Articles | Volume 14, issue 2
https://doi.org/10.5194/amt-14-1127-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-14-1127-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Arctic observations and numerical simulations of surface wind effects on Multi-Angle Snowflake Camera measurements
Department of Atmospheric Sciences, University of Utah, Salt Lake City, UT, USA
Department of Engineering Physics, Air Force Institute of Technology, Wright-Patterson Air Force Base, OH, USA
Chaoxun Hang
Department of Civil Engineering, Monash University, Clayton, Australia
School of Oceanography, Shanghai Jiao Tong University, Shanghai, China
Ahmad Talaei
Department of Atmospheric Sciences, University of Utah, Salt Lake City, UT, USA
Timothy J. Garrett
Department of Atmospheric Sciences, University of Utah, Salt Lake City, UT, USA
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Short summary
Snow measurements are very sensitive to wind. Here, we compare airflow and snowfall simulations to Arctic observations for a Multi-Angle Snowflake Camera to show that measurements of fall speed, orientation, and size are accurate only with a double wind fence and winds below 5 m s−1. In this case, snowflakes tend to fall with a nearly horizontal orientation; the largest flakes are as much as 5 times more likely to be observed. Adjustments are needed for snow falling in naturally turbulent air.
Snow measurements are very sensitive to wind. Here, we compare airflow and snowfall simulations...