Wednesday, May 5, 2010

April 30 - Ice Age theories warming up

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Ice Age theories warming up

By Mark S. Lawson - posted Friday, 30 April 2010
One of the more interesting results from recent research into climate is that for the past million years or so, the earth’s climate has shown a distinct 100,000 cycle of long ice ages punctuated by a brief, warm intergalacials. We are in one of those brief warm periods, an interglacial period that is called the Holocene.
This cycle can be seen in the temperature graph below taken from publically available Vostok ice core data. The ice cores are very long sections of ice in which ancient climates can be worked out by careful analysis of atomic isotopes of layers of ice, where each wafer thin layer represents a year. Although there are other ways to determine past climatic conditions the Vostok cores (the site is in Antarctica but run by Russian scientists) are remarkable in being a connected track of temperatures of several hundred thousand years.
As you can see climate changes by about 14 degrees C from the top of the interglacial to the bottom of the ice age, but even the 420,000 or so years covered by the Vostok cores is just a moment in earth’s geological history. As noted, the 100,000 year cycle has been a feature of climate for about a million years. For two million years before that the cycle was the same except that it was 40,000 years long and temperatures were warmer. The whole three million years, in turn, is part of an ice age phase of the earth in which temperatures have generally been falling. There have also been hot house phases.

Temperatures over the most recent 420,000 years of earth’s history. Note that the graph time line is from left to right. All of recorded human history is in a couple of squiggles on the far right. Source: Vostok cores and Petit et al, 1999. Also note that the temperature scale is relative and the zero line is just a handy reference point. It has nothing to do with the freezing point of water.

