Arctic and sub-arctic watersheds are undergoing significant changes due to recent climate warming and degrading permafrost, engendering enhanced monitoring of arctic rivers. Smaller catchments ...provide understanding of discharge, solute flux and groundwater recharge at the process level that contributes to an understanding of how larger arctic watersheds are responding to climate change. The North Klondike River, located in west central Yukon, is a sub-alpine permafrost catchment, which maintains an active hydrological monitoring station with a record of >40 years. In addition to being able to monitor intra-annual variability, this data set allows for more complex analysis of streamflow records. Streamflow data, geochemistry and stable isotope data for 2014 show a groundwater-dominated system, predominantly recharged during periods of snowmelt. Radiocarbon is shown to be a valuable tracer of soil zone recharge processes and carbon sources. Winter groundwater baseflow contributes 20 % of total annual discharge, and accounts for up to 50 % of total river discharge during the spring and summer months. Although total stream discharge remains unchanged, mean annual groundwater baseflow has increased over the 40-year monitoring period. Wavelet analysis reveals a catchment that responds to El Niño and longer solar cycles, as well as climatic shifts such as the Pacific Decadal Oscillation.
Dedicated to Professor Peter Fritz on the occasion of his 80th birthday
A palynological reconstruction (n = 25 profiles) suggests that the northern extent of lodgepole pine (Pinus contorta var. latifolia Engelmann ex S. Watson) occurred between 59° and 60°N latitude in ...northwest North America from 10,000 to 7000 calendar years before present (cal. yr BP) prior to entering Yukon. Although specific migration pathways could not be resolved with the available palynological data, mountains along the southern edge of Yukon appear to have diverted lodgepole pine migration through the Carcross and Frances Lake areas in southwest and southeast Yukon, respectively. Migration in the southwest (70 m/yr) was likely confined to lower elevations of the Yukon and Teslin river valleys, with lodgepole pine reaching 61°N ~2000 cal. yr BP. Along the eastern route, migration was channeled through a 15–20 km wide pass in a 200 km mountainous front. After breaching the Liard drainage divide north of Frances Lake ~4000 cal. yr BP, migration progressed northwest (160–220 m/yr) along the Tintina Trench. Lodgepole pine was estimated to have reached its near present-day northern limit (~63°N) ~1790 cal. yr BP, which is ~1290 years earlier than previously thought. This difference in arrival dates is due the use of a >5% rather than a >15% pine pollen content threshold, which appears to correspond with >1% pine tree cover in the landscape. Climatic cooling after 1000 cal. yr BP that caused a population decline at higher elevations is hypothesized to explain the present-day sparse and disjunct distribution of pine across Yukon north of 61°N.
Celotno besedilo
Dostopno za:
DOBA, IZUM, KILJ, NUK, OILJ, PILJ, PNG, SAZU, UILJ, UKNU, UL, UM, UPUK
Objective: To determine if Canadians are getting value for money in providing health services to our northern residents.
Method: Secondary analyses of data from Statistics Canada, the Canadian ...Institute of Health Information and territorial government agencies on health status, health expenditures and health system performance indicators.
Results: Per capita health expenditures in Canada's northern territories are double that of Canada as a whole and are among the highest in the world. The North lags behind the rest of the country in preventable mortality, hospitalization for ambulatory care sensitive conditions and other performance indicators.
Discussion: The higher health expenditure in the North is to be expected from its unique geography and demography. If the North is not performing as well as Canada, it is not due to lack of money, and policy makers should be concerned about whether healthcare can be as good as it could be.
We tested the adaptive stress hypothesis that male arctic ground squirrels (Urocitellus parryii) exhibit a stress response over the course of the breeding season that is characterized by increasing ...free cortisol concentrations, increasing mobilization of stored energy, and decreasing physical condition. We assessed the functioning of the hypothalamic-pituitary-adrenal axis by measuring cortisol levels in response to the stress of capture and in response to a hormone challenge protocol (dexamethasone suppression and adrenocorticotropic hormone stimulation). We measured blood glucose levels, free fatty acids, white blood cells, and hematocrit to assess the downstream physiological responses to cortisol. Immediately after spring emergence, male arctic ground squirrels had ample free abdominal fat and few signs of wounding. By the end of the breeding season 3 wk later, visible fat reserves were almost entirely gone, and most males had extensive wounds. Total plasma cortisol concentrations increased over this period, but so did corticosteroid-binding capacity, resulting in no change in the free cortisol response to capture. We found no significant changes in how the animals responded to our hormone challenges, contrary to our prediction that the stress axis should increase free cortisol production. Even though we found no change in the functioning of the stress axis, all of the downstream measures suggested that male arctic ground squirrels are chronically exposed to high cortisol concentrations. Over the breeding season, blood glucose increased, fat stores and circulating free fatty acids were depleted, and both hematocrit levels and white blood cell counts decreased significantly. Our data suggest that a more complex relationship between the stress axis and downstream measures of stress exists than that proposed by the adaptive stress hypothesis. We propose several nonexclusive, testable mechanisms that could explain our observations.
