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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Paleoclimatology--Holocene. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (494 pages)
    Edition: 1st ed.
    ISBN: 9783662103135
    Series Statement: GKSS School of Environmental Research Series
    DDC: 551.6/09/01
    Language: English
    Note: GKSS School of Environmental Research -- The Climate in Historical Times -- Copyright -- Preface -- Contents -- List of Contributors -- 1 The Holocene: Considerations with Regard to its Climate and Climate Archives -- 2 Nonlinear Dynamics of the Climate System -- 3 A Discourse About Quasi-realistic Climate Models and Their Applications in Paleoclimatic Studies -- 4 Holocene Climate Variability from Model Simulations - State of the Art -- 5 Marine Paleoclimatology - Motivation, Tools, and Results -- 6 Corals as Climate Archive -- 7 Annually Laminated Lake Sediments and Their Palaeoclimatic Relevance -- 8 Interpreting Climate Proxies from Tree-rings -- 9 The Environmental and Climate Record in Polar Ice Cores -- 10 Reconstructing Large-scale Variability from Palaeoclimatic Evidence by Means of Data Assimilation Through Upscaling and Nudging (DATUN) -- 11 Mid- to Late Holocene Lake Ecosystem Response to Catchment and Climatic Changes- A Detailed Varve Analysis of Lake Holzmaar(Germany) -- 12 Holocene Palaeoclimate in the Saharo-ArabianDesert -- 13 Transfer Functions for PaleoclimateReconstructions - Theory and Methods -- 14 Transfer Functions for Paleoclimate Reconstructions - Applications -- 15 Climate Information from Stable Hydrogenand Carbon Isotopes of C3 Plants - GrowthChamber Experiments and Field Observations -- 16 Detection of Climate Modes as Recorded in a Seasonal-resolution Coral Record Covering the Last 250 Years -- 17 Phase Stability of the Solar Schwabe Cycle in Lake Holzmaar, Germany, and G ISP2, Greenland, between 10,000 and 9,000 cal. BP -- 18 Variable Freshwater Input to the Arctic Ocean During the Holocene: Implications for Large-Scale Ocean-Sea Ice Dynamics as Simulated by a Circulation Model -- 19 Forced Climate Variability During the Last Millennium with the Earth System Model CLIMBER-2. , 20 The Contribution of High-resolution Magnetostratigraphic Analyses to Paleoclimatic Reconstructions -- 21 Internal Climate Variability in Global and Regional Climate Models -- 22 Climate Diagnostics by Adjoint Modelling: A Feasibility Study -- 23 Evidence for the Climate During the Late Maunder Minimum from Proxy Data and Model Simulations Available Within KIHZ -- References -- Index.
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  • 2
    Keywords: climate ; Antarctica
    In: Deutsche Bahn AG, DB mobil, Hamburg : G+J Corporate Media GmbH, 1999, (2003), 3, Seite 70-75, 2510-5418
    In: year:2003
    In: number:3
    In: pages:70-75
    Description / Table of Contents: Im Eispanzer der Antarktis schlummert das Klimaarchiv der Erde. Aus dem Schnee von gestern ziehen die Eisforscher des Alfred-Wegener-Insituts in Bremerhaven Schlüsse auf das Weltklima von morgen
    Type of Medium: Article
    Pages: Ill., Kt
    ISSN: 2510-5418
    Language: Undetermined
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  • 3
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    International Glaciological Society
    In:  EPIC3International Symposium on Ice Cores and Climate, Kangerlussuaq, Hotel and Conference Center, 2001-08-19-2001-08-23Kangerlussuaq, Greenland, International Glaciological Society
    Publication Date: 2018-09-18
    Description: The paper presents first results from the upper 54 m of a 723.91 m ice core drilled on Academy of Sciences Ice Cap in 1999-2001, supplemented by data from shallow ice cores. The glacier's peculiarity is the infiltration and refreezing of melting water thereby changing original isotopic and chemical signals. Therefore, stratigraphical observations in these ice cores are more difficult than in those from central Greenland or Antarctica. However, the 1963 maximum of artificial radioactivity from atmospheric nuclear tests is clearly detectable in the deep ice core and the d180 profile of a 12.82 m shallow core shows annual variations. Consequently, an almost seasonal time resolution of paleoclirnate record could be expected at least for the upper part of the main core. The Chemobyl layer was detected by increased 137 Cs activity in depths between 11.81 m and 12.51 m related to the 2000 surface. The resulting mean annual net mass balance is 53 ± 2 g cm-2 a- 1. Data from dielectric profiling (DEP) of the main core show considerable peaks in conductivity; one of them was interpreted as volcano event. According to the resulting chronology this part of the core represents approximately the last 100 years.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 4
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    INT GLACIOL SOC
    In:  EPIC3Annals of Glaciology, INT GLACIOL SOC, 37, pp. 207-212, ISSN: 0260-3055
    Publication Date: 2017-12-11
