Ruzica Dadic

TL;DR: In this article, a nonhydrostatic and compressible atmospheric prediction model was applied to steep alpine topography and compared the results to a fully distributed data set of snow depth estimations.

TL;DR: In this paper, the authors used topographic parameters to model the snow depth distribution on the catchment-scale by applying multiple linear regressions and found that by averaging out the substantial spatial heterogeneity at the metre scales, i.e. individual drifts and aggregating snow accumulation at the landscape or hydrological response unit scale (cell size 400 m), that 30 to 91% of the variability can be explained by models that are calibrated to local conditions at the single study areas.

TL;DR: In this article , the physical properties and processes that govern the ice pack evolution and its interaction with the atmosphere and the ocean were conducted during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition of the research vessel Polarstern in the Arctic Ocean from October 2019 to September 2020.

TL;DR: Spectral albedo was measured along a 6 km transect near the Allan Hills in East Antarctica as mentioned in this paper, showing a systematic progression of decreasing albed at all wavelengths, as well as decreasing specific surface area (SSA) and increasing density.

TL;DR: The albedo and transmittance of melting first-year Arctic sea ice were measured during two cruises of the Impacts of Climate on the Eco-Systems and Chemistry of the Arctic Pacific Environment (ICESCAPE) project during the summers of 2010 and 2011 as discussed by the authors.