Scientists have no real idea why the earth has been cooling over the past three million years and, in particular, are puzzled over the shift from 40,000 to 100,000 cycles. But until recently they thought they had a mechanism for explaining the current ice age cycle. This to be found in the Milankovitch cycles which are known, slight changes in the earth’s orbit and the angle of the earth’s pole. The theory was first proposed by James Croll, a self-taught 19th century physicist and greatly extended by a Serbian civil engineer and geophysicist Milutin Milankovitch who died in 1958. The theory, which has fallen in and out of favour a couple of times since it was first proposed, supposes that the orbital variations changes the strength of the seasons. Summers may become hotter or colder, winters may become colder or milder. That very slight change then becomes amplified in some way, perhaps by melting ice exposing rock which absorbs more heat.
As is generally accepted once the warming is underway it warms the oceans, and warmer oceans hold less carbon dioxide so there is more in the atmosphere, and those increased concentrations should cause more warming. Global warmers say that the CO2 increases then drive the warming. One problem with that supposition is the long time lag between warming and increases in CO2 levels. This point has been explored through a series of scientific papers with the latest published in the journal Science last year by a team led by Lowell Scott of the Department of Earth Sciences, University of Southern California. Entitled Southern Hemisphere and Deep-Sea Warming Led Deglacial Atmospheric CO2 Rise and Tropic Warming, the paper puts the lag at 1,000 years.
Another glance at the graph indicates that temperatures in the previous two interglacials seem to spike to well above modern temperatures, but the ice core readings for the time show that CO2 levels were at about 300 parts per million or far less than present levels. The Arctic Climate Impact Assessment Report 2005, compiled by a group called the International Arctic Science Committee and used as a source for the 2007 IPCC report says that during the inter-glacial preceding this one, known as the Eemian, conditions were generally warmer than they are now. The 2007 IPCC report says that polar temperatures at the time were 3 to 5 degrees higher than now, but attributes the difference to Milankovitch cycles.
Conditions were also warmer just a few thousand years ago in what is usually called the mid-Holocene maximum, and again the IPCC blames this on orbital cycles reinforced by natural CO2 emissions. Perhaps. The orbital cycles theory has come under major attack of late with recent work suggesting that the Milankovitch cycles peak thousands of years after the effect they are supposed to cause. That work is all subject to argument but there are other puzzles.
As you can see from the graph the Holocene is already longer than the preceding three interglacial periods at least. Estimating from graphs that are better than mine, the Eemian lasted less than 10,000 years and the previous two interglacials lasted perhaps just 5,000 years. The Holocene, in contrast, has clocked up 10,000 years plus. Further, those 10,000 years have remained comparatively warm, in contrast to the previous interglacials in which temperatures spiked then fell away again very quickly. In all cases the final collapse into an ice age has been abrupt - perhaps just a few generations. The atmosphere-oceanic system just seems to trip over itself to fall 10 degrees and more, and with climate theory in its present state there is no way to predict when it will occur. Orbital cycles theory suggests the Holocene has another 14,000 or so, although the theory doesn’t have much to say about how interglacials end. Then there is the comparative newcomer, solar magnetic theory, which is set to sweep orbital cycles off the board. For the evidence that the sun’s magnetic field affects climate is overwhelming.
The sun has an 11 year cycle marked by sun spots that astronomers can observe on the face of the sun. They have been counting and tracking these spots for more than 300 years. At the height of the solar cycle there are lots of these sunspots and the sun is said to be very active, generating plenty of flares and solar storms which affect satellites, and its magnetic field is stronger. At the bottom of the cycle there are few or no spots, and distinctly less solar magnetic activity. The sun is quiet. But that cycle is just part of the changes in solar magnetism which scientists have now being able to track through thousands of years by measuring very fine changes in isotopes of carbon in living and fossilised trees.
Just how solar magnetic activity affects climate is still a matter of argument but, scientists suppose, a stronger field helps shield the earth from solar radiation which is supposed to help in forming clouds. The stronger the solar magnetic field (which is different from the overall amount of energy the sun emits) the fewer clouds, and the warmer the earth. When the field weakens there are more clouds which cool the earth – or so the theory goes.
Dedicated global warmers hoping that the solar magetic theory cannot possibly be right should look at Recently opposite directed trends in climate forcings and the global mean surface temperature (Proceedings of the Royal Society A, July 13, 2007) by Mike Lockwood, a physicist at the Rutherford Appleton laboratory (and strongly in the global warming camp) and Claus Frolich, of the word radiation centre in Davos, Switzerland.
Lockwood and Davos use the first two pages of their paper to acknowledge the mass of evidence for the influence of changes in the sun’s magnetic field on climate, including the key work of Gerard Bond of the Lamont-Doherty Earth Observatory of Colombia University and nine others which linked solar activity to changes in drift ice in the North Atlantic over thousands of years (Persistent Solar Influence on North Atlantic Climate During the Holocene, Science, December 7, 2001). After waving around a lot of graphs and numbers, however, the pair conclude that the link breaks down in 1985, with the implication being that the warming after that must be due to industrial gases.
That conclusion has been heavily challenged but we will not linger on that issue. The point is that solar magnetic fields affect climate. One other often cited piece of evidence is that of the depths of the little ice age (a cold period last centuries up to the 1850s) was associated with an absence of sun spots. The link may be deep indeed, as shown by an interesting although still speculative paper by Charles A. Perry, of the US Geological Survey, and Swiss scientist Kenneth J. Hsu - Geophysical, archaeological and historical evidence support a solar-output model for climate change (Proceedings of the National Academy of Sciences, November 7, 2000; available online).
The paper presents evidence of larger and longer cycles in the sun than just the 11 year basic sunspot cycle, and that the cycles fall into a noticeable pattern. The two scientists then extrapolate that work to suppose that there are 13 individual cycles, ranging from 11 years through to 90,000 years, or the length of an ice age.
Using the end of the last ice age as an anchor point, they combined all those cycles to give a pattern which follows the highlights of known climate history including the holocene maximum, medieval warm period and little ice age. No need to bother with orbital cycles at all. The warm periods are when one or more than one cycles are up, cold periods are when they are down. Far more importantly the analysis also forecasts a sharp fall in solar activity off a peak sometime after 2000, and that seems to have happened, albeit a few years later which is not bad considering the scale of the work. As has been widely reported the sun’s 11 cycle stopped mysteriously in 2007 with no sunpots for long periods and then only two or three. The spots are not building up into a peak. (A last check as this was being written showed none at all.)
Perry and Hsu’s work also indicates that the present intergalacial, which has proved so comfortable for humans, will last another 10,000 years with occasional bouts of colder climate which may happen from now thanks to the fall of in solar activity. Whatever affect industrial activity is supposed to have had on climate may well be swamped by natural cooling. Cannot possibly happen you say? We shall see.

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How to Digitally Record/Video a UFO sighting:

Como registar digitalmente ou gravar um vídeo de um avistamento de um UFO:

Stabilize the camera on a tripod. If there is no tripod, then set it on top of a stable, flat surface. If that is not possible lean against a wall to stabilize your body and prevent the camera from filming in a shaky, unsteady manner.

