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Very high frequency deep radio sounding systems for ice thickness measurements are practically the only useful apparatuses for large scale radar flight surveys in polar regions. The morphology of the ...
During three Antarctic summer campaigns (1995/97/99) Radio Echo Sounding (RES) system data from some glacier ice tongues in the East Antarctic regions between Victoria Land and George V Land were coll...
The monterey bay broadband ocean bottom seismic observatory     seismic station  San Gregorio Fault  earthquake       font style='font-size:12px;'> 2015/9/7
We report on the installation of a long-term buried ocean-floor broadband seismic station (MOBB) in Monterey Bay, California (USA), 40km off-shore, at a water depth of 1000 m. The station was instal...
From bottom landers to observatory networks     landers  multidisciplinary long term observatories  global change       font style='font-size:12px;'> 2015/9/7
For a long time, deep-sea investigation relied on autonomous bottom landers. Landers can vary in size from 200 kg weight to more than 2 t for the heaviest scientific landers and are used during explo...
Analysis of ADCP data above a bottom observatory     ADCP sensitivity  current lines inclination  observatory’  s wake       font style='font-size:12px;'> 2015/9/7
A 300-kHz ADCP was set on GEOSTAR, a six-m3 deep-sea observatory. It was operated with cells of 80 cm during a three-week test experiment at 42-m water depth in the northern Adriatic sub-basin. Altho...
For the update 2012 of CORINE Land Cover, in Germany a new approach has been developed in order to profit from the higher accuracies of the national topographic database. In agreement between the Fe...
We examine the interaction of near-surface and near- bottom flows over bottom topography. A set of asymptotic equations for geostrophic currents in a three-layer fluid is derived. The depths of the ac...
In this paper we study the transformation of an internal solitary wave at a bottom step in the framework of two-layer flow, for the case when the interface lies close to the bottom, and so the solitar...
About Bottom Friction Caused by an Alternating Wind     Bottom Friction  Alternating Wind  friction law       font style='font-size:12px;'> 2009/6/18
About Bottom Friction Caused by an Alternating Wind.

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