IMAGE: Henning Åkesson
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Credit score: Henning Åkesson

The kind of materials current underneath glaciers has a big effect on how briskly they slide in the direction of the ocean. Scientists face a difficult process to accumulate information of this under-ice panorama, not to mention tips on how to signify it precisely in fashions of future sea-level rise.

“Selecting the flawed equations for the under-ice panorama can have the identical impact on the expected contribution to sea-level rise as a warming of a number of levels”, says Henning Åkesson, who led a brand new revealed examine on Petermann Glacier in Greenland.

Glaciers and ice sheets around the globe at the moment lose greater than 700,000 Olympic swimming swimming pools of water day-after-day. Glaciers kind by the transformation of snow into ice, which is later melted by the ambiance in summer time, or slides all the way in which into the ocean. With local weather change, glaciers are breaking apart and drop icebergs into the ocean at an accelerating tempo. Precisely how briskly relies upon to a big extent on the mattress under all of the ice. Glaciers conceal a panorama underneath the ice coated by rocks, sediments and water. A brand new examine reveals that the way in which we signify this under-ice panorama in laptop fashions means an ideal deal for our predictions of future sea-level rise. Extra particularly, how we incorporate the friction between the bottom and the ice sliding over it in glacier fashions is what impacts our predictions. This was discovered by a crew of Swedish and American scientists, after they simulated the way forward for Petermann Glacier, the most important and quickest glacier in northern Greenland.

Petermann is without doubt one of the few glaciers within the northern hemisphere with a remaining ice tongue, a sort of floating glacier extension in any other case primarily present in Antarctica, the place they’re referred to as ice cabinets. These floating extensions have been discovered to be uncovered to heat subsurface water flowing from the open ocean in the direction of the glaciers. This occurs each in Antarctica and in lots of fjords round Greenland, together with the Petermann Fjord.

“Peterman misplaced 40% of its floating ice tongue over the past decade. It nonetheless has a forty five km tongue, however we discovered {that a} barely hotter ocean than at present would result in its break up, and set off a retreat of the glacier”, says Henning Åkesson, a postdoctoral researcher at Stockholm College who led the examine.

Many glaciers in Greenland and Antarctica circulate in the direction of the ocean a lot quicker than they did a number of a long time in the past, and due to this fact contribute extra to world sea-level rise. Scientists have due to this fact mobilized nice efforts into studying what’s going on in these environments. This has spurred new insights into the panorama underneath glaciers and the form of the seafloor the place they drain. We now additionally know far more about what occurs to the ice when glaciers meet the ocean.

Nonetheless, the distant polar areas are notoriously tough to check due to sea ice, icebergs, and infrequently harsh climate. The under-ice panorama is a selected problem as a result of, frankly, it’s laborious to measure one thing coated by a kilometer of ice on prime. Even in areas of recognized under-ice topography, describing its bodily properties utilizing mathematical equations is tough. Pc fashions are due to this fact nonetheless considerably in the dead of night in terms of tips on how to signify issues like sediments, rocks, ponds and rivers underneath glaciers within the equations that describe ice circulate. These equations are finally the inspiration of the fashions utilized by the IPCC to estimate how briskly glaciers circulate and the way a lot sea ranges will rise underneath future local weather warming.

“As we mentioned, selecting the flawed equations for the under-ice panorama can have the identical impact on the contribution to sea-level rise as a warming of a number of levels”, Åkesson says.

“In actual fact, predicted sea-level rise for this Greenland glacier can quadruple relying on how we signify friction underneath the ice. We nonetheless do not know which approach is the very best, however our examine illustrates that ice-sheet fashions nonetheless must progress on this respect, with a purpose to enhance our estimates of mass loss from Earth’s polar ice sheets.”


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