Articles | Volume 9, issue 18
https://doi.org/10.5194/acp-9-6881-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-9-6881-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
21 Sep 2009
Physical properties of High Arctic tropospheric particles during winter
L. Bourdages
Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Canada
T. J. Duck
Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Canada
G. Lesins
Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Canada
J. R. Drummond
Department of Physics and Atmospheric Science, Dalhousie University, Halifax, Canada
E. W. Eloranta
Space Science and Engineering Center, University of Wisconsin, Madison, USA
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- The vertical distribution of thin features over the Arctic analysed from CALIPSO observations: Part I: Optically thin clouds A. Devasthale et al. 10.1111/j.1600-0889.2010.00516.x
- Water vapor intrusions into the High Arctic during winter J. Doyle et al. 10.1029/2011GL047493
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- Thin ice clouds in the Arctic: cloud optical depth and particle size retrieved from ground-based thermal infrared radiometry Y. Blanchard et al. 10.5194/amt-10-2129-2017
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- Astronomical Sky Quality Near Eureka, in the Canadian High Arctic E. Steinbring et al. 10.1086/664444
- Influence of Humidified Aerosol on Lidar Depolarization Measurements below Ice-Precipitating Arctic Stratus B. van Diedenhoven et al. 10.1175/JAMC-D-11-037.1
- Short-cut transport path for Asian dust directly to the Arctic: a case study Z. Huang et al. 10.1088/1748-9326/10/11/114018
- Selected topics in arctic atmosphere and climate W. Perrie et al. 10.1007/s10584-012-0493-6
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- Cloud Microphysical Properties Retrieved from Downwelling Infrared Radiance Measurements Made at Eureka, Nunavut, Canada (2006–09) C. Cox et al. 10.1175/JAMC-D-13-0113.1
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