Showing posts with label glaciers. Show all posts
Showing posts with label glaciers. Show all posts

Wednesday, June 25, 2014

Glaciers As Global Warming Drama, Part Of The Big Lie

The nonsense about man-caused global warming and climate change just keeps coming.  It is the grandest hoax of our age, and that is saying a lot.  What is the latest outrage to irk me?  Glaciers.  Plain old ice.

Everyone responds to dramatic effects.  The news media knows that.  Hollywood knows that.  We are a culture bred to respond to video or photographic images.  Man was first influenced by verbal story tellers, then accompanied by song, then came the written word, then the drawn or painted visual word, followed by photographs, then moving photographs, now video and everything digitized and available anywhere at the speed of light. 

This is why glaciers are used so often to depict "catastrophic" global warming, because they are visual, huge, dramatic, and awe-inspiring.  Imagine, people take cruises to places like Alaska, Patagonia, Argentina, and Antarctica, for what?  To see big ice cubes (glaciers) melt.  Then they attribute the melting to man's burning of fossil fuels and the emission of carbon dioxide (CO2).  Apparently, many people are so awed by this melting ice they are willing to open their wallets and freely give money to those who promise stop the calamity of big melting ice cubes.  This melting and freezing of glacial ice has always been going on.  It is nothing new.  Al Gore did not invent it.  It is not a catastrophe because President Obama's teleprompter says so, or because John Kerry is instructed to say it is.  It all sounds insane, doesn't it.  Well, it is.

Why do they continue lying to us about global warming and climate change as being (or implied to be) man-caused in articles like the following? The only answer is we are being manipulated. What is the reason? If this effort is based on lies, it is wrong, and our money (taxes) are being taken unfairly and we ought to be outraged. Can it be much simpler than that? Are we so afraid to dissent and disagree that we march along like sheep to the slaughter? Have we as a people, as a nation, sunk so low, become so passive, so obedient? I hope not, even if recent election results seem to indicate otherwise.
Peter




http://www.newscientist.com/article/mg22229752.600-ice-sheets-may-have-already-passed-point-of-no-return.html#.U6uKCjco6eQ

"THE cracks are beginning to show. Greenland's ice sheets slid into the sea 400,000 years ago, when Earth was only a little warmer than it is today. That could mean we are set for a repeat performance.
The finding, along with data from Antarctica, suggests both of Earth's big ice sheets may have already passed a crucial tipping point, condemning them to collapse – either melting, or sliding into the ocean. That will mean sea levels rising by as much as 13 metres, leading to massive coastal flooding. So how fast will the ice collapse, and can we stop it?"
 
(Is the above statement from the linked article complete sensationalist nonsense, or what?  Of course it is, and it is typical of what our young people are being fed and considered science.  Think of what a steady diet of this poison does.  And we wonder why people vote the way they do?  Peter)

Tuesday, July 16, 2013

Planet Earth Does Not "Lose" Ice

Breaking news: planet Earth does not "lose" ice or water.  Ice either melts into water and is stored in the oceans, lakes, rivers, atmosphere or underground reservoirs.  When ice is not melting, water is being added to glaciers as snow and ice.  This cycle of cooling and warming, melting and freezing, has been going on essentially since the creation of the Earth.  Note this has been going on longer and is controlled by forces far greater than humans burning fossil fuels.

Here is a summary of what is known as the Earth's Hydrologic Cycle, taken from this blog.  You can do a search of this blog and find much more.
Peter

Jan 24, 2008
It seems a refresher course in the basics of the Earth's hydrologic cycle is in order. First of all, it needs to be understood that there is a finite, or relatively fixed amount of water on or in the Earth. This does not, has not, and can ...



Chilling Report: Earth Loses 300 Billion Tons of Ice Each Year

It is amazing to see because it feels so clearly out of place, but in some spots along Antarctica’s coast you can actually find hints of grass and other plant life—green evidence that in parts of the long-frozen continent the ice is thinning, and fast.
 
But just how much ice is being lost? A new, ten-year study conducted by Bristol University’s Glaciology Centre says that between Antarctica and Greenland, the answer is 300 billion tons a year.
That’s a lot of ice cubes.

In scientific terms, a decade makes for a short study; this one can’t forecast whether this kind of loss will sustain into the future. (Though reasoned experts believe it will and may even accelerate.) But if it continues at this pace, goodbye Miami, Hong Kong, New York City, etc., as well as the homes of hundreds of millions who live on estuaries, deltas, coral atolls and great city river basins around the globe.

The two massive ice sheets in Greenland and Antarctica combined—the ice in Antarctica is three miles thick at some places—contain 99.5 percent of the earth’s glacier ice. If it were all to melt (which would admittedly take centuries), sea levels would rise by 500 to 600 feet.
I’ve been to Antarctica on a couple dozen different trips, mostly along it’s long, skinny Peninsula, which because it is surrounded by warming ocean on both sides is the area most-impacted by the planet’s changing climate. It’s there each austral summer that more shorelines are exposed thanks to disappearing ice, and where you find hints of plant life. (How did the seeds get there? Most likely hitchhiking on fishing boats and visiting tourist ships, both growing in numbers.)

Another satellite study, conducted over the past 20 years by NASA and the European Space Agency, confirms the Bristol study, reporting that the planet’s ice sheets have melted faster in the last 20 years than in the last 10,000.

