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  • 1
    facet.materialart.12
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    Russian-German Cooperation SYSTEM LAPTEV SEA [Elektronische Ressource] : the expedition Lena 2009 (2009)
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    Associated volumes
    Details Availability
    Call number: ZSP-168-600
    In: Berichte zur Polar- und Meeresforschung
    Description / Table of Contents: This report summarizes activities and field work results of the joint Russian-German expedition "Lena 2009". The 11th expedition to the Lena River Delta is part of the Russian-German science cooperation "System Laptev Sea" and continues the long-term investigations of permafrost and periglacial environmentsi n Arctic Siberia. [...] The expedition took place during the period June 24 to August 26, 2009 in different regions. The study areas comprise (i) the central Lena River Delta, with the Russian German station on Samoylov as base camp (ii) a north-south transect extending from the western part of the lower Lena River into the Lena Delta (realized by helicopter) and (iii) the eastern part of the delta (realized by riverboat).
    Type of Medium: 12
    Pages: Online-Ressource
    ISSN: 1866-3192
    Series Statement: Berichte zur Polar- und Meeresforschung 600
    URL: http://hdl.handle.net/10013/epic.33540
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
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    Physical oceanography during POLARSTERN cruise ARK-IX/3 (2010)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2023-03-17
    Keywords: ARK-IX/3; AWI_PhyOce; Calculated; Calculated from conductivity; Chlorophyll fluorescence, Dr. Haardt Instruments; Chlorophyll fluorescence raw data; Computed; CTD, Sea-Bird, SBE 911plus [SN: 0485]; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; MULT; Multiple investigations; Northeast Water Polynya; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS26/109-0; PS26/109-1; PS26/110-0; PS26/110-1; PS26/111-0; PS26/112-0; PS26/113-0; PS26/114-0; PS26/115-0; PS26/115-1; PS26/115-2; PS26/116-0; PS26/117-0; PS26/118-0; PS26/119-0; PS26/119-1; PS26/119-2; PS26/120-0; PS26/121-0; PS26/121-1; PS26/122-0; PS26/123-0; PS26/124-0; PS26/125-0; PS26/126-0; PS26/127-0; PS26/128-0; PS26/129-0; PS26/130-0; PS26/130-1; PS26/131-0; PS26/132-0; PS26/133-0; PS26/134-0; PS26/134-1; PS26/135-0; PS26/135-1; PS26/136-0; PS26/136-1; PS26/137-0; PS26/137-1; PS26/138-0; PS26/138-1; PS26/138-2; PS26/139-0; PS26/140-0; PS26/140-1; PS26/140-2; PS26/141-0; PS26/141-1; PS26/142-0; PS26/142-1; PS26/143-0; PS26/143-2; PS26/144-0; PS26/144-1; PS26/145-0; PS26/145-1; PS26/145-2; PS26/146-0; PS26/147-0; PS26/148-0; PS26/149-0; PS26/150-0; PS26/151-0; PS26/152-0; PS26/153-0; PS26/154-0; PS26/155-0; PS26/155-1; PS26/155-2; PS26/156-0; PS26/157-0; PS26/158-0; PS26/159-0; PS26/160-0; PS26/161-0; PS26/162-0; PS26/163-0; PS26/165-0; PS26/165-1; PS26/165-2; PS26/166-0; PS26/167-0; PS26/168-0; PS26/168-1; PS26/169-0; PS26/170-0; PS26/171-0; PS26/172-0; PS26/173-0; PS26/175-0; PS26/176-0; PS26/177-0; PS26/178-0; PS26/179-0; PS26/179-1; PS26/179-2; PS26/180-0; PS26/181-0; PS26/182-0; PS26/182-1; PS26/183-1; PS26/184-0; PS26/185-0; PS26/186-0; PS26/186-1; PS26/187-0; PS26/188-0; PS26/189-0; PS26/189-1; PS26/190-0; PS26/191-0; PS26/192-0; PS26/192-1; PS26/193-0; PS26/194-0; PS26/195-0; PS26/196-0; PS26/196-1; PS26/197-0; PS26/198-0; PS26/199-0; PS26/200-0; PS26/201-0; PS26/202-0; PS26/203-0; PS26/204-0; PS26/205-0; PS26/206-0; PS26/206-1; PS26/207-0; PS26/208-0; PS26/209-0; PS26/210-0; PS26/211-0; PS26/212-0; PS26/213-0; PS26/214-0; PS26/215-0; PS26/216-0; PS26/217-0; PS26/217-1; PS26/217-2; PS26/218-0; PS26/219-0; PS26/220-0; PS26/221-0; PS26/221-1; PS26/222-0; PS26/223-0; PS26/223-1; PS26/224-0; PS26/225-0; PS26/226-0; PS26/226-1; PS26/227-0; PS26/228-0; PS26/229-0; PS26/229-1; PS26/231-0; PS26/232-0; PS26/233-0; PS26/234-0; PS26/235-0; PS26/236-0; PS26/237-0; PS26/238-0; PS26/240-0; PS26/241-0; PS26/242-0; PS26/243-0; PS26/244-0; PS26/245-0; PS26/246-0; PS26/247-0; PS26/248-0; PS26/249-0; PS26/250-0; PS26/251-0; PS26/252-0; PS26/253-0; PS26/254-0; PS26/257-0; PS26/258-0; PS26/259-0; PS26/260-0; PS26/261-0; PS26/262-0; PS26/263-0; PS26/264-0; PS26/265-0; PS26/266-0; PS26/267-0; PS26/271-0; PS26/272-0; PS26/273-0; PS26/279-2; PS26 NEW; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 260636 data points
