Metamorphism of Arctic marine snow during the melt season. Impact on spectral albedo and radiative fluxes through snow

• Main Authors: Vérin, Gauthier, Domine, Florent, Babin, Marcel, Picard, Ghislain, Arnaud, Laurent
• Format: Text
• Language: English
• Published: 2022
• Subjects: Arctic; Baffin Bay; albedo; Baffin; Sea ice
• Online Access: https://doi.org/10.5194/tc-2022-76; https://tc.copernicus.org/preprints/tc-2022-76/

The energy budget of Arctic sea ice is strongly affected by the snow cover. Intensive sampling of snow properties was conducted near Qikiqtarjuak in Baffin Bay on typical landfast sea ice during two melt seasons in 2015 and 2016. The sampling included stratigraphy, vertical profiles of snow specific surface area (SSA), density and irradiance, and spectral albedo (300–1100 nm). Both years featured four main phases: I) dry snow cover, II) surface melting, III) ripe snowpack and IV) melt pond formation. Each phase was characterized by distinctive physical and optical properties. A high SSA value of 49.3 m 2 kg -1 was measured during phase I on surface wind slabs together with a corresponding broadband albedo of 0.87. Phase II was marked by alternating episodes of surface melting which dramatically decreased the SSA below 3 m 2 kg -1 and episodes of snowfall reestablishing pre-melt conditions. Albedo was highly time-variable with minimum values at 1000 nm around 0.45. In Phase III, continued melting led to a fully ripe snowpack composed of clustered rounded grains. Albedo began to decrease in the visible as snow thickness decreased but remained steady at longer wavelengths. Moreover, significant spatial variability appeared for the first time following snow depth heterogeneity. Spectral albedo was simulated by radiative transfer using measured SSA and density vertical profile, and impurity contents based on measurements. Simulations were most of the time within 1 % of measurements in the visible and within 2 % in the infrared. Simulations allowed the calculation of albedo and of the spectral flux at the top of the sea ice. These showed that photosynthetically active radiation fluxes at the bottom of the snowpack durably exceeded 5 W m -2 (about 9.2 µmol m -2 s -1 ) only when the snowpack thickness started to decrease at the end of Phase II.