According to this study, melting ice from both poles has been responsible for a fifth of the global rise in sea levels since 1992. The rest was caused by the thermal expansion of the warming ocean, the melting of mountain glaciers, small Arctic ice caps and groundwater mining. The share of the polar ice melt, however, is rising and most concerning.

When it comes to Antarctica, though, it can be tricky to generalize. It is a huge continent; the U.S. could easily fit inside its borders. In the huge area of East Antarctica, where the ice is mostly above sea level, the air temperature is also much lower, and the experts do not expect the ice to melt on account of rising temperatures. In this part of Antarctica, the ice sheet is actually growing as a consequence of increased snowfall.

But today, using a variety of satellite reports and on-the-ice studies that have been going on for many decades, even conservative scientists say sea levels are rising 60 percent faster than what the Intergovernmental Panel on Climate Change predicted in 2007.

Tuesday, January 13, 2009

USGS Website On Glaciers And Climate Change

Here is an excellent website created by the USGS (United States Geological Survey). It illustrates and explains the basics about glaciers, their history, and how they respond and relate to the Earth's changes in climate. In trying to understand all of the concern over global warming, this website is a good place to learn what we do know about glaciers and climate change from past history. This way we can put current events in perspective and hopefully be better able to separate fact from fiction, or reality from global warming alarmist hype.
Peter


Glaciers and Climate Change
January 13, 2009 USGS (source)

The USGS has a website that illustrates how Earth’s glaciers and landscapes are responding to climate change. The site focuses on the glaciers of Alaska.

For example, some interesting facts about glaciers and sea level:

Glaciers and Sea Level
Grinnell Glacier in Glacier National Park, Montana; photograph by Carl H. Key, USGS, in 1981. The glacier has been retreating rapidly since the early 1900's. The arrows point to the former extent of the glacier in 1850, 1937, and 1968. Mountain glaciers are excellent monitors of climate change; the worldwide shrinkage of mountain glaciers is thought to be caused by a combination of a temperature increase from the Little Ice Age, which ended in the latter half of the 19th century, and increased greenhouse-gas emissions.

Worldwide, most mountain glaciers have been retreating since the end of the "Little Ice Age". Although this date varies from region to region, in most locations, retreat was underway by the late 1800s. As a consequence of glacier meltwater entering the global ocean, global sea level has risen about 30 centimeters (about one foot). Glaciers vary in size in response to changes in global and regional climate.

Sea-level changes, especially in densely populated, low-lying coastal areas and on islands, have significant effects on human activities and facilities. The present volume of the Earth’s glacier ice, if totally melted, represents about 80 meters in potential sea-level rise.

If all of Alaska's glaciers melted, sea level would rise ~ 0.05 meters (about 0.16 feet).

If all of Earth's temperate glaciers melted, sea level would rise ~ 0.3 meters (about one foot).

If all of Greenland's glaciers melted, sea level would rise ~ 6 meters (about 19.7 feet).

If all of Antarctica's glaciers melted, sea level would rise ~ 73 meters (about 240 feet).

The geologic record documents that glaciers have existed on Earth for billions of years. During that time, glaciers have repeatedly expanded and shrunk in response to changes in global and regional climate. During glacial stages (ice ages), periods of time dominated by colder climate, global sea level was lowered by as much as 200 meters. This is the result of water evaporating from the oceans being precipitated as snow and frozen into continental scale glaciers.

About 21,000 years ago, during the last glacial maximum (LGM), sea level was about 125 meters (about 410 feet) lower than it is today.

About 125,000 years ago, during a warmer climatic interval in the last interglacial stage, sea level was about 6 meters (about 19.7 feet) higher than it is today.

About 2.2 million years ago, during an even warmer inter­val, sea level is estimated to have been 25 to 50 meters (about 82 to 164 feet) higher.

Less than 20,000 years ago, during the last phase of the Pleistocene, the Last Glacial Maximum (LGM), glaciers covered: ~ 8 % of Earth's surface ~ 25 % of Earth's land area ~ 30% of Alaska.

Following the LGM (beginning ~ 15,000 yr B.P.), continental glaciers retreated and sea level began to rise. By ~ 6,000 yr B.P. sea level reached its current height. It has fluctuated ever since.
Today, glaciers cover: ~ 3.1 % of Earth's surface, ~ 10.7 % of Earth's land area ~ 5 % of Alaska.

For more information visit the USGS Web site Sea Level and Climate.

Monday, April 7, 2008

Glaciers and Sea Ice: Melting Or Growing?

Here is a link to a good website which deals with the issue of glaciers and sea ice. Are they melting or expanding? We've been bombarded with pictures of melting glaciers and rising sea levels. We're told we're headed for catastrophe because of global warming. Is any of this true? Check out this website: http://www.iceagenow.com/Growing_Glaciers.htm

For example:

Here's a (partial) list of the specific glaciers that are growing:
NORWAY Ålfotbreen Glacier Briksdalsbreen Glacier Nigardsbreen Glacier Hardangerjøkulen Glacier Hansebreen Glacier Jostefonn Glacier Engabreen glacier (The Engabreen glacier is the second largest glacier in Norway. It is a part (a glacial tongue) of the Svartisen glacier, which has steadily increased in mass since the 1960s when heavier winter precipitation set in.)
Norway's glaciers growing at record pace. The face of the Briksdal glacier, an off-shoot of the largest glacier in Norway and mainland Europe, is growing by an average 7.2 inches (18 centimeters) per day. (From the Norwegian daily Bergens Tidende.) See http://www.sepp.org/controv/afp.htmlClick here to see mass balance of Norwegian glaciers: http://www.nve.no/ Choose "English" (at top of the page), choose "Water," then "Hydrology," then "Glaciers and Snow" from the menu. You'll see a list of all significant glaciers in Norway. (Thanks to Leif-K. Hansen for this info.)

