1. Introduction and Present State of Art
Polar scientists presently lack access to effective capabilities in ice-margin and under-ice environments for examining the submerged features of ice shelves, icebergs, and sea ice as well as the seafloor under ice shelves. Conventionally-tethered ROV systems have been deployed under ice (Bono 1999, Nokin 2000), but are limited to horizontal ranges of a few hundred meters from their support ships or the ice-edge, and, consequently, impose severe restrictions in environments where under sea-ice and ice shelf ice is too thick to break. The inspection-class Submersible Capable of under Ice Navigation and Imaging (SCINI) is an exception (Cazenave 2011), having been designed for deployment through 8” diameter bore holes in sea ice. SCINI's operational record has demonstrated the value of an under-ice inspection capability but is unproven through the relatively deep holes that would be required to access the sub-glacial environment, and the vehicle's size limits it to a modest sensing payload. Autonomous underwater vehicles (AUVs) have operated successfully under sea-ice since the 1970s, e.g. Theseus (Ferguson 1999), and, more recently, under ice shelves, e.g. Autosub (McPhail 2009). These missions have yielded invaluable physical oceanographic measurements and maps of ice draft and seafloor bathymetry; however, close-up high-resolution inspection remains beyond the scope of present-day and long range acoustic telemetry.