You are welcome. Getting through this thread is certainly daunting to be sure.Red Baron Farms and aleCcowaN
Many thanks for replies and links.
Short of a melting East Antarctica ~7m is worst case, and that takes 200-500 years. Melting East Antarctica is 500+ years away even under some of the worst case warming scenarios and would progress at 2m-5m per 100 years. 50m isn’t impossible but it’s probably something on a 5000+ year time scale.
Consider tho the microclimate of East Antarctica means with a warmer and more moist atmosphere there is already evidence that ice is building faster than losses....given the current Milankovich position I think that will be very hard to dislodge as a limiting factor.
Oh, I'm not expecting to be woken by an unexpected Antarctic tsunami. I do think, however, that 1-3 meters of sea level rise is a reasonable min. between now and the end of the 21rst Century, with a maximum likely in the 3-5 meter range, and in either case most of that rise will occur in the in the last 2-3 decades of the 21rst Century. If these expectations are met, I see no mechanism to brake the phenomena and prevent an accelerated level of rise in the 2-3 decades after the start of the 21rst century, and so on.

A little number crunching says it all.
Imagine Antarctica is giving up yearly 10 times what she lost last year and take for that the upper limit of 600 km3 to do the calculation...
Congratulations! It's a boy!
Last week's indexes: 1-2 = +1.5°C; 3= +0.7°C; 4=-0.2°C; 3-4=+0.1°C
[qimg]http://i63.tinypic.com/14djcsh.gif[/qimg]
(hurricane season by the beginning of Autumn looks like it might be eventful on the Atlantic but not the Caribbean)
Why not simply look to the geological record comparisons to current conditions to perform such extrapolations?
While it is almost impossible to perform a one-to-one analysis (as there really is not a perfectly comparable geologic period), we can look at the peak melt rates during the Eemian and a few other interglacial periods and we can see that during the peak melt periods of these epochs the average peak rate of sea level rise seems to be about 1.2m/century. Our problem is that the current anthropogenic warming is to natural, cyclical, warming as steroidal induced competitive hypertrophic musculature development is to typical adolescent musculature development.
That's not good news, I was really hoping for a brief respite, but we play the hand we're dealt.
The globally averaged temperature over land and ocean surfaces for January 2017 was 0.88°C (1.58°F) above the 20th century average of 12.0°C (53.6°F). This was the third highest January temperature in the 1880–2017 record, behind 2016 (highest) and 2007 (second highest).
According to NOAA's Climate Prediction Center, ENSO-neutral conditions were present during January 2017 and are favored to continue through the Northern Hemisphere spring (March–May) 2017.
From the same link:
But I see a problem with your reasoning. It's implied that quickly changing anthropogenic forcing can disrupt every level of the global system with a similar speed.
An extremely oversimplified comparison is thinking that doubling the voltage in a voltage step would speed up to a double the transient response of the circuit.
The truth is that the world deep ocean and the Antarctic ice blanket are dozens of levels away from any human harmful action, so they'll respond in their own time.
If you took all the waters in the hydrosphere and make a ball orbiting the earth, it would need to be just 2/3 of the Moon's distance to both be seen the same size. The deep reality is perceived just doing a little more of number crunching: if the current imbalance in the planet's energy budget was managed just by the oceans, their average temperature would rise 0.002°C per year! Of course the deep ocean may remain cool as a cucumber while AGW plays havoc with everything on the surface.
On the other hand, Antarctica not only has a location that has defined the global climate for million of years, but it also creates its own local conditions by a high plateau made of ice which is at points just 4 km away from the troposphere and remains weeks in the dark under clear skies. Constant blizzards are her best insulation.
Anything you can think attacking Antarctica's ice also provokes balancing responses: warmer weather melting the edges also increases the formation of new ice way above from the current 600-800 cubic kilometres per year.
There's no reason for expecting important differences in the rising of the oceans this time.
