ON THE RELATIONSHIP BETWEEN ENERGY FLUXES, DIELECTRIC-PROPERTIES, ANDMICROWAVE-SCATTERING OVER SNOW COVERED FIRST-YEAR SEA-ICE DURING THE SPRING TRANSITION PERIOD
Dg. Barber et al., ON THE RELATIONSHIP BETWEEN ENERGY FLUXES, DIELECTRIC-PROPERTIES, ANDMICROWAVE-SCATTERING OVER SNOW COVERED FIRST-YEAR SEA-ICE DURING THE SPRING TRANSITION PERIOD, J GEO RES-O, 99(C11), 1994, pp. 22401-22411
In this research we investigate the seasonal nature of the co-variabil
ity in surface energy balance variables, volume dielectrics, and micro
wave scattering (ERS 1) of a snow-covered first-year sea ice surface d
uring a spring transitional period. Variables required to derive the c
omponents of the energy balance and dielectric properties were measure
d during the Seasonal Sea Ice Monitoring and Modeling site in the Cana
dian Arctic Archipelago in 1992. We observed that both the energy term
s and dielectric properties followed a pattern similar to the total re
lative scattering cross section (sigma(o)) over the seasonal transitio
n from winter to spring. We explain this relationship through the impa
ct of surface fluxes on dielectric and geophysical properties of the s
now-covered first-year sea ice. We speculate that ice surface scatteri
ng dominated the total scattering cross section sigma(o) prior to Juli
an day 120 and that the snow volume contributed an increasing amount o
f scattering to sigma(o) over the remainder of the season. From a mult
ivariate statistical analysis we find that the surface temperature T-S
and the net shortwave energy flux K explained a statistically signif
icant amount of the variation observed in the seasonal evolution of si
gma(o). An inverse relationship existed between both T-S and K relati
ve to sigma(o), and the influence of T-S was approximately twice that
of K in explaining the observed variation in sigma(o).