CANADA Helm Glacier Place Glacier
FRANCE Mt. Blanc
ECUADOR Antizana 15 Alpha Glacier
SWITZERLAND Silvretta Glacier
KIRGHIZTAN Abramov
RUSSIA Maali Glacier (This glacier is surging. See below)
GREENLAND See Greenland Icecap Growing Thicker Greenland glacier advancing 7.2 miles per year! The BBC recently ran a documentary, The Big Chill, saying that we could be on the verge of an ice age. Britain could be heading towards an Alaskan-type climate within a decade, say scientists, because the Gulf Stream is being gradually cut off. The Gulf Stream keeps temperatures unusually high for such a northerly latitude.
One of Greenland’s largest glaciers has already doubled its rate of advance, moving forward at the rate of 12 kilometers (7.2 miles) per year. To see a transcript of the documentary, go to http://www.bbc.co.uk/science/horizon/2003/bigchilltrans.shtml
NEW ZEALANDAll 48 glaciers in the Southern Alps have grown during the past year.The growth is at the head of the glaciers, high in the mountains, where theygained more ice than they lost. Noticeable growth should be seen at the foot of the Fox and Franz Josef glaciers within two to three years.(27 May 2003) Fox, Franz Josef glaciers defy trend - New Zealand's two best-known glaciers are still on the march - 31 Jan 07 - See Franz Josef Glacier

SOUTH AMERICA - Argentina's Perito Moreno Glacier (the largest glacier in Patagonia) is advancing at the rate of 7 feet per day. The 250 km² ice formation, 30 km long, is one of 48 glaciers fed by the Southern Patagonian Ice Field. This ice field, located in the Andes system shared with Chile, is the world's third largest reserve of fresh water. http://en.wikipedia.org/wiki/Perito_Moreno_Glacier - Chile's Pio XI Glacier (the largest glacier in the southern hemisphere) is also growing.

UNITED STATES - Colorado (scroll down to see AP article) - Washington (Mount St. Helens, Mt. Rainier* and Mt. Shuksan) (scroll down to see photo of Mt. Baker) - California (Mount Shasta - scroll down for info) - Montana (scroll down for info) - Alaska (Mt. McKinley and Hubbard). (scroll down to see article on Hubbard Glacier)
Antarctic ice grows to record levels 13 Sep 07 - While the Antarctic Peninsula area has warmed in recent years and ice near it diminished during the Southern Hemisphere summer, the interior of Antarctica has been colder and ice elsewhere has been more extensive and longer lasting,See Antarctic ice grows to record levels..
Global Warming? New Data Shows Ice Is Back19 Feb 08 - A Feb. 18 report in the London Daily Express showed that there is nearly a third more ice in Antarctica than usual, challenging the global warming crusaders and buttressing arguments of skeptics who deny that the world is undergoing global warming.See Most snow cover since 1966..
Mount St. Helens’ Crater Glacier Advancing Three Feet Per Day 25 Jun 07 - See Crater Glacier..
Mount St. Helens glacier (Crater Glacier) growing 50 feet per year September 20, 2004 - See Mount St. Helens
Glaciers growing on California's Mount Shasta! 12 Oct 03 - See Mount Shasta Glaciers Growing
Geologists Unexpectedly Find 100 Glaciers in Colorado 7 Oct 01 See Colorado Glaciers Growing
Washington's Nisqually Glacier is GrowingSee Nisqually Glacier
Glaciers in Montana's Glacier Park on the verge of growing 5 Oct 2002. See Glacier Park
Antarctic Ice Sheet is growing thickerSee Antarctic Icecap Growing ThickerSee construction crane buried in the Antarctic Ice Sheet
* * *
Himalayan Glaciers Not ShrinkingGlacial Experts Question Theory of Global Warming15 Feb 07 - See Himalayan Glaciers Not Shrinking..Many people have asked why some glaciers in South America are melting. I think it is perfectly understandable. Remember, we have had two of the strongest El Ninos on record during the past 21 years. During an El Nino, a narrow band of the Pacific Ocean warms by as much as 14 degrees. This band of warm water travels east essentially along the equator until it slams into South America.
It seems logical that the increased rainfall caused by El Nino, plus the warmer winds blowing across the warmer water, could hasten glacial melt. But let me say it again. I do not believe that this is caused by humans, I think it is caused by the El Nino phenomenon, which is caused by underwater volcanism, which is increasing due to the ice-age cycle.
With this said, let me point out many glaciers in South America remain stable, and some - including the Pio XI Glacier and the Perito Moreno Glacier - are growing. The Pio XI Glacier is the largest glacier in the southern hemisphere. The Moreno Glacier is the largest glacier in Patagonia.
I find it curious that news reports do not mention these two glaciers.
* * *
Contrary to previous reports, Arctic ice did not thin during the 1990s, say researchers at the Department of Oceanography at Göteborg University in Göteborg, Sweden. http://www.envirotruth.org/images/ice-in-90s.pdf

.. Alaska Glacier Surges -17 Mar 06 See McGinnis Glacier ..Look at what's happening on Mt. Baker, in Washington State. (Mt. Baker is near Mt. Shukson, where glaciers are now growing.)
This is a photo of my friend Jim Terrell taken onMt. Baker, Washington. Jim is more than six feettall. See the black line about six feet above his head?That's where the snow from the winter of 1998/99stopped melting. Above that, is snow that nevermelted from the winter of 1999/2000. Why isn'tthe media reporting this sort of thing?..Click here to read this in Espanol: http://mitosyfraudes.8k.com/articulos-3/PorHielo.html
Thanks to Eduardo Ferreyra, who translated this material into Spanish for the Argentinean Foundation for a Scientific Ecology.)
Photo by Mazz Terrell19 July 2000
..See also Growing_Glaciers See also Greenland Icecap Growing Thicker and Antarctic Icecap Growing Thicker






Thursday, January 3, 2008

Jim Hansen Wins Award....

