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  • 1
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Harwood Academic Publishers
    Call number: AWI P5-01-0028
    Description / Table of Contents: By demonstrating the importance of communication between natural scientists, social scientists and local stakeholders, and in response to the tremendous challenges and opportunities facing the Arctic, this book provides a comprehensive overview of the region's rapidly changing physical and human dimensions. It is an essential resource for all Arctic researchers, particularly those developing multidisciplinary projects. Representing a state of the art overview of key areas of Arctic research by renowed specialists in the field, each chapter forms a detailed, varied and accessible account of current knowledge. Each author introduces the subject to a non-specialist readership, while retaining intellectual integrity and relevance for specialists. Overall, the richness of the material presented in this volume reflects the ecological and cultural diversity of this vast and environmentally critical part of the globe.
    Type of Medium: Monograph available for loan
    Pages: XXXVIII, 647 Seiten , Illustrationen
    ISBN: 9058230872
    Language: English
    Note: Contents: List of Figures. - List of Colour Illustrations. - List of Tables. - Contributors. - Foreword. - Map. - Introduction / Mark Nuttall and Terry V. Callaghan. - PART 1 THE PHYSICAL STRUCTURE AND PROCESSES OF THE ARCTIC. - 1. The geological development of the Arctic / Maurits Lindstrom. - 2. Glaciology / Martin J. Siegert and Julian A. Dowdeswell. - 3. Permafrost and hydrology / Ming-Koo Woo. - 4. Arctic oceanography, sea ice and climate / Norman Davis. - 5. Upper atmosphere physics and chemistry / Sheila Kirkwood. - 6. The weather and climate of the Arctic / Gunter Weller. - PART 2 LIFE SCIENCES IN THE ARCTIC. - 7. Marine biology: Biomass productivity distributions and their variability in the Barents and Bering Seas / Egil Sakshaug and John Walsh. - 8. Ecology of Arctic lakes and rivers / Warwick F. Vincent and John E. Hobbie. - 9. Biodiversity of terrestrial ecosystems / Nadya Matveyeva and Yuri Chernov. - 10. Arctic terrestrial ecosystems and ecosystem function / Sven Jonasson, Terry V. Callaghan, Gaius R. Shaver and Lena A. Nielsen. - 11. Arctic medical science / Bent Harvald and the late Jens Peder Hart Hansen. - 12. Physical anthropology of the Arctic / G. Richard Scott, Scott Legge, Robert W. Lane, Susan L. Steen and Steven R. Street. - PART 3 SOCIAL AND POLITICAL DIMENSIONS OF THE ARCTIC. - 13. Indigenous peoples, self-determination and the Arctic environment / Mark Nuttall. - 14. The social anthropology of the Russian Far North / Peter P. Schweitzer. - 15. Arctic geopolitics then and now / Sanjay Chaturvedi. - 16. The population of the circumpolar north / Gunnar Knapp. - 17. The political economy of renewable resource management in the Arctic / Richard A. Caulfield. - PART 4 ANTHROPOGENIC IMPACTS ON THE ARCTIC ENVIRONMENT: REGIONAL AND GLOBAL CONSEQUENCES AND POLICY RESPONSES. - 18. Integrated global change impact assessments / Manfred A. Lange. - 19. Ozone depletion and UV-B radiation / Edward De Fabo and Lars Olof Björn. - 20. Local and transboundary pollution / Lars Otto Reiersen. - 21. International co-operation in the Arctic environment / Clive Archer and David Scrivener. - 22. Indigenous peoples' organisations and Arctic environmental co-operation / Mark Nuttall. - Index.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © National Academy of Sciences, 2006. This article is posted here by permission of National Academy of Sciences for personal use, not for redistribution. The definitive version was published in Proceedings of the National Academy of Sciences of the United States of America 103 (2006): 1342-1346, doi:10.1073/pnas.0503198103.
    Description: Recent observations of changes in some tundra ecosystems appear to be responses to a warming climate. Several experimental studies have shown that tundra plants and ecosystems can respond strongly to environmental change, including warming; however, most studies were limited to a single location and were of short duration and based on a variety of experimental designs. In addition, comparisons among studies are difficult because a variety of techniques have been used to achieve experimental warming and different measurements have been used to assess responses. We used metaanalysis on plant community measurements from standardized warming experiments at 11 locations across the tundra biome involved in the International Tundra Experiment. The passive warming treatment increased plant-level air temperature by 1-3°C, which is in the range of predicted and observed warming for tundra regions. Responses were rapid and detected in whole plant communities after only two growing seasons. Overall, warming increased height and cover of deciduous shrubs and graminoids, decreased cover of mosses and lichens, and decreased species diversity and evenness. These results predict that warming will cause a decline in biodiversity across a wide variety of tundra, at least in the short term. They also provide rigorous experimental evidence that recently observed increases in shrub cover in many tundra regions are in response to climate warming. These changes have important implications for processes and interactions within tundra ecosystems and between tundra and the atmosphere.
