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  #31 (permalink)  
Old 21-July-2007, 02:01 PM
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This seems to be his basis of thinking:
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If all the ice melts from there, the water level would not rise because the land would rise up, eliminating water displacement.
I'm thinking this falls under "not even wrong" at most, or "just plain wrong".
Indeed, I'm confused as to this thinking.
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  #32 (permalink)  
Old 21-July-2007, 02:04 PM
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Originally Posted by hhEb09'1 View Post
I see that. As ice is removed, the rebound is not instantaneous. It's a function of the viscosity of the material--and the viscosity is great enough that the material is actually considered to be solid.

The ice sheets were extensive, and thick, and they depressed the area for a long time--otherwise, the viscosity would have prevented the land from depressing. When the majority of the ice disappeared, the land started to rebound.

I've been trying to find a reference stating that Scandinavia and Hudson Bay are rebounding, but can't find it. I don't doubt it; it's just to show my denier friend (he tried a search too and came up with nothing).
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Old 21-July-2007, 03:09 PM
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Actually, what's wrong with this reasoning? We assume Antarctica's (2 C's, by the way, Grand_Lunar) landmass is denser than water.
Whoa, stretching the limits of credulity there!
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Originally Posted by Grand_Lunar View Post
I've been trying to find a reference stating that Scandinavia and Hudson Bay are rebounding, but can't find it. I don't doubt it; it's just to show my denier friend (he tried a search too and came up with nothing).
Most of the upper mantle rebound has occurred, but I'll see what I can come up with.

Science 23 March 2001:
Quote:
Fennoscandia has been rising since the retreat of a massive glacier at the end of the Pleistocene.
Geodynamics Program of the Geological Survey of Canada:
Quote:
The Global Change component of the Geodynamics Program focuses on the effects of postglacial rebound. The weight of the continental glaciers of the last great ice age (which peaked about 20,000 years ago) depressed the surface of the Earth. As the great ice sheets retreated and shrank, the Earth's crust began to rebound to its former level. Peak regions of rebound under the former ice sheets are located in Canada and Fennoscandia. Antarctica, which is still glaciated, is also experiencing substantial rebound because the Antarctic ice sheet has shrunk. Postglacial rebound has affected, and continues to affect, the drainage patterns of lakes and rivers through the continuing tilting of the Earth's surface.
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Old 21-July-2007, 04:53 PM
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Originally Posted by Ronald Brak View Post
Okay, lets start again. If all the Antartic ice melted sea levels would rise by about 60 meters because most of the ice is on land and above sea level. Does that sound right, Eburacum45?
Actually a little more than that, I understand. But isostatic recovery will add more than half an extra metre (eventually). I'm sorry to have confused the point.
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Old 21-July-2007, 05:55 PM
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Quote:
Originally Posted by Grand_Lunar View Post
I've been trying to find a reference stating that Scandinavia and Hudson Bay are rebounding, but can't find it. I don't doubt it; it's just to show my denier friend (he tried a search too and came up with nothing).
There are a lot of maps showing the total rebound since the end of the last ice age, such as the ones here. Scroll down to the section headed "Regional Vertical Movements of the Crust" for the maps, and notice the remark:
Quote:
Note that in both places there is a shallow epicontinental sea directly under the center of the ice sheets, evidence that the rebound is not yet complete.
Maps showing that the land is still rising are a little harder to come by, but here is one for Scandinavia. showing that the ongoing rate across a broad swathe of the area is measurable in mm/yr. Likewise, here is a description and map of the ongoing rebound in Canada (reference to the original article in Science appears at the bottom).
Finally, some supporting evidence for Scandinavia is here. The first paragraph under "Examples of Vertical Land Movements in Tide Gauge Records" contains a link to a "First example plot" of sea levels at various European stations. Over the last 200-year span, it's clear that Stockholm is bucking the local trend and rising out of the sea, an effect the parent page ascribes to "Glacial Isostatic Adjustment (sometimes called Post Glacial Rebound, PGR) in Scandinavia".

