Quantcast
Channel: Pakalolo
Viewing all articles
Browse latest Browse all 1268

The fingernails clinging onto Thwaites Glacier appear to be peeling off.

$
0
0

Thwaites glacier front in the vulnerable West Antarctica sector is very broad (70 miles wide where it meets the ocean) and, in its entirety, is the size of Florida. The glacier is the most feared as it decays rapidly and threatens coastal cities worldwide. The cork in the bottle for the entirety of West Antarctica holds ten feet of sea level rise. The collapse of the marine extension will not add to sea level rise as it already floats. When it collapses, the cork pops, and the land ice is free to slide into the Weddel Sea and the Amundsen Sea, raising sea levels.

All the damage to Thwaites's stability is occurring below the ice. The upwelling of warm ocean water softens and erodes the soft white underbelly of the glacier. The upwelling also lifts the ice, where warmer waters can flow to the ridges and beyond the grounding line, furthering the ice's decay with a faster flow, more shattering and fracturing with the threat of collapse. The water can do that because the ice is no longer anchored on the bedrock.

The ocean at the front of the glacier is still quite cold, approximately 34-36 degrees Fahrenheit. That is above freezing, and if you think of your afternoon cocktail filled with ice, that is similar to the temperature of the ocean water eating away at the glacier. Sipping your cocktail, you observe that the ice is melting, which is precisely what is occurring to the underside of the massive marine extension of Thwaites glacier. The glacier by itself holds two feet of sea level rise. 

Geophysicists were able to map the front of the glacier's seafloor. Like you and me, we have a history, and so does Thwaites.  

A 3D-rendered view of the multibeam bathymetry (seafloor shape) colored by depth, collected by Rán across a seabed ridge just in front of Thwaites Ice Shelf

A recent study by the University of South Florida:

At some point in the last 200 years, over a duration of less than six months, the front of glacier lost contact with a seabed ridge and retreated at a rate of more than 2.1 kilometers per year (1.3 miles per year) -- twice the rate documented using satellites between 2011 and 2019.  

“Our results suggest that pulses of very rapid retreat have occurred at Thwaites Glacier in the last two centuries, and possibly as recently as the mid-20th Century,” said Graham.

“Thwaites is really holding on today by its fingernails, and we should expect to see big changes over small timescales in the future – even from one year to the next – once the glacier retreats beyond a shallow ridge in its bed,” said marine geophysicist and study co-author, Robert Larter, from the British Antarctic Survey.  

The tongue of Thwaites is fifty miles wide. You can make a distinction on the tongue depending on its stability and whether it is anchored on a ridge. While in peril, the western part of the tongue is still relatively stable. The eastern part is shedding chunks of ice like there is no tomorrow, and the eastern side also holds the majority of land ice. Sooner rather than later for chaos, in my estimation.

In 2001, a significant iceberg named Iceberg B22a broke from the Thwaites' tongue and became stuck in front of the doomsday glacier’s marine extensions tongue. For twenty-two years, B22a protected the calving front from the open ocean.

The iceberg was fifty-three miles long and forty miles wide. It is also subjected to warming waters, and the berg was thinned enough that it was freed from the undersea mount it was stuck on in September of 2022.

That means a brutal assault on Thwaites from the stormy southern ocean will occur. A flotilla of icebergs calving from the front is expected following the iceberg exiting the Amundsen Sea and entering the Weddel. If you did not know, West Antarctica passed the tipping point many years ago. We are witnessing the rapdity of the consequences.

There is satellite imagery that the front is in serious trouble. No one has reported it yet, as it happened in early December 2022. Still, the images are posted on Twitter by folks alarmed by the inevitability of collapse who dissect images on NASA’s worldview and post them to Twitter.

1300 kilometers of open ocean along the #thwaites area.. Despite cold temperatures and cold SSTs No word nowhere. And no clouds....perfectly clear image today 🤣🤣🤣🤣 pic.twitter.com/Gj7XKKIId5

— 🇺🇦Christopher Cartwright🇺🇦 (@chriscartw83) November 30, 2022

I forgot to underline the most important fact. The Thwaites Glacier will really end up in dangerous waters when the blocking iceberg B22a will have removed from the Amundsen Sea. B22a now turns very fast to squeeze itself out from between the 2 undersea cliffs in the west & east. pic.twitter.com/2QVMhaw1H9

— Kris Van Steenbergen (@KrVaSt) December 1, 2022

Yikes. Over a less than 6-month period, the Thwaites Glacier's grounding zone retreated at a rate of more than 1.3 miles per year, which is twice the rate that had been previously observed by satellite from 2011 to 2019. https://t.co/tFi4S1vg8l

— Poppy Davis (@psmorehouse1) December 2, 2022

We're waiting until the sea ice barrier in front of the Thwaites Glacier & in front of the Crosson Ice Shelf will crumble. In the end TG, the PIG Tongue & the Crosson Ice Shelf will collapse due to extra lift & warm underflows. 1 year, 2 years, maybe 4! It could happen anytime. pic.twitter.com/xzAXhAP9UQ

— Kris Van Steenbergen (@KrVaSt) December 2, 2022

A larget sat photo of the #Thwaites area and West #Antarctica 03.12.2022 Even the sea ice further out is very damaged 80 days to minimum. Humankind needs to pray for no massive heatwave. pic.twitter.com/b0I1H7L3NT

— 🇺🇦Christopher Cartwright🇺🇦 (@chriscartw83) December 4, 2022

Crumbling sea ice is normal at this time of the year. Iceberg B22a turning around & leaving the Amundsen Sea after 21 years is the thing we need to worry about. Thwaites Glacier is a lost cause without its blocking chunk of ice. There nothing upstream coming close to a new B22a! pic.twitter.com/D8iYNfrSsf

— Kris Van Steenbergen (@KrVaSt) December 4, 2022

This is the giant iceberg in front of #Thwaites... And it is imploding quickly. WTF is going on in #Antarctica? pic.twitter.com/v1AwFPUuLJ

— 🇺🇦Christopher Cartwright🇺🇦 (@chriscartw83) December 7, 2022

This is the centre & the weakest spot of Thwaites Glacier's calving front, right above a steep retrograde slope (its last stable grounding line). The blue area is 1 km deep! Its fingernails seem to break. The TG Tongue has reached a speed of 1km/month now!https://t.co/OL60cKzbdWpic.twitter.com/Btp4pwyGgb

— Kris Van Steenbergen (@KrVaSt) December 3, 2022

It looks like only a corner of the tongue broke off (The tongue is where the marker is) This sequence is early November through 7 December. Note that the large sheets took some time to move off. I suspect this was from the grounding. pic.twitter.com/of67LwjPwm

— USGS: Sea Level Rise in Melting Glaciers: 263' (@CassandrasGhost) December 8, 2022

As I pointed out earlier, there is no reporting from anyone yet. Citizens working on monitoring Antarctica have broken the news. You can see their names above. 

My kindred spirits who read this news care. Everybody else, not so much. It's important news, and you, my friends, are some of the first to know. If you live on the coast and own a home, take this information to heart for any future plans that you may have.

Thwaites marine extension is predicted to collapse within three to five years. 


Viewing all articles
Browse latest Browse all 1268

Trending Articles



<script src="https://jsc.adskeeper.com/r/s/rssing.com.1596347.js" async> </script>