Extending the QuikSCAT record of seasonal melt-freeze transitions over Arctic sea ice using ASCAT

- Seasonal melt-freeze transitions were obtained over Arctic sea ice with ASCAT/QSCAT.
- The retrieval differences between ASCAT/QSCAT over Arctic sea ice are characterized.
- ASCAT is shown to be applicable for extending the seasonal-transition record of QSCAT.

The seasonal melt-freeze transitions are important to continuously monitor over Arctic sea ice in order to better understand Arctic climate variability. The Ku-band scatterometer QuikSCAT (13.4 GHz), widely used to retrieve pan-Arctic seasonal transitions, discontinued its decadal long record in 2009. In this study, we show that the C-band scatterometer ASCAT (5.3 GHz), in orbit since 2006 and with an anticipated lifetime through 2021, can be used to extend the QuikSCAT record of seasonal melt-freeze transitions. This is done by (1) comparing backscatter measurements over multiyear and first-year ice, and by (2) retrieving seasonal transitions from resolution-enhanced ASCAT and QuikSCAT measurements and comparing the results with independent datasets. Despite operating in different frequencies, ASCAT and QuikSCAT respond similarly to surface transitions. However, QuikSCAT measurements respond slightly stronger to the early melt of first-year ice, making it less sensitive to sea-ice dynamics. To retrieve the transitions, we employed an improved edge-detector algorithm, which was iterated and constrained using sea-ice concentration data, efficiently alleviating unreasonable outliers. This gives melt-freeze transitions over all Arctic sea ice north of 60°N at a 4.45 km resolution during 1999-2009 and 2009-2012 for QuikSCAT and ASCAT, respectively. Using the sensor overlap period, we show that the retrieved transitions retrieved from the different instruments are largely consistent across all regions in the Arctic sea-ice domain, indicating a robust consistency.