Automated Detection and Depth Determination of Melt Ponds on Sea Ice in
ICESat-2 ATLAS Data — The Density-Dimension Algorithm for Bifurcating
Sea-Ice Reflectors (DDA-bifurcate-seaice)
Abstract
As climate warms and the transition from a perennial to a seasonal
Arctic sea-ice cover is imminent, understanding melt ponding is central
to understanding changes in the new Arctic. NASA’s Ice, Cloud and land
Elevation Satellite (ICESat-2) has the capacity to provide measurements
and monitoring of the onset of melt in the Arctic and on melt
progression. Yet ponds are currently not reported on the ICESat-2
standard sea-ice products because of the low resolution of the products,
in which only a single surface is determined.
The objective of this paper is to introduce a mathematical algorithm
that facilitates automated detection of melt ponds in ICESat-2 ATLAS
data, retrieval of two surface heights, pond surface and bottom, and
measurements of depth and width of melt ponds. With the Advanced
Topographic Laser Altimeter System (ATLAS), ICESat-2 carries the first
space-borne multi-beam micro-pulse photon-counting laser altimeter
system, operating at 532~nm frequency. ATLAS data are
recorded as clouds of discrete photon points. The Density-Dimension
Algorithm for bifurcating sea-ice reflectors (DDA-bifurcate-seaice) is
an auto-adaptive algorithm that solves the problem of pond detection
near the 0.7m nominal alongtrack resolution of ATLAS data, utilizing
the radial basis function for calculation of a density field and a
threshold function that automatically adapts to changes in background,
apparent surface reflectance and some instrument effects. The
DDA-bifurcate-seaice is applied to large ICESat-2 data sets from the
2019 and 2020 melt seasons in the multi-year Arctic sea-ice region.
Results are evaluated by comparison to those from a manually forced
algorithm.