Polar Push & Bounce Back -Trends at the Extremes NEW ZT

**NEW ZETATALK**

This blog is about the Arctic,Antarctica and Extreme Northern/Southern Hemispheres.  Are New Trends happening at the Poles? Weather Patterns, Charts, Images and Unusual Anomalies may be telling us something!

According to the Zetas,  the Wobble Effect has now combined with a new Polar Push!!  

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https://poleshift.ning.com/forum/topics/zetatalk-chat-for-november-...

Both poles the sea ice loss is off the charts this month!  Seems something has changed?
[and from another] Is it related to the warming of the oceans from the bottom and the wobble? Where will this lead?[and from another]
https://www.wunderground.com/blog/JeffMasters/crazy-cryosphere-reco...
Sea ice extent and area have both plummeted to record lows for this time of year in both the Arctic and Antarctic. Such dramatic losses rarely occur at the same time, which means that the global total of sea ice coverage is phenomenally low for this time of year. The weirdness extends to midlatitudes: North America as well as the Arctic have been bathed in unusual mildness over the last several weeks, while Eurasia deals with a vast zone of above-average snowfall and below-average temperatures. [and from another]
https://www.theguardian.com/environment/2016/nov/22/extraordinarily...



SOZT
It is clear from the charts that the Earth wobble has increased. First, despite Siberia being on the same latitude with Eastern Canada and Europe, there are vast temperature differences. The globe around the Arctic seems to be divided in half in this way at the current time. Just months ago, in July,
http://www.zetatalk.com/ning/23jy2016.htm
we stated that the hot and cold regions in the Northern Hemisphere were divided into four parts, due to the Polar Push and Bounce Back, and the lean to the Left and Right. Now the increased wobble has created a duality, not the quadrant arrangement of the Figure 8 that had been present since 2004.  

The Polar Push wherein the N Pole of Earth is shoved away from the approaching N Pole of Nibiru continues to create cold temperatures in Siberia, where the magnetic N Pole of Earth currently resides. This has also warmed Antarctica, which is getting more sunlight.  The Bounce Back is more fierce, so that Europe and eastern N America are also getting more sunlight, and thus the melting Arctic. What is missing is the temperature anomalies due to the tilt to the Left and Right. They have been lost in the more aggressive back and forth motion of the Polar Push and Bounce Back.  
EOZT

Prior ZT: http://www.zetatalk.com/ning/23jy2016.htm
The weather maps continue to document the daily Earth wobble, showing abnormal heat over the N American southwest and up into Alaska, and abnormal heat through Europe. Both these regions come under more equatorial sun due to the wobble, due to the lean to the left and then to the right. This is distinctly balanced by cold spots in between. Canada’s eastern provinces and the region above Hudson Bay receive less sunlight due this tilt to one side and then the other. Russia’s Far East and the Siberian region above China of course are pushed into the cold by the daily Polar Push, when the N Pole of Nibiru shoves the Earth magnetic N Pole away.

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The Polar Push Effect:

http://zetatalk.com/index/zeta103.htm

 

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Ecliptic Rise

http://www.zetatalk.com/index/earthtil.htm

Planet X approaches from the south, and the Pole Shift occurs because the S. Pole is pulled north with the N. Pole of Planet X during the passage. This stress is already evident in that many have noted that the Sun is too far south, rising too far to the south, for the time of year. Possible explanations for this are that the S. Pole has been pulled toward Planet X, creating a different tilt, but the constellations seem to be in their proper place. An alternate explanation is that the Earth's plane of the Ecliptic has changed, rising up, putting the Northern Hemisphere into a different slant, and placing the S. Pole more in line with the N. Pole of Planet X, an alignment Magnets Prefer.    

Natives to the Arctic,  the Inuit years ago already noticed many changes:

Uqalurait: the Snow is Speaking
November 23, 2009
http://www.isuma.tv/hi/en/inuit-knowledge-and-climate-change/uqalur...

An Igloolik elder, describes that uqalurait are changing because the earth itself has "tilted" and has thrown off the consistent wind patterns of the past. The earth tilting on its axis is another re-occuring observation that we are hearing from Inuit, which they know because of how the sun, moon and stars have changed in the sky. Indeed, elders simultaneously know the complexities of the cosmos, land, wind and sky.

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Both Poles are affected!

https://www.wunderground.com/blog/JeffMasters/crazy-cryosphere-reco...