There's a lot more around, I've just picked the first few samples that do the job and appear to have credibility. Searching on "Glacial Isostatic Adjustment" or "Post Glacial Rebound" will find you much more.

Grant Hutchison
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  #36 (permalink)  
Old 21-July-2007, 08:17 PM
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From Grant's link
http://www.uwgb.edu/dutchs/STRUCTGE/EarthMvts.HTM
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Note that in both places there is a shallow epicontinental sea directly under the center of the ice sheets, evidence that the rebound is not yet complete.
This is exactly the situation that will occur when and if the Antarctic sheet melts; a shallow, central sea will exist between East and West Antarctica which will gradually empty into the ocean and disappear as the continent rebounds, thereby raising the ocean level.

One interesting aspect is the question of how isostatic recovery occurs at all; does it include a flow of material in the upper mantle towards the rebounding region, or is it simply due to a decrease in density in the local rock? I expect it would be a bit of both.

But note that a flow of material in the upper mantle towards Antarctica could, just conceivably, lower the level of the sea-bed and so lower the level of the ocean a little. But I think this effect would disappear after a while as the plastic aesthenosphere found its own level.
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  #37 (permalink)  
Old 22-July-2007, 02:30 AM
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Originally Posted by eburacum45 View Post
One interesting aspect is the question of how isostatic recovery occurs at all; does it include a flow of material in the upper mantle towards the rebounding region, or is it simply due to a decrease in density in the local rock? I expect it would be a bit of both.
If it's going to be isostatic, it not going to be the second one at all. A decrease in density does nothing for isostatic compensation.
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  #38 (permalink)  
Old 22-July-2007, 08:55 AM
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Quote:
Originally Posted by eburacum45 View Post
One interesting aspect is the question of how isostatic recovery occurs at all; does it include a flow of material in the upper mantle towards the rebounding region, or is it simply due to a decrease in density in the local rock? I expect it would be a bit of both.
Density and expansion are very interesting factors. I notice when one freezes water in a sealed container there is a fair bit of expansion. It is supposed to happen at 4 degrees Celsius which is 39.2 degrees Fahrenheit.

If there was a significant volume of water cross this expansion point wouldn't the action of enough of it cause the water in the in the oceans to swell?

Isostatic recovery variations could be far less immediate than crossing a thermal expansion point. Then there is the water to salt ratios to consider. It does become quite a complex model.
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  #39 (permalink)  
Old 22-July-2007, 05:35 PM
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If it's going to be isostatic, it not going to be the second one at all. A decrease in density does nothing for isostatic compensation.
True; but the decrease in density would contribute to the rise in the land surface, and hence to the rise in sea level.
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  #40 (permalink)  
Old 23-July-2007, 01:35 PM
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I was just addressing your comment: "One interesting aspect is the question of how isostatic recovery occurs at all;"

Still, solid rock materials don't usually expand a whole lot.
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  #41 (permalink)  
Old 23-July-2007, 04:55 PM
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that's only true for the northern polar ice cap. there is ice on land in Antartica.
Just for clarification, I wasn't trying to say anything about ice caps melting. I was responding to something somebody claimed on that other forum, which is that the water level in a glass of ice water should drop as the ice melts.
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  #42 (permalink)  
Old 23-July-2007, 04:55 PM
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it's true of course that the water level does not change.
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  #43 (permalink)  
Old 23-July-2007, 05:10 PM
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So here's a kiddie pool analogy that I think might be a little more closely related to reality: Fill a kiddie pool with water. Simulate the rebound by pushing the underside of the pool so that it sticks up out of the water. Now, I predict that the water level in the pool will be quite a bit higher because that "island" we've created will displace so much water. I also predict that higher we push this "island" up out of the water, the more it will displace.

