Tag Archives: Sentinel

Shock News – Massive Calving of Jakobshavn Isbræ

Jakobshavn Isbræ is a glacier in Western Greenland made (more?) famous by James Balog in his “Chasing Ice” movie. Here’s the “official video”:

which claims that it:

Captures [the] largest glacier calving ever filmed. On May 28, 2008, Adam LeWinter and Director Jeff Orlowski filmed a historic breakup at the Ilulissat Glacier in Western Greenland.

Depending on which languages you prefer to mix and match “Ilulissat Glacier” is another name for the self same glacier. So is “Sermeq Kujalleq”. Now comes news that something similar has just happened, albeit captured only by satellites in the twilight of the Arctic “spring”. Over on the Arctic Sea Ice Forum Espen Olsen posted late last night (UTC):

Believe it or not! Massive calving seen at the southern branch of Jakobshavn Isbræ

together with this animation created using images from the Landsat 8 Operational Land Imager:

Jakobshavn-feb12-feb19-2015-2

We’ve just grabbed this Sentinel-1A synthetic aperture radar image from February 15th 2015 via Polarview, which appears to suggest that the calving took place before 20:38 UTC on that date:

S1A_Jakobshavn_20150215T203828

Here’s a Sentinel-1A image via “nukefix” at the Arctic Sea Ice Forum, which confirms that the calving took place on or before February 16th:

subset_0_of_S1A_IW_GRDH_1SSH_20150216T095944_20150216T100009_004647_005BB8_B43C_Calib_EC_Sigma0_HH_db

This is a before/after animation from “A-Team” on the Arctic Sea Ice Forum, using 15m resolution Landsat images:

Jakobshavn-anim

Finally, for the moment at least, Espen Olsen provides an illustration of the retreat of the calving face of Jakobshavn Isbræ since 1851:

Jakobshavn-calving1851-2014

This most recent event does not bring the calving face further east than the position in summer 2014. However the sun’s rays are only just returning to that part of the planet, and the next one may well do so.

[Edit – 24/02/2015]

We’ve phoned DMI and NSIDC as well, but Jason Box who is a Professor at the Geological Survey of Denmark and Greenland has been the first to respond with an opinion about how unusual this event is:

It’s an interesting finding. In the attached prepared by Karina Hansen you will see a light yellow polygon illustrating the end of melt season 2014 ice. Jakobshavn front position retreated from the Feb 2014 (pink line) and Feb 2015 (green line) positions. The Feb 2014 and Feb 2015 positions are roughly the same with 2014 Feb being further retreated than Feb 2015:

Jaki_2015

A cautious response: even if this calving were abnormal, we will likely see an advance in the next weeks that will fill the void. Why?

A) This glacier flows fast, and

B) Now with less flow resistance there will likely be an acceleration making the void filling happen even faster.

Here are annual end of melt season area changes measured by PROMICE.org. These are being updated. I will ask Karina Hansen today to update for 2014 and 2015. We could have that result in a few hours.

1999/00 -2.750
2000/01 -2.473
2001/02 -16.357
2002/03 -45.617
2003/04 -21.235
2004/05 -10.015
2005/06 -4.151
2006/07 -3.830
2007/08 -3.202
2008/09 -2.174
2009/10 -8.725
2010/11 -6.693
2011/12 -13.743
2012/13 -2.826

In context of the ongoing retreat, I would speculate that this retreat could make further retreat more likely because the acceleration from B) would cause ‘dynamic thinning’ that through a positive feedback would reduce glacier bed friction facilitating further thinning and acceleration. This feedback is an amplifier and not runaway but being activated would precondition Jakobshavn glacier for further retreat.

[Edit – 01/03/2015]

Espen Olsen suggests on the Arctic Sea Ice Forum:

Watch the speed of Jakobshavn over 9 days:

Jak-20150228

New Antarctic Sea Ice Resources

In the Arctic the refreeze is slowing down as the March maximum extent approaches. Meanwhile in the southern hemisphere Antarctic sea ice extent has taken a tumble as the annual minimum extent approaches.

Over the long cold Arctic winter “Wipneus” of ArctischePinguin fame has been porting his northern hemisphere regional sea ice area/extent methodology to cover the South Pole as well. We are pleased to be able to reveal the fruits of his labours on our new regional Antarctic Sea Ice Graphs page. The ultimate source of the information is the University of Hamburg’s sea ice concentration data based on a 3.125 km grid that uses data from the from the AMSR2  instrument on board the Japan Aerospace Exploration Agency’s SHIZUKU satellite. Here’s an overview of Antarctic sea ice area:

2015-02-07-Ant-Area and here’s a close up on the sea ice extent in the Bellingshausen and Amundsen Seas region, where what sea ice there is helps buttress the West Antarctic Ice Sheet:

2015-02-07-West-Extent

In future we will also be bringing you satellite images from Antarctica. By way of example, here’s the latest “Shock News!!!” from the Antarctic, courtesy of LandSat 8:

I
NASA report that:

While large icebergs calve regularly from fast-flowing ice shelves in West Antarctica, the coast of cooler, drier East Antarctica tends to be less active. That made it a mild surprise when a 70-square-kilometer chunk of ice broke off from the King Baudouin Ice Shelf in January 2015. The last time that part of King Baudouin calved such a large iceberg was in the 1960s.

and you can track the current position of the latest large chunk of ex ice shelf on their WorldView web site:

The recently calved King Baudouin Ice Shelf on February 3rd 2015
The recently calved King Baudouin Ice Shelf on February 3rd 2015

Thanks also to “Arcticio” from the Arctic Sea Ice Blog who pointed me in the direction of PolarView, where it was remarkably easy to locate this Sentinel-1A synthetic aperture radar image of the large iceberg in question on January 30th 2015:

RoiBaudouin-600