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  • 1
    UID:
    kobvindex_GFZ91646
    Format: 231 Seiten , Illustrationen
    ISSN: 1618-3193
    Series Statement: Berichte zur Polar- und Meeresforschung 489
    Note: MAB0014.001: ZSP-168-489 , MAB0014.002: ZS-090(489) , 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
    In: Berichte zur Polar- und Meeresforschung, 489
    Language: English
    Keywords: Aufsatzsammlung
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  • 2
    UID:
    gbv_599585196
    Format: graph. Darst
    ISSN: 1879-0119
    Content: Inflow of Atlantic water (AW) from Fram Strait and the Barents Sea into the Arctic Ocean conditions the intermediate (100-1000 m) waters of the Arctic Ocean Eurasian margins. While over the Siberian margin the Fram Strait AW branch (FSBW) has exhibited continuous dramatic warming beginning in 2004, the tendency of the Barents Sea AW branch (BSBW) has remained poorly known. Here we document the contrary cooling tendency of the BSBW through the analysis of observational data collected from the icebreaker Kapitan Dranitsyn over the continental slope of the Eurasian Basin in 2005 and 2006. The CTD data from the R.V. Polarstern cruise in 1995 were used as a reference point for evaluating external atmospheric and sea-ice forcing and oxygen isotope analysis. Our data show that in 2006 the BSBW core was saltier (by ~0.037), cooler (~0.41 ʿC), denser (by ~0.04 kg/m3), deeper (by 150-200 m), and relatively better ventilated (by 78 mymol/kg of dissolved oxygen, or by 1.11.7% of saturation) compared with 2005. We hypothesize that the shift of the meridional wind from off-shore to on-shore direction during the BSBW translation through the Barents and northern Kara seas results in longer surface residence time for the BSBW sampled in 2006 compared with samples from 2005. The cooler, more saline, and better-ventilated BSBW sampled in 2006 may result from longer upstream translation through the Barents and northern Kara seas where the BSBW was modified by sea-ice formation and interaction with atmosphere. The data for stable oxygen isotopes from 1995 and 2006 reveals amplified brine modification of the BSBW core sampled downstream in 2006, which supports the assumption of an increased upstream residence time as indicated by wind patterns and dissolved oxygen values.
    In: Deep-sea research. Part 1, Oceanographic research papers, Amsterdam [u.a.] : Elsevier Science, 1993, 56(2009), 4, Seite 513-527, 1879-0119
    In: volume:56
    In: year:2009
    In: number:4
    In: pages:513-527
    Language: English
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  • 3
    UID:
    gbv_092357776
    In: Russian-German cooperation, Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 1995
    Language: English
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  • 4
    UID:
    gbv_609543792
    Format: 19 , graph. Darst
    ISSN: 2169-9291
    Content: Through the analysis of observational mooring data collected at the northeastern Laptev Sea continental slope in 2004-2007, we document a hydrographic seasonal signal in the intermediate Atlantic Water (AW) layer, with generally higher temperature and salinity from December-January to May-July and lower values from May-July to December-January. At the mooring position, this seasonal signal dominates, contributing up to 75% of the total variance. Our data suggest that the entire AW layer down to at least 840 m is affected by seasonal cycling, although the strength of the seasonal signal in temperature and salinity reduces from 260 m (±0.25ʿC and ±0.025 psu) to 840 m (±0.05ʿC and ±0.005 psu). The seasonal velocity signal is substantially weaker, strongly masked by high-frequency variability, and lags the thermohaline cycle by 45-75 days. We hypothesize that our mooring record shows a time history of the along-margin propagation of the AW seasonal signal carried downstream by the AW boundary current. Our analysis suggests that the seasonal signal in the Fram Strait Branch of AW (FSBW) at 260 m is predominantly translated from Fram Strait, while the seasonality in the Barents Sea branch of AW (BSBW) domain (at 840 m) is attributed instead to the seasonal signal input from the Barents Sea. However, the characteristic signature of the BSBW seasonal dynamics observed through the entire AW layer leads us to speculate that BSBW also plays a role in seasonally modifying the properties of the FSBW.
    In: Journal of geophysical research. C, Oceans, Hoboken, NJ : Wiley, 1978, 114(2009), 6, 2169-9291
    In: volume:114
    In: year:2009
    In: number:6
    In: extent:19
    Language: English
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