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  • 3
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    Geometric parameters of shoreface profiles of Laptev Sea erosion coast (Table 1)
    PANGAEA
    In:  Supplement to: Are, Felix; Grigoriev, Mikhail N; Hubberten, Hans-Wolfgang; Rachold, Volker; Razumov, Sergey O; Schneider, Waldemar (2002): Comparative shoreface evolution along the Laptev Sea coast. Polarforschung, 70, 135-150, hdl:10013/epic.29866.d001
    Details
    Publication Date: 2023-05-12
    Description: Field investigations of the Laptev Sea shoreface morphology were carried out (1) off erosional shores composed of unconsolidated sediments, (2) off the modern delta shores of the Lena River, and (3) off rocky shores. It was found that profiles off erosional shores had a concave shape. This shape is not well described by commonly applied power functions, a feature, which is in disagreement with the generally accepted concept of the equilibrium shape of shoreface profiles. The position of the lower shoreface boundary is determined by the elevation of the coastal lowland inundated during the last transgression (at -5 to -10 m) and may easily be recognized by a sharp, an order of magnitude decrease in the mean inclination of the sea floor. The mean shoreface inclination depends on sediment grain-size and ranges from 0.0022 to 0.033. The concave shape of the shoreface did not change substantially during the last 20-30 years, which indicates that shoreline retreat did not slow down and hence suggests continued intensive coastal erosion in the 21st century. The underwater part of the Lena River delta extends up to 35 km offshore. Its upper part is formed by a shallow and up to 18-km wide bench, which reaches depths of 2-3 m along the outer edge. The evolution of the delta was irregular. Whereas some parts of the delta are advancing rapidly (58 m/year), other parts are eroding. Comparison of measured profiles with older bathymetric data gave an opportunity to evaluate the changes of the underwater delta over past decades. Bathymetric surveys of the seabed around the delta can thus contribute towards a quantification of the sediment budget of the river-sea system. In addition, some sections of the Laptev Sea coast are composed of bedrock that has a comparatively low resistance to wave erosion. These sections may supply a considerable amount of sediment, especially if the cliffs are high. This source must therefore also be taken into account when assessing the contribution of shore erosion to the Laptev Sea sediment budget.
    Keywords: Area/locality; Inclination; Laptev Sea System; LATITUDE; Lithology/composition/facies; LONGITUDE; LSS; Measured; Shoreface depth; Visual description; Width
    Type: Dataset
    Format: text/tab-separated-values, 104 data points
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  • 4
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    Digital Elevation Model of Samoylov Island, Lena River Delta, Siberia, Russia, with link to ArcGIS files (2012)
    PANGAEA
    Details
    Publication Date: 2024-01-18
    Keywords: Arctic; Arctic Tundra; AWI_PerDyn; Digital Elevation/Digital Terrain Models; island; MULT; Multiple investigations; Permafrost Research (Periglacial Dynamics) @ AWI; river delta; Samoylov_Island; Samoylov Island, Lena Delta, Siberia
    Type: Dataset
    Format: application/zip, 126.1 kBytes
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  • 5
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    Physical oceanography during POLARSTERN cruise ARK-IX/2 (2010)
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Details
    Publication Date: 2024-06-25