From abstract - Polar temperatures over the last several million years have, at times, been slightly warmer than today, yet global mean sea level has been 6-9 metres higher as recently as the Last Interglacial (130,000 to 115,000 years ago) and possibly higher during the Pliocene epoch (about three million years ago). In both cases the Antarctic ice sheet has been implicated as the primary contributor, hinting at its future vulnerability...
Abstract - Interdisciplinary studies of geologic archives have ushered in a new era of deciphering magnitudes, rates, and sources of sea-level rise from polar ice-sheet loss during past warm periods. Accounting for glacial isostatic processes helps to reconcile spatial variability in peak sea level during marine isotope stages 5e and 11, when the global mean reached 6 to 9 meters and 6 to 13 meters higher than present, respectively. Dynamic topography introduces large uncertainties on longer time scales, precluding robust sea-level estimates for intervals such as the Pliocene. Present climate is warming to a level associated with significant polar ice-sheet loss in the past. Here, we outline advances and challenges involved in constraining ice-sheet sensitivity to climate change with use of paleo–sea level records.
Certainly, but, I don't see how the fact that we've gotten a lot better at our ability to tease out much finer scale discriminations in the data preserved in ice cores, is in anyway presuming this type of oversimplified comparison.
First, I'm not talking about estimating data based on theory, I'm talking about measurements of changes which occurred at the same regions over the same time frames under conditions of the same atm. partial pressures of GHGs and in general, the same global background setting. The only real difference is the rate at which we have climbed from atm. ppGHG min. to atm. ppGHG max. (it took the Eemian tens of thousands of years to transition from ppGHG min. to ppGHG max, whereas anthropogenic forcing has taken us from a point above the Holocene min. (probably close to the mid point between Holocene min. and max.) to a point near, if not already above, the (pre-Anthropocene) Holocene max. in around 2 centuries.
I understand the issues of thermal inertia implicit in the melting and freezing of huge masses water, I'm just not sure why I should look at the same area under greatly similar conditions, and expect one to be greatly different than the other in terms of how it reacts to those greatly similar conditions?
Thermal inertia? Really?
...You are educated enough in the specifics to understand that the speed of the ocean level rise isn't the first derivative of the GHG concentration in the atmosphere ... nor its second derivative ... nor its third or fourth.
...you cannot ever have forgotten that now the general rise of temperatures is preceded by anthropogenic GHGs building up in the atmosphere, what I'm sure enough it's not the case with the Eemian and the like.
- excerpted from Skeptical Science with my apologies, as I don't have the time right now to provide a more proper exegesis of my apparently cultish fringe science understandings. I'll address the rest later, after I'm in a more relaxed and less hungry state of being....For example, the orbital cycles triggered warming at high latittudes approximately 19,000 years ago, causing large amounts of ice to melt, flooding the oceans with fresh water. This influx of fresh water then disrupted the Atlantic meridional overturning circulation (AMOC), in turn causing a seesawing of heat between the hemispheres (Shakun 2012).* The Southern Hemisphere and its oceans warmed first, starting about 18,000 years ago.* As the Southern Ocean warms, the solubility of CO2 in water falls (Martin 2005).* This causes the oceans to give up more CO2, emitting it into the atmosphere. The exact mechanism of how the deep ocean gives up its CO2 is not fully understood but believed to be related to vertical ocean mixing (Toggweiler 1999).
The outgassing of CO2 from the ocean has several effects.*The increased CO2 in the atmosphere amplifies the original warming. The relatively weak forcing from Milankovitch cycles is insufficient to cause the dramatic temperature change taking our climate out of an ice age (this period is called a deglaciation). However, the amplifying effect of CO2 is consistent with the observed warming.
CO2 from the Southern Ocean also mixes through the atmosphere, spreading the warming north (Cuffey 2001). Tropical marine sediments record warming in the tropics around 1000 years after Antarctic warming, around the same time as the CO2 rise (Stott 2007). Ice cores in Greenland find that warming in the Northern Hemisphere lags the Antarctic CO2 rise (Caillon 2003).