-------------------------------------------------------------------- > Quote by Andrew Dodds / Additionally, there is a relation between
ocean basin volume and seafloor speading rates, the higher the spreading rate the higher sea level is for a given climate / ocean temperature.
Additionally, there is a relation between
ocean basin volume and seafloor speading rates, the higher the spreading rate the higher sea level is for a given climate / ocean temperature.
And I'm totally confused on this point: is there a loss of
ocean basin volume as the below sea level bed of Greenland rises up and displaces it?
Can we consider
the ocean basin volume as static for the purpose of sea level change prediction because the speed of water inputs will far outstrip the speed of mantle movements?
Not exact matches
The new find confirms that the ancient lavas formed at midocean ridges and found throughout deep
ocean basins are by
volume the largest ecosystem on Earth, scientists say.
Sea level rise has two primary components: the expansion in
volume of seawater with increased temperature and the addition of water in
ocean basins from the melting of land - locked ice, including Antarctica and Greenland.
Changes in sea floor spreading rates effect the
volume of the mid-oceanic ridges which may contribute to changes in the
volume of the
ocean basins.
Vertical land movements such as resulting from glacial isostatic adjustment (GIA), tectonics, subsidence and sedimentation influence local sea level measurements but do not alter
ocean water
volume; nonetheless, they affect global mean sea level through their alteration of the shape and hence the
volume of the
ocean basins containing the water.
SLR satellite data includes things such as the «GIA Adjustment» — which is the amount of SLR that there would have been if the
ocean basin hadn't increased in
volume and in the case of this new study, how much higher the sea surface would have been if it had not been suppressed by the Mount Pinatubo volcanic eruption, another correction for ENSO / PDO «computed via a joint cyclostationary empirical orthogonal function (CSEOF) analysis of altimeter GMSL, GRACE land water storage, and Argo - based thermosteric sea level from 2005 to present», as well as other additions and adjustments — NONE OF WHICH can actually be found manifested in any change to the physical Sea Surface Height.»
Eustatic change (as opposed to local change) results in an alteration to the global sea levels due to changes in either the
volume of water in the world's
oceans or net changes in the
volume of the
ocean basins.
We show that the influx of water into the
volume created by this subsidence produces a sea - level fall at locations distant from these margins — indeed over the major
ocean basins — that is comparable in amplitude to the syphoning mechanism isolated by Mitrovica and Peltier (1991).»
Other simple methods for controlling sea level are almost as simple, using heavy equipment to move shoreline dirt inland, thus increasing the total
volume of the
ocean basin.
The former redistributes
ocean volume within the
basins, while the latter alters Earth's gravitational field and rate of rotation enough to change the distribution of
ocean mass around the surface of the Earth.
A recent comprehensive review [7] reveals that there are still wide uncertainties about the Earth's sea - level history that are especially large for time scales of tens of millions of years or longer, which is long enough for substantial changes in the shape and
volume of
ocean basins.
«We have to account for the fact that the
ocean basins are actually getting slightly bigger... water
volume is expanding,» he said, a phenomenon they call glacial isostatic adjustment (GIA).
b) volumetric effects — change in the
volume of water contained in the
oceans and the geometry and areal extent of the
ocean basins c) gravitational effects — change in the gravitational attraction of the earth (induced by deformation), by the change in distribution of ice and by the change in self - attraction of the water d) rotational effects — change in the moment of inertia caused by a change in the distribution of mass within the earth and on its surface.
And I DO know that ANYTHING that changes the
volume of the
ocean OR the
volume of the
ocean basins by 36O km ^ 3 will result in a change in sea level by 1 mm.
You can just plug a huge pneumatic hose into the nearest volcano and inflate the earth with CO2, and that way the
ocean basins would increase in area and
volume, and the sea level would fall again.