This review article makes six observations about the current body of research on the societal impacts of a changing Arctic. First, climate change and globalisation are the dominant drivers of societal impacts in the Arctic. Second, many contributions focus on the impacts in concrete sectors of society, often from an opportunities-and-risks perspective, which tends to blur the boundary to more policy-oriented work. Third, the mantra of the sustainable development of the Arctic or Arctic sustainability pervades considerations of Arctic societal impacts. Fourth, societal and environment change in the Arctic is increasingly analysed using the image of the Global Arctic, highlighting the inextricable linkages between Arctic and global processes and systems and thus the entangled fate of the North and the entire globe. Fifth, an increasing number of actors is seen as being involved in societal and environmental transformations in the Arctic, often conveyed through the (often ill-defined) stakeholder concept. Sixth, Arctic indigenous peoples are depicted as the group most vulnerable to the societal impacts of a changing Arctic, but are increasingly the subject of research in the form of rights-holders and active participants in governance, law, politics, and research. Challenges for future research include achieving greater clarity and reflexivity around key concepts, and de-essentialising the Arctic via the use of comparative methods on cases both within and beyond the Arctic.
The seafloor is recognized as one of the major sinks for microplastics (MPs). However, to date there have been no studies reported the MP contamination in benthic organisms from the Arctic and sub-Arctic regions. Therefore, this study provided the first data on the abundances and characteristics of MPs in a total of 413 dominant benthic organisms representing 11 different species inhabiting in the shelf of Bering and Chukchi Seas. The mean abundances of MP uptake by the benthos from all sites ranged from 0.02 to 0.46 items g−1 wet weight (ww) or 0.04–1.67 items individual−1, which were lower values than those found in other regions worldwide. The highest value appeared at the northernmost site, implying that the sea ice and the cold current represent possible transport mediums. Interestingly, the predator A. rubens ingested the maximum quantities of MPs, suggesting that the trophic transfer of MPs through benthic food webs may play a critical role. Fibers constituted the major type (87%) in each species, followed by film (13%). The colors of fibers were classified as red (46%) and transparent (41%), and the film was all gray. The predominant composition was polyamide (PA) (46%), followed by polyethylene (PE) (23%), polyester (PET) (18%) and cellophane (CP) (13%). The most common sizes of MPs concentrated in the interval from 0.10 to 1.50 mm, and the mean size was 1.45 ± 0.13 mm. Further studies about the temporal trends and detrimental effects of MPs remain to be carried out in benthic organisms from the Arctic and sub-Arctic regions.
This policy brief focuses on the opening of the Central Arctic Ocean and the subsequent questions this poses to regional governance. This change has the potential to radically alter the nature of Arctic governance as non-Arctic states will have to play a significant role in the rules that will apply in the Arctic high seas. Talks about a regional fisheries regime will define the future of this region. The creation of a coordinating agreement would have the benefit of not challenging Arctic states too fundamentally while at the same time incorporating non-Arctic states in a meaningful way in the regional governance infrastructure.
Microplastics (MP) are recognized as a growing environmental hazard and have been identified as far as the remote Polar Regions, with particularly high concentrations of microplastics in sea ice. Little is known regarding the horizontal variability of MP within sea ice and how the underlying water body affects MP composition during sea ice growth. Here we show that sea ice MP has no uniform polymer composition and that, depending on the growth region and drift paths of the sea ice, unique MP patterns can be observed in different sea ice horizons. Thus even in remote regions such as the Arctic Ocean, certain MP indicate the presence of localized sources. Increasing exploitation of Arctic resources will likely lead to a higher MP load in the Arctic sea ice and will enhance the release of MP in the areas of strong seasonal sea ice melt and the outflow gateways.
Paleoclimate research define the baselines for the natural climate change and is imperative to help us to set the recent observed changes in the long-term natural climate context. Fossil marine diatoms have proved to be an excellent tools for the paleoclimatic reconstructions, e.g. for the reconstruction of sea surface temperature (SST) and sea ice. A number of studies have been conducted from the northern high latitude region using diatoms as potential proxy. Nevertheless, these studies are scattered and thus there is a need to expand diatom research in the Arctic regions. Due to the possibilities offered by an emerging trend of diatom-based research, it is important to identify both the research themes and geographical areas of highest importance in order to obtain the best possible scientific outcome in the research. Here we review some of up-to-date diatom-based reconstruction methods applicable for paleoceanographic research for the northern North Atlantic and Arctic regions, and discuss the knowledge gaps in the Arctic research, which potentially can be solved by diatom applications. The modern diatom research has progressively concentrated on quantitative reconstruction based on diatoms and statistical transfer function providing the most useful data for the climate research. However, also qualitative reconstruction methods are still needed; the recent studies show that although the quantitative reconstruction method for SST appears to be statistically robust, there are uncertainties in quantitative reconstructions for sea-ice, and thus it is still recommended to use the Marginal Ice Zone diatom taxa as a qualitative reconstruction method for the Arctic sea ice. Diatom applications offer highly potential tools for filling the knowledge gaps in the Arctic research.