Celotno besedilo
Dostopno za:
BFBNIB, DOBA, IZUM, KILJ, NMLJ, NUK, PILJ, PNG, SAZU, SIK, UILJ, UKNU, UL, UM, UPUK
Appropriate representation of landscape heterogeneity at small to medium scales is a central issue for hydrological modelling. Two main hydrological modelling approaches, deductive and inductive, are ...generally applied. Here, snow-cover ablation and basin snowmelt runoff are evaluated using a combined modelling approach that includes the incorporation of detailed process understanding along with information gained from observations of basin-wide streamflow phenomena. The study site is Granger Basin, a small sub-arctic basin in the mountains of the Yukon Territory, Canada. The analysis is based on the comparison between basin-aggregated and distributed landscape representations. Results show that the distributed model based on "hydrological response" landscape units best describes the observed magnitudes of both snow-cover ablation and basin runoff, whereas the aggregated approach fails to represent the differential snowmelt rates and to describe both runoff volumes and dynamics when discontinuous snowmelt events occur.
The transboundary governance of Pacific salmon fisheries requires interactions between institutions that can enable collective action, collaboration, and continuous learning. However, relatively ...little is known concerning how civil servants in different institutions and jurisdictions interact with each other within transboundary policy settings. In this paper, we explore the interactions of civil servants from agencies in five jurisdictions: United States (federal), Canada (federal), British Columbia, Yukon, and Alaska, to assess the extent to which they interact within the Pacific salmon policy network and also the social capital (i.e., formal and informal communication and trust) present among these working relationships. Our results reveal patchy patterns of interagency communication, and relatively low levels of interagency trust between jurisdictions, suggesting the potential for improved collaboration on Pacific salmon governance. Our analysis also revealed that the binational Pacific Salmon Commission had the highest levels of trust within the network, suggesting it is likely well placed to foster collaboration.
Upper Cambrian to Middle Ordovician mafic volcanic rocks of the Donjek assemblage comprise the oldest exposed units of the Alexander terrane in the Saint Elias Mountains of northwestern Canada. In ...this study, we use the geochemical and geological characteristics of these rocks to decipher their tectonic setting, petrogenetic history, and relationship to the early Paleozoic Descon arc system of the Alexander terrane in southeastern Alaska. Donjek assemblage volcanic rocks are subdivided into three geochemical types: transitional basalt (type I), light rare earth–enriched island-arc tholeiite to calc-alkaline basalt (type II), and enriched mid-ocean ridge basalt to ocean-island basalt (type III). Simple petrogenetic models illustrate that the basalts were generated by the decompressional partial melting of enriched asthenospheric mantle and variably mixed with depleted mantle and subduction-related components. Analogous geochemical signatures for modern Sumisu Rift and Okinawa Trough lavas imply that the Donjek assemblage basalts erupted during the rifting of the Descon arc. This model provides a new comparative framework for terranes of Siberian, Baltican, and Caledonian affinity in the North American Cordillera and, in particular, suggests a paleogeographic connection to rift-related magmatism in the Seward Peninsula region of the Arctic Alaska–Chukotka terrane.
Celotno besedilo
Dostopno za:
BFBNIB, DOBA, IZUM, KILJ, NMLJ, NUK, PILJ, PNG, SAZU, SIK, UILJ, UKNU, UL, UM, UPUK
Analyses of sediment cores from Marcella Lake, a small, hydrologically closed lake in the semi-arid southwest Yukon, provides effective moisture information for the last ∼4500 years at century-scale ...resolution. Water chemistry and oxygen isotope analyses from lakes and precipitation in the region indicate that Marcella Lake is currently enriched in
18O by summer evaporation. Past lake water values are inferred from oxygen isotope analyses of sedimentary endogenic carbonate in the form of algal Charophyte stem encrustations. A record of the
δ
18O composition of mean annual precipitation at Jellybean Lake, a nearby evaporation-insensitive system, provides data of simultaneous
δ
18O variations related to decade-to-century scale shifts in Aleutian Low intensity/position. The difference between the two isotope records, Δδ, represents
18O-enrichment in Marcella Lake water caused by summer effective moisture conditions. Results indicate increased effective moisture between ∼3000 and 1200
cal
BP and two marked shifts toward increased aridity at ∼1200 and between 300 and 200
cal
BP. These prominent late Holocene changes in effective moisture occurred simultaneously with changes in Aleutian Low circulation patterns over the Gulf of Alaska indicated by Jellybean Lake. The reconstructed climate patterns are consistent with the topographically controlled climatic heterogeneity observed in the coastal mountains and interior valleys of the region today.
