Seasonal evolution of L-band SAR backscatter over landfast Arctic sea ice

We construct and present the first baseline, time series evolution of L-band SAR microwave backscatter (sigma 0HH) for landfast Arctic first-year (FYI) and multi-year (MYI) sea ice from ALOS PALSAR. We compare the winter to freeze-up seasonal L-band sigma 0HH signatures with C-band RADARSAT-2 SAR imagery and Ku-band QuikSCAT scatterometer data. We also explored the utility of L-band sigma 0HH to detect FYI and MYI melt onset dates. For both ice types, L-band exhibited a similar sigma 0HH evolution to Cand Ku-bands. A rise in L-band sigma 0HH was observed from winter to melt onset, however, with a lower magnitude attributed to the larger penetration of L-band microwaves through the snow-covered sea ice medium. Over FYI, L-band sigma(0)(HH) exhibited the most robust response and greater diversity in melt onset signature, compared to Cand Ku-bands. Over MYI, L-band sigma(0)(HH) declined during the winter to melt onset transition contrasting the Cand Ku-band evolution of sigma(0)(HH) during melt onset. Although, a distinct L-band sigma(0)(HH) response was not found during pond onset, a very strong sigma(0)(HH) response was found during sea ice break-up, which could operationally be utilized to identify sea ice break-up timing. During freeze-up, L-band sigma(0)(HH) showed greater diversity compared to Cand Ku-bands. Our study also found that, L-band detected melt onset dates were up to 6 days later than Cand Ku-band detected dates, for both ice types. The melt response was the strongest at L-band for FYI, where C-band detected a robust melt onset date for MYI. Therefore, for operational sea ice monitoring, L-band suits better for FYI, whereas C-band is still a better choice for MYI. In the warming Arctic, where FYI has become the dominant ice type, L-band demonstrates promise to be the optimal choice for sea ice operational monitoring with high spatiotemporal data acquisition from existing, upcoming and proposed L-band SAR missions.