NASA's Jim Hansen is tempting fate by continually venturing out onto thinner, and thinner ice. The charade he has been putting on about man-caused global warming is falling apart around him. Read the following article by Cliff Ollier of The University of Western Australia about how glaciers really behave and you'll understand just how misleading Jim Hansen has been.
Peter

The Biggest Whopper of 2007
Julie Walsh, CEIJanuary 2, 2008
Among the candidates for the biggest cock-and-bull story in 2007 must be NASA’s James Hansen with his work of creative genius on Greenland’s and Antarctica’s ice sheets and his wannabes, who subsequently copied his imaginative tour de force.
Even the facts are no match for James Hansen and his incredible modeling machine! Though Greenland’s and Antarctica’s ice rests in deep bowls, Hansen declares them inclined planes. Then despite ice cores that show little to no movement for the past 400,000 years (including the warm periods), he shamelessly states that these gigantic ice sheets are slip, slidin’ away and the world will be flooded.
The idea of “meltwater lakes on the surface finding their way down through cracks in the ice and lubricating the bottom of the glacier is not compatible with accumulation of undisturbed snow layers. It might conceivably work on valley glaciers but it tells us nothing of the ‘collapse’ of ice sheets,” according to Cliff Ollier, School of Earth and Geographical Science at the University of Western Australia, “Indeed ‘collapse’ is impossible.”
Alarmists have to be thrilled with the successfulness of Hansen’s 2007 con—without this lie there is no catastrophic flooding, and all they are left with is the IPCC’s non-eventful one-foot-in-a-century sea level rise.
I wonder if Hansen’s modeler can also make Everlasting Gobstoppers!

Tuesday, September 11, 2007

Visual Depiction Of Global Warming From Last Ice Age

This map shows the approximate distribution of glacial ice covering North America, beginning approximately 18 thousand years ago.



Go to the following link to see an animated depiction of the ice melting and the glaciers shrinking.

http://www.museum.state.il.us/exhibits/ice_ages/

Tuesday, August 7, 2007

Louis Agassiz, Great American Geologist........

Just something to ponder and remember.......some quotes from Louis Agassiz, the first to recognize glaciers, glaciation, and climate change.
Peter

Louis Agassiz
From Wikiquote
Jean Louis Rodolphe Agassiz (May 28, 1807-December 14, 1873) was a Swiss-born American zoologist, glaciologist, and geologist, the husband of educator Elizabeth Cabot Cary Agassiz, and one of the first world-class American scientists.

The time has come when scientific truth must cease to be the property of the few, when it must be woven into the common life of the world.
Methods of Study in Natural History (1863), ch. 4

The eye of the trilobite tells us that the sun shone on the old beach where he lived; for there is nothing in nature without a purpose, and when so complicated an organ was made to receive light, there must have been light to enter it.
Geological Sketches (1870), ch. 2

The facts will eventually test all our theories, and they form, after all, the only impartial jury to which we can appeal.
Geological Sketches (1870), ch. 9

Sunday, June 17, 2007

Sacred River, (The Ganges) Endangered By Global Warming

I must publish this and save it for comment later. The effects of global warming are indeed profound. We must take all things into consideration. Two huge countries we must consider are China, and as illustrated in this article, India.
Peter

Sacred river endangered by global warming
Ganges' glacial source is receding
washingtonpost.com);
VARANASI, India - With her eyes sealed, Ramedi cupped the murky water of the Ganges River in her hands, lifted them toward the sun, and prayed for her husband, her 15 grandchildren and her bad hip. She, like the rest of India's 800 million Hindus, has absolute faith that the river she calls Ganga Ma can heal.

Around Ramedi, who like some Indians has only one name, people converged on the riverbank in the early morning, before the day's heat set in. Women floated necklaces of marigolds on a boat of leaves, a dozen skinny boys soaped their hair as they bathed in their underwear, and a somber group of men carried a body to the banks of the river, a common ritual before the dead are cremated on wooden funeral pyres. To be cremated beside the Ganges, most here believe, brings salvation from the cycle of rebirth.

"Ganga Ma is everything to Hindus. It's our chance to attain nirvana," Ramedi said, emerging from the river, her peach-colored sari dripping along the shoreline.
But the prayer rituals carried out on the water's edge may not last forever -- or even another generation, according to scientists and meteorologists. The Himalayan source of Hinduism's holiest river, they say, is drying up.

In this 3,000-year-old city known as the Jerusalem of India for its intense religious devotion, climate change could throw into turmoil something many devout Hindus thought was immutable: their most intimate religious traditions. The Gangotri glacier, which provides up to 70 percent of the water of the Ganges during the dry summer months, is shrinking at a rate of 40 yards a year, nearly twice as fast as two decades ago, scientists say.