Possibly G_L's friend should actually be arguing that the rebound will be extremely slow, since it sounds to me like a whole continent lifting higher out of the water should have the opposite effect of what was claimed.


As for causes of the rebound, the link I posted a while back suggests that the sinking is due to deformation of the lithosphere. Evidence for this includes that as Scandanavia rises the Netherlands is sinking, which fits with the theory in that a region of the lithosphere pressing down should displace the asthenosphere, which will put some upward pressure on the lithosphere in the surrounding area.

While I'm sure packing of the strata happens, I would guess that it doesn't contribute much to the isostatic rebound for about the same reason that a canister of flour doesn't fluff itself.
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  #44 (permalink)  
Old 24-July-2007, 09:31 AM
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But a flow of upper mantle from beneath the ocean floor of the Great Southern Ocean towards the Antarctic isostatic adjustment would actually lower the seafloor in that region, lowering sealevels somewhat.

I proposed a (semi-serious) solution to rising ocean levels a while ago on this forum; by excavating the continental shelf and building new countries from scratch, we could lower the net sea-floor level and thereby the level of the ocean surface. By causing a net flow in the mantle beneath the Great Southern Ocean towards Antarctica there could be a slight lowering of the Ocean after all.

Eventually, that depression in the seafloor would also adjust istself, as upper mantle flows in from the rest of the world... wouldn't it? Hmm. This is somewhat more complex than I thought at first.
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  #45 (permalink)  
Old 24-July-2007, 09:37 AM
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continent/ country building?


that takes a lot of gasoline.
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  #46 (permalink)  
Old 24-July-2007, 09:45 AM
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A cheaper method should be to pump seawater into antartica and either let it run and freeze or pump it into giant dams. This would of course still be massively expensive. Pumping a ton of water a hundred kilometers is expensive. Pumping gigatons is even more expensive. (Could never figure out why in those fat Kim Stanley Robinson novels they could teraform all of mars but earth couldn't handle rising sea levels.)
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Old 24-July-2007, 10:35 AM
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science fiction.





one other thing, Mars has a pretty stable environment with fewer influences than earth. By adding bacteria or whatever they used - this created a huge influence that wasn't there before. Kind of like adding Kudzu to the eastern US - only more powerful.
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  #48 (permalink)  
Old 24-July-2007, 01:01 PM
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Thanks for all the replies. Quite a bit to digest.

And kudos, Nauthiz for a visualization that makes more sense (about the kiddie pool and displacement). I think that is what I was missing in my mental image.

About rebounds, I suppose the nature of the magma underneath an area effects wether or not an area does rise after ice melts from it, yes?
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  #49 (permalink)  
Old 24-July-2007, 01:12 PM
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Quote:
Originally Posted by nauthiz View Post
So here's a kiddie pool analogy that I think might be a little more closely related to reality: Fill a kiddie pool with water. Simulate the rebound by pushing the underside of the pool so that it sticks up out of the water. Now, I predict that the water level in the pool will be quite a bit higher because that "island" we've created will displace so much water. I also predict that higher we push this "island" up out of the water, the more it will displace.
Part of the problem with the kiddie pool analogy like that is that a displacement of the bottom in one area will be compensated in another. Like what you mention about the Netherlands in the last part of your post.
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About rebounds, I suppose the nature of the magma underneath an area effects wether or not an area does rise after ice melts from it, yes?
Just whether or not?

Not on Earth, I don't think. It could be possible that an accumulation of ice on a particular part could result in a rise of that part, because of the interaction of water weight on the rest of the surface, but I don't think the conditions obtain on the Earth if they can at all.
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Old 24-July-2007, 05:15 PM
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Originally Posted by hhEb09'1 View Post
Part of the problem with the kiddie pool analogy like that is that a displacement of the bottom in one area will be compensated in another. Like what you mention about the Netherlands in the last part of your post.
Right, and like ebracum suggested I imagine that there's a good chance that the net effect (ignoring any other factors) would be to lower the sea levels a bit. It's definitely not a good version of the kiddie pool; I think you're right that the analogy is fundamentally unsound.
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Old 24-July-2007, 08:35 PM
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It's definitely trickier than the kiddie pool. Due to conservation-of-crust, if a cubic mile of crust "rises" somewhere, another cubic mile must "sink" somewhere.

