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Astronomical Sky Quality Near Eureka, in the Canadian High Arctic
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Drone measurements of surface-based winter temperature inversions in the High Ar...
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Lidar measurements of thin laminations within Arctic clouds
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The Relationship between Clouds Containing Multiple Layers 7.5–30 m Thick and Su...
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The Polar Environment Atmospheric Research Laboratory (PEARL): A Scientific Faci...
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The Relationship between Clouds Containing Multiple Layers 7.5–30 m Thick and Su...
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Calibration and validation of the advanced E-Region Wind Interferometer
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total columns measured in the Canadian high Arctic
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Five years of CO, HCN, C 2 H 6 , C 2 H 2 , CH 3 OH, HCOOH and H 2 CO total colum...
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Physical properties of High Arctic tropospheric particles during winter
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Conclusions References
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© Author(s) 2009. This work is distributed under the Creative Commons Attributio...
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Large surface radiative forcing from topographic blowing snow residuals measured...
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Methane cross-validation between three Fourier transform spectrometers: SCISAT A...
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Three-channel single-wavelength lidar depolarization calibration
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Ozone Measurements Using the Refurbished Eureka Stratospheric Differential Absor...
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Vertical and interhemispheric links in the stratosphere-mesosphere as revealed b...
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Year-round retrievals of trace gases in the Arctic using the Extended-range Atmo...
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Transient climate simulations of the deglaciation 21–9 thousand years before pre...
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Characteristics of Arctic winds at CANDAC-PEARL (80° N, 86° W) and Svalbard (78°...
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