The Baltic, sheltered from the strong North Sea tides, is remarkable for the general absence of tidal currents. Although the greatinfluxofriverwater andsurface runoff, including spring snowmelt, causes an outflow of surface water into the North Sea, a deeper countercurrent of densersalt waterflo...
generally are not smooth, whether considered from the viewpoint of either speed or direction. They are chiefly influenced by blowing winds. Water temperatures in the Aegean are influenced by the cold-water masses of low temperature that flow in from theBlack Seato the northeast. The sea surface...
The views are rotated to match the orientation of the Red Sea map (panel a) with the plume always located towards the bottom of each map (see north-indicators). PD = Plume Domain, roughly indicated by the black dashed line. The colour-key is the same as in Fig. 3 for all ...
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Introduction Fig. 1: Overview map of the study area in the German Bight of the North Sea. Results Modern echosounding of seafloor depressions in the German Bight Fig. 2: High-resolution bathymetric data from the formerly reported pockmark field north of Heligoland. ...
Figure 1.1.Map of the Mediterranean Sea, where the main geographical names mentioned in the book are indicated. Background: bathymetry and topography with blue and gray scales, respectively. The topographic data set used is the GEBCO Compilation Group (2020) GEBCO 2020 Grid (https://doi.org/10...
Fig. 25.1.Map of Sulawesi and the Sulawesi Seas, with provincial boundaries, capitals, major island groups, and features mentioned in the text. While most of the volcanoes along the northern arm of Sulawesi Island and forming the Sangihe Islands, stretching north toward the Philippines, are extin...
The Sea Level Rise app allows anyone to map the flooding in their community, helping document sea level rise and other flooding impacts. While virtually everyone in and around a low-lying coastal region is or will be affected by sea level rise, we started our work in Hampton Roads, Virginia...
system north of the bay produces northeast winds (the northeast monsoon)characteristicof the winter season. During the northern summer (June–September) the rain-bearing southwest monsoon prevails, as intense heat produces a low-pressure system over the continent and a subsequent air flow from the...
From the histogram of wind direction in Figure 6B, one may notice that prevailing CCLM-CMCC winds are triggered by northeasterly Bora storms. The peak’s observed and model flow direction (around 230° N) are consistent, accounting for the mentioned angular difference. We note the good match...