NASA video tour of the Cryosphere 2009

WUWT commenter Ray tips us to a new video from NASA “The Tour of the Cryosphere 2009”. With all the interest in sea ice right now, it seems like a good item to review.

LIMA image of Antarctica
The new version of "A Tour of the Cryosphere" features the world’s highest-resolution map of the icy continent, from the NASA-USGS Landsat Image Mosaic of Antarctica (LIMA) project. Credit: NASA/USGS - click for a larger image

I found one thing about it really interesting though, the zoom in of the Larsen B ice shelf saying: “After twelve thousand years, the Larsen B ice shelf collapsed in just five weeks.”. While they didn’t say directly that it was attributable to “global warming”, many others have said so. Watch how that melt pool continues through the animation of sea ice growth as refreeze occurs. That’s a hint. There’s quite a number of volcanic peaks in the area, as listed here. Here’s a ground pix from the scene. and some BAS research that found some unexpected things. More on that another time.

From NASA News

Back in 2002, NASA created a film using satellite data that took viewers on a tour of Earth’s frozen regions. This year, NASA visualizers are taking viewers on a return trip to see how things have changed over the years.

“The Tour of the Cryosphere 2009” combines satellite imagery and state-of-the-art computer animation software to create a fact-filled and visually stunning tour that shows viewers the icy reaches of Antarctica, the glacier-pocked regions along the Andes Mountains, the winter snows of the American West, the drifting expanse of polar sea ice, and the shrinking Jakobshavn glacier in Greenland.

However, viewers who saw the original will notice differences in the new version, also created by the Scientific Visualization Studio (SVS) at NASA’s Goddard Space Flight Center, Greenbelt, Md. The new “Tour of the Cryosphere” video can be seen and downloaded from the Scientific Visualization Studio’s Web site.

“What we did was incorporate more recent data and kept all scenes from the original that were dramatic and interesting,” said film director and editor Horace Mitchell, who began updating the animation seven months ago, with help from visualizers Alex Kekesi and Cindy Starr. “The biggest change is that the entire film is in high definition.”

Another significant difference is evident as soon as the 5-minute animation opens. At the request of Earth scientists, who thought the film could be improved by a more realistic rendering of Antarctica, the team replaced the original imagery provided by Canada’s RADARSAT with the Landsat Image Mosaic of Antarctica (LIMA). Created from more than 1,000 high-resolution Landsat 7 scenes, the LIMA dataset seamlessly shows the entire continent in unprecedented and realistic detail.

Watch the YouTube Video:

HiDef › View video (30 Mb mov)

As the updated film takes viewers northward from Antarctica, the film treats viewers to the precise locations of glaciers scattered along the Andes Mountains in South America. The locations literally pop as the film continues its grand tour toward the planet’s northern climes.

After a quick tour of snowfall in the American West and its impact on vegetation in 2002 and 2003, the film moves across Canada and Alaska to show more recent satellite data of annual snow and ice overlaying these regions. From there, viewers travel to Earth’s North Pole where they see the monthly average concentration of Arctic sea ice in 2009.

To help drive home the point that minimum sea ice levels have declined dramatically since 1979, the SVS team inserted a chart that tracks the levels of minimum ice cover, which typically occurs in September.

The animation then moves from Arctic sea ice to Greenland. More recent data now are used to show changes in the Jakobshavn glacier, which receded only slightly from 1942 to 2001. Beginning in 2002, the rate of ice loss jumped dramatically. The film shows the continued rates of recession over the past four years.

The animation shows the world in a single “shot” — uninterrupted by cuts or scene changes, a technique that conveys the interconnectedness of the cryosphere and the reason scientists gather satellite data to monitor changes in the first place.

The film gives anyone who watches it a wealth of data collected from satellite observations, showing in detail the impact that recent changes are making on the planet, he said.

“We’re trying to tell NASA’s story with Hollywood’s tools,” Mitchell said.

==================================

Here is the transcript from NASA:

“A Tour of the Cryosphere 2009” Transcript

Though cold and often remote, the icy reaches of the Arctic, Antarctic, and other frozen

places affect the lives of everyone on Earth.

We start our tour in Antarctica. Where they meet the sea, mountains of ice crack and

crumble. The resulting icebergs can float for years. Ice shelves surround half the

continent. They slow the relentless march of ice streams and glaciers like dams hold

back rivers. But the region is changing. As temperatures increase, we see a growing

number of melt ponds. As this heavy melt water forces its way into cracks, ice shelves

weaken and can ultimately collapse. After twelve thousand years, the Larsen B ice

shelf collapsed in just five weeks.

