Climates Of History
#1
Posted 03 November 2010 - 17:34
Mark Twain
All views I express are either my own or the dog's; often it's difficult to discern which of us is spouting the most gibberish.
#2
Posted 03 November 2010 - 23:39
http://www.intechope...-little-ice-age
Mark Twain
All views I express are either my own or the dog's; often it's difficult to discern which of us is spouting the most gibberish.
#3
Posted 04 November 2010 - 02:40
Edited by nimbilus, 04 November 2010 - 03:00 .
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#4
Posted 04 November 2010 - 02:53
Edited by nimbilus, 04 November 2010 - 02:55 .
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#5
Posted 05 November 2010 - 17:46
nimbilus, on 04 November 2010 - 02:53 , said:
Interesting you should ask that. I asked the better half what the atmosphere did for earth just last night to see what a non-weather/science freak thinks. I asked did the atm...
(1) keep the earth's surface warmer than it would be without it?
(2) keep the earth's surface cooler than it would be without it?
She looked at me funny and answered 'the first of course - that's the greenhouse effect!'.However, they are both actually correct as written with respect to a person standing on earth. The atmopshere does not specifically keep us warm, nor cold, at least not locally, it stablises temperature. Without it, the surface of the earth would be more like the moon - hot enough (above +100 C) to boil water in the middle of the day, below -100 C at night. The correct way to think about it is what the atmosphere specifically does is to buffer these extremes to a large extent, depending on where you are, giving a global average temperature which is generally higher (estimate is often 33 C, but still debated) than what it would be without it.
If you want to see the extremes, you need to go where there is little water; surface, vegaetative, not atmospheric - e.g. the sahara desert. Then you can see what a less water-buffered (the main greenhouse gas with the highest heat capacity) atmosphere feels like; +45 C in the day dropping to freezing at night. Bit more like the surface of the moon...
Cheers,
SS
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#6
Posted 06 November 2010 - 02:38
right this is about (think im going off topic) climate history, so what caused the medieval warm period?
the evidence from ice cores, tree rings, and i think insects? shows warming and cooling periods.
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#7
Posted 12 November 2010 - 17:29
More is known now than when this book was first published about the exchanges that go on between the Arctic seas and the climate over wider areas and longer times (which we return to on p. 271). The great increase of ice on the East Greenland Sea in the mid-I960s, and the low salinity water that accompanied it, migrated from there slowly to affect the western Atlantic in the years that followed and, after a long clockwise circuit over the western ocean, was carried back into the Iceland region after fourteen more years. In the meantime there had been a rather warmer, more saline phase near Iceland. A study by Dickson and others in 19881 followed the progress of the anomaly and the cycle of changes that went with it over nearly two decades. And this inspired others, notably Mysak and his co-workers at the Centre for Climate and Global Change Research and the Department of Meteorology at McGill University, Montreal, to trace the anomaly back through its earlier history before it first reached the Greenland Sea. Its origin is found to have been in a greatly boosted. runoff into the Arctic Ocean north of Canada from the North Amencan rivers, mainly the Mackenzie River system in the western part of northern Canad.a, in the early 1960s.
The paper by Mysak, Manack and Marsden , Sea –Ice Anomalies Observed in the Greenland and Labrador Seas during 1901-1984 and their relation to an interdecadal Arctic climate cycle.
http://www.geog.mcgi...no.-1989-14.pdf
Edited by weather ship, 12 November 2010 - 17:30 .
Neils Bohr
#8
Posted 12 November 2010 - 19:42
weather ship, on 12 November 2010 - 17:29 , said:
Very interesting read. I had not heard/thought about this factor before; i.e. the contribution from surface run-off of fresh water into the arctic from the surrounding continents... This water should of course float outwards over the denser saline sea water, potentially increasing the freezing temperature of the surface water from -2.3 C back towards zero. Without signficant currents/redistribtuion and turnover (vertical mixing) it would make perfect sense that this could cause very signficant increases in sea ice, at least locally. Increased temperatures cause increased rainfall over certain regions causing increased fresh runoff into the arctic causing an increase in ice cover and increased cooling before the cycle turns on itself and reverses. Such work shows the common belief that ice in Arctic has been constant until AGW came along as complete rubbish.
