0557
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 420 S.
    ISBN: 186239136X
    Series Statement: Geological Society special publication 213
    Classification:
    Petrology, Petrography
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Publication Date: 2024-04-16
    Keywords: Abrupt Climate Changes and Environmental Responses; Accumulation model; ACER; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Charcoal; Classical age-modeling approach, CLAM (Blaauw, 2010); DEPTH, sediment/rock; Megali_Limni; Sample ID; Type of age model; Unit
    Type: Dataset
    Format: text/tab-separated-values, 676 data points
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  • 4
    Publication Date: 2024-04-16
    Keywords: Abies; Abrupt Climate Changes and Environmental Responses; Accumulation model; Acer; ACER; Alnus; Apiaceae; Armeria; Artemisia; Asteraceae; Betula; Brassicaceae; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Campanula; Carpinus betulus; Carpinus orientalis/Ostrya; Caryophyllaceae; Castanea; Centaurea; cf. Asphodelus albus; cf. Cephalanthera; cf. Echium; cf. Hypecoum; cf. Hypericum; cf. Iris; cf. Linum; cf. Saxifraga stellaris; Chenopodiaceae; Cistus; Classical age-modeling approach, CLAM (Blaauw, 2010); Convolvulus; Corylus; Counting, palynology; Cyperaceae; DEPTH, sediment/rock; Dipsacaceae; Dryopteris; Ephedra distachya-type; Ephedra fragilis-type; Ericaceae; Euphorbiaceae; Fagus; Filipendula; Fraxinus; Gentianaceae; Hedera helix; Helianthemum; Hippophae; Ilex; Indeterminable; Juniperus; Knautia; Lamiaceae; Leguminosae; Lemna; Ligustrum; Liliaceae; Lycopodium; Lythrum; Megali_Limni; Mentha-type; Moraceae; Myriophyllum; Myrtus; Nuphar; Nymphaea alba-type; Olea; Papaveraceae; Phillyrea; Pinus; Plantago; Poaceae; Polygonum; Polypodiales; Polypodium; Potamogeton; Primulaceae; Quercus; Ranunculus; Rhamnaceae; Rosaceae; Rubiaceae; Rumex; Salix; Sample ID; Sanguisorba; Saxifragaceae; Scrophulariaceae; Sparganium; Thalictrum; Tilia cordata; Type of age model; Typha latifolia-type; Ulmus; Urtica; Utricularia; Valerianaceae
    Type: Dataset
    Format: text/tab-separated-values, 22125 data points
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 362 (1993), S. 787-788 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] THE development of successful models for predicting volcanic eruptions hinges on answering two questions: how long do volcanoes live, and how much magma do they store? On page 831 of this issue1, Chen and colleagues report the discovery of a correlation between lava chemistry and eruption volume at ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillan Magazines Ltd.
    Nature 393 (1998), S. 415-417 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The summer of 1601 was, by all accounts, truly awful. Across England, “the month of June was very colde, frosts every morning”. It was a similar story in northern Italy, where freezing weather extended into July, and the sky was ‘overcast’ for much of the year. Iceland and ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 378 (1995), S. 134-135 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] TWICE this century, large towns have been laid waste in minutes by volcanic eruptions. The fifty thousand resulting deaths in St Pierre, Martinique, and Armero, Colombia, account for over two-thirds of volcano-related deaths since 1900, and give an indication of the potent volcanic threat to the ...
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 51 (1989), S. 1-15 
    ISSN: 1432-0819
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract An improved empirical method for the plotting of field data and the calculation of tephra fall volumes is presented. The widely used “area” plots of ln(thickness) against ln(isopach area) are curved, implying an exponential thinning law. Use of ln(thickness)−(area)1/2 diagrams confirm the exponential dependence of many parameters (e.g. thickness, maximum and median clast size) with distance from source, producing linear graphs and allowing volumes to be calculated without undue extrapolation of field data. The agreement between theoretical models of clast dispersion and observation is better than previously thought. Two new quantitative parameters are proposed which describe the rates of thinning of the deposit (b t the thickness half-distance) and the maximum clast size (b c the clast half-distance). Many deposits exhibit different grainsize and thickness thinning rates, with the maximum clast size diminishing 1–3 times slower than the thickness. This implies that the entrained grainsize population influences the morphologic and granulometric patterns of the resulting deposit, in addition to the effects of column height and wind-speed. The grainsize characteristics of a deposit are best described by reference to the half-distance ratio (b c /b t ). A new classification scheme is proposed which plots the half-distance ratio against the thickness half-distance and may be contoured in terms of the column height.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 57 (1996), S. 663-671 
    ISSN: 1432-0819
    Keywords: Key words Volcano-climate interaction ; Stratospheric sulphur ; Holocene ice-core records
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Two methods were used to quantify the flux of volcanic sulphur (as the equivalent mass of SO2) to the stratosphere over different timescales during the Holocene. A combination of satellite-based measurements of sulphur yields from recent explosive volcanic eruptions with an appropriate rate of explosive volcanism for the past 200 years constrains the medium-term (∼102 years) flux of volcanic sulphur to the stratosphere to be ∼1 Mt a–1, with lower and upper bounds of 0.3 and 3 Mt a–1. The short-term (∼10- to 20-year) flux due to small magnitude (1010–1012 kg) eruptions is of the order of 0.4 Mt a–1. At any time the instantaneous levels of sulphur in the stratosphere are dominated by the most recent (0–3 years) volcanic events. The flux calculations do not attempt to address this very short timescale variability. Although there are significant errors associated with the raw sulphur emission data on which this analysis is based, the approach presented is general and may be readily modified as the quantity and quality of the data improve. Data from a Greenland ice core support these conclusions. Integration of the sulphate signals from presumed volcanic sources recorded in the GISP2 core provides a minimum estimate of the 103–year volcanic SO2 flux to the stratosphere of 0.5–1 Mt a–1 over the past 9000 years. The short-term flux calculations do not account for the impact of rare, large events. The ice-core record does not fully account for the contribution from small, frequent events.
    Type of Medium: Electronic Resource
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  • 10
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