Offshore, sea ice forms when the surface of the ocean freezes, pushing salt out of the

ice. The cold salty surface water starts to sink, pumping deeper water out of the way,

powering global ocean circulation. These currents influence climate worldwide.

Most ice exists in the cold polar regions, but we see glaciers like these in the Andes all

over the world. Most are shrinking.

Here in North America, millions of people experience the cryosphere every year.

Eastward moving storms deposit snow like thick paint brushes. Mountain snow packs

store water. Snow melt provides three-quarters of the water resources used in the

American west. Substantial winter snows produced a green Colorado in 2003, but

dryer conditions the previous year limited vegetation growth and increased the risk of

fires.

In the Rocky Mountains, there are patches of frozen ground called permafrost that

never thaw. These regions are unusual in the mid-latitudes. But farther north,

permafrost is more widespread and continuous, covering nearly a fifth of the land

surface in the Northern Hemisphere.

Sea ice varies from season to season and from year to year. Data show that Arctic sea

ice has shrunk dramatically in the last few decades. The effects could be profound.

As polar ice decreases, more open water could promote greater heating. More heating

could lead to faster melting, reinforcing the cycle. If this trend continues, the Arctic

Ocean could be ice-free in the summer by the end of the century.

These changes in ice cover are not limited to oceans. Greenland’s ice sheet contains

nearly ten percent of the Earth’s glacial ice. Glaciers in western Greenland produce

most of the icebergs in the North Atlantic. After decades of stability, Greenland’s

Jakobshavn ice stream, one of the fastest flowing glaciers in the world, has changed

dramatically. The ice has thinned, and the front retreated significantly. Between 1997

and 2003, the glacier’s flow rate nearly doubled to five feet an hour.

These are just some of the cryospheric processes that NASA satellites observe from

space. Continued observation provides a critical global perspective, as our home

planet continues to change – day to day, year to year, and further into the future.

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David Gladstone
September 9, 2009 1:33 pm

That’s a great site, Smokey and a very useful post! The video is stunning and by turning the sound off, one lowers the seething anger level caused by listening to propaganda.

Kevin Kilty
September 9, 2009 7:11 pm

That is a great graphic, and luckily I had no headphones so I didn’t have to listen to anything. By the way, the graph of Arctic ice extent, which goes dismayingly downhill, starts in 1979 just after the mid 1960s to mid 1970s growth of “permanent ice and snow in North America” to paraphrase NAS in 1975. It is too bad there isn’t equivalent data from long before.

OceanTwo
September 10, 2009 9:15 am

When I first heard about the Larsen-B shelf, the impression left was that half of Antarctica has just melted (!).
So, as a curious sort, I decided to dig a little deeper into the reports and pictures. And, as already mentioned, finding this shelf on a map is, well, a needle-haystack kind of thing. As already stated, the images indicated a breaking off, and not necessarily melting.
One point I found curious, though, is the mention of the mid-latitudes permafrost being ‘unusual’. I was expecting the commentary to indicate that it’s shrinking. In addition, it indicated 2003 was normal but 2002 was a much drier year; reversing the chronological order of occurrence is pretty disingenuous.

OceanTwo
September 10, 2009 9:34 am

And another point:
“After twelve thousand years, the Larsen B ice shelf collapsed in just five weeks.”
Such statements are pure propaganda and doublespeak. Implying that some outside influence caused something to happen can be acceptable, but in the current context it is disingenuous.
There are numerous natural and geological events ‘which just happen’ after decades, centuries or milennia of stability, particularly when someone is not sitting right on top of it monitoring it. Additionally, these events are not tied to a single unifying cause.
Man has always liked to think that he is in control of his surroundings; and if he isn’t, strives for this. But a lot of the time, S*** Happens. Sometimes you can go something about them, sometimes you can’t. Volcanoes, Hurricanes, Earthquakes, Tsunamis. It would be ‘nice’ to attribute through some convoluted chain these effects to something under our control, because it means we’d be (potentially) able to do something about them. Sadly, that’s not the way the real world works. Being all touchy feely ‘world unite’ for a common good is great while you are trying to get laid, but science it ain’t.

John S.
September 10, 2009 3:55 pm

The unacknowleged limitation of satellite data is that it begins in the late 70s, when temperatures were starting to rebound from a deep multidecadal dip, and extends only a decade past the 1998 peak. That’s too short a record for drawing long-term conclusions, especially about lagging processes such as sea-ice extent and glacial variations. It’s irresponsible to create and maintain the impression that the available data constitutes an unmistakable secular trend.

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