This paper is from a while back (20+ years is a long time in science). Whether it is a good example, I'm not sure as I don't know how much such work is incorportated into current theories but.... Often in science, the same things are studied twice or more. Someone notices something and reports it in a paper. However, at that point in time it is not 'hot' science, so it goes rather unoticed. Then, 10, 20 years later the topic is hot and someone studies the same thing again, unaware that there is already a study on it, publishing findings without considering earlier studies. I had a classic example of this a few years ago. Nature paper announces that hydrogen can form clathrate hydrates - hydrates could be a new clean H2 storage material! Authors very pleased with themselves until, someone says - actually, this was discovered 20 years ago but nobody cared too much about it then, so it went in standard journal to gather dust.... All you have done is rediscovered it.
I wonder how much early, pre-AGW work on ice, glaciers etc goes 'unoticed'. Old stuff is often better than modern science too - scientists of the past were often much more methodical as they were less driven to get the latest out asap.. things went at a slower pace.
Edited by scottish skier, 12 November 2010 - 19:45 .
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#9
Posted 14 November 2010 - 11:02
jethro, on 03 November 2010 - 23:39 , said:
http://www.intechope...-little-ice-age
Interesting read , people can always jump to page 20 for the summary.
Suggest at least a Nothern Hempishere pattern of changes rather then just for example the MWP just effecting a few areas (e.g NW Europe).
#10
Posted 14 November 2010 - 15:33
Interestingly the southward limit polar water east of Iceland has sometimes been approached over short periods of up to a few weeks in recent years. For example , in April 1968 and again in 1969 this water-mass advanced to near the Faeroe Islands, and more briefly a number of times in the first half of 1979.
Positions of the boundary in the ocean surface between water of Gulf Stream origin and the polar ocean current from near northeast Greenland in the twentieth-century warmest years and at various times past.
Excuse the drawing=I'm no Picasso!
Yellow- Warm Period 20th century.
A.D 1675-1700
7-8000BC
8300BC
White-65-70,000 years ago.
Ice Age climax, 17,000-20,000 years ago.
Edited by weather ship, 14 November 2010 - 15:38 .
Neils Bohr
#11
Posted 16 November 2010 - 19:57
weather ship, on 14 November 2010 - 15:33 , said:
Positions of the boundary in the ocean surface between water of Gulf Stream origin and the polar ocean current from near northeast Greenland in the twentieth-century warmest years and at various times past.
Excuse the drawing=I'm no Picasso!
Yellow- Warm Period 20th century.
A.D 1675-1700
7-8000BC
8300BC
White-65-70,000 years ago.
Ice Age climax, 17,000-20,000 years ago.
Interesting , where did you get the data from, any link ?
I assume the 'gulf stream' still played its part but was switch off re last ice age 17000 yrs ago ?
#12
Posted 17 November 2010 - 06:54
Water of 'Gulf Stream' origin still played its part in the sense it was the boundary between the cold water down as far as Biscay and the warmer water, somewhat different to today, but it has to be remembered that atmospheric circulation was vastly different. So it wasn't so much a swithch off but a completely different ball game.
Neils Bohr
#13
Posted 18 November 2010 - 16:06
weather ship, on 17 November 2010 - 06:54 , said:
Water of 'Gulf Stream' origin still played its part in the sense it was the boundary between the cold water down as far as Biscay and the warmer water, somewhat different to today, but it has to be remembered that atmospheric circulation was vastly different. So it wasn't so much a swithch off but a completely different ball game.
