Rob Larter Profile picture
Mar 26 11 tweets 5 min read
Any post about declining #seaice extent triggers replies pointing out that as the ice is already floating it doesn’t make any difference to sea level. This is correct of course (well, nearly). So why does sea-ice loss matter? There are several reasons. 1/11
Firstly there is the high “albedo” of the ice. It reflects a lot of incoming solar radiation. Reduced summer sea-ice extent exposes more of the ocean surface, which is darker (lower albedo) and thus absorbs more radiant energy, warming the water. 2/11
A second reason is that the normal seasonal fluctuations in sea-ice extent are of great ecological importance. The plankton bloom that occurs each Spring as the sea-ice edge retreats is the foundation of the Southern Ocean food chain. 3/11
A decline in Antarctic sea-ice extent will result in this Spring bloom occurring earlier and further south, with uncertain ecological consequences. 4/11
A third reason is that sea ice in front of ice shelves (parts of the ice sheet that flow out over the sea) protects them from ocean swell, and in some areas continuous “landfast” sea ice sheets buttress ice shelves directly.
doi.org/10.1038/s41586…
doi.org/10.5194/tc-12-…
5/11
A fourth reason is that “brine rejection” during seasonal formation of sea ice is a key process in the formation of dense water masses that sink to the depths of the ocean and are critical to driving the global overturning thermohaline circulation. 6/11
Reduced sea-ice formation means less dense water production, which weakens the overturning circulation. One component of this is the Gulf Stream, which is important to the climate stability of northwest Europe.
ucl.ac.uk/news/2021/feb/…
7/11
Another common response to posts about declining sea-ice extent is that the satellite record only extends back to 1979, so may not capture some longer-term cyclic variations. While this is true it is disingenuous to suggest that the decline is unrelated to recent warming. 8/11
During the recent RV Polarstern #PS134 research cruise we witnessed a very clear indication of longer term change, as we were working in ice-free seas in the same area as the Belgica was trapped in sea ice 125 years ago.
discoveringbelgium.com/voyage-of-the-…
9/11
Although Antarctic sea-ice extent varies somewhat from year to year, so we need to be cautious in identifying trends, it is unthinkable that the conditions experienced on the Belgica expedition could occur these days even in a high sea-ice year. 10/11
Finally, for any nerds who want to look further into the comment I made in the tweet at the start of this thread, about sea-ice melting not making any difference to sea-level only being nearly correct, here is some further reading on the topic. 11/11
doi.org/10.1029/2007GL…

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More from @rdlarter

Feb 15, 2022
I was privileged to be invited to write a commentary on an interesting recent paper about the roughness of ice shelves by Watkins et al. (2021).
Commentary features this schematic diagram of the #ThwaitesGlacier Eastern Ice Shelf by @MarloWordyBird doi.org/10.1029/2021GL…
1/N
The paper that was the subject of the commentary is available here -
doi.org/10.1029/2021GL…
2/N
Background -
Ice shelves are floating extensions of glaciers that flow on beds hundreds of meters below sea level. They contribute "backstress" restricting outflow from many of the largest glaciers in Antarctica, thus limiting the Antarctic contribution to sea-level rise.
3/N
Read 15 tweets
Dec 18, 2021
Great to see @GlacierThwaites research covered in national media, but a few points in this @guardian article need correction or further explanation.
1/n theguardian.com/world/2021/dec…
Firstly, “great cracks and fissures” have not “opened up both on top of and underneath the Thwaites glacier” itself, but on the floating ice shelf in front of it.
2/n
Secondly, the processes the triggered the ultimate break-up of the Larsen B Ice Shelf were different from those that are destabilising the Thwaites Eastern Ice Shelf. Larsen B break-up was triggered by extensive surface melt filling crevasses and causing hydrofracture.
3/n
Read 8 tweets
Aug 15, 2020
While @GlacierThwaites fieldwork is postponed for the coming Antarctic summer, how much ongoing ice loss is there from #ThwaitesGlacier and nearby glaciers in the Amundsen Sea, and how big is their contribution to sea-level rise? Thread, 1/23
3 separate recent studies provide measurements for individual glaciers or drainage basins based on satellite remote sensing observations:
Rignot et al. (2019) doi.org/10.1073/pnas.1…
Shepherd et al. (2019) doi.org/10.1029/2019GL…
Smith et al. (2020) doi.org/10.1126/scienc…
2/23
In summary, the results of these studies show rates of net ice mass loss from Thwaites and nearby glaciers are now more than six times what they were 30 years ago. This graph shows the progressive increase in net ice loss from Thwaites from the results of Rignot et al. 3/23 Image
Read 23 tweets
Dec 21, 2019
A thread listing some of the sources of info, video clips and animations I included in my talk on The Polar Oceans at the outreach event following on from @BSRG19 earlier this week. Thanks to @FJavierHernnde2 for this photo and for organizing the event. 1/n Image
This figure, as seen in the previous tweet, shows an Antarctic-centred view of the global thermohaline circulation system from a recent article by @meredith_mmm challenger-society.org.uk/oceanchallenge…. It highlights how the Southern Ocean connects the other major oceans. 2/n Image
To further illustrate the thermohaline circulation I showed an animation by Greg Shirah of @NASAViz , which can be found at svs.gsfc.nasa.gov/3658. 3/n
Read 24 tweets

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