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Hydrological response to warm and dry weather: do glaciers compensate?
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Hydrological response to warm and dry weather: do glaciers compensate?
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Climate change will increase potential hydropower production in six Arctic Counc...
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Ten-year trends of atmospheric mercury in the high Arctic compared to Canadian s...
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Springtime aerosol load as observed from ground-based and airborne lidars over n...
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High levels of ultraviolet radiation observed by ground-based instruments below...
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A 50 % increase in the mass of terrestrial particles delivered by the Mackenzie...
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Seasonality of aerosol optical properties in the Arctic
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Light-absorbing impurities in Arctic snow
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Variations in the vertical profile of ozone at four high-latitude Arctic sites f...
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Evaluating modelled tropospheric columns of CH4, CO and O3 in the Arctic using g...
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Similarities and differences in polar mesosphere summer echoes observed in the A...
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Monitoring Sudden Stratospheric Warmings using radio occultation: a new approach...
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Characteristics of Arctic winds at CANDAC-PEARL (80° N, 86° W) and Svalbard (78°...
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Arctic tidal characteristics at Eureka (80° N, 86° W) and Svalbard (78° N, 16° E...
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Special Observing Period (SOP) Data for the Year of Polar Prediction site Model...
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Evaluating modelled tropospheric columns of CH4, CO, and O3 in the Arctic using...
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Data Quality of OpenStreetMap for Industrial Sites in the Arctic
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Hocking, W. K.
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Raut, Jean-Christophe
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Beagley, Stephen
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