The evolution of Miocene ocean circulation controlled by the Greenland-Scotland Ridge Michael Stärz

It is shown that an accurate knowledge of wind conditions is crucial for de- riving internal wave parameters and hence parameters of the interior ocean dynamics from the

Simulated northward, southward, and net northward (northward-southward) volume (Sv), heat flow (TW) and fresh water flux (0.01 Sv) through the Denmark Strait (DS), across

Produced by a mixture of overflow waters from the Iceland-Scotland Ridge and Northeast Atlantic Water, the Charlie Gibbs Fracture Zone (CGFZ) Water forms the middle

HOLSER et al. It is easy to estimate the effect of young evaporite extractions on lowering the salinity of the ocean, but because of the supply of salt from

A major reason for this low variability found in the DYNAMO (and also CME) models is the lack of horizontal resolution which does not allow a full res- olution of eddy dynamics,

The comparison of the corresponding bottom pressure anomalies (mean annual cycle) to the geoid variations estimated from the GRACE mission (in cm watercolumn analog, lower left

The predominant effect of model friction on small scales can also be seen in instantaneous fields of sea surface height: Fig- ure 9 displays SSH maps for a small region of

The horizontal heat flux (relative to 0.1C) pattern integrated over the upper 500 m watercolumn which is associated with the time series of net heat transport from the Nordic seas