EGU21-8966
https://doi.org/10.5194/egusphere-egu21-8966
EGU General Assembly 2021
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Unmanned Aerial System measurements of surface albedo for the melting season during the MOSAiC expedition

Radiance Calmer1,3, Gijs de Boer1,2, Jonathan Hamilton4, John Cassano1,3, Gina Jozef1,3, Dale Lawrence4, Steve Borenstein4,5, Abhiram Doddi4, Brian Argrow4,5, Matthew Shupe1,2, and Christopher Cox2
Radiance Calmer et al.
  • 1Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80304, USA
  • 2NOAA Physical Sciences Laboratory, Boulder, CO 80305, USA
  • 3National Snow and Ice Data Center, University of Colorado Boulder, Boulder, CO 80304, USA
  • 4Department of Aerospace Engineering, University of Colorado Boulder, Boulder, CO, USA
  • 5Integrated Remote and In Situ Sensing (IRISS), University of Colorado Boulder, Boulder, CO, USA

The University of Colorado, Boulder, deployed unmanned aerial systems (UAS) over the sea ice during Leg 4 (June-August 2020) of the MOSAiC expedition. Among the different UAS platforms operated, a hexacopter, the HELiX, was dedicated for characterizing the surface properties, such as the surface albedo and the sea ice/melt pond fractions. The HELiX was equipped with two pyranometers to measure incoming and reflected broadband shortwave irradiance, and a multispectral camera to map the surface of the ice floe. Three flight plans were conducted with this platform, including (1) grid patterns at 10 m.asl to map out the distribution of albedo at this altitude, (2) hovering flights at 3 m.asl over identified surfaces (sea ice, melt pond, ocean, ridge, etc.) to get a detailed look at the albedo of each surface individually, and (3) profiles up to 100 m.asl. to evaluate the convergence height where surface heterogeneity is obscured when using a hemispheric sensor. In total, 34 flights took place in varied weather conditions, from clear sky to foggy weather with very low visibility. The UAS observations bring complementary results to a variety of other albedo observations collected during MOSAiC (albedo lines, sled-based, tethered balloon-based, and ship-based measurements).  These observations spanned the majority of the melt season, capturing seasonal evolution in surface reflectivity, as well as melt pond fraction and resulting impact on surface albedo.  In this presentation, we will present results from these flight activities and offer perspectives on the evolving sea ice pack during the summer portion of the MOSAiC expedition.

How to cite: Calmer, R., de Boer, G., Hamilton, J., Cassano, J., Jozef, G., Lawrence, D., Borenstein, S., Doddi, A., Argrow, B., Shupe, M., and Cox, C.: Unmanned Aerial System measurements of surface albedo for the melting season during the MOSAiC expedition, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-8966, https://doi.org/10.5194/egusphere-egu21-8966, 2021.

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