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The missing player

 
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Jan29-07, 12:23 PM   #1
 
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The missing player


In the NERC discussions and somewhere here in a thread I remarked that the great mysteries of the Pleistocene Ice Age cannot be solved without finding the "missing player"






We got him.

Anyone curious? I'm ready to discuss.

BTW my earlier threads about the role of clathrate for the extinction of the megafauna remains roughly valid, we're only one "why?" further. However Many "why's" to go before I sleep.

hint
 
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Jan29-07, 12:46 PM   #2
 
What the hell are you talking about?
 
Jan29-07, 01:06 PM   #3
 
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So you still think that there is no problem or two or twenty with the hypotheses of the ice age? In that case we still need to do a little demolishion, like this fragment from the NERC discussions:

http://home.wanadoo.nl/bijkerk/refut...hermometer.pdf

I mentioned the missing player here: post #361

I repeat, about a dispute of the role of the ocean floor; knowing what happened at the onset of the Bolling Allerod and the Preboreal is essential for understanding what had happened to the late Pleistocene climate after the switch to the 100ka world.

Did not ocean currents fluctuate strongly at those transitions? THC shut and acceleration have been proposed. But why? and why so abrupt, considering the gigantic inertia of that ocean flow. We know now that it was not the sudden temperature change at the onset of the Bolling since that happened 2000+ years earlier (long masked by not calibrating carbon dates).

Believe me, there is another player to be found, who also can explain the dying of the coral during the MWP1a, and the concurrent worldwide d13C depletion spike etc, and ultimately the extinction of the megafauna.

If you don't have all the players on the field, the models won't do any good. And when the picture is complete, the reason of the passive CO2 reaction will be obvious. But that's called paradigm shift, of which Thomas Kuhn has shown why it is so difficult to get that accomplished within a generation.
It's about that missing player
 
Jan29-07, 01:28 PM   #4
 

The missing player


Andre, did you write or can cite a paper which would coherently describe and present your point and what you are trying to tell us here?

I am not an expert on climate so i would appreciate something explanatory and cohesive which i could read and understand. These links, and online discussions are just getting accross ideas. That does not count much as anything without the proper work. To be honest i have only slight idea what you trying to say but i fail to see any connection to GW, glaciers, radiation, etc from those separate, unconnected links.

Would something like that be in your powers to write?
 
Jan29-07, 01:42 PM   #5
 
You are saying,Andre,that people should not base current models of anthropogenic greenhouse forcing on Pleistocene data because co2 data and radioisotope data from the Pleistocene do not agree.I have also read on Wikipedia that Milankovitch cycles cannot account for all the glacial-interglacial periods in the Pleistocene, on their own.Coral died in the Pleistocene because of something that changed in the deep ocean?
 
Jan29-07, 01:55 PM   #6
 
I have been reading papers all day, none of them made any sense!!!
(note: nothing to do with this discussion)
Why did I chose geophysics??

But yes, sneez is right, you're a specialist in a field that I personally have been to a few 1 hour seminars on/skimmed past in other reading. If you want us to make intelligent comments you need to give us something a little more solid, something that gives us the relevant background, and is accessible to someone who doesn't necessarily know all the nomenclature.
 
Jan29-07, 02:32 PM   #7
 
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Okay that makes sense. It makes a difference talking to a quartenary specialist or somebody whose textbook says in two paragraphs that there aint no mysteries in the ice age.

I can cite loads of assumed facts that are proven wrong, papers that actually contradict but I don't think that anybody is waiting for that.

One of the major problem areas is the ocean. ocean flows are slow and the body of water has a tremendous inertia. Nevertheless, ocean ice age papers are all about shift ands quick reactions of the ocean to any changes. If you compare the deep sea bed sediment proxies with the ice core proxies, they are not only virtually identical but also it appears that the ocean could be leading. Nobody appears to think that is this weird.

Then there are the sea level problems. Only along the equator and for the last transition from the glacial there is some consistency in equatorial proxies but not elsewhere. That's even in the TAR of the IPCC. However strange things have happened before the former interglacial, the sea level rise appeared to be completed before the deglaciation started. There is plenty plenty more. I hinted to a few in several threads.

The most aggravating non consistency with any hypothesis is probably the reason why so many easy errors have been introduced like the fake 100ka Milankovitch cycle. Things need to be in an orderly explainable fashion, but they aint.