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The Zetas describe the Final Days of the Wobble:

http://www.zetatalk.com/index/zeta582.htm

During the last weeks, the Earth changes from being in an end-to-end alignment with Planet X to being in a side-by-side alignment. It is during the end-to-end alignment, when Planet X is pointing its N Pole directly at the Earth, that the lean to the left and 3 days of darkness occur. But as Planet X continues in its retrograde orbit, its N Pole is no longer coming from the right, but is located to the left of the Earth, and the Earth adjusts by slinging its N Pole to the right. Thus, during the 6 days of sunrise west, the Earth still has its N Pole tipped away from the Sun and the approaching Planet X, but rather than a lean to the left, it has a lean to the right.
 
It is at this point that the Earth switches from being in an end-to-end alignment to being in a side-by-side alignment with Planet X. When Planet X is just at the Ecliptic, it stands upright in alignment with the Sun. As it switches from pointing its N Pole at Earth the Earth follows suit.
ZetaTalk: September 12, 2009

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Some charts to follow and/or post in this blog are HERE:

Climate ReAnalyzer

http://cci-reanalyzer.org

Google has the biggest collection of charts to view/post here!

https://sites.google.com/site/arcticseaicegraphs/

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NEW ZETATALK SEPT 30, 2017 **

http://zetatalk.com/ning/30sp2017.htm

With a stronger Polar Push the bounce back would likewise be more extreme, and the bounce back occurs when the Sun is over the Atlantic.  As the wobble continued to get worse, the Figure 8 corrective lean to the right and left also got more extreme. This sets the stage for the current 2017 hurricane season.

(Modified Earth images are from Google Earth)

Sunlight on Earth reflection based on image in the Planet X Related Captures Blog

The Figure 8 of the wobble creates a churning in the Atlantic:

1.) First land on either side of the Atlantic is pushed under water during the Polar Push,

2.) Then the N American Continent is slung to the East

3.) Then to the West as the day dawns and

4.) Then the bounce back pulls this land back up to the North. 

The wobble, in short, is churning the North Atlantic in a circular motion. Where this fits with the Coriolis effect, where the winds and water curl up from the Equator in a circular motion, moving clockwise in the Northern Hemisphere, the lean to the left does a direct clash, pushing the storm back in a path toward the US coastline.

This is the current Wobble pattern, but the Wobble is subject to change:

5.) A lean into Opposition has occurred, the N Pole leaning toward the Sun. **NEW LEAN**

6.) And a temporary Lean to the Left could occur,

7.) as well as a temporary Day of Darkness for the Northern Hemisphere.

This is not a static situation. (this will occur more than once, in other words).

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Comment by SongStar101 on November 30, 2016 at 10:39am

Antarctica Ice Shelf is Breaking from the Inside Out

https://www.scientificamerican.com/article/antarctica-ice-shelf-is-...

An ice sheet in West Antarctica is breaking from the inside out.

The significant new findings published yesterday in Geophysical Research Letters show that the ocean is melting the interior of the Pine Island Glacier, which is about the size of Texas. The crack seems to be accelerating, said Ian Howat, associate professor of earth sciences at Ohio State University and the study’s lead author. The findings are the first confirmation of something glaciologists have long suspected was happening, he said.

“It’s showing a new weakness in the ice shelf, and it’s showing the weakness may be extending far up the glacier,” he said. “That’s the alarming thing from our standpoint.”

Higher ocean temperatures are causing the ice to shrink at an accelerating rate, and it’s eroding the ice fringing the continent. That, in turn, opens the ice sheet to further contact with warmer ocean water and increases the amount of ice running into the ocean, the researchers found.

“More importantly, it gives us a mechanism for even faster retreat in the future. Before, we used to have a slow retreat at the edges of the ice shelf,” Howat said. "The ocean had to nibble away at it on the edges. This allows the ice shelf to break apart way further inland from the inside out."

This latest retreat is particularly noteworthy because it’s farther inland than anything scientists have previously observed, he said. It also shows that the region could be more vulnerable than previously thought.

If Antarctica were not covered in ice, it would be a series of islands. That means much of the ice in the region is already under constant pressure from the ocean, as its movements dislodge the ice that covers the area between the land masses. Cracking is more likely to occur in the valleys located on the ice sheet, where the ocean is in closer contact with the ice, researchers found.

The currents off Antarctica are warmer and carry saltier water that encourages melting. The sea temperature is about 5 degrees Celsius, which is far warmer than the average surface temperature of minus 20 C. That causes a twofold vulnerability for the ice, because some of it is located underwater and because it is exposed to the warm sea around it.

Similar rifts have already been observed in Greenland, as the Arctic warms and ocean water flows along the bedrock, causing the ice to melt. The Pine Island Glacier and a similar-sized neighboring glacier are unique because they block ice flows from reaching the sea. That’s enough to keep about 10 percent of the ice sheet from toppling into the warmer water.

