57A182
Changes in SAR backscatter and the seasonal evolution of snow
and sea-ice properties on Miquelon Lake, a small saline lake in Alberta
Justin F. Beckers, Christian Haas, Benjamin A. Lange
Corresponding author: Justin F. Beckers –
beckers@ualberta.ca
Sea-ice coverage in the Arctic is changing more rapidly
than expected. To better understand these changes, more information on ice and
snow thickness is required. However, little is known about their spatial
distribution and change. Improved snow-thickness information is required for ice
thermodynamic models and ice-thickness retrieval from satellite altimetry. In
order to refine observations and modeling of the properties of snow on sea ice
and to support satellite radar algorithms for the retrieval of snow properties,
we have performed a seasonal study of snow and ice properties on Miquelon Lake,
a saline lake in Alberta, which serves as a sea-ice analogue. In the winters of
2008/09 and 2009/10, measurements of snow and ice thickness and temperatures
were performed at hourly intervals using an autonomous station. Additional snow
and ice sampling was conducted every 2–3 weeks to gather data of snow
density, stratigraphy and the spatial variability of snow and ice thickness.
Airborne measurements of ice thickness and freeboard were performed by means of
electromagnetic sounding and laser altimetry to develop advanced algorithms for
snow- and ice-thickness retrieval. Results of the seasonal development of snow
and ice thickness and properties from the field measurements are compared with
changes in X- and C-band backscatter imagery from the TerraSAR and Envisat
platforms.
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