Tc. Grenfell et al., EVOLUTION OF ELECTROMAGNETIC SIGNATURES OF SEA-ICE FROM INITIAL FORMATION TO THE ESTABLISHMENT OF THICK FIRST-YEAR ICE, IEEE transactions on geoscience and remote sensing, 36(5), 1998, pp. 1642-1654
The spatial and temporal distribution of new and young sea ice types a
re of particular interest because of the influence this can exert on t
he heat and mass balance of the polar sea ice. The objective of the pr
esent work is to characterize the temporal evolution of the electromag
netic (EM) signatures of sea ice from initial formation through the de
velopment of first-year (FY) ice on the basis of the temporal variatio
ns in the physical properties of the ice. The time series of young sea
ice signatures, including microwave emissivity, radar backscatter, an
d visible and infrared spectral albedo, has been measured at successiv
e stages in the growth and development of sea ice, both under laborato
ry and field conditions. These observations have been accompanied by s
tudies of the physical properties that influence the interaction betwe
en radiation and the ice. This has resulted in a consistent data set o
f concurrent multispectral observations that covers essentially all ph
ases of the development of the different types of sea ice from initial
formation to thick FY ice. Mutually consistent theoretical models cov
ering the entire wavelength range of the observations are applied to s
elected cases and successfully match the observations. Principal compo
nent analysis (PCA) of the data set suggests combinations of the set o
f frequencies to effectively distinguish among different stages in the
temporal evolution of the sea ice.