‘Significant collapse’ possible

A separate study published last week in Nature suggests that the melting of the Pine Island Glacier started in the 1940s, likely as a result of El Niño activity. Scientists obtained sediment cores from beneath the glacier to show that a cavity started forming before the mid-1940s. Warmer seawater flowed into the space and caused the glacier to lift off the sea-floor ridge that held it in place.

The thinning of the glacier shows that it is responding to shifts in sea temperatures that occur elsewhere in the world, even in the Pacific, researchers found. Once the melting begins, it can continue for decades, they said.

Understanding what caused the changes to the Pine Island Glacier and how long they could continue is important, said David Vaughan, director of science at British Antarctic Survey and a co-author of the study published in Nature.

“Ice loss from this part of West Antarctica is already making a very significant contribution to global sea-level rise, and is actually one of the largest uncertainties in global sea-level predictions,” he said.

The melting in Antarctica has a direct result on coastal cities across the globe. Imagine Antarctica as a dam, holding back ice instead of water, Howat said. It holds about half of the world’s fresh water. The spillways at the top of the dam are now open, increasing in volume and draining the reservoir. That increase will be felt as the sea levels rise and cities are inundated by increased flooding.

Scientists used satellite imagery to observe how the rift, located 20 miles inland, formed in 2013. Within two years, the rift had broken through the ice and caused a 225-square-mile iceberg to break off the glacier in the summer of 2015.

Howat said the rift is further evidence that it’s not a matter of if, but when the larger West Antarctic Ice Sheet will melt. It adds “to the probability that we may see significant collapse of West Antarctica in our lifetimes,” he said.

 

Comment by SongStar101 on November 30, 2016 at 10:20am

Huge Cracks In the West Antarctic Ice Sheet May Signal Its Collapse

http://gizmodo.com/huge-cracks-in-the-west-antarctic-ice-sheet-may-...

Last year, a 225 square-mile chunk of West Antarctica’s Pine Island Glacier broke off and tumbled into the sea. Now, Earth scientists at Ohio State University have pinpointed the root cause of the iceberg calving event: a crack that started deep below ground and 20 miles inland.

It’s like nothing scientists have witnessed in West Antarctica before, and it doesn’t bode well for the ice sheet’s future.

A frozen fortress containing enough water to raise global sea levels many feet should it melt, the West Antarctic ice sheet is separated from the ocean by a series of large glaciers. For now, these glaciers act like corks in wine bottles to hold the ice at bay, but that may not be the case for much longer. Recent research has shown that Pine Island, Thwaites, and other glaciers along the Amundsen sea are retreating rapidly, as warm ocean waters lap against their margins. At this point, NASA says, collapse of the entire Amundsen sea sector appears to be “unstoppable.”

“This event gives us a new mechanism for ice sheets falling apart quickly. It fits into that picture of a rapid retreat.”

The biggest question on everyone’s mind is how quickly all of that ice will go, and to find out, we need to pinpoint the mechanisms responsible for ice sheet collapse. To that end, a study published today in Geophysical Research Letters takes a deep dive into an iceberg calving event in the summer of 2015. It arrives at a startling conclusion.

“The calving event itself wasn’t a big deal,” lead study author Ian Howat of Ohio State University told Gizmodo, noting that iceberg break-offs of this size happen about every 5 to 6 years at Pine Island. “What made this one different is how it got started.”

At Pine Island and elsewhere along the Amundsen sea embayment, calving occurs at the glacier’s outer margin, where the ice shelf is detached from bedrock. “It’s kinda like a diving board sticking out over a pool,” Howat said. Normally, cracks will start to form in areas experiencing extreme shear from ice flowing off the continent. They’ll propagate laterally across the shelf, eventually causing the entire diving board to break away.

Not so with last year’s Pine Island calving event. Analyzing several years of images taken by the Sentinel-1A satellite, Howat and his colleagues traced the break-off to a rift that formed at the base of the ice shelf nearly 20 miles inland, in 2013. Over the course of two years, the rift propagated all the way from bottom to top, until finally, it spat out an iceberg ten times the size of Manhattan.

What could have caused so much ice to break away in this unusual manner? In all likelihood, melting that started at the contact point between ice and bedrock is to blame. This would explain why the rift overlapped with a topographic valley—a place where the ice appeared to have thinned—in satellite images taken before the calving.

“I think what we’re seeing is the surface expression of a much bigger valley at the base of the ice shelf,” Howat said. “This tells us the ice shelf has weaknesses that are being exploited by increased ocean temperatures.”

