Abstract The tides are a major driver of global oceanic mixing. While global tidal elevations are very well observed by satellite altimetry, the global tidal transports are much less well known. For twenty years, magnetic signals induced by the ocean tides have been detectable in satellite magnetometer observations, such as Swarm or CHAMP. Here, we demonstrate how satellite magnetometer observations can be used to directly derive global ocean tidal transports. As an advantage over other tidal transport estimates, our tidal estimates base on very few and very loose constraints from numerical forward models
The solar quiet (Sq) source morphology changes on a daily basis and becomes disturbed during periods...
The European Space Agency's three-satellite constellation Swarm, launched in November 2013, has prov...
Motional induction in the ocean by tides has long been observed by both land and satellite measureme...
The tides are a major driver of global oceanic mixing. While global tidal elevations are very well o...
Satellite-measured tidal magnetic signals are of growing importance. These fields are mainly used to...
Ocean-generated magnetic field models of the Principal Lunar, M2, and the Larger Lunar elliptic, N2,...
Periodic tidal ocean currents induce electric currents and, therefore, magnetic field signals that a...
Conducting ocean water, as it flows through the Earth’s magnetic field, generates secondary electric...
Due to their sensitivity to conductivity and oceanic transport, magnetic signals caused by the movem...
Over a decade ago the semidiurnal lunar M2 ocean tide was identified in CHAMP satellite magnetomete...
The recently upgraded barotropic tidal model TiME is employed to study the influence of fundamental ...
The tidal flow of electrically conductive oceans through the geomagnetic field results in the genera...
Tides are the most predictable of oceanographic phenomena, due both to the simplicity and predictabi...
Two factors govern Earth\u27s elastic response to the periodic redistribution of ocean tides: the pr...
Abstract The European Space Agency’s three-satellite constellation Swarm, launched in November 2013,...
The solar quiet (Sq) source morphology changes on a daily basis and becomes disturbed during periods...
The European Space Agency's three-satellite constellation Swarm, launched in November 2013, has prov...
Motional induction in the ocean by tides has long been observed by both land and satellite measureme...
The tides are a major driver of global oceanic mixing. While global tidal elevations are very well o...
Satellite-measured tidal magnetic signals are of growing importance. These fields are mainly used to...
Ocean-generated magnetic field models of the Principal Lunar, M2, and the Larger Lunar elliptic, N2,...
Periodic tidal ocean currents induce electric currents and, therefore, magnetic field signals that a...
Conducting ocean water, as it flows through the Earth’s magnetic field, generates secondary electric...
Due to their sensitivity to conductivity and oceanic transport, magnetic signals caused by the movem...
Over a decade ago the semidiurnal lunar M2 ocean tide was identified in CHAMP satellite magnetomete...
The recently upgraded barotropic tidal model TiME is employed to study the influence of fundamental ...
The tidal flow of electrically conductive oceans through the geomagnetic field results in the genera...
Tides are the most predictable of oceanographic phenomena, due both to the simplicity and predictabi...
Two factors govern Earth\u27s elastic response to the periodic redistribution of ocean tides: the pr...
Abstract The European Space Agency’s three-satellite constellation Swarm, launched in November 2013,...
The solar quiet (Sq) source morphology changes on a daily basis and becomes disturbed during periods...
The European Space Agency's three-satellite constellation Swarm, launched in November 2013, has prov...
Motional induction in the ocean by tides has long been observed by both land and satellite measureme...