Polar Research (E-Journal)
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Review of Climate change and globalization in the Arctic: an integrated approach to vulnerability assessment, by E. Carina H. Keskitalo
In the past decade, much of the research on global environmental change has adopted a new conceptual and methodological framing: vulnerability. This framing draws on decades of prior research—from multiple disciplinary perspectives and traditions—on how people produce, and respond to, conditions in their biophysical environments. The novelty in this framing is the recognition of the need to integrate existing ideas and methods, so as to paint a more holistic picture of the complex problems under study. Naturally, these conceptual (e.g., Kelly & Adger 2000; McCarthy et al. 2001; Turner et al. 2003) and methodological (e.g., O’Brien & Leichenko 2000; Luers et al. 2003; Schröter et al. 2005; Polsky et al. 2007) developments have outpaced the production of empirical vulnerability assessments that employ/operationalize these framings
Survey of waste water disposal practices at Antarctic research stations
To inform the future practices to be employed for handling waste water and grey water at the Swedish Antarctic station,Wasa, in Dronning Maud Land, the Swedish Polar Research Secretariat took the initiative to survey the practices of the 28 nations with stations in Antarctica. A questionnaire was sent out to all members of the Antarctic Environment Officers Network during the autumn of 2005. Questions were asked about the handling of waste water and grey water, the type of sewage treatment, and installation and operational costs. The response to the questionnaire was very good (79%), and the results showed that 37% of the permanent stations and 69% of the summer stations lack any form of treatment facility. When waste water and grey water containing microorganisms are released, these microorganisms can remain viable in lowtemperature Antarctic conditions for prolonged periods. Microorganisms may also have the potential to infect and cause disease, or become part of the gut flora of local bird and mammal populations, and fish and marine invertebrates. The results from 71 stations show that much can still be done by the 28 nations operating the 82 research stations in Antarctica. The technology exists for effective waste water treatment in the challenging Antarctic conditions. The use of efficient technology at all permanent Antarctic research stations would greatly reduce the human impact on the pristine Antarctic environment. In order to protect the Antarctic environment from infectious agents introduced by humans, consideration should also be given to preventing the release of untreated waste water and grey water from the smaller summer stations
Diet of wolverines (Gulo gulo) in the western Brooks Range, Alaska
Migratory caribou herds are an important component of the North American tundra. We investigated the wolverine (Gulo gulo) diet in the migratory range of the Western Arctic Caribou Herd in north-western Alaska. Within this area, caribou are absent or occur at low densities for large parts of the year, and thus show a strong seasonality in abundance. Analyses of stomach and colon contents suggested that wolverines primarily consumed caribou during the winter, and that the dietary dependence was related more to caribou mortality than to caribou abundance in the area. We also found indications that wolverines may switch between moose and caribou during periods of low caribou abundance, but that such a switch did not affect wolverine body condition. Our results thus support previous observations that wolverines primarily consume ungulates. However, a better knowledge of how alternative food sources are utilized will be necessary to predict the dietary and demographic responses of wolverines to variations in caribou abundance. We also suggest that further efforts should be made to investigate the effects of other ungulate-dependent predators on wolverine feeding ecology, because such predators may function both as competitors and as suppliers of carrion for scavenging
Review of Arctic fox. Life at the top of the world, by Gary Hamilton
The Arctic fox is the only truly Arctic species among the terrestrial carnivorous mammals of the world. It is distributed across the circumpolar Arctic region. Like polar bears, Arctic foxes regularly traverse the pack ice of the polar basin, a fact that astonished Fridtjof Nansen during his attempt to reach the North Pole more than 100 years ago. However, despite its unique lifestyle, which in some respects is more fascinating than that of the polar bear, there has been no popular book (except a book for children) aimed at compiling our present knowledge about the Arctic fox for an international audience. This omission is in stark contrast to all of the writing about the polar bear. Finally, just such an Arctic fox book is now available, written by the freelance journalist Gary Hamilton
Hydrological and hydrochemical observation status in the pan-Arctic drainage basin
In order to identify and understand the ongoing changes in the Arctic hydrological cycle, and the impacts on the Arctic Ocean, timely and open access to water and water-chemistry data is essential. By synthesizing and analysing all openly accessible water-discharge and water-quality data, we present an updated, quantitative picture of the status of observational data on hydrological and hydrochemical fluxes from the pan-Arctic drainage basin (PADB) to the ocean. We identify and compare the characteristics of monitored and unmonitored areas, and the differences between them, across the continents in the PADB. Results indicate significant gaps in monitoring data for water chemistry, in particular for high-latitude near-coastal areas. The differences in characteristics between monitored and unmonitored areas may bias assessments of hydrological and hydrochemical fluxes to the Arctic Ocean. The reliable identification and understanding of important biogeochemical processes in the PADB require extended monitoring, particularly in high-latitude permafrost ground, and more ready access to harmonized and integrated hydrochemical data
Canadian Inuit subsistence and ecological instability—if the climate changes, must the Inuit?
Considerable attention has been devoted to the possible effects of global climate change on the environment of the circumpolar world.With regard to the Inuit, the aboriginal culture of Arctic Canada, research interest has focused principally on the vulnerability of the hunting and harvesting component of the traditional food system, otherwise frequently referred to as the subsistence system, if wild terrestrial and marine resources become less available. Although also concerned with the traditional Inuit food economy, this paper concentrates on the customary institutional mechanisms by which the Inuit distribute and share the products obtained from hunting. After analysing this social economy, a review of the data on recent climate-related range changes of a number of Arctic animal populations is carried out, in terms of how projected environmental changes may affect this other aspect of Inuit subsistence. After tentatively concluding that some species substitution and/or replacement will occur, the final aspect of the paper considers the potential for the possible exclusion of these “replacements” as a result of the political aspect of climate change
Organic carbon and microbial biomass in a raised beach deposit under terrestrial vegetation in the High Arctic, Ny-Ålesund, Svalbard
Raised beach deposits are widespread on the north-western coast of Spitsbergen, Svalbard. To elucidate the importance of these deposits in an ecosystem carbon cycle, we measured the concentrations of organic carbon and adenosine 5-triphosphate (ATP; an index of living microbial biomass) in a raised beach deposit found under terrestrial vegetation in Ny-Ålesund. A shell in the deposit found at a depth of ca. 20 cm below the ground surface had a (not calibrated) 14C age of 11080 _ 140 yr BP, whereas soil organic carbon in the same deposit showed an older 14C age (22380 _ 90 yr BP). Organic carbon concentration in the layer of 20–40 cm belowground was about 1–2%, which was comparable to those in shallower mineral soil layers. Results of ATP analyses suggested that low but non-negligible amounts of microorganisms existed in the deposit. The proportion of biomass carbon to soil organic carbon tended to decrease with increasing depth, suggesting that organic carbon in the deep layer was less available to microorganisms than that in the shallow layers