    Description: The projects represented here were supported by many sources, including the National Science Foundation, Swedish Natural Science Research Council, United Kingdom Natural Environment Research Council, Natural Sciences and Engineering Research Council of Canada, Research Council of Norway, Icelandic Centre for Research, and the Academy of Finland. Coordination of activities was made possible with support from the Bonanza Creek Long-Term Ecological Research site.
    Keywords: Arctic and alpine ecosystems ; Biodiversity ; Climate change ; Vegetation change
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: 353582 bytes
    Format: application/pdf
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  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of John Wiley & Sons for personal use, not for redistribution. The definitive version was published in Journal of Ecology 99 (2011): 1481-1488, doi:10.1111/j.1365-2745.2011.01859.x.
    Description: Climate change in northern high latitudes is predicted to be greater in winter rather than summer, yet little is known about the effects of winter climate change on northern ecosystems. Among the unknowns are the effects of an increasing frequency of acute, short-lasting winter warming events. Such events can damage higher plants exposed to warm, then returning cold, temperatures after snow melt and it is not known how bryophytes and lichens, which are of considerable ecological importance in high-latitude ecosystems, are affected by such warming events. However, even physiological adaptations of these cryptogams to winter environments in general are poorly understood. Here we describe findings from a novel field experiment that uses heating from infrared lamps and soil warming cables to simulate acute mid-winter warming events in a sub-Arctic heath. In particular, we report the growing season responses of the dominant lichen, Peltigera aphthosa, and bryophyte, Hylocomium splendens, to warming events in three consecutive winters. While summertime photosynthetic performance of P. aphthosa was unaffected by the winter warming treatments, H. splendens showed significant reductions of net photosynthetic rates and growth rates (of up to 48% and 52% respectively). Negative effects were evident already during the summer following the first winter warming event. While the lichen develops without going through critical phenological stages during which vulnerable organs are produced, the moss has a seasonal rhythm, which includes initiation of growth of young, freeze-susceptible shoot apices in the early growing season; these might be damaged by breaking of dormancy during warm winter events. Synthesis. Different sensitivities of the bryophyte and lichen species were unexpected, and illustrate that very little is known about the winter ecology of bryophytes and lichens from cold biomes in general. In sharp contrast to summer warming experiments that show increased vascular plant biomass and reduced lichen biomass, these results demonstrate that acute climate events in mid-winter may be readily tolerated by lichens, in contrast to previously observed sensitivity of co-occurring dwarf shrubs, suggesting winter climate change may compensate for (or even reverse) predicted lichen declines resulting from summer warming.
    Description: This research was supported by a grant from the Research Council of Norway (project no. 171542/V10) awarded to J.W.B., by a Leverhulme Trust (UK) grant to G.K.P. and T.V.C. (grant F/00 118/AV), by ATANS grants (EU Transnational Access Program, FP6 Contract no. 506004) to J.W.B., S.B., M.Z. and G.K.P., and by the Norwegian Institute for Nature Research. J.W.B.’s position at the Tromsø University Museum was financed by the Norwegian-Swedish Research School in Biosystematics, which received funding from the Research Council of Norway and the Norwegian Biodiversity Information Centre.
    Keywords: Arctic ; Climate change ; Ecophysiology ; Extreme events ; Hylocomium splendens ; Lichenized ascomycete ; Moss ; Peltigera aphthosa ; Plant–climate interactions ; Warming experiment
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2009. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Soil Biology and Biochemistry 42 (2010): 611-617, doi:10.1016/j.soilbio.2009.12.011.