'Hurt our very religion'"This may be the first place on Earth where global warming could hurt our very religion. We are becoming an endangered species of Hindus," said Veer Bhadra Mishra, an engineer and director of the Varanasi-based Sankat Mochan Foundation, an organization that advocates for the preservation of the Ganges. "The melting glaciers are a terrible thing. We have to ask ourselves, who are the custodians of our culture if we can't even help our beloved Ganga?"

Environmental groups such as Mishra's have long focused on pollution of the Ganges. More than 100 cities and countless villages are situated along the 1,568-mile river, which stretches from the foothills of the Himalayas to the Bay of Bengal, and few of them have sewage treatment plants.

But recent reports by scientists say the Ganges is under an even greater threat from global warming. According to a U.N. climate report, the Himalayan glaciers that are the sources of the Ganges could disappear by 2030 as temperatures rise.

Asia's water supply threatenedThe shrinking glaciers also threaten Asia's supply of fresh water. The World Wildlife Fund in March listed the Ganges among the world's 10 most endangered rivers. In India, the river provides water for drinking and farming for more than 500 million people.

The immediate effect of glacier recession is a short-lived surplus of water. But eventually the supply runs out, and experts predict that the Ganges eventually will become a seasonal river, largely dependent on monsoon rains.

"There has never been a greater threat for the Ganges," said Mahesh Mehta, an environmental lawyer who has been filing lawsuits against corporations dumping toxins in the Ganges. He is now redirecting his energies toward the melting glaciers. "If humans don't change their interference, our very religion, our livelihoods are under threat."

Mehta and other environmentalists want to see the Indian government here enforce strict reductions of greenhouse gas emissions, the primary cause of climate change.
But during this month's Group of Eight conference of the major industrialized nations, both India and China, eager to protect their market growth, joined the United States in refusing to support mandatory limits on greenhouse gas emissions. President Bush has instead pushed a plan for nonbinding goals to reduce emissions.

"It is a fact that more and not less development is the best way for developing countries to address themselves to the issues of preserving the environment," Indian Prime Minister Manmohan Singh said in a public statement before leaving for the G-8 summit in Germany.
A top emitter of greenhouse gases While India is one of the world's top producers of greenhouse gas emissions -- along with the United States, China, Russia and Japan -- it argues that the United States and other developed countries should reduce their own emissions before expecting developing nations to follow suit.

Environmentalists say that kind of thinking is shortsighted and that India desperately needs strong laws in place at a time when the country is growing so quickly.
"Economic growth is important, but can you imagine a billion cars in India?" Mehta asked. "As people become affluent, they want cars and air conditioners and refrigerators. What effect is that going to have on the environment?"

About 1 million pilgrims a year visit this ancient, hardscrabble city, many traveling hundreds of miles on foot. Many of them leave with vials of Ganges water to wear around their necks or display in their homes, sometimes sprinkling droplets of water into their town's wells, spiritually purifying their drinking water.

On the stone steps leading up to the Ganges' famous temple ghats, graffiti reads: "Happy is the person who lives by Ganga, Ma" and "I love my India."
"The government should realize that climate change will hurt not just communities, but also businesses and even the Ganga itself, our most sacred river," said Srinivas Krishnaswamy, a climate and energy expert for Greenpeace in India.
"When the Ganga River is threatened, Indians will have to wake up the government to this crisis."

Monday, April 30, 2007

North Atlantic Sediments....yet more

Here is yet another article demonstrating global warming and cooling going on long before man's usage of coal and oil.
Peter


Science 17 February 1995:Vol. 267. no. 5200, pp. 1005 - 1010DOI: 10.1126/science.267.5200.1005
Prev Table of Contents Next
Articles
Iceberg Discharges into the North Atlantic on Millennial Time Scales During the Last Glaciation Gerard C. Bond 1 and Rusty Lotti 1
1 Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.
High-resolution studies of North Atlantic deep sea cores demonstrate that prominent increases in iceberg calving recurred at intervals of 2000 to 3000 years, much more frequently than the 7000-to 10,000-year pacing of massive ice discharges associated with Heinrich events. The calving cycles correlate with warm-cold oscillations, called Dansgaard-Oeschger events, in Greenland ice cores. Each cycle records synchronous discharges of ice from different sources, and the cycles are decoupled from sea-surface temperatures. These findings point to a mechanism operating within the atmosphere that caused rapid oscillations in air temperatures above Greenland and in calving from more than one ice sheet.
Submitted on October 17, 1994Accepted on December 28, 1994

THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Signatures of rapid climatic changes in organic matter records in the western Mediterranean Sea during the last glacial period.
F. Baudin, N. Combourieu-Nebout, and R. Zahn (2007)Bulletin de la Societe Geologique de France 178, 3-13 Abstract » Full Text » PDF »
Near-synchronous interhemispheric termination of the last glacial maximum in mid-latitudes..
J. M. Schaefer, G. H. Denton, D. J. A. Barrell, S. Ivy-Ochs, P. W. Kubik, B. G. Andersen, F. M. Phillips, T. V. Lowell, and C. Schluchter (2006)Science 312, 1510-1513 Abstract » Full Text » PDF »
Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters.
A. Husinec and J. F. Read (2006)GSA Bulletin 118, 550-556 Abstract » Full Text » PDF »
The last deglaciation of the southeastern sector of the Scandinavian ice sheet..
V. R. Rinterknecht, P. U. Clark, G. M. Raisbeck, F. Yiou, A. Bitinas, E. J. Brook, L. Marks, V. Zelcs, J.-P. Lunkka, I. E. Pavlovskaya, J. A. Piotrowski, and A. Raukas (2006)Science 311, 1449-1452 Abstract » Full Text » PDF »
Glacial-Marine or Subglacial Origin of Diamicton Units from the Southwest and North Iceland Shelf: Implications for the Glacial History of Iceland.
S. M. Principato, A. E. Jennings, G. B. Kristjansdottir, and J. T. Andrews (2005)Journal of Sedimentary Research 75, 968-983 Abstract » Full Text » PDF »
Morphometry of Coccolithus pelagicus s.l. (Coccolithophore, Haptophyta) from offshore Portugal, during the last 200 kyr..
A. Parente, M. Cachao, K.-H. Baumann, L. de Abreu, and J. Ferreira (2004)Micropaleontology 50, 107-120 Abstract » Full Text » PDF »
Fine-grained sediment lofting from meltwater-generated turbidity currents during Heinrich events.
(2004)Geology 32, 449-452
Bipolar correlation of volcanism with millennial climate change.
R. C. Bay, N. Bramall, and P. B. Price (2004)PNAS 101, 6341-6345 Abstract » Full Text » PDF »
Does the Trigger for Abrupt Climate Change Reside in the Ocean or in the Atmosphere?.
W. S. Broecker (2003)Science 300, 1519-1522 Abstract » Full Text » PDF »
Catastrophic arid episodes in the Eastern Mediterranean linked with the North Atlantic Heinrich events.
(2003)Geology 31, 439-442
Interplay between tectonics and glacio-eustasy: Pleistocene succession of the Crotone basin, Calabria (southern Italy).
(2002)GSA Bulletin 114, 1183-1209
Enhanced aridity and atmospheric high-pressure stability over the western Mediterranean during the North Atlantic cold events of the past 50 k.y..
(2002)Geology 30, 863-866
Ocean circulation and iceberg discharge in the glacial North Atlantic: Inferences from unmixing of sediment size distributions.
(2002)Geology 30, 555-558
Widespread evidence of 1500 yr climate variability in North America during the past 14 000 yr.
(2002)Geology 30, 455-458
Calving glaciers.
C. J. van der Veen (2002)Progress in Physical Geography 26, 96-122 Abstract » PDF »
Late Pleistocene glacially-influenced deep-marine sedimentation off NW Britain: implications for the rock record.
S. Davison and M. S. Stoker (2002)Geological Society, London, Special Publications 203, 129-147 Abstract » PDF »
Grain-size characteristics and provenance of ice-proximal glacial marine sediments.
J. T. Andrews and S. M. Principato (2002)Geological Society, London, Special Publications 203, 305-324 Abstract » PDF »
Millennial and sub-millennial-scale variability in sediment colour from the Barra Fan, NW Scotland: implications for British ice sheet dynamics.
L. J. Wilson and W. E. N. Austin (2002)Geological Society, London, Special Publications 203, 349-365 Abstract » PDF »
Glacier-influenced sedimentation on high-latitude continental margins: introduction and overview.
J. A. Dowdeswell and C. O Cofaigh (2002)Geological Society, London, Special Publications 203, 1-9 Abstract » PDF »
Diatom-based conductivity reconstruction and palaeoclimatic interpretation of a 40-ka record from Lake Zeribar, Iran.
J. A. Snyder, J. A. Snyder, K. Wasylik, S. C. Fritz, and H. E. Wright Jr (2001)The Holocene 11, 737-745 Abstract » PDF »
Timing of Millennial-Scale Climate Change in Antarctica and Greenland During the Last Glacial Period.
T. Blunier and E. J. Brook (2001)Science 291, 109-112 Abstract » Full Text »
Modulation and amplification of climatic changes in the Northern Hemisphere by the Indian summer monsoon during the past 80 k.y.
(2001)Geology 29, 63-66
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic.
E. Bard, F. Rostek, J.-L. Turon, and S. Gendreau (2000)Science 289, 1321-1324 Abstract » Full Text »
Millennial-Scale Instability of the Antarctic Ice Sheet During the Last Glaciation.
S. L. Kanfoush, D. A. Hodell, C. D. Charles, T. P. Guilderson, P. G. Mortyn, and U. S. Ninnemann (2000)Science 288, 1815-1819 Abstract » Full Text » PDF »
Century- to millennial-scale sedimentological-geochemical records of glacial-Holocene sediment variations from the Barra Fan (NE Atlantic).
D. Kroon, D. KROON, G. SHIMMIELD, W. E. N. AUSTIN, S. DERRICK, P. KNUTZ, and T. SHIMMIELD (2000)Journal of the Geological Society 157, 643-653 Abstract » Full Text » PDF »