It's not immediately obvious that isostatic rebound would have any effect on global sea-levels
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Old 24-July-2007, 10:02 PM
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It's definitely trickier than the kiddie pool. Due to conservation-of-crust, if a cubic mile of crust "rises" somewhere, another cubic mile must "sink" somewhere.

It's not immediately obvious that isostatic rebound would have any effect on global sea-levels
It'd depend on the details on those two cubic miles.

If the bit that rises consists entirely of dry land, and the bit that sinks is entirely covered by water, then the net effect would be for sea levels to drop by whatever 1 cubic mile divided by the surface area of the ocean is.

If the aquatic status of the two bits of land were switched, then the sea levels would rise by the same amount.
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Old 24-July-2007, 11:31 PM
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Geology (or is this another subject?) sure is tricky.

I figured that with the situation, that the shifting of the level of Antartica doesn't really alter sea level, because the volume of water is what really matters. All the shifting and rebounding does is alter the shape of the container.

Or am I totally wrong in this?
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Old 25-July-2007, 05:19 AM
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Originally Posted by Grand_Lunar View Post
I figured that with the situation, that the shifting of the level of Antartica doesn't really alter sea level, because the volume of water is what really matters. All the shifting and rebounding does is alter the shape of the container.

Or am I totally wrong in this?
Depends on how the container is shaped, doesn't it? Haven't we all squeezed a styrofoam cup of coffee and got it all over us? Or is it just me?
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Old 25-July-2007, 10:40 AM
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Depends on how the container is shaped, doesn't it? Haven't we all squeezed a styrofoam cup of coffee and got it all over us? Or is it just me?
What about the weight per cubic kilometre of water to average crust. Water would quickly adjust. Due to the slower rebound could that make a change to rebound?

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Old 25-July-2007, 04:37 PM
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Depends on how the container is shaped, doesn't it? Haven't we all squeezed a styrofoam cup of coffee and got it all over us? Or is it just me?
No - when I need to get out of a meeting, I prefer to pour the coffee over my head and run out of the room while laughing maniacally. That way nobody will think I'm uncoordinated.
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Old 26-July-2007, 12:56 AM
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Interesting, I might have to try that. Do you sit long enough to let the coffee cool? That could be a negative.
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Old 26-July-2007, 01:37 AM
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Depends on how the container is shaped, doesn't it? Haven't we all squeezed a styrofoam cup of coffee and got it all over us? Or is it just me?
I had in mind a container in the shape of the ocean floor.

I would suppose if THAT was squeezed, we'd have a mess. And not just jumbo squid.
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Old 26-July-2007, 03:16 AM
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I had in mind a container in the shape of the ocean floor.
Still, the devil is in the details. For instance, if you have a perfectly round planet with a water layer at the surface, and the center of mass of the solid portion is not at the center of figure, the water will be displaced to one side. A "continent" will emerge on the other side. As the center of mass moves towards the center of figure, the floor of the ocean will rise, and the sea level on the continent will rise.

The shape of the container can make almost anything happen. That's a simplified model, but it has real world analogues.
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Old 26-July-2007, 06:54 PM
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Still, the devil is in the details. For instance, if you have a perfectly round planet with a water layer at the surface, and the center of mass of the solid portion is not at the center of figure, the water will be displaced to one side. A "continent" will emerge on the other side. As the center of mass moves towards the center of figure, the floor of the ocean will rise, and the sea level on the continent will rise...
That makes sense.

Now suppose the water warms. Due to thermal expansion the sea level will rise. But what if the continents also warm?
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