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  • Artikel  (6)
  • 2020-2024  (2)
  • 2000-2004  (4)
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  • 1
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    Copernicus Publications
    In:  EPIC3The Cryosphere, Copernicus Publications, 14(7), pp. 2205-2216, ISSN: 1994-0416
    Publikationsdatum: 2024-01-30
    Beschreibung: Previous studies show accelerations of West Antarctic glaciers, implying that basal melt rates of these glaciers were previously small and increased in the middle of the 20th century. This enhanced melting is a likely source of the observed Ross Sea (RS) freshening, but its long-term impact on the Southern Ocean hydrography has not been well investigated. Here, we conduct coupled sea ice-ice shelf-ocean simulations with different levels of ice shelf melting from West Antarctic glaciers. Freshening of RS shelf and bottom water is simulated with enhanced West Antarctic ice shelf melting, while no significant changes in shelf water properties are simulated when West Antarctic ice shelf melting is small. We further show that the freshening caused by glacial meltwater from ice shelves in the Amundsen and Bellingshausen seas can propagate further downstream along the East Antarctic coast into the Weddell Sea. The freshening signal propagates onto the RS continental shelf within a year of model simulation, while it takes roughly 5-10 and 10-15 years to propagate into the region off Cape Darnley and into the Weddell Sea, respectively. This advection of freshening modulates the shelf water properties and possibly impacts the production of Antarctic Bottom Water if the enhanced melting of West Antarctic ice shelves continues for a longer period.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
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  • 2
    Publikationsdatum: 2020-02-12
    Schlagwort(e): 550 - Earth sciences
    Materialart: info:eu-repo/semantics/article
    Format: application/pdf
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  • 3
    Publikationsdatum: 2024-01-12
    Beschreibung: Sulawesi comprises of about 182,870 km\xc2\xb2 of land and fewer botanical specimens (about 23 specimens per 100 km\xc2\xb2, Whitten et al., 1987) have been collected here than in any other major island in Indonesia. This island is up to date botanically poorly explored and according to Van Steenis (1950) about 32,500 specimens of plants were recorded, the number is probably only a rough estimation and certainly in the precomputer era not based on real specimens. Within the framework of STORMA (Stability of Rainforest Margins) we analyzed the vegetation in several plots of one hectare of different land use systems at the Lore Lindu National Park, Central Sulawesi, Indonesia. Rapidly we were faced with the problem that the identification of the mostly sterile trees would be almost impossible without a sound basic checklist. Because previous hardcopies (Hildebrand, 1950; Soewanda & Tantra, 1973; Whitmore et al., 1989) were either outdated or incomplete (especially for the small diameter trees) we decided to create a new one using data of actual plant specimens housed at the National Herbarium of the Netherlands, Universiteit Leiden branch (with duplicate specimens in several other herbaria like BO, E, K and others), and enter them in the BRAHMS (Botanical Research and Herbarium Management Systems) database developed by Denis Filer, University of Oxford.\nMore than 120 woody families have been screened and the label information of all specimens (c. 13,000) checked and partly analysed. The density index calculated from our figures is very low (7) but for the first time underpinned by hard, retrievable data. As we did not include species \xe2\x80\x94 and specimens rich herbaceous families in our calculations (Orchidaceae, Poaceae, Zingiberaceae, ferns, etc.) the much lower collection index can be at least partially explained.
    Repository-Name: National Museum of Natural History, Netherlands
    Materialart: info:eu-repo/semantics/article
    Format: application/pdf
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  • 4
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    University of Potsdam
    In:  EPIC3University of Potsdam, 96 p.
    Publikationsdatum: 2023-03-13
    Beschreibung: The Yedoma region is unique in the permafrost region of the Northern Hemisphere and is characterized by a particularly high ground ice content in the sediment. These frozen deposits store a large amount of carbon and thus have the potential to influence the global climate. Especially the upper layers are susceptible to thaw processes, as they are exposed to increasingly rising mean annual air temperatures. The Northeastern Siberian Yedoma domain is of particular interest in this study. The morphology of ground ice is highly variable and the exact abundance and distribution is still unknown in large parts of Siberia. For an accurate overview of the distribution of intrasedimentary ground ice content, data from 26 sites in Northeastern Siberia were examined. The data were taken from data repositories (e.g., PANGAEA), expedition reports, scientific papers etc. and has been synthesized in a template in Excel. Of relevance was the absolute ice content (wt%) at different depths. Five depth classes were investigated: depth class 1: 0-0.99m; depth class 2: 1-1.99m; depth class 3: 2-2.99m; depth class 4: 3-24.99m; depth class 5: 25-65m. Using the mean absolute ice content for each depth class, ArcGIS was used to create a map for the distribution of ice content. R was applied to represent the ground ice content distribution at the different depths. Furthermore, the focus was on other parameters such as stratigraphy, total organic carbon content and landscape types, which were also examined with respect to the absolute ice content. The ice content is distributed very heterogeneously in Northeastern Siberia, averaging between 30 and 60 wt% over all depths. In large parts of the study area, the ice content in the upper three meters is with 40 to 65 wt% much higher than in the deeper sediment layers. In the depths of 3-65m, the ice content ranges from 20 to 50 wt%. Investigations of the age classes showed that the mean absolute ice content in thermokarst deposits (MIS 1) is with 48.60 wt% higher than in older sedimentary units. The TOC content also decreases significantly with depth. The Yedoma sediment composition and depositional regimes are highly variable. Even on a small scale, large differences in ice content could be observed. With the given data basis, no concrete statements about the vertical and horizontal ice content could be made for the whole study area. The model created in this study can be applied to model the absolute ground ice content based on the TOC content. Assessing the nature and content of ground ice in the upper layers in Northeastern Siberia is fundamental to environmental assessment and important for quantifying carbon fluxes and understanding permafrost response to climate change.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Thesis , notRev
    Format: application/pdf
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  • 5
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    Rheinischen Friedrich–Wilhelms–Universität
    In:  EPIC3Bonn, Rheinischen Friedrich–Wilhelms–Universität
    Publikationsdatum: 2019-07-17
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: PANGAEA Documentation , notRev
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  • 6
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    IUGG Secretariat, CIRES Cooperative Institute for Research in Environmental Sciences
    Publikationsdatum: 2020-02-12
    Sprache: Englisch
    Materialart: info:eu-repo/semantics/conferenceObject
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