Were the North Atlantic Heinrich events triggered by the behavior of the European ice sheets?.
(2000)Geology 28, 123-126
Seismic stratigraphy of the Gulf of Cadiz continental shelf: a model for Late Quaternary very high-resolution sequence stratigraphy and response to sea-level fall.
F. J. Hernandez-Molina, L. Somoza, and F. Lobo (2000)Geological Society, London, Special Publications 172, 329-362 Abstract » PDF »
Abrupt Climate Change at the End of the Last Glacial Period Inferred from Trapped Air in Polar Ice.
J. P. Severinghaus and E. J. Brook (1999)Science 286, 930-934 Abstract » Full Text »
Late-Holocene climate in central West Greenland: meteorological data and rock-glacier isotope evidence.
O. Humlum and O. Humlum (1999)The Holocene 9, 581-594 Abstract » PDF »
A Mid-European Decadal Isotope-Climate Record from 15,500 to 5000 Years B.P..
U. v. Grafenstein, H. Erlenkeuser, A. Brauer, J. Jouzel, and S. J. Johnsen (1999)Science 284, 1654-1657 Abstract » Full Text »
Sudden climate transitions during the Quaternary.
J. Adams, M. Maslin, and E. Thomas (1999)Progress in Physical Geography 23, 1-36 Abstract » PDF »
Ice-flow stages and glacial bedforms in north central Ireland: a record of rapid environmental change during the last glacial termination.
A. M. McCABE, J. KNIGHT, and S. G. McCARRON (1999)Journal of the Geological Society 156, 63-72 Abstract » PDF »
Early-Holocene aridity in tropical northern Australia.
J. Nott, E. Bryant, and D. Price (1999)The Holocene 9, 231-236 Abstract » PDF »
Abrupt Climate Events 500,000 to 340,000 Years Ago: Evidence from Subpolar North Atlantic Sediments.
D. W. Oppo, J. F. McManus, and J. L. Cullen (1998)Science 279, 1335-1338 Abstract » Full Text »
Cyclic sedimentation on the Faeroe Drift 53-10 ka BP related to climatic variations.
T. L. Rasmussen, E. Thomsen, and T. C. E. Van Weering (1998)Geological Society, London, Special Publications 129, 255-267 Abstract » PDF »
Natural gas hydrates: searching for the long-term climatic and slope-stability records.
B. U. Haq (1998)Geological Society, London, Special Publications 137, 303-318 Abstract » PDF »
Thermohaline Circulation, the Achilles Heel of Our Climate System: Will Man-Made CO2 Upset the Current Balance?.
W. S. Broecker (1997)Science 278, 1582-1588 Abstract » Full Text »
A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates.
G. Bond, W. Showers, M. Cheseby, R. Lotti, P. Almasi, P. deMenocal, P. Priore, H. Cullen, I. Hajdas, and G. Bonani (1997)Science 278, 1257-1266 Abstract » Full Text »
Dating and rhythmicity from the last deglacial cycle in the British Isles.
A. M. McCABE (1996)Journal of the Geological Society 153, 499-502 Abstract » PDF »
Response: Testing for Bias in the Climate Record.
D. J. Thomson (1996)Science 271, 1881-1883 PDF »
Abrupt changes in marine conditions, Sunneshine Fiord, eastern Baffin Island, NWT during the last deglacial transition: Younger Dryas and H-0 events.
J. T. Andrews, L. E. Osterman, A. E. Jennings, J. P. M. Syvitski, G. H. Miller, and N. Weiner (1996)Geological Society, London, Special Publications 111, 11-27 Abstract » PDF »
Shelf erosion and glacial ice proximity in the Labrador Sea during and after Heinrich events (H-3 or 4 to H-0) as shown by foraminifera.
A. E. Jennings, K. A. Tedesco, J. T. Andrews, and M. E. Kirby (1996)Geological Society, London, Special Publications 111, 29-49 Abstract » PDF »
Deglaciation of the inner Scotian Shelf, Nova Scotia: correlation of terrestrial and marine glacial events.
R. R. Stea, R. Boyd, O. Costello, G. B. J. Fader, and D. B. Scott (1996)Geological Society, London, Special Publications 111, 77-101 Abstract » PDF »
Rock (mineral)-magnetic properties of post-glacial (16-0.5 ka) sediments from the Emerald Basin (Scotian Shelf), Canada.
F. R. Hall and S. J. Reed (1996)Geological Society, London, Special Publications 111, 103-115 Abstract » PDF »
Late Quaternary glacial history and short-term ice-rafted debris fluctuations along the East Greenland continental margin.
R. Stein, S.-i. Nam, H. Grobe, and H. Hubberten (1996)Geological Society, London, Special Publications 111, 135-151 Abstract » PDF »
Late glacial air temperature, oceanographic and ice sheet interactions in the southern Barents Sea region.
T. O. Vorren and J. S. Laberg (1996)Geological Society, London, Special Publications 111, 303-321 Abstract » PDF »
Interhemispheric Correlation of Late Pleistocene Glacial Events.
T. V. Lowell, T. V. Lowell, C. J. Heusser, B. G. Andersen, P. I. Moreno, A. Hauser, L. E. Heusser, C. Schluchter, D. R. Marchant, and G. H. Denton (1995)Science 269, 1541-1549 Abstract » PDF »
The Seasons, Global Temperature, and Precession.
D. J. Thomson (1995)Science 268, 59-68 Abstract » PDF »
Instability of Glacial Climate in a Model of the Ocean- Atmosphere-Cryosphere System.
A. Schmittner, M. Yoshimori, and A. J. Weaver (2002)Science 295, 1489-1493 Abstract » Full Text » PDF »