Here is the idea in a nutshell (let me know if there are difficult words in there):

Diagnoses of the Ice Ages: Pulsating Equator

Abstract

We demonstrate that if the size of the equatorial bulge would pulsate around an equilibrium in an irregular 100ka cycle and with some ten-hundred meters ROM amplitude, then it would explain most of the symptoms of the ice age. Periods of maximum equatorial bulge size represent interglacials with high sea levels due to relatively small oceanic basins. Periods with a minimum equatorial bulge have low sea levels due to equatorial enlargement of the Oceanic basins. Furthermore, during contraction of the equatorial bulge, the poles are pushed upwards to much higher elevations, both effects combined, increase orographic effects enough to trigger glacier growth at high latitudes, which accumulates in ice sheet build ups. In this scenario, the reverse process, with an expanding equator and sinking poles are leading to the interglacials, in which transient effects like Heinrich events, Dansgaard Oeschger interstadials, melt water pulses find an easy explanation.
here is a modest animation that may help visualizing what has happened, advise to use page down/up keys.
 
Jan29-07, 03:42 PM   #8
 
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I also said: "And when the picture is complete, the reason of the passive CO2 reaction will be obvious"

And indeed, Verdigris, With this completely different picture in mind, it will be clear why I think that the role of CO2 for climate thoughout the Pleistocene was (and is) completely insignificant.
 
Jan29-07, 03:59 PM   #9
 
That's quite a neat little mechanism, have you checked the timescales? what kind of strain rates would you need, wouldn't there have been an increase in seismicity? have you run any computer simulations? have you published anything on this, I'd be interested in checking it out.
 
Jan30-07, 12:57 AM   #10
 
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Quote by billiards View Post
That's quite a neat little mechanism, have you checked the timescales?
Yes, course of events appear to match, but of course a lot of things need to be addressed

what kind of strain rates would you need,
It would be nice if specialist would be interested to judge that.

wouldn't there have been an increase in seismicity?
That would have been a neat prediction, if it wasn't for the puzzling volcanic activity peak during the last glacial transition we already know about. For instance both the German Eifel and the French Massiv Central, mostly dormant, had very active volcanism during that period.

have you run any computer simulations?
It's a pristine idea however with dazzling matches of geologic features.

have you published anything on this, I'd be interested in checking it out.
You're most welcome. A lot needs to be done.

first witness: The Mid Pleistocene Stilostomella extinction tells us when this mechanism started. These species could not cope with the dramatic changes in deep water waterflows which this mechanism triggered.

When things seems logical all of sudden, you know that you're on to something.
 
Jan30-07, 04:21 AM   #11
 
ANDRE said:

"These species could not cope with the dramatic changes in deep water waterflows which this mechanism triggered"

What in particular did the stilostomella have trouble coping with - water temperature change,nutrient availability changing?

There is a nice photo of stilostomella here:
http://homepages.ihug.co.nz/~bw.hayw...ges/plate3.jpg
 
Jan30-07, 10:23 AM   #12
 
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Who knows. It's just likely that a typical darwian selection took place, when conditions changed, the species that were too specialized disappeared, while the most adaptable survived.

As mentioned, one thing that did change was isotopes captured by those creatures in the deep sea beds, almost exactly at the same time as isotopes of Antarctic ice cores like this:

http://home.wanadoo.nl/bijkerk/LR05-Epica-dome-c.gif

It could be suggested that the oceanic isotopes were leading the ice cores, although the error bars are rather uncertain and the dating methods may easily get into circular reasoning when time scales are tuned to each other.

However, ice sheets take centuries to millenia build up as can be derived from geologic data. This would determine the slope of the ice core proxies. However the THC circulation also takes more than a millenium to distribute that signal over the sea beds but also it mixes with the deep water so it would take even longer to get the ice build up signal to the deep sea. But it did not. The sea beds knew that the deglaciation started, practically before it actually did.

Consequently the idea that both those isotopes represent ice sheet build up is clearly wrong. Whatever it is, it started at the sea beds and now we can assume that it represent mostly currents generated by the pulsating equator
 
Jan30-07, 12:56 PM   #13
 
ANDRE said:
"Whatever it is, it started at the sea beds "

What if material from the surface sank to the sea beds e.g plankton,because of a high mortality rate from ozone depletion at the poles and increased uv light.
 
