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originally posted by: Infinitis
a reply to: cuckooold
Antarctica Is Losing So Much Ice It's Throwing Off Earth's Gravity
lmao!!!!!!!!!!!!!!!!!!!!!!
The things people will believe....
And this revelation is backed up by the findings of a number of other scientific satellites. The joint US-German Grace satellite has been detecting similar gravitational disturbances — albeit at a much coarser resolution — for more than a decade and the ESA’s own CryoSat satellite has found that West Antarctic Ice Sheet’s rate of loss has tripled every year since 2009 and has caused the entire continent to shrink by 125 cubic kilometres a year since 2011.
originally posted by: LeviWardrobe
a reply to: Klassified
Seems like it eh? Indistinguishable from normal fluctuations? And what exactly are your qualifications? What makes you say that? Oh, a gut feeling or something. Gotcha. Thanks.
Local variations in topography (such as the presence of mountains) and geology (such as the density of rocks in the vicinity) cause fluctuations in the Earth's gravitational field, known as gravitational anomalies. Some of these anomalies can be very extensive, resulting in bulges in sea level, and throwing pendulum clocks out of synchronisation.
The study of these anomalies forms the basis of gravitational geophysics. The fluctuations are measured with highly sensitive gravimeters, the effect of topography and other known factors is subtracted, and from the resulting data conclusions are drawn. Such techniques are now used by prospectors to find oil and mineral deposits. Denser rocks (often containing mineral ores) cause higher than normal local gravitational fields on the Earth's surface. Less dense sedimentary rocks cause the opposite.
A perfect sphere of spherically uniform density (density varies solely with distance from centre) would produce a gravitational field of uniform magnitude at all points on its surface, always pointing directly towards the sphere's centre. However, the Earth deviates slightly from this ideal, and there are consequently slight deviations in both the magnitude and direction of gravity across its surface.
Apparent gravity on the earth's surface varies by around 0.7%, from 9.7639 m/s2 on the Nevado Huascarán mountain in Peru to 9.8337 m/s2 at the surface of the Arctic Ocean.[5] In large cities, it ranges from 9.766 in Kuala Lumpur, Mexico City, and Singapore to 9.825 in Oslo and Helsinki.
originally posted by: Grimpachi
So would you say because on the opposite side of the globe from antarctica which would be the Arctic N pole which is seeing a heavy loss of Ice each year would that would be adding to the changes in gravity?
originally posted by: Kali74
a reply to: SlapMonkey
SEA ICE
Rising sea levels inundating coastal cities are the least of our global warming problems. According to a new report by the European Space Agency, the loss of snowpack along the antarctic ice shelf is throwing off Earth’s gravitational field.
originally posted by: Grimpachi
So would you say because on the opposite side of the globe from antarctica which would be the Arctic N pole which is seeing a heavy loss of Ice each year would that would be adding to the changes in gravity?
originally posted by: Grimpachi
a reply to: SlapMonkey
For you to understand it would need to be taken in context with who I was responding to and my question in reference to inverse square law.
My understanding is gravity on one side of the earth can be affected by the amount of mass on the opposite.
It is no wonder you would be confused if you didn't get the context of my reply to stormcell BTW I am still hoping stormcell will reply. Only time will tell.
inside a solid sphere of constant density the gravitational force varies linearly with distance from the centre, becoming zero by symmetry at the centre of mass.
An approximate depth dependence of density in the Earth can be obtained by assuming that the mass is spherically symmetric (it depends only on depth, not on latitude or longitude). In such a body, the gravitational acceleration is towards the center. The gravity at a radius r depends only on the mass inside the sphere of radius r; all the contributions from outside cancel out. This is a consequence of the inverse-square law of gravitation.
inside a solid sphere of constant density the gravitational force varies linearly with distance from the centre, becoming zero by symmetry at the centre of mass.
Changes in density can also do this (Ice becoming water, Oil deposits being drained, voids being dug aka tunnels), but again, it will not affect the opposite side of the Earth from where that is.
That's not in question, here. Your claim concerning the arctic sea ice is.
nsidc.org...
On September 17, 2014, sea ice extent dropped to 5.02 million square kilometers (1.94 million square miles). This appears to have been the lowest extent of the year. In response to the setting sun and falling temperatures, ice extent will now climb through autumn and winter. However, a shift in wind patterns or a period of late season melt could still push the ice extent lower. The minimum extent was reached two days later than the 1981 to 2010 average minimum date of September 15.
originally posted by: Grimpachi
a reply to: eriktheawful
inside a solid sphere of constant density the gravitational force varies linearly with distance from the centre, becoming zero by symmetry at the centre of mass.
Changes in density can also do this (Ice becoming water, Oil deposits being drained, voids being dug aka tunnels), but again, it will not affect the opposite side of the Earth from where that is.
Thanks that is what I wanted to know. I assume by your response that the same will hold true even though the Earth is an oblate spheroid instead of a sphere.
Side question: Would the gravity experienced at the equator be less than at the poles?
The surface of the Earth is rotating, so it is not an inertial frame of reference. At latitudes nearer the Equator, the outward centrifugal force produced by Earth's rotation is larger than at polar latitudes. This counteracts the Earth's gravity to a small degree – up to a maximum of 0.3% at the Equator – and reduces the apparent downward acceleration of falling objects.
The second major reason for the difference in gravity at different latitudes is that the Earth's equatorial bulge (itself also caused by inertia) causes objects at the Equator to be farther from the planet's centre than objects at the poles. Because the force due to gravitational attraction between two bodies (the Earth and the object being weighed) varies inversely with the square of the distance between them, an object at the Equator experiences a weaker gravitational pull than an object at the poles.
In combination, the equatorial bulge and the effects of the Earth's inertia mean that sea-level gravitational acceleration increases from about 9.780 m/s2 at the Equator to about 9.832 m/s2 at the poles, so an object will weigh about 0.5% more at the poles than at the Equator.