Warming weather conditions in the Arctic are already resulting in changes in both sea ice extent and thickness. The resulting extended ‘open water’ season has many implications for vessel traffic and marine life. For example, an increase in vessel traffic due to ice-free waters will most likely lead to an increased risk of impact on cetaceans through increased noise pollution, strike risk for some cetacean species, and the possibility of exposure to chemical pollutants. The objective of this study was to pre-empt a predicted increase in vessels by investigating and exploring possible management scenarios, with the aim of mitigating negative impacts on locally important species such as bowhead and beluga whales. Utilizing insights gained from established vessel management schemes in more southerly regions, this paper evaluates the current suite of tools being implemented and their appropriateness for implementation in a more extreme Arctic environment.
Although there is no fishing activity within the central Arctic Ocean at present, commercial fishing activity does occur in the high seas areas of the North Atlantic and North Pacific, and within the exclusive economic zone of the Arctic coastal States. Climate change will most probably lead to an increase in fishing activity, through the reduction in sea ice, opening up new areas of the Arctic to fisheries, including the Central Arctic Ocean. This prospect has fuelled intensive negotiations—still ongoing—for the signing of a legally binding agreement to prevent unregulated fisheries therein. What seems missing, though, from both the ongoing negotiations on this agreement and the scholarly literature is reference to fisheries enforcement in the Arctic. Accordingly, this article identifies the most effective tools that could be employed for fisheries enforcement purposes, including port and flag State measures, and addresses their potential application in the Arctic.
Polar oceans, though remote in location, are not immune to the accumulation of plastic debris. The present study, investigated for the first time, the abundance, distribution and composition of microplastics in sub-surface waters of the Arctic Central Basin. Microplastic sampling was carried out using the bow water system of icebreaker Oden (single depth: 8.5 m) and CTD rosette sampler (multiple depths: 8–4369 m). Potential microplastics were isolated and analysed using Fourier Transform Infrared Spectroscopy (FT-IR). Bow water sampling revealed that the median microplastic abundance in near surface waters of the Polar Mixed Layer (PML) was 0.7 particles m−3. Regarding the vertical distribution of microplastics in the ACB, microplastic abundance (particles m−3) in the different water masses was as follows: Polar Mixed Layer (0–375) > Deep and bottom waters (0–104) > Atlantic water (0–95) > Halocline i.e. Atlantic or Pacific (0–83).
This paper assesses the value and environmental feasibility of Arctic shipping by reviewing the relevant scientific and economic peer-reviewed literature. From the physical perspective, this paper examines the impact of climate change on sea ice and marine weather and considers the resultant consequences for Arctic shipping accessibility. From an economic perspective, it reviews the major research investigating the economic feasibility of diverting ships from conventional shipping routes to Arctic routes, the attitudes of shipping stakeholders, and other major factors affecting the prospect of Arctic shipping. This review also identifies important research gaps. Ultimately, we find that the complex environmental and economic dynamics of the Arctic suggest that an appropriate understanding of Arctic shipping will require close collaboration between natural and social scientists.
Global changes in climate, connectivity, and commerce are having profound impacts on the Arctic environment and inhabitants. There is widespread recognition of the value of incorporating different worldviews and perspectives when seeking to understand the consequences of these impacts. In turn, attention to local needs, perspectives, and cultures is seen as essential for fostering effective adaptation planning, or more broadly, the resilience of local peoples. The emerging literature on “knowledge co-production” identifies factors that can help incorporate such local information. This field focuses on how different models of what has been termed the “science-policy interface” can incorporate multiple epistemologies. Such an approach goes beyond observing or assessing change from different scales and perspectives, to defining conditions that support the co-production of actionable knowledge. This approach requires the development of response tools that can accommodate the dynamic relationships among people, wildlife, and habitats that straddle cultures, timescapes, and sometimes, national boundaries. We use lessons from seven Alaskan cases studies to describe a typology of five elements important for the co-production of locally relevant actionable knowledge. Three elements are consistent with earlier work, including 1) evolving communities of practice, 2) iterative processes for defining problems and solutions, and 3) presence of boundary organizations, such as a government agency, university, or co-management council. Our results for the Alaskan Arctic also emphasize the critical need to incorporate 4) the consistent provision of sufficient funds and labor that may transcend any one specific project goal or funding cycle, and 5) long temporal scales (sometimes decades) for achieving the co-production of actionable knowledge. Our results have direct relevance to understanding the mechanisms that might foster greater success in more formalized co-management regimes.