    Keywords: ARK-IX/2; AWI_PhyOce; Calculated; Calculated from conductivity; Chlorophyll fluorescence, Dr. Haardt Instruments; Chlorophyll fluorescence raw data; Computed; CTD, Sea-Bird, SBE 911plus [SN: 0485]; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Northeast Water Polynya; Physical Oceanography @ AWI; Polarstern; Pressure, water; PS25/003-0; PS25/004-0; PS25/005-0; PS25/006-0; PS25/007-0; PS25/008-0; PS25/008-1; PS25/009-0; PS25/010-0; PS25/011-0; PS25/012-0; PS25/012-1; PS25/013-0; PS25/014-0; PS25/015-0; PS25/015-1; PS25/016-0; PS25/017-0; PS25/018-0; PS25/019-0; PS25/020-0; PS25/021-0; PS25/021-1; PS25/022-0; PS25/023-0; PS25/024-0; PS25/025-0; PS25/026-0; PS25/027-0; PS25/027-1; PS25/028-0; PS25/029-0; PS25/030-0; PS25/030-1; PS25/030-2; PS25/031-0; PS25/032-0; PS25/033-0; PS25/033-1; PS25/034-0; PS25/035-0; PS25/035-1; PS25/036-0; PS25/036-1; PS25/037-0; PS25/038-0; PS25/039-0; PS25/040-0; PS25/041-0; PS25/042-0; PS25/043-0; PS25/044-0; PS25/045-0; PS25/046-0; PS25/046-1; PS25/047-0; PS25/047-1; PS25/048-0; PS25/049-0; PS25/051-0; PS25/052-0; PS25/053-0; PS25/054-0; PS25/055-0; PS25/055-1; PS25/056-0; PS25/057-0; PS25/058-0; PS25/059-0; PS25/059-1; PS25/060-0; PS25/060-1; PS25/060-2; PS25/060-3; PS25/061-0; PS25/062-0; PS25/063-0; PS25/064-0; PS25/065-0; PS25/066-0; PS25/067-0; PS25/068-0; PS25/069-0; PS25/070-0; PS25/071-0; PS25/072-0; PS25/073-0; PS25/074-0; PS25/075-0; PS25/076-0; PS25/077-0; PS25/080-0; PS25/081-0; PS25/082-0; PS25/083-0; PS25/084-0; PS25/085-0; PS25/085-1; PS25/085-2; PS25/086-0; PS25/087-0; PS25/088-0; PS25/089-0; PS25/089-1; PS25/090-0; PS25/091-0; PS25/092-0; PS25/093-0; PS25/093-1; PS25/094-0; PS25/094-1; PS25/095-0; PS25/095-1; PS25/098-0; PS25/099-0; PS25/100-0; PS25/101-0; PS25/102-0; PS25/103-0; PS25/104-0; PS25/105-0; PS25 NEW; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 123495 data points
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  • 6
    Electronic Resource
    Electronic Resource
    Untersuchungen an N-haltigen Brückenringsystemen (1965)
    Weinheim : Wiley-Blackwell
    Zeitschrift für die chemische Industrie 77 (1965), S. 550-551 
    Details
    ISSN: 0044-8249
    Keywords: Chemistry ; General Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1002/ange.19650771220
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    Paper (German National Licenses)
    Fulltext
  • 7
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    Phase-stable single-pass cryogenic amplifier for high repetition rate few-cycle laser pulses (2009)
    Institute of Physics
    Details
    Publication Date: 2009-08-24
    Electronic ISSN: 1367-2630
    Topics: Physics
    Published by Institute of Physics
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    PAPER CURRENT
  • 8
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    Nearshore arctic subsea permafrost in transition (2007)
    American Geophysical Union
    Details
    Publication Date: 2007-03-27
    Print ISSN: 0096-3941
    Electronic ISSN: 2324-9250
    Topics: Geosciences
    Published by American Geophysical Union
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  • 9
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    Offshore coastal studies - shoreface profiles measurements (2003)
    AWI
    In:  In: Russian-German Cooperation SYSTEM LAPTEV SEA The Expedition LENA 2002. , ed. by Grigoriev, M. N., Rachold, V., Bolshiyanov, D. Y., Pfeiffer, E. M., Schirrmeister, L., Wagner, D. and Hubberten, H. W. Berichte zur Polar- und Meeresforschung, 466 . AWI, Bremerhaven, Germany, pp. 316-325.
    Details
    Publication Date: 2020-10-26
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 10
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    Seasonal progression of thaw depth depended on microrelief (2003)
    AWI, Alfred-Wegener-Institut für Polar- und Meeresforschung
    In:  In: Russian-German Cooperation SYSTEM LAPTEV SEA : the Expedition LENA 2002. , ed. by Grigoriev, M. N., Rachold, V., Bolshiyanov, D. Y., Pfeiffer, E. M., Schirrmeister, L., Wagner, D. and Hubberten, H. W. Berichte zur Polar- und Meeresforschung, 466 . AWI, Alfred-Wegener-Institut für Polar- und Meeresforschung, Bremerhaven, pp. 49-50.
    Details
    Publication Date: 2020-10-26
    Type: Book chapter , PeerReviewed
    Format: text
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