Dear William, thanks for your interest, let's go over all this.
William Astley said:
Hi Andre:
Why don't you start a new thread, to discuss the Pulsating Equator Hypothesis. I would be interested to discuss,
We could revive this thread:
https://www.physicsforums.com/showthread.php?t=153634
but I need a better base from which to start the discussion. What is the hypothesized mechanism? What drives it? Is it periodic?
I know the part of the scientific method saying that the hypothesis requires a physically sound mechanism. We know that the Earth has a pulsating equator now, albeit in millimeters. Why can't it be ~100 meters order of magnitude on a millenium time scale on an equatorial bulge of 21 km. But a mechanism, is far from understood. To explain the ice ages it would have to be the cause of the 100,000 years cycle, which cannot be explained as a Milankovitch wobble.
Since the milankovitch cycles are fairly stable on a multi million years time scale and the 100,000 years cycle emerged only 900,000 years ago, the only factor I can think of such a behavior, is the solid inner core of the earth, which is assumed to be growing under the pressure and the cooling. 900,000 years ago it may have exceeded a critical size to break the physical stability of the core spin axis. The resultant misaligment of core and mantle spin axis would have caused turbulence, excess heat, which reduced the core size again, which could have permitted the spin axes to realign eventually, starting a new cycle of cooling and core growing. I know there is an old publication that assumes that the size of the equatorial bulge is also a function of the total fluidity of planet (haven't found it back yet). Perhaps it is. But surely that's all highly speculative.
Point is that it seems physically not impossible to have a pulsating equator and we have one now.
http://www.space.com/scienceastronomy/equator_bulge_020801.html
Others have thought about it:
http://adsabs.harvard.edu/abs/1982Prir...46M
As to significantly warmer temperatures, at LGM. Does the sea level reflect higher or lower temperatures, at the LGM? i.e. Is there data that does not support significantly warmer temperatures?
There is an abundance of proxy data considering paleo sea surface temperatures (Mg/Ca Ca/Sr, d18O, alkenones etc). The problem is however the dependence of those data on assumed chemical conditions. Ion ratios and biota activity are sentitive to pH, the biota producing the proxies may have reacted on changing conditions and you bet that the oceans reacted vigourously on the moving of the ocean bottom, amplified by massive methane hydrate decomposition events on record (Bryn et al 2005, Evans et al 2005, Maslin et al 2005, Mienert et al 2005) Refs here:
http://home.wanadoo.nl/bijkerk/ext-refs-new.pdf
Does other data support the hypthosis? If not why not?
Perhaps have a look at that ref list and realize that there must be a common denominator that fits for all of those phenomenons. There is the puzzle of the Pleistocene.
Sea levels is perhaps the most important evidence. We know that there are many anomalies actually refuting the common paradigm. We also know that there was not nearly enough ice during the LGM (due to the alleged but missing ice on Siberia) to cause the 127 meters sea level rise for instance. We also know that there is no source for melt water pulse 1A. See:
https://www.physicsforums.com/showthread.php?t=113807
however a moving equatorial bulge would be a splendid explanation instead.
See the attached link to a paper that discusses sea level last 350 kyrs.
http://www.geol.ucsb.edu/faculty/lea/pdfs/Lea%20QSR%202002.pdf
As usual papers like that fill in the blanks with assumptions based on the current paradigms, ignoring the anomalies. There are only a few areas from where sea level proxies are used notably the corals of Barbados and the mangroves of the Indonesian Sunda shelf, both on rather low lattitudes. A pulsating equator is probably explaning the sea level changes much better.
As to the high latitudes being warm during the LGM, can you provide a link to a full paper rather than to an abstract? Without data and analysis there is nothing to discuss.
Interesting warm indicator are insect assemblages for instance in my ref list:
Alfimov et al 2003, Kuzmuni 2001, Schirrmeister et al 2002, Sher et al 2002
Most of the papers are behind bars and not directly assessable online. Sometimes reports of conferences help. Dig into this one for instance:
http://www.yukonmuseums.ca/mammoth/progabst.htm
Click the abstracts on the bottom of the page for a wealth of information, for instance:
http://www.yukonmuseums.ca/mammoth/abstrmol-mor.htm containing basically the same information of Mol et al 2006.
Furthermore, my pdf library is a few gigs, containing most, if not all of those listed publications. Not free papers have been accumulated by visiting homepages of authors, and/or mailing them with requests for papers (works very well. Sometimes, you get more than you ask for) or asking around. My study partner is very good at that. You could PM me an email address.