  Young sea ice composed of grease and pancake ice (GPI), as well as thin
floes, considered to be the most common form of sea ice fringing Antarctica, is
now becoming the 'new normal' also in the Arctic. Investigations to determine
how an increase in GPI is affecting the climate in the far north and globally,
require specific tools to monitor the GPI's thickness distribution. Directional
wave spectra from satellite SAR imagery are used to determine the change in
wave dispersion as a wave train enters GPI fields. The ice cover thickness is
then estimated by fitting the dispersion data with two models of wave
propagation in ice cover ocean: the Keller's model and the close-packing (CP)
model.
  For both models, an empirical constitutive equation for GPI viscosity as a
function of the ice thickness is derived and discussed. Examples of GPI
thickness retrievals are shown for a Sentinel-1 C band SAR image taken in the
Beaufort Sea on 1 November 2015, and three CosmoSkyMed X band SAR images taken
in the Weddell Sea on March 2019. The estimated GPI thicknesses are consistent
with concurrent SMOS measurements and the available local samplings.
