Modeling the impediment of methane ebullition bubbles by seasonal lake ice

The measured amounts of (a) CH 4 and (b) O 2 dissolved in the water column of Goldstream Lake during the study period, and those calculated in the baseline and “less diffusion”

We have presented in detail the Elmer/Ice ice sheet flow model, from the equations implemented to the way they are solved using the FE method. Elmer/Ice contains a high me-

Based on their PC1 mean brightness values, bubble patches identified in aerial images as C- and A-type seeps, Hotspot and A-type seeps, and Hotspot and B-type seeps for 2011; and C-

One major di ff erence lies in the specific combination of bed deep- ness and ice thickness: while a large area of the ice sheet in the Weddell Sea Sector (namely the Institute

number of strandings of migrants species results from the release of ice barriers and distribution changes in winter and early summer [51]; low ice volume into the Gulf could yield

4, we finally compare the magnitude and pacing of past temperature changes reconstructed from deep ice cores to the changes simulated by coupled ocean-atmosphere-sea- ice models

The mean values and uncertainties of snow depth and ice and snow densities, determined for FY ice and MY ice, were used to calculate the total error in ice thickness retrieval

On account of both the inhibition of ice crystallisation and the likely limited uptake of water into highly viscous organic acid solution droplets it seem probable that