Wj. Emery et al., ARCTIC SEA-ICE CONCENTRATIONS FROM SPECIAL SENSOR MICROWAVE IMAGER AND ADVANCED VERY HIGH-RESOLUTION RADIOMETER SATELLITE DATA, J GEO RES-O, 99(C9), 1994, pp. 18329-18342
Nearly coincident data from the special sensor microwave imager (SSM/I
) and the advanced very high resolution radiometer (AVHRR) are used to
compute and compare Arctic sea ice concentrations for different regio
ns and times of the year. To help determine overall accuracies and to
highlight sources of differences between passive microwave, optical wa
velength, and thermal wavelength data, ice concentrations are estimate
d using two operational SSM/I ice concentration algorithms and with vi
sible- and thermal-infrared wavelength AVHRR data. All algorithms capt
ure the seasonal patterns of ice growth and melt. The ranges of differ
ences fall within the general levels of uncertainty expected for each
method and are similar to previous accuracy estimates. The estimated i
ce concentrations are all highly correlated, with uniform biases, alth
ough differences between individual pairs of observations can be large
. On average, the NASA Team algorithm yielded 5% higher ice concentrat
ions than the Bootstrap algorithm, while during nonmelt periods the tw
o SSM/I algorithms agree to within 0.5%. These seasonal differences ar
e consistent with the ways that the 19-GHz and 37-GHz microwave channe
ls are used in the algorithms. When compared to the AVHRR-derived ice
concentrations, the Team-algorithm results are more similar on average
in terms of correlation and mean differences. However, the Team algor
ithm underestimates concentrations relative to the AVHRR output by 6%
during cold months and overestimates by 3% during summer. Little seaso
nal difference exists between the Boostrap and AVHRR results, with a m
ean difference of about 5%. Although the mean differences are less bet
ween the SSM/I-derived concentrations and concentrations estimated usi
ng AVHRR channel 1, the correlations appear substantially better betwe
en the SSM/I data and concentrations derived from AVHRR channel 4, par
ticularly for the Team algorithm output.