Climate change in the Arctic leads to permafrost degradation and to associated changes in freshwater geochemistry. There is a limited understanding of how disturbances such as active layer ...detachments or retrogressive thaw slumps impact water quality on a catchment scale. This study investigates how permafrost degradation affects concentrations of dissolved organic carbon (DOC), total dissolved solids (TDS), suspended sediment, and stable water isotopes in adjacent Low Arctic watersheds. We incorporated data on disturbance between 1952 and 2015, as well as sporadic runoff and geochemistry data of streams nearby. Our results show that the total disturbed area decreased by 41% between 1952 and 2015, whereas the total number of disturbances increased by 66% in all six catchments. The spatial variability of hydrochemical parameters is linked to catchment properties and not necessarily reflected at the outflow. Degrading ice‐wedge polygons were found to increase DOC concentrations upstream in Ice Creek West, whereas hydrologically connected disturbances were linked to increases in TDS and suspended sediment. Although we found a great spatial variability of hydrochemical concentrations along the paired watershed, there was a linear relationship between catchment size and daily DOC, total dissolved nitrogen, and TDS fluxes for all six streams. Suspended sediment flux on the contrary did not show a clear relationship as one hydrologically connected retrogressive thaw slump impacted the overall flux in one of the streams. Understanding the spatial variability of water quality will help to model the lateral geochemical fluxes from Arctic catchments.
Plain Language Summary
One effect climate change has in the Arctic is the thawing of permafrost. Permafrost is defined as ground that remains below 0 °C for at least two consecutive years. The low temperatures in the High North lead to very slow decomposition rates of organic material from plants and animals. A lot of this material has accumulated over thousands of years. As air temperatures in the Arctic are rising, permafrost is thawing. This is also termed permafrost degradation. It can occur in two forms: (1) The gradual deeper thawing of permafrost is called thermal perturbation. It might lead to a subsidence (sinking) of the ground, because water that was previously frozen runs off. (2) Thawing of the ground may lead to a destabilization of the ground and connected landslides. This is termed physical or surface disturbance. These two forms of permafrost degradation have an impact on the water quality of rivers flowing through the terrain. In this study, we investigated the impacts of permafrost degradation on stream hydrochemistry on Herschel Island, Yukon Territory, Canada. We identified active physical disturbances in the past using aerial photographs from 1952 and 1970 and satellites images from 2011 and 2015. This was done for the areas from which rainwater flows into the same river (catchment area) of six streams named Water Creek, Beach Creek, Fox Creek, Ice Creek West, Ice Creek East, and Eastern Gully. In 2016, we collected water samples along two neighboring streams (Ice Creek West and Ice Creek East) to compare the impacts of local physical disturbances on the hydrochemistry. In these two streams, we also measured water flow (discharge) during the monitoring season. We further collected samples at the outflow of the other four streams nearby. Water samples were analyzed in the laboratory for different chemical properties that help us to understand the influence of permafrost degradation. For the six streams, we found that the total disturbed area decreased by 41% between 1952 and 2015, whereas the total number of disturbances increased by 66%. We were able to link permafrost degradation to changes in chemical water composition within the two neighboring streams. It is important that disturbances are “hydrologically connected” to impact concentrations of inorganic compounds (total dissolved solids) and mud (suspended sediment) in the streams. Essentially, this means that water needs to flow through these disturbances to mobilize the material and influence the concentration in the stream. Taking all studied streams together, the overall flux of dissolved organic carbon, total dissolved solids, and total dissolved nitrogen (i.e., the amount of chemical compound in kg transported away in every liter of river water) depends on catchment size. The larger the catchment, the more of this material is transported away. This relationship could not be confirmed for suspended sediment, because a hydrologically connected retrogressive thaw slump heavily impacted the flux in one of the streams. This study is important because the river water ultimately drains into the Arctic Ocean and might change the water quality there. This may have consequences for the animals and plants living in the ocean. We need to understand the influence of permafrost degradation on stream water quality to assess future changes of the Arctic Ocean.
Key Points
Between 1952 and 2015, the total disturbed area decreased by 41%, and the number of disturbances increased by 66%
Hydrological connectivity of permafrost disturbances is essential to impact suspended sediment and solute concentrations in the stream
There is a linear relationship between catchment size and daily flux of dissolved organic carbon, total dissolved nitrogen, and solutes
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