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#14
Posted 18 November 2010 - 18:47
*The Polynesian expansion that coincided with Europe's "Medieval Warm period"; Scandinavians settling Greenland was impressive, but people from tropical islands sailing to southern New Zealand and settling there (they even reached the Auckland Islands below 50S) was phenomenal. And was the cooling asociated with the LIA behind the population collapse on Easter Island? Looking at the climate data, that island is currently right on the tropical/subtropical border line; 2-3C warmer (AD1000?) and they'd have no trouble growing stuff from Tahiti. 2-3C cooler (AD1600?) and most of their tropical crops would fail, except perhaps the sweet potato which still grows there now.
*All the central Asian tribes that suddenly appeared on the borders of Europe in the 1200s. Hell-bent on world domination, or sensing a cold period was starting in their homelands and looking for somewhere more amenable? (Some of them had done the same thing at the start of the cold period around 4-500 as well).
*The rise of civilisations in the Americas that also coincided with the Medieval Warm Period
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#15
Posted 05 December 2010 - 12:58
scottish skier, on 05 November 2010 - 17:46 , said:
(1) keep the earth's surface warmer than it would be without it?
(2) keep the earth's surface cooler than it would be without it?
She looked at me funny and answered 'the first of course - that's the greenhouse effect!'.However, they are both actually correct as written with respect to a person standing on earth. The atmopshere does not specifically keep us warm, nor cold, at least not locally, it stablises temperature. Without it, the surface of the earth would be more like the moon - hot enough (above +100 C) to boil water in the middle of the day, below -100 C at night. The correct way to think about it is what the atmosphere specifically does is to buffer these extremes to a large extent, depending on where you are, giving a global average temperature which is generally higher (estimate is often 33 C, but still debated) than what it would be without it.
If you want to see the extremes, you need to go where there is little water; surface, vegaetative, not atmospheric - e.g. the sahara desert. Then you can see what a less water-buffered (the main greenhouse gas with the highest heat capacity) atmosphere feels like; +45 C in the day dropping to freezing at night. Bit more like the surface of the moon...
Cheers,
SS
Where exactly in the Sahara is it 45+ by day and freezing at night. Or any desert in fact.
If there is one common misconception that gets my goat it is the "boiling by day, freezing by night in the desert" comments.
There is no site on earth that commonly gets 45 degrees in the afternoon and 0 at night. If such a site exists show it to me.
Go to Las Vegas, or Phoenix, or Luxor, in the summer when it is 40-45º by day, or Baghdad or Death Valley where it is more like 45-50 and tell me what the night time temperatures are on those days? A frost doesn't enter the equation.
These fabled 45/0 desert locations do not exist.
Anyway, sorry about picking one sentence, back to the topics at hand...
Edited by paul tall, 05 December 2010 - 13:02 .
#16
Posted 05 December 2010 - 13:06
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#17
Posted 05 December 2010 - 13:11
Yes we've all heard very rare stories of temperatures in winter/spring rising from -20 to +10 in a matter of hours due to warm fronts and fohn winds etc - but that is really the opposite of 45 degree afternoon heat in the summer under established stagnant hot air (nowhere that I am aware of gets 45 degrees in winter) somehow turning into an air frost. It just doesn't happen.
And meteorological records from 10s of thousands of places back this up.
#18
Posted 05 December 2010 - 17:40
Neils Bohr
#19
Posted 05 December 2010 - 18:52
Thanks
#20
Posted 05 December 2010 - 19:08
Pocatello max/min for July 30/10. That's quite extreme to be fair. But again, it's not in the same league as the boiling/freezing type desert climates that I've heard of but never seen any evidence of.
Also looking at the map, it appears that the Snake River Plain is in a giant valley surrounded by very high mountains, so I'd guess an excellent natural frost hollow, as cold air would readily sink down to the plain - this is in fact evidenced in the climatic averages, as places that average 32º in the summer you'd expect night temperatures to be approaching 20º, not 10º.
But with all the geological advantages it's temperatures come nowhere near the sort of diurnal ranges that people claim for deserts.













