Only near the edge does the ice flow accelerate toward the ocean, and the unique vertical velocity profile in Figure 2 then becomes clear. Moreover, right south of the Byrd Ice Stream, there is a stagnant region with ice flow speed less than 50 m/yr. The small ice velocities for ...
IDW is rich in remineralized carbon and correspondingly less enriched in 13C (Talley et al., 2013), leading to the δ13CDIC minimum we observed in the east of our study region, particularly within the Perth Basin. Immediately south of Broken Ridge (line C–D in Figure 2b), there is ...
This layer can likely store water in the very near surface as observed at another wetland by Strobach et al. [2013] that may evaporate after rainfall and explain delayed wetting. Regime III at HHW is a combination of a vegetated test site and several indurated and cemented soil horizons. ...