Physical and mechanical properties of ice from a refrozen ship channel ice in Bay of Bothnia

The pleasure of the private bath notwithstanding, the Japanese still like to go into town to visit the sento, or to the hot spring to benefit from the onsen. where they

However, if the polygon is concave, it is first triangulated using constrained Delaunay triangulation library Poly2Tri (Green, 2013). During this process the software discards

Figure 26: h − ν curve obtained when the vessel is running astern (the scaled model-scale sim- ulation results and the full-scale simulation results with scaled ice and

The weak points in all of the reconstruction are the missing magnetic spreading anomalies north of the Greenland Fracture Zone and the lack of any geophysical data along the

Liu and Meek [41] presented the Likelihood Ratio Test (LRT) Polarimetric SAR (PolSAR) Ship Detection Application, which detects vessels in different polarimetric SAR systems,

Macroporosity values from the brash ice can be obtained by estimating the ice volume from the weight of the lifted ice mass and divide this by the total volume of brash ice

The same approach to determine total porosity was used by Shafrova and Hoyland (2007) and Moslet (2006) for their compression tests, which amongst others will be used as

- Ice strengthening (hull strength & machinery power etc.) => Ice class requirements - Restrictions to navigation (ice class & ship size). -