Ray Jay wrote:So, there's still something that confuses me about this density argument. The article and website that Dr. Fate quoted said that the math is off by 7X. That the land ice including glacier melt does not have sufficient volume to increase the ocean rise to the extent feared. In fact, his math suggests only 5 inches by 2100 based on land ice melt because of the volume of water and that oceans represent 70% of the earth's surface.
Freeman than provided a scholarly report that supports the two factors: ice melt and density change as both important. I quoted from the report that says that ice melt is the more important factor:
For thermal expansion alone, IPCC has estimated a rise by between 60 and 200 cm over the next thousand years if global warming is stabilised between 2 and 4 ºC above present temperatures. However, the bulk of long-term sea level rise may be expected to come from ice melt.
Basically it says if we stabilize temperature ( a big if since it means that we don't increase carbon levels beyond what the planet can handle) there will be an increase of between 18 inches and 7 feet because of density over 1,000 years, but that ice melt will be the more important factor.
However, we still haven't disputed that ice melt only causes 1/7th of the sea level rise at current rates. And we've learned that the density factor is significantly less important so will cover less than 1/7th. Where is the rest of the increase coming from? Or is that just a function of more extreme weather and varying ocean levels across the planet? Next I'll Google how much land ice there really is.
The difference is largely because of a conflation between what is happening now, and what is predicted for the future. DF's link & quote was based on a mathematican exercise trying to look at the current rate of ice loss and compare that to the total volume of expansion required to get the sea level rise.
My point was that for a start they had not considered factors other than ice loss. That was where the density comes in.
There are again two things going on. Firstly that we can observe the current temperature increase of the ocean, the current rate of ice loss, and any other factors, and observe a current rate of sea level increase, and note that about 30% comes from thermal expansion, 55% from ice that was on land and 15% from other factors.
And both my mathematics and the projections that freeman cites are looking at the long term. I was just looking at a simple proposition, and I did not indicate how long it would take because I don't know. Freeman's citation was looking at the effects of a long term stable increase in temperature, which would not only warm up the ocean, but would also hit ice loss.
I think what you are asking is if we can take the math that DF's link did, and assume that is the 55% and any thermal expansion is 30%. I don't think we can, because...
The other major failing in the math that DF found for us is that the rate of ice loss is not constant, as it was assumed. It has doubled in the last few years, apparently. So while it is true that at the current rate of ice loss, you get about 15% of the volume required for a 3 foot rise over 86 years, that cannot necessarily be extrapolated as a constant rate. If you extrapolate that as a linear rate of change, one of about 34 cubic miles more each year, and do that for 86 year from now starting at 136 cubic miles now, it will come to about 75,000 cubic miles (so about 93% of the target). If the rate is exponential (doubling every x years), then it could be much more.
If temperatures rise, the ocean will see thermal expansion. If temperatures rise, then it means that ice is more likely to melt (unless somehow the increase does not affect the main locations of land-bound ice - and if that does happen, it could be that the sea level is more impacted by thermal expansion than by ice loss). This does not need to include aspects like severe weather - a storm is not going to make much difference really, even lots of them, unless it results in quick erosion or subsidence).
Ray Jay wrote:Ray Jay wrote:http://www.johnstonsarchive.net/environment/waterworld.html
worth checking out ... he is an extreme skeptic ... he does provide very good info on the volume of sea ice.
Indeed he does. Sea Ice is a very small proportion of the total ice on Earth. And if the sea ice melts it will have no effect on sea levels really because it is already 'in' the oceans (as Archimedes proved). It may effect how currents work, and loca / regional temperatures (and so what density, and so what the sea level is), but the average across the globe averaged out would be negligible.
But given that 97.2% of the ice is on the land, and any of that which melts and runs into the sea would affect the overall sea level, that is the more important bit to look at.
The 80,000 cubic miles that DF's mathematics quote comes up with for a 3 foot increase, or 330,000 cubic kilometers, is about 1.1% of the land-bound ice.