Estabilize a camera com um tripé. Se não tiver um tripé, então coloque-a em cima de uma superfície estável. Se não for possível, então encoste-se a uma parede para estabilizar o corpo e evitar que a camera registe de maneira tremida e instável.

Provide visual reference points for comparison. This includes the horizon, treetops, lampposts, houses, and geographical landmarks (i.e., Horsetooth Reservoir, Mt. Adams, etc.) Provide this in the video whenever is appropriate and doesn’t detract from what your focus is, the UFO.

Forneça pontos visuais de referência para comparação. Isso inclui o horizonte, cimo das árvores, postes de iluminação, pontos de referência geográficos (como o Reservatório de Horsetooth, Mone Adams, etc) Forneça esses pontos no vídeo sempre que for apropriado e não se distraia do que é o seu foco, o UFO/a Nave.

Narrate your videotape. Provide details of the date, time, location, and direction (N,S,E,W) you are looking in. Provide your observations on the weather, including approximate temperature, windspeed, any visible cloud cover or noticeable weather anomalies or events. Narrate on the shape, size, color, movements, approximate altitude of the UFO, etc and what it appears to be doing. Also include any unusual physical, psychological or emotional sensations you might have. Narrate any visual reference points on camera so they correlate with what the viewer will see, and thereby will be better able to understand.

Faça a narração do vídeo. Forneça pormenores sobre a data, hora, local e direcção (Norte, Sul, Este, Oeste) que está a observar. Faça observações sobre as condições atmosféricas, incluindo a temperatura aproximada, velocidade do vento, quantidade de nuvens, anomalias ou acontecimentos meteorológicos evidentes. Descreva a forma, o tamanho, a cor, os movimentos, a altitude aproximada onde se encontra o UFO/nave, etc e o que aparenta estar a fazer. Inclua também quaisquer aspectos pouco habituais de sensações físicas, psicológicas ou emocionais que possa ter. Faça a narração de todos os pontos de referência visual que o espectador irá ver e que, deste modo, será capaz de compreender melhor.

Be persistent and consistent. Return to the scene to videotape and record at this same location. If you have been successful once, the UFO sightings may be occurring in this region regularly, perhaps for specific reasons unknown, and you may be successful again. You may also wish to return to the same location at a different time of day (daylight hours) for better orientation and reference. Film just a minute or two under “normal” circumstances for comparison. Write down what you remember immediately after. As soon as you are done recording the experience/event, immediately write down your impressions, memories, thoughts, emotions, etc. so it is on the record in writing. If there were other witnesses, have them independently record their own impressions, thoughts, etc. Include in this exercise any drawings, sketches, or diagrams. Make sure you date and sign your documentation.

Seja persistente e não contraditório. Volte ao local da cena e registe o mesmo local. Se foi bem sucedido uma vez, pode ser que nessa região ocorram avistamentos de UFOs/naves com regularidade, talvez por razões específicas desconhecidas, e talvez possa ser novamente bem sucedido. Pode também desejar voltar ao mesmo lugar a horas diferentes do dia (durante as horas de luz)para ter uma orientação e referência melhor. Filme apenas um ,inuto ou dois em circunstâncias “normais” para ter um termo de comparação. Escreva tudo o que viu imediatamente após o acontecimento. Logo após ter feito o registo da experiência/acontecimento, escreva imediatamente as impressões, memórias, pensamentos, emoções, etc para que fiquem registadas por escrito. Se houver outras testemunhas, peça-lhes para registar independentemente as suas próprias impressões, pensamentos, etc. Inclua quaisquer desenhos, esbolos, diagramas. Certifique-se que data e assina o seu documento/testemunho.

Always be prepared. Have a digital camera or better yet a video camera with you, charged and ready to go, at all times. Make sure you know how to use your camera (and your cell phone video/photo camera) quickly and properly. These events can occur suddenly, unexpectedly, and often quite randomly, so you will need to be prepared.

Esteja sempre preparado, Tenha sempre uma camera digital, melhor ainda, uma camera vídeo consigo, carregada e pronta a usar sempre que necessário. Certifique-se que sabe como lidar com a sua camera (ou com o seu celular/camera fotográfica) rápida e adequadamente. Esses acontecimentos podem acontecer súbita e inesperadamente e, por vezes, acidentalmente, por isso, necessita estar preparado.

Look up. Be prepared. Report. Share.

Olhe para cima, Esteja preparado, Relate, Partilhe.



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