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  • 1
    Buch
    Buch
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    UID:
    b3kat_BV011676746
    Umfang: XIV, 104 S. , graph. Darst., Kt.
    Serie: Berichte zur Polarforschung 242
    Anmerkung: Zsfassung in dt. Sprache. - Zugl.: Potsdam, Univ., Diss., 1997 , Zugl.: Potsdam, Univ., Diss., 1997
    Sprache: Englisch
    Fachgebiete: Geographie
    RVK:
    RVK:
    Schlagwort(e): Dauerfrostboden ; Schmelzen ; Wärmestrom ; Taimyr ; Schmelzen ; Wärmestrom ; Taimyr ; Dauerfrostboden ; Oberflächennahe Schichtenfolge ; Geothermik ; Hydrologie ; Geochemie ; Taimyr ; Dauerfrostboden ; Schmelzen ; Gefrieren ; Hochschulschrift ; Hochschulschrift ; Hochschulschrift ; Forschungsbericht
    Mehr zum Autor: Boike, Julia 1967-
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 2
    Buch
    Buch
    Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung
    UID:
    gbv_550208003
    Umfang: 30 S. , Ill., graph. Darst., Kt.
    Serie: Berichte zur Polar- und Meeresforschung 566
    Sprache: Englisch
    Schlagwort(e): Laptewsee ; Jakutien ; Lenadelta ; Expedition ; Geschichte 2006 ; Aufsatzsammlung
    Mehr zum Autor: Boike, Julia 1967-
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 3
    UID:
    kobvindex_GFZ84953
    Umfang: 104 S. : Abb. ; 30 cm
    Anmerkung: MAB0014.001: AWI G3-97-0206 , Univ. Potsdam, Wiss.-disz. Mineralogie, Diss. 1997
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 4
    UID:
    b3kat_BV024860585
    Umfang: XIV, 104 Bl. , graph. Darst., Kt.
    Anmerkung: Zsfassung in dt. Sprache , Potsdam, Univ., Diss., 1997
    Sprache: Englisch
    Fachgebiete: Geographie
    RVK:
    RVK:
    Schlagwort(e): Dauerfrostboden ; Schmelzen ; Wärmestrom ; Taimyr ; Schmelzen ; Wärmestrom ; Taimyr ; Dauerfrostboden ; Oberflächennahe Schichtenfolge ; Geothermik ; Hydrologie ; Geochemie ; Taimyr ; Dauerfrostboden ; Schmelzen ; Gefrieren ; Hochschulschrift
    Mehr zum Autor: Boike, Julia 1967-
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 5
    UID:
    kobvindex_IGB000023864
    In: Journal of Geophysical Research : Atmospheres. - 123(2018)10, S. 5222-5239
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 6
    UID:
    kobvindex_IGB000022694
    In: Journal of Geophysical Research : Earth Surface. - 121(2016)12, S. 2446-2470
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 7
  • 8
    UID:
    edochu_18452_25623
    Umfang: 1 Online-Ressource (14 Seiten)
    Inhalt: Amplified climate warming has led to permafrost degradation and a shortening of the winter season, both impacting cost-effective overland travel across the Arctic. Here we use, for the first time, four state-of-the-art Land Surface Models that explicitly consider ground freezing states, forced by a subset of bias-adjusted CMIP5 General Circulation Models to estimate the impact of different global warming scenarios (RCP2.6, 6.0, 8.5) on two modes of winter travel: overland travel days (OTDs) and ice road construction days (IRCDs). We show that OTDs decrease by on average −13% in the near future (2021–2050) and between −15% (RCP2.6) and −40% (RCP8.5) in the far future (2070–2099) compared to the reference period (1971–2000) when 173 d yr−1 are simulated across the Pan-Arctic. Regionally, we identified Eastern Siberia (Sakha (Yakutia), Khabarovsk Krai, Magadan Oblast) to be most resilient to climate change, while Alaska (USA), the Northwestern Russian regions (Yamalo, Arkhangelsk Oblast, Nenets, Komi, Khanty-Mansiy), Northern Europe and Chukotka are highly vulnerable. The change in OTDs is most pronounced during the shoulder season, particularly in autumn. The IRCDs reduce on average twice as much as the OTDs under all climate scenarios resulting in shorter operational duration. The results of the low-end global warming scenario (RCP2.6) emphasize that stringent climate mitigation policies have the potential to reduce the impact of climate change on winter mobility in the second half of the 21st century. Nevertheless, even under RCP2.6, our results suggest substantially reduced winter overland travel implying a severe threat to livelihoods of remote communities and increasing costs for resource exploration and transport across the Arctic.
