C-band SAR backscatter characteristics of Arctic sea and land ice during winter

• Published in: Tropical Medicine and Health
• Main Authors: Steffen, Konrad, Heinrichs, John
• Format: Text
• Language: unknown
• Published: FHSU Scholars Repository 2001
• Subjects: Geology; Nunavut; polar night; Sea ice
• Online Access: https://scholars.fhsu.edu/geo_facpubs/4; https://doi.org/10.1080/07055900.2001.9649682; https://scholars.fhsu.edu/context/geo_facpubs/article/1003/viewcontent/Steffen_Heinrichs_2000_C_band_SAR_backscatter.pdf

Synthetic Aperture Radar (SAR) data has become an important tool for studies of polar regions, due to high spatial resolution even during the polar night and under cloudy skies. We have studied the temporal variation of sea and land ice backscatter of twenty-four SAR images from the European Remote Sensing satellite (ERS-1) covering an area in Lady Ann Strait and Jones Sound, Nunavut, from January to March 1992. The presence of fast ice in Jones Sound and glaciers and ice caps on the surrounding islands provides an ideal setting for temporal backscatter studies of ice surfaces. Sample regions for eight different ice types were selected and the temporal backscatter variation was studied. The observed backscatter values for each ice type characterize the radar signatures of the ice surfaces. This time series of twenty-four SAR images over a 3-month period provides new insights into the degree of temporal variability of each surface. Ice caps exhibit the highest backscatter value of -3.9 dB with high temporal variability. Valley glacier ice backscatter values decrease with decreasing altitude, and are temporally the most stable, with standard deviations of 0.08–0.10 dB over the 90-day period. First-year ice and lead ice show a negative trend in backscatter values in time and a positive correlation of up to 0.59 with air temperature over the 90-day period. For first-year ice and lead ice, episodes of large temperature fluctuations (±12°C) are associated with rapid changes in backscatter values (±2 dB). We attribute the backscatter increase to a temperature-induced increase in brine volume at the base of the snow pack. Multi-year ice, conglomerate ice and shore ice are relatively stable over the 3-month period, with a backscatter variation of only a few dBs. An observed lag time of up to three days between backscatter increase/decrease and air temperature can be attributed to the insulation effect of the snow cover over sea ice. The net range of the backscatter values observed on the most temporally stable ...