Troublingly, as waters around West Antarctica heat up, those weaknesses could be exploited more and more often. “If the ice sheet was going to retreat very slowly on long timescales, we’d just expect to see the usual calving,” Howat said. “This event gives us a new mechanism for ice sheets falling apart quickly. It fits into that picture of a rapid retreat.”

Comment by SongStar101 on November 29, 2016 at 9:23am

Odd how the recent speed of melting ice appears a bit different than the Wobble.  From the last years the Wobble has been increasingly ongoing,  and changes happening gradually.  This now is a DAY of change abruptly?

Did Föhn Winds Just Melt Two Miles of East Antarctic Surface Ice in One Day?

https://robertscribbler.com/2016/11/28/did-fohn-winds-just-melt-two...

It’s right there in the satellite image. A swatch of blue that seems to indicate an approximate 2-mile long melt lake formed over the surface of East Antarctica in just one day. If confirmed, this event would be both odd and concerning. A part of the rising signal that melt stresses for the largest mass of land ice on the planet are rapidly increasing.

(Possible large melt lake on the surface of an ice shelf along the Scott Coast appears in this NASA satellite image. The melt lake seems to have formed after just one day during which föhn winds ran downslope from the Transantarctic Mountain Range — providing a potential period of rapid heating of the glacier surface.)

Surface Melt Now Showing Up in East Antarctica

While scientists and environmentalists are understandably concerned... — resulting in risks for rapid sea level rise for the near future, another consequence of global warming is also starting have a more visible impact on the frozen and now thawing continent. Surface melt, which was hitherto unheard of for most of East Antarctica, is now starting to pop up with increasing frequency.

East Antarctica, according to Stewart Jamieson, a glaciologist at Durham University ..., is “the part of the continent where people have for quite a long time assumed that it’s relatively stable, there’s not a huge amount of change, it’s very, very cold, and so, it’s only very recently that the first supraglacial lakes, on top of the ice, were identified.”

But now, even in austral springtime, we find evidence of surface melt in the satellite record.

On November 27, 2016, what looks like an approximate 2 mile long melt pond appeared in a section of ice shelf along the Scott Coast and just North of the Drygalski Ice Tongue in the region of McMurdo Sound. The lake — which is visible as a light blue swatch at center mass in the NASA-MODIS satellite image above — suddenly showed up in November 27 satellite image along a region where only white ice was visible before. And it appears in a region of East Antarctica that, before human-forced warming altered the typically-stable Antarctic climate, had rarely, if ever, seen surface melt.

(Near melting point temperatures appear along the Scott Coast in conjunction with an apparent föhn wind event. Image source: Earth Nullschool.)

The pond shows up coordinate with recorded near 0 C surface temperatures in the GFS monitor for November 26-27 and along with evidence of downsloping (föhn) winds. GFS indicators show downsloping winds gusting to in excess of 50 mph over the period. Such winds have the potential in increase surface temperatures by a.... And they have, increasingly, produced surface glacial melt events in regions of Greenland and Antarctica during recent years.

Surface Melt as a Feature of Glacial Destabilization

Supraglacial lake is just another word for a surface glacial melt lake. And these new lakes pose a big issue for ice sheet stability. Surface melt lakes are darker than white glacier surfaces. They act as lenses that focus sunlight. And the comparatively warm waters of these lakes can flood into the glacier itself — increasing the overall heat energy of the ice mass.

(A NASA researcher investigates a surface melt pond in Greenland. During recent years, these climate change related features have become more common in Antarctica. Image source: NASA.)

But water at the glacier surface doesn’t just sit there. It often bores down into the ice sheet — producing impacts for months and years after the surface lake’s formation. Sub surface lakes can form in the shadow of surface ponds. Transferring heat into the glacier year after year. In other cases, water from these lakes punches all the way to the glacier’s base. There the added lubrication of water speeds the glacier’s flow. All of these processes generate stresses and make glaciers less stable. And it is the presence of surface melt ponds that has been responsi....

Now, a similar process is impacting the largest concentration of land ice on the planet. And while Greenland holds enough ice to raise sea levels by around 21 feet, East Antarctica contains enough to lift the world’s oceans by about 195 feet. Surface melt there, as a result, produces considerably more risk to the coastal cities of the world.

Links:

NASA-MODIS (#ThankYouNASA)

These Stunning Blue Lakes Give us New Reason to Worry About Antarctica

Earth Nullschool

New Maps Chart Greenland Glaciers’ Melting Risk

Comment by SongStar101 on November 25, 2016 at 12:20pm

Note the Push & Bounce being very intense in the last weeks!   http://zetatalk.com/menukons.htm

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