    Inhalt: Peer Reviewed
    In: Bristol : IOP Publishing, 2021, 16,2
    Sprache: Englisch
    URL: Volltext  (kostenfrei)
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 9
    UID:
    edochu_18452_25774
    Umfang: 1 Online-Ressource (20 Seiten)
    Inhalt: Boreal forests efficiently insulate underlying permafrost. The magnitude of this insulation effect is dependent on forest density and composition. A change therein modifies the energy and water fluxes within and below the canopy. The direct influence of climatic change on forests and the indirect effect through a change in permafrost dynamics lead to extensive ecosystem shifts such as a change in composition or density, which will, in turn, affect permafrost persistence. We derive future scenarios of forest density and plant functional type composition by analyzing future projections provided by the dynamic global vegetation model (LPJ-GUESS) under global warming scenarios. We apply a detailed permafrost-multilayer canopy model to study the spatial impact-variability of simulated future scenarios of forest densities and compositions for study sites throughout eastern Siberia. Our results show that a change in forest density has a clear effect on the ground surface temperatures (GST) and the maximum active layer thickness (ALT) at all sites, but the direction depends on local climate conditions. At two sites, higher forest density leads to a significant decrease in GSTs in the snow-free period, while leading to an increase at the warmest site. Complete forest loss leads to a deepening of the ALT up to 0.33 m and higher GSTs of over 8 ∘C independently of local climatic conditions. Forest loss can induce both, active layer wetting up to four times or drying by 50%, depending on precipitation and soil type. Deciduous-dominated canopies reveal lower GSTs compared to evergreen stands, which will play an important factor in the spreading of evergreen taxa and permafrost persistence under warming conditions. Our study highlights that changing density and composition will significantly modify the thermal and hydrological state of the underlying permafrost. The induced soil changes will likely affect key forest functions such as the carbon pools and related feedback mechanisms such as swamping, droughts, fires, or forest loss.
    Inhalt: Peer Reviewed
    In: Bristol : IOP Publ., 2021, 16,8
    Sprache: Englisch
    URL: Volltext  (kostenfrei)
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 10
    UID:
    edochu_18452_28262
    Umfang: 1 Online-Ressource (13 Seiten)
    Inhalt: Soils are warming as air temperatures rise across the Arctic and Boreal region concurrent with the expansion of tall-statured shrubs and trees in the tundra. Changes in vegetation structure and function are expected to alter soil thermal regimes, thereby modifying climate feedbacks related to permafrost thaw and carbon cycling. However, current understanding of vegetation impacts on soil temperature is limited to local or regional scales and lacks the generality necessary to predict soil warming and permafrost stability on a pan-Arctic scale. Here we synthesize shallow soil and air temperature observations with broad spatial and temporal coverage collected across 106 sites representing nine different vegetation types in the permafrost region. We showed ecosystems with tall-statured shrubs and trees (〉40 cm) have warmer shallow soils than those with short-statured tundra vegetation when normalized to a constant air temperature. In tree and tall shrub vegetation types, cooler temperatures in the warm season do not lead to cooler mean annual soil temperature indicating that ground thermal regimes in the cold-season rather than the warm-season are most critical for predicting soil warming in ecosystems underlain by permafrost. Our results suggest that the expansion of tall shrubs and trees into tundra regions can amplify shallow soil warming, and could increase the potential for increased seasonal thaw depth and increase soil carbon cycling rates and lead to increased carbon dioxide loss and further permafrost thaw.
    Inhalt: Peer Reviewed
    In: Bristol : IOP Publ., 16,1
    Sprache: Englisch
    URL: Volltext  (kostenfrei)
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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