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Trichinella nativa and Trichinella T6 in arctic foxes (Vulpes lagopus) from northern Canada
Published 2020-12-01Get full text
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102
Seasonal evolution of the effective thermal conductivity of the snow and the soil in high Arctic herb tundra at Bylot Island, Canada
Published 2016-11-01“…We have monitored <i>k</i><sub>snow</sub> and <i>k</i><sub>soil</sub> using heated needle probes at Bylot Island in the Canadian High Arctic (73° N, 80° W) between July 2013 and July 2015. …”
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Microbial diversity in Antarctic Dry Valley soils across an altitudinal gradient
Published 2023-07-01Get full text
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104
N/P Addition Is More Likely Than N Addition Alone to Promote a Transition from Moss-Dominated to Graminoid-Dominated Tundra in the High-Arctic
Published 2022-04-01“…An annual fertilization experiment simulating these nutrient inputs was conducted for 17 years in the Canadian High-Arctic to assess the impact on aboveground net primary productivity, floristic composition, and plant nutrient concentration. …”
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105
An interhemispheric comparison of GPS phase scintillation with auroral emission observed at the South Pole and from the DMSP satellite
Published 2013-06-01“…The South Pole (SP) station is approximately conjugate with two Canadian High Arctic Ionospheric Network stations on Baffin Island, Canada, which provided the opportunity to study magnetic conjugacy of scintillation with support of riometers and magnetometers. …”
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106
Soil moisture, wind speed and depth hoar formation in the Arctic snowpack
Published 2018-12-01“…At Ward Hunt Island (Canadian high Arctic, 83°05′N, 74°07′W) almost no depth hoar was observed in spring 2016 despite favorable thermal conditions. …”
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107
Depolarization calibration and measurements using the CANDAC Rayleigh–Mie–Raman lidar at Eureka, Canada
Published 2017-11-01“…In remote and meteorologically significant locations, such as the Canadian High Arctic, the ability to add new measurement capability to an existing well-tested facility is extremely valuable. …”
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108
Standardized monitoring of permafrost thaw: a user-friendly, multiparameter protocol1
Published 2022-03-01Get full text
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109
Temporally delineated sources of major chemical species in high Arctic snow
Published 2018-03-01“…To identify the sources of key contaminants entering the Canadian High Arctic an intensive campaign of snow sampling was completed at Alert, Nunavut, from September 2014 to June 2015. …”
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Phytoplankton and dimethylsulfide dynamics at two contrasting Arctic ice edges
Published 2020-03-01“…In July–August 2014, two contrasting ice edges in the Canadian High Arctic were explored: a FYI-dominated ice edge in Barrow Strait and a MYI-dominated ice edge in Nares Strait. …”
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113
Assessing the impact of shipping emissions on air pollution in the Canadian Arctic and northern regions: current and future modelled scenarios
Published 2018-11-01“…In particular, the model is able to simulate the observed O<sub>3</sub> and PM components well at the Canadian high Arctic site, Alert. The model assessment shows that, at the current (2010) level, Arctic shipping emissions contribute to less than 1 % of ambient O<sub>3</sub> concentration over the eastern Canadian Arctic and between 1 and 5 % of ambient PM<sub>2.5</sub> concentration over the shipping channels. …”
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114
Vegetation type is an important predictor of the arctic summer land surface energy budget
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115
Results of a long-term international comparison of greenhouse gas and isotope measurements at the Global Atmosphere Watch (GAW) Observatory in Alert, Nunavut, Canada
Published 2023-12-01“…<p><span id="page5910"/>Since 1999, Environment and Climate Change Canada (ECCC) has been coordinating a multi-laboratory comparison of measurements of long-lived greenhouse gases in whole air samples collected at the Global Atmosphere Watch (GAW) Alert Observatory located in the Canadian High Arctic (82<span class="inline-formula"><sup>∘</sup></span>28<span class="inline-formula"><sup>′</sup></span> N, 62<span class="inline-formula"><sup>∘</sup></span>30<span class="inline-formula"><sup>′</sup></span> W). …”
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Environmental controls of winter soil carbon dioxide fluxes in boreal and tundra environments
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