Navigation Research Projects
Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003 - 2015

The presence of sea-ice leads represents a key feature of the Arctic sea ice cover. Leads promote the flux of sensible and latent heat from the ocean to the cold winter atmosphere and are thereby crucial for air-sea-ice-ocean interactions. We here apply a binary segmentation procedure to identify leads from MODIS thermal infrared imagery on a daily time scale. The method separates identified leads into two uncertainty categories, with the high uncertainty being attributed to artifacts that arise from warm signatures of unrecognized clouds. Based on the obtained lead detections, we compute quasi-daily pan-Arctic lead maps for the months of January to April, 2003 - 2015. Our results highlight the marginal ice zone in the Fram Strait and Barents Sea as the primary region for lead activity. The spatial distribution of the average pan-Arctic lead frequencies reveals, moreover, distinct patterns of predominant fracture zones in the Beaufort Sea and along the shelf-breaks, mainly in the Siberian sector of the Arctic Ocean as well as the well-known polynya and fast-ice locations. Additionally, a substantial inter-annual variability of lead occurrences in the Arctic is indicated.

Willmes, S. and G. Heinemann, 2013: Pan-Arctic lead detection from MODIS thermal infrared imagery.
Annals of Glaciology, 56(69):29-37. DOI: 10.3189/2015AoG69A615

Willmes, S. and G. Heinemann, 2016: Sea-Ice Wintertime Lead Frequencies and Regional Characteristics in the Arctic, 2003 - 2015.
Remote Sensing, 8(1), 4; DOI: 10.3390/rs8010004

Quasi-daily pan-Arctic lead maps, 2003 - 2015:

(click on individual year number to access monthly maps and animations)

Annual lead frequencies, January to April, 2003 - 2015, frequency values are cut off at 0.5 to better highlight the variability at lower values. Grey areas denote regions with a clear-sky frequency less then 15%.