(Table 1) White ice and melt pond characteristics in Darnley and Franklin Bay, Canada

• Main Authors: Ehn, Jens K, Mundy, Christopher John, Barber, David G, Hop, Haakon, Rossnagel, Andrea L, Stewart, Jeremy
• Format: Dataset
• Language: English
• Published: PANGAEA 2011
• Subjects: Amundsen Gulf; Canada; Darnley_Bay_Site1; Darnley_Bay_Site3; DATE/TIME; Event label; Franklin_Bay_Site2; Franklin_Bay_Site4; Freeboard; Ice draft; ICEM; Ice measurement; International Polar Year (2007-2008); International Polar Year 2007-2008; IPY; IPY-4; Irradiance; incident; photosynthetically active; Melt pond depth; Melt pond freeboard; Sample type; Sea ice thickness; Site; Transmittance; Water level; Arctic; Arctic Ocean; Darnley; albedo; Franklin Bay; International Polar Year; Sea ice
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.809476; https://doi.org/10.1594/PANGAEA.809476

Melt pond covered sea ice is a ubiquitous feature of the summertime Arctic Ocean when meltwater collects in lower-lying areas of ice surfaces. Horizontal transects were conducted during June 2008 above and below landfast sea ice with melt ponds to characterize surface and bottom topography together with variations in transmitted spectral irradiance. We captured a rapid progression from a highly flooded sea ice surface with lateral drainage toward flaws and seal breathing holes to the formation of distinct melt ponds with steep edges. As the mass of the ice cover decreased due to meltwater drainage and rose upward with respect to the seawater level, the high-scattering properties of ice above the water level (i.e., white ice) were continuously regenerated, while pond waters remained transparent compared to underlying ice. The relatively stable albedos observed throughout the study, even as ice thickness decreased, were directly related to these surface processes. Transmission through the ice cover of incident irradiance in the 400-700 nm wave band ranged from 38% to 67% and from 5% to 16% beneath ponded and white ice, respectively. Our results show that this transmission varied not only as a function of surface type (melt ponds or white ice) areal coverage but also in relation to ice thickness and proximity to other surface types through the influence of horizontal spreading of light. Thus, in contrast to albedo, this implies that regional transmittance estimates need to consider melt pond size and shape distributions and variations in optical properties and thickness of the ice cover.