    Description: Arctic climate change is expected to lead to a greater frequency of extreme winter warming events. During these events, temperatures rapidly increase to well above 0ºC for a number of days, which can lead to snow melt at the landscape scale, loss of insulating snow cover and warming of soils. However, upon return of cold ambient temperatures, soils can freeze deeper and may experience more freeze-thaw cycles due to the absence of a buffering snow layer. Such loss of snow cover and changes in soil temperatures may be critical for litter decomposition since a stable soil microclimate during winter (facilitated by snow cover) allows activity of soil organisms. Indeed, a substantial part of fresh litter decomposition may occur in winter. However, the impacts of extreme winter warming events on soil processes such as decomposition have never before been investigated. With this study we quantify the impacts of winter warming events on fresh litter decomposition using field simulations and lab studies. Winter warming events were simulated in sub-Arctic heathland using infrared heating lamps and soil warming cables during March (typically the period of maximum snow depth) in three consecutive years of 2007, 2008, and 2009. During the winters of 2008 and 2009, simulations were also run in January (typically a period of shallow snow cover) on separate plots. The lab study included soil cores with and without fresh litter subjected to winter warming simulations in climate chambers. Litter decomposition of common plant species was unaffected by winter warming events simulated either in the lab (litter of Betula pubescens ssp. czerepanovii), or field (litter of Vaccinium vitis-idaea, and B. pubescens ssp. czerepanovii) with the exception of Vaccinium myrtillus (a common deciduous dwarf shrub) that showed less mass loss in response to winter warming events. Soil CO2 efflux measured in the lab study was (as expected) highly responsive to winter warming events but surprisingly fresh litter decomposition was not. Most fresh litter mass loss in the lab occurred during the first 3-4 weeks (simulating the period after litter fall). In contrast to past understanding, this suggests that winter decomposition of fresh litter is almost non-existent and observations of substantial mass loss across the cold season seen here and in other studies may result from leaching in autumn, prior to the onset of “true” winter. Further, our findings surprisingly suggest that extreme winter warming events do not affect fresh litter decomposition.
    Description: This research was supported by a Leverhulme Trust (UK) grant to GKP and TVC, by a grant from the Norwegian Research Council awarded to JWB, and by ATANS grants (EU Transnational Access Programme) to JWB, GKP and SB.
    Keywords: Arctic ; Betula pubescens ssp. czerepanovii ; Climate change ; Decomposition ; Extreme weather ; Freeze-thaw ; Snow ; Vaccinium vitis-idaea ; V. myrtillus ; Winter warming event
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 5
    Publication Date: 2023-05-12
    Keywords: Abisko_ANS; Abisko, Lappland, northern Sweden; Abisko Scientific Research Station; Precipitation, annual total; Year of publication
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
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  • 6
    Publication Date: 2023-05-12
    Keywords: Abundance per area; AH_Slattatj-Njulla; Area; BC_Slattatjakka; BIO; Biology; BS_Abisko; Cryptogams, vascular; DATE/TIME; Date/time end; Event label; Forbs; Grass and sedges; Identification; Lapland, northern Sweden; Latitude of event; Longitude of event; Number; Number of species; Number of years; PMK_Patjujaure; PMK_Ridonjira; PMK_Slattatjakka; Proportion; Reference/source; Sample amount; Shrubs; Trees; UE_Karkevagge
    Type: Dataset
    Format: text/tab-separated-values, 281 data points
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  • 7
    Publication Date: 2023-05-12
    Keywords: Abisko_ANS; Abisko, Lappland, northern Sweden; Abisko Scientific Research Station; Alnus incana, basal area; Alnus incana, diameter at breast height; Alnus incana, number of trunks; Alnus incana, total dry weight; Betula pubescens czerepanovii, basal area; Betula pubescens czerepanovii, diameter at breast height; Betula pubescens czerepanovii, number of trunks; Betula pubescens czerepanovii, total dry weight; DATE/TIME; Pinus sylvestris, basal area; Pinus sylvestris, diameter at breast height; Pinus sylvestris, number of trunks; Pinus sylvestris, total dry weight; Salix spp., basal area; Salix spp., diameter at breast height; Salix spp., number of trunks; Salix spp., total dry weight; Sorbus aucuparia, basal area; Sorbus aucuparia, diameter at breast height; Sorbus aucuparia, number of trunks; Sorbus aucuparia, total dry weight; Standard deviation; Tree biomass, total dry weight; Tree density; Trees, living, basal area; Tree trunk diameter; Type
    Type: Dataset
    Format: text/tab-separated-values, 342 data points
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  • 8
    Publication Date: 2023-05-12
    Keywords: Abisko_ANS; Abisko, Lappland, northern Sweden; Abisko Scientific Research Station; DATE/TIME; Empetrum hermaphroditum, shoot growth per season; Incubation of surface soil/sediment, in-situ; Standard error; Treatment; Vaccinium myrtillus, shoot growth per season; Vaccinium vitis-idaea, shoot growth per season
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
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  • 9
    Publication Date: 2023-05-12
    Keywords: Alaska, USA; Alaska-Toolik; Area/locality; Biological sample; BIOS; DATE/TIME; Event label; Latnja-Abisko; Species richness; Sweden
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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  • 10
    Publication Date: 2023-05-12
    Keywords: Abisko_ANS; Abisko, Lappland, northern Sweden; Abisko Scientific Research Station; Biological sample; BIOS; Elevation of event; Environment; Event label; Joatka_Fjellstue; Latitude of event; Longitude of event; Norway; Seiland; Species; Sweden; Time coverage; Treatment; Vassijaure; Vegetation biomass, rate of change; Vegetation biomass, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 810 data points
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