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Originally posted by weedwhacker
reply to post by teklordz
I really wish this would get more attention.
Yes, I know....there are multiple threads on this subject....but before you tell the OP about other threads, we should consider WHY there are so many threads popping up?
HERE's an observation.....if those who are online NOW at ATS do not live near a Coastal Area....then, they just don't give a whit if MSL rises...(MSL=Mean Sea Level).
Regardless....average Ocean levels are going to be, in Human terms, fairly gradual. What I mean is, barring any huge Storms....any rise in average water levels is going to be gradual.
Problem is, it is so gradual....it tends to sneak up on the unsuspecting...
An Antarctic ice shelf has disappeared -scientists
www.reuters.com...
WASHINGTON, April 3 (Reuters) - One Antarctic ice shelf has quickly vanished, another is disappearing and glaciers are melting faster than anyone thought due to climate change, U.S. and British government researchers reported on Friday.
They said the Wordie Ice Shelf, which had been disintegrating since the 1960s, is gone and the northern part of the Larsen Ice Shelf no longer exists. More than 3,200 square miles (8,300 square km) have broken off from the Larsen shelf since 1986.
Climate change is to blame, according to the report from the U.S. Geological Survey and the British Antarctic Survey, available at pubs.usgs.gov/imap/2600/B.
"The rapid retreat of glaciers there demonstrates once again the profound effects our planet is already experiencing -- more rapidly than previously known -- as a consequence of climate change," U.S. Interior Secretary Ken Salazar said in a statement.
"This continued and often significant glacier retreat is a wakeup call that change is happening ... and we need to be prepared," USGS glaciologist Jane Ferrigno, who led the Antarctica study, said in a statement.
"Antarctica is of special interest because it holds an estimated 91 percent of the Earth's glacier volume, and change anywhere in the ice sheet poses significant hazards to society," she said.
In another report published in the journal Geophysical Letters, the National Oceanic and Atmospheric Administration reports that ice is melting much more rapidly than expected in the Arctic as well, based on new computer analysis and recent ice measurements.
The U.N. Climate Panel projects that world atmospheric temperature will rise by between 1.8 and 4.0 degrees Celsius because of emissions of greenhouse gases that could bring floods, droughts, heat waves and more powerful storms.
As glaciers and ice sheets melt, they can raise overall ocean levels and swamp low-lying areas.
Parkinson examined 21 years (1979-1999) of Antarctic sea ice satellite records and discovered that, on average, the area where southern sea ice seasons have lengthened by at least one day per year is roughly twice as large as the area where sea ice seasons have shortened by at least one day per year. One day per year equals three weeks over the 21-year period.
Originally posted by Long Lance
..
when it gets serious, the numbers plummet, take the following example:
www.sciencemag.org...
After a century of polar exploration, the past decade of satellite measurements has painted an altogether new picture of how Earth's ice sheets are changing. As global temperatures have risen, so have rates of snowfall, ice melting, and glacier flow. Although the balance between these opposing processes has varied considerably on a regional scale, data show that Antarctica and Greenland are each losing mass overall. Our best estimate of their combined imbalance is about 125 gigatons per year of ice, enough to raise sea level by 0.35 millimeters per year. This is only a modest contribution to the present rate of sea-level rise of 3.0 millimeters per year. However, much of the loss from Antarctica and Greenland is the result of the flow of ice to the ocean from ice streams and glaciers, which has accelerated over the past decade. In both continents, there are suspected triggers for the accelerated ice discharge—surface and ocean warming, respectively—and, over the course of the 21st century, these processes could rapidly counteract the snowfall gains predicted by present coupled climate models.
now, the total is supposed to be 3mm/a with 0.35mm being attributed to GW, taken from
www.abovetopsecret.com...
Net gain
Geologists have previously traced the landward retreat of the line where the base of the ice in West Antarctica meets the ocean. This has averaged 120 metres a year since the end of the last ice age. The studies had estimated the Ross Ice Streams region was losing 20.9 billion tons of ice per year.
But now Ian Joughin of the Jet Propulsion Laboratory and Slawek Tulaczyk of the University of California at Santa Cruz report a net gain of 26.8 billion tons per year. This represents about a quarter of the annual snow accumulation.