North Atlantic Sediments.....con't.

I found this almost immediately......hmmmmm.......where the heck is the carbon dioxide causing the warming coming from? Or could it be CO2 plays little if any role?
Peter


Nature 365, 143 - 147 (09 September 1993); doi:10.1038/365143a0
Correlations between climate records from North Atlantic sediments and Greenland ice
Gerard Bond*, Wallace Broecker*, Sigfus Johnsen†‡, Jerry McManus*, Laurent Labeyrie§, Jean Jouzel¶ & Georges Bonani
*Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA†The Niehls Bohr Institute, Department of Geophysics, University of Copenhagen, Haraldsgade 6, DK-2200, Copenhagen N, Denmark‡Science Institute, Department of Geophysics, University of Iceland, Dunghaga 3, IS-107 Reykjavik, Iceland§CFR Laboratoire mixte CNRS-CEA, Domaine du CNRS, 91198, Gif-sur-Yvette, Cedex, France¶Laboratorie de Modération du Climat et de I'Environnement, CEA/DSM, CE Saclay 91191, FranceLaboratorie de Glaciologie et Géophysique de 1'Environnement, CNRS, BP96, 38402 St. Martin d'Hères Cedex, France£Institute fur Mittelenergiephysik, ETH Honggerberg, CH-8093 Zurich, Switzerland
OXYGEN isotope measurements in Greenland ice demonstrate that a series of rapid warm-cold oscillations—called Dansgaard–Oeschger events—punctuated the last glaciation1. Here we present records of sea surface temperature from North Atlantic sediments spanning the past 90 kyr which contain a series of rapid temperature oscillations closely matching those in the ice-core record, confirming predictions that the ocean must bear the imprint of the Dansgaard–Oeschger events2,3. Moreover, we show that between 20 and 80 kyr ago, the shifts in ocean-atmosphere temperature are bundled into cooling cycles, lasting on average 10 to 15 kyr, with asymmetrical saw-tooth shapes. Each cycle culminated in an enormous discharge of icebergs into the North Atlantic (a 'Hein-rich event'4,5), followed by an abrupt shift to a warmer climate. These cycles document a previously unrecognized link between ice sheet behaviour and ocean–atmosphere temperature changes. An important question that remains to be resolved is whether the cycles are driven by external factors, such as orbital forcing, or by inter-nal ice-sheet dynamics.

References
1.
Dansgaard, W. et al. Nature 364, 218−220 (1993). Article ISI
2.
Broecker, W. S. et al. Quat. Res. 30, 1−6 (1988). Article
3.
Broecker, W. S., Bond, G. & Klas, M. Paleoceanogr. 5(4), 469−477 (1990).
4.
Bond, G. et al. Nature 360, 245−249 (1992). Article ISI
5.
Broecker, W. S., Bond, G., Klas, M., Clark, E. & McManus, J. Clim. Dynamics 6, 265−273 (1992).
6.
Bé, A. W. H. & Tolderlund, D. S. Micropaleontology of Oceans (eds Funnell, B. M. & Riedel, W. R.) 105−149 (Cambridge Univ. Press, 1971).
7.
Kellogg, T. B. Boreas 9, 115−137 (1980). ISI
8.
Broecker, W. S. Paleoceanogr. 3(1), 1−19 (1988).
9.
Lehman, S. J. & Keigwin, L. D. Nature 356, 757−762 (1992). Article ISI
10.
Karpuz, N. C. & Jansen, E. Paleoceanogr. 7(4), 499−520 (1992).
11.
Bond, G., Broecker, W., Lotti, R. & McManus, J. in Start of a Glacial (eds Kukla, G. J. & Went, E.) 185−205 (Springer, Berlin, 1992).
12.
Johnsen, S. J. et al. Nature 359, 311−313 (1992). Article ISI
13.
Alley, R. B. et al. Nature 362, 527−529 (1993). Article ISI
14.
Bard, E., Arnold, M., Fairbanks, R. G. & Hamelin, B. Radiocarbon 3(1), 191−199 (1993).
15.
Martinson, D. G. et al. Quat. Res. 27, 1−29 (1987). Article ISI ChemPort
16.
Dansgaard, W., White, J. W. C. & Johnsen, S. J. Nature 339, 532−533 (1989). Article ISI
17.
Taylor, K. C. et al. Nature 361, 432−436 (1993). Article ISI
18.
Heinrich, H. Quat. Res. 29, 142−152 (1988). Article ISI
19.
Ruddiman, W. F. & McIntyre, A. Paleogeogr. Palaeoclimatol. Palaeoecol. 35, 145−214 (1981). ChemPort
20.
Duplessy, J-C. Labeyrie, L., Juillet-LeClerc, A. & Duprat, J. in The Last Deglaciation: Absolute and Radiocarbon Chronologies (eds Bard, E. & Broecker, W. S.) 201−208 (Springer, Berlin, 1992).
21.
Andrews, J. T., Tedesco, K., Briggs, W. M. & Evans, L. W. Can. J. Earth Sci. (in the press).
22.
MacAyeal, D. R. Nature 359, 29−32 (1992). Article ISI
23.
Ruddiman, W. F. in Northern America and Adjacent Oceans during the Last Deglaciation: The Geology of North America (eds Ruddiman, W. F. & Wright, H. E. Jr) 137−154 (Geol. Soc. of Am, Boulder, 1987).
24.
Sancetta, C., Imbrie, J. & Kipp, N. G. Quat. Res. 3, 110−116 (1973). Article
25.
Woillard, G. & Mook, W. G. Science 215, 159−161 (1982). ISI ChemPort
26.
Shakleton, N. J., Imbrie, J. & Hall, M. A. Earth planet. Sci. Lett. 65, 233−244 (1983). Article ISI ChemPort
27.
Bloom, A. L., Broecker, W. S., Chappell, J. M. A., Matthews, R. K. & Mesolella, K. J. Quat. Res. 4, 185−205 (1974). Article ISI ChemPort