Jan30-07, 01:26 PM   #14
 
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Unlikely,

The d18O is measured from shells of identified foraminifera species which are bottom dwellers (benthic). Isotopes are usually considered temperature proxies. Since the temperature at those depth around 2-4km are rather constant, be at at the equator or pole, it is thought that these isotope spikes represent the actual isotope ratio of the deep water. Then it was recognised that the ice sheets have very little heavy isotopes due to the fractination of the physical processes involved (evaporation - condensation). So the idea was that the oceanic d18O ratio was a measurement for the amount of ice locked on the poles. A sort of distilling process.

However, if you consider the supposed global (eustatic) sea-level difference of ~125 meters then you're still about half a mil out of ~1,5 mil short of the required values, but you'd need already to put 15.4 Greenland ice sheets equivalents away somewhere. There is not too many room for that on Antarctica, already loaded with ice, perhaps 2-3 ice sheets. North America can have some 5-6 Greenland ice sheets equivalents before it is filled up like it was at the hight of the last Wisconsan ice age. So we need to tuck away ~7 Greenland ice sheet. No problem: in the 1980ies when this was all invented; there was a large and very unknown Siberia, lots of space out there. Plenty for so many Greenland ice sheets.

It was not before the turn of the century when the researchers were allowed to swarm over that area that it became clear that had been no ice on Siberia at all during the Last Glacial maximum. This is all you get, perhaps just enough for two Greenland ice sheet equivalents.

So I still have about 5 Greenland ice sheets left to stow away somewhere and that only covers the ~120 sea level change, not enough to balance the isotopes. That would have required some 20.2 Greenland ice sheet equivalents in total as well as a sealevel lowering of 164.5 meters which is not attained anywhere except perhaps for a certain lost Cuban city.

So both the sea level yoyo as well the isotope balance hypothesis (Rutherford) do not match the actual numbers and can be considered falsified. Not that they are considered that, it's still used every day because it's the best there is perhaps.
 
Jan30-07, 03:51 PM   #15
 
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Looking again here it appears that the bulging reaction of the North Pole was not symmetrical. Plenty of ice on N-America, little ice in the east.

Now, a little bit more to the East, just off the map at #1 the Laptev Sea, close to the coast, the Yukagir mammoth was found, with a calibrated age of some 22,000 years, just at the onset of the Last Glacial Maximum. As I elaborate upon here, page 5 in his intestine were remains of the greater burnet, a herb with limited winter hardiness, basically trashing the ice age idea.

Now if we assume orographic effects, Scandinavia way above sea level in a less elliptical world then there would not be a requirement for Siberia to be that much colder because evidently it was warmer then as today.

Interesting study:

http://www.advances-in-geosciences.n...1-103-2003.pdf
 
Jan30-07, 05:34 PM   #16
 
Nakada et al. 2000 gives a current rate of isostatic rebound for the continent of Antarctica as 1.7 mm yr-1. I don't know how long you propose these cycles take, I guess between 10,000 - 100,000 yrs. Which if we take the current rate and be a little generous, let's say 2 mm yr-1 you're getting about a 20 - 200 m change in elevation over those time scales. I guess maybe you'd have to half that to find the amplitude of a cycle, so maybe 10 - 100 m actual elevation change. Do these changes seem reasonable? Could they account for the orographic effects you mentioned?
 
Jan30-07, 05:49 PM   #17
 
ANDRE said:
"However the THC circulation also takes more than a millenium to distribute that signal over the sea beds "

Why does it take this long? Are you talking about the entire surface of the sea bed around the world?


ANDRE said:
"Consequently the idea that both those isotopes represent ice sheet build up is clearly wrong. "

Perhaps not - if the ice sheets built up in the sea around Antarctic.
Then the weight of ice on water would influence currents and the flow of information just as the Odden feature does in Greenland.I have also read that Stilostomella thrive when the carbon flux is high.In a colder climate with low biomass - and low carbon flux - the stilostomella could have been starved and the increased sea water salinity may have killed them.Also the circumpolar current would have been weak because of less wind energy in the atmosphere.This would have helped ice to form on the sea.

At this link: http://www.space.com/scienceastronom...ge_020801.html
Christopher Cox suggests that shifting ocean currents can account for the pulsing equator.Would this also account for the satellite orbital anomaly of 1998 (there were also anomalies in 1985 and 1989)?
 
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