Nature Geoscience 1, 106 - 110 (2008)
Published online: 13 January 2008 | doi:10.1038/ngeo102
Recent Antarctic ice mass loss from radar interferometry and regional climate modelling
Eric Rignot1,2,3, Jonathan L. Bamber4, Michiel R. van den Broeke5, Curt Davis6, Yonghong Li6, Willem Jan van de Berg5 & Erik van Meijgaard7
Top of pageLarge uncertainties remain in the current and future contribution to sea level rise from Antarctica. Climate warming may increase snowfall in the continent's interior1, 2, 3, but enhance glacier discharge at the coast where warmer air and ocean temperatures erode the buttressing ice shelves4, 5, 6, 7, 8, 9, 10, 11. Here, we use satellite interferometric synthetic-aperture radar observations from 1992 to 2006 covering 85% of Antarctica's coastline to estimate the total mass flux into the ocean. We compare the mass fluxes from large drainage basin units with interior snow accumulation calculated from a regional atmospheric climate model for 1980 to 2004. In East Antarctica, small glacier losses in Wilkes Land and glacier gains at the mouths of the Filchner and Ross ice shelves combine to a near-zero loss of 461 Gt yr-1. In West Antarctica, widespread losses along the Bellingshausen and Amundsen seas increased the ice sheet loss by 59% in 10 years to reach 13260 Gt yr-1 in 2006. In the Peninsula, losses increased by 140% to reach 6046 Gt yr-1 in 2006. Losses are concentrated along narrow channels occupied by outlet glaciers and are caused by ongoing and past glacier acceleration. Changes in glacier flow therefore have a significant, if not dominant impact on ice sheet mass balance.
Public release date: 2-Mar-2006
University of Colorado at Boulder
Antarctic ice sheet losing mass, says University of Colorado study
University of Colorado at Boulder researchers have used data from a pair of NASA satellites orbiting Earth in tandem to determine that the Antarctic ice sheet, which harbors 90 percent of Earth's ice, has lost significant mass in recent years.
The team used measurements taken with the Gravity Recovery and Climate Experiment, or GRACE, to conclude the Antarctic ice sheet is losing up to 36 cubic miles of ice, or 152 cubic kilometers, annually. By comparison, the city of Los Angeles uses about 1 cubic mile of fresh water annually.
Changes in West Antarctic ice stream dynamics observed with ALOS PALSAR data
Changes in West Antarctic ice stream dynamics observed with ALOS PALSAR data
Eric Rignot
Earth System Science, University of California, Irvine, California, USA
Jet Propulsion Laboratory, Pasadena, California, USA
The Advanced Land Observation System (ALOS) Phased-Array Synthetic-Aperture Radar (PALSAR) is an L-band frequency (1.27 GHz) radar capable of continental-scale interferometric observations of ice sheet motion. Here, we show that PALSAR data yield excellent measurements of ice motion compared to C-band (5.6 GHz) radar data because of greater temporal coherence over snow and firn. We compare PALSAR velocities from year 2006 in Pine Island Bay, West Antarctica with those spanning years 1974 to 2007. Between 1996 and 2007, Pine Island Glacier sped up 42% and ungrounded over most of its ice plain. Smith Glacier accelerated 83% and ungrounded as well. Their largest speed up are recorded in 2007. Thwaites Glacier is not accelerating but widening with time and its eastern ice shelf doubled its speed. Total ice discharge from these glaciers increased 30% in 12 yr and the net mass loss increased 170% from 39 ± 15 Gt/yr to 105 ± 27 Gt/yr. Longer-term velocity changes suggest only a moderate loss in the 1970s. As the glaciers unground into the deeper, smoother beds inland, the mass loss from this region will grow considerably larger in years to come.
Received 21 January 2008; accepted 10 March 2008; published 28 June 2008.
Citation: Rignot, E. (2008), Changes in West Antarctic ice stream dynamics observed with ALOS PALSAR data, Geophys. Res. Lett., 35, L12505, doi:10.1029/2008GL033365.
Originally posted by Long Lance
reply to post by melatonin
it may not be recent and i wouldn't be all that surprised if a modern chart featured a 'hockey stick' style presentation which wholly omits the data presented in the article(s).
you're going to Hansenize the following graph, too?
icecap.us...
let's see pack ice season increasing 1day/1year, documented net gain reported in 2002 (where's that elusive contemporary data again??), temp curves going the 'wrong' way but not being reported anywhere...
i'm supposed to buy into all of this? not even at gunpoint.
Originally posted by TheRedneck
Can I make some predictions here?
- The Wilkins ice shelf will break off and float away from the Antarctic mainland.
- The ice shelf will then melt into liquid water as it leaves the colder antarctic regions.
- The sea will not rise perceptibly despite this.
- Someone will come up with a 'scientific explanation' as to why sea level did not rise enough to make Florida disappear.
...
And admit that Al Gore and Jim Hansen are total buffoons who belong in a freak show as the 'Men Without a Brain'.
Hmm, yeah, I would guess those total buffoons already know that the ice sheet floats on water and will make no direct contribution to sea level rises.
“This looks like a pretty good analysis, but I have to say I remain somewhat skeptical. It is hard to make data where none exist.
The sea ice is relevant, but the melting land mass of ice is most pertinent for obvious reasons. And as the ice shelves fall away, the land mass is next in line - and the research suggests that the land mass is melting and at increasing rates.
Originally posted by TwiTcHomatic
reply to post by melatonin
The future problem of the ice shelf breaking off is what is behind the concern.
The shelf itself acts as a plug for the ice that is on land behind it. When the shelf goes, the "land ice" will have free passage to the sea. That ice can raise the water levels.
Where the Arctic is mainly "ice already in the water", the majority of Antarctica is "land-locked ice".