    Description: From temperature measurements down through the 3001 m deep borehole at the North Greenland Icecore Project (NorthGRIP) drill site, it is now clear that the ice at the base, 3080 m below the surface, is at the pressure-melting point. This is supported by the measurements on the ice core where the annual-layer thicknesses show there is bottom melting at the site and upstream from the borehole. Surface velocity measurements, internal radio-echo layers, borehole and ice-core data are used to constrain a time-dependent flow model simulating flow along the north-northwest-trending ice-ridge flow-line, leading to the NorthGRIP site. Also time-dependent melt rates along the flowline are calculated with a heat-flow model. The results show the geothermal heat flow varies from 50 to 200 mW m–2 along the 100km section of the modeled flowline. The melt rate at the NorthGRIP site is 0.75 cm a–1, but the deep ice in the NorthGRIP core originated 50 km upstream and has experienced melt rates as high as 1.1 cm a–1.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
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    International Workshop Ice Drilling Technology 2000
    In:  EPIC35th International Workshop Ice Drilling Technology 2000, Nagaoka, 2000-10-30-2000-11-01Nagaoka University of Technology, Japan, International Workshop Ice Drilling Technology 2000
    Publication Date: 2018-09-10
    Description: In May 1999, drilling of a borehole through the entire ice strata (around 750 m) was initiated on the Akademiya Nauk glacier of Komsomolets Island, Severnaya Zemlya Archipelago. The Arctic and Antarctic Research Institute (AARI), St. Petersburg Mining Institute (SPMI) and Alfred Wegener Institute (AWI, Germany) take part in this venture. For undertaking drilling activities, a dismantling drilling complex was designed and manufactured at SPMI by request of AWI. It includes a drilling house, land drilling equipment and two sets of the electromechanical drill KEMS-127 that also allows drilling of subglacial mountain rocks. The core has a maximum length of 1.5 m and a diameter of 106 mm. Drilling started in spring of 1999 and 54 m was drilled. In April 2000, the borehole drilling was continued. Up to a depth of 109 m, a "dry" method was used. Then the borehole was filled with aviation kerosene TS-1. By the end of seasonal work (May 9, 2000), the borehole bottom reached a depth of 504.7 m. After the drilling was stopped, a complex of geophysical observations was carried out that included measurements of the borehole diameter, the axis deviation angle from the vertical, temperature at different depths and drilling fluid pressure. An analysis of the data obtained allows a conclusion about the reliability and stability of the drilling technology and equipment and developing recommendations to continue drilling that is planned to do during 2001 season.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 6
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 7
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 8
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    In:  EPIC3Geophysical Research Letters, 28(8), pp. 1499-1502, ISSN: 0094-8276
    Publication Date: 2019-12-03
    Description: It has been shown that NOx is produced photochemically within the snowpack of polar regions. If emitted to the atmosphere, this processcould be a major source of NOx in remote snowcovered regions. We report here on measurements made at the German Antarctic station,Neumayer, during austral summer 1999, aimed at detecting and quantifying emissions of NOx from the surface snow. Gradients of NOxwere measured, and fluxes calculated using local meteorology measurements. On the 2 days of flux measurements, the derived fluxesshowed continual release from the snow surface, varying between similar to0 and 3x10(8) molecs/cm(2)/s. When not subject toturbulence, the variation was coincident with the uv diurnal cycle, suggesting rapid release once photochemically produced. Scaling thediurnal average of Feb. 7th (1.3x10(8) molecs/cm(2)/s) suggests an annual emission over Antarctica of the order 0.0076TgN.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 9
    Publication Date: 2019-07-16
    Description: Microstructure and thermal evolution of sea-ice brine inclusions were investigated with magnetic resonance imaging (MRI) techniques. Ice samples were kept at temperatures between -2°C and -25°C during 1H imaging in a 4.7-T magnet at 200 MHz. Measurements were completed in a 20-cm diameter cylindrical probe and actively shielded gradient coils (max. 50 mT m-1, pixel dimensions 〉0.2 mm, slice thicknesses 〉1 mm), and for higher resolution in a mini-imaging unit with a 9-cm diameter probe with gradient coils of 200 mT m-1 (pixel dimensions 〈0.1 mm, slicethickness 〈0.4 mm). Absorption of radio-frequency (RF) signals in the dielectrically lossy brine resulted in degraded signals and was alleviated by use of a contrast agent (decane). MRI data and sea-ice thin section images agree very well (〈5% deviation for pore microstructural parameters). Analysis of ice grown under different current speeds indicates that pores are smaller and pore number densities larger at higher current speeds. The thermal evolution of fluid inclusions was studied on cold first-year ice samples, maintained at close to in-situ temperatures prior to experiments. Warming from -21°C to -10°C to -6°C is associated with a distinct increase in pore size (from 1.5 to 1.7 to 2.6 mm forthe upper 10-percentile in the vertical) and elongation (4.0 to 4.2 to 6.2 for ratio of major to minor pore axes in the vertical) and a decrease in number densities (0.75 to 0.62 to 0.58 mm-3 in the vertical). Aspect ratios increased from 4:2:1 to 6:2:1 (upper 10-percentile), indicating expansion and merging of pores in the vertical, possibly promoted by microscopic residual brine inclusions.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 10
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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