” If we miss this emission goal, the ice sheets will melt and break down at an accelerated speed, according to our calculations. If we do not take any action, pulling away ice sheets would continue to increase sea level by at least 100 cm within the next 130 years. “We see that sea ice and climatic circulation changes around Antarctica likewise play a vital function in controlling the amount of ice sheet melting with effects for international sea level forecasts,” she adds.
Sea level rise contributions from the Antarctic and Greenland ice sheets, and maps of predicted 2150 CE Antarctic ice sheet surface area elevation following different greenhouse gas emission situations (SSP1-1.9, strong emission cuts; SSP2-4.5, medium emission cuts; SSP5-8.5, weak emission cuts). Credit: Institute for Basic Science Jun-Young Park
A research study published in Nature Communications today (February 14) by an international group of scientists shows that an irreparable loss of the West Antarctic and Greenland ice sheets, and a matching fast velocity of sea level rise, might loom if worldwide temperature change can not be supported below 1.8 ° C, relative to the preindustrial levels.
Coastal populations worldwide are currently bracing for increasing seas. Preparing for counter-measures to prevent inundation and other damages has been very challenging because the latest environment model forecasts presented in the 6th assessment report of the Intergovernmental Panel on Climate Change (IPCC) do not agree on how quickly the significant ice sheets will respond to worldwide warming.
Melting ice sheets are potentially the largest factor to water level modification, and traditionally the hardest to forecast since the physics governing their behavior is infamously complicated. “Moreover, computer system designs that replicate the characteristics of the ice sheets in Greenland and Antarctica typically do not represent the reality that ice sheet melting will impact ocean processes, which, in turn, can feed back onto the ice sheet and the atmosphere,” says Jun Young Park, PhD student at the IBS Center for Climate Physics and Pusan National University, Busan, South Korea and first author of the study.
Utilizing a new computer design, which catches for the very first time the coupling in between ice sheets, icebergs, ocean, and atmosphere, the group of environment researchers discovered that an ice sheet/sea level run-away impact can be avoided only if the world reaches net absolutely no carbon emissions before 2060.
” If we miss this emission goal, the ice sheets will melt and break down at an accelerated rate, according to our calculations. If we do not take any action, pulling away ice sheets would continue to increase water level by a minimum of 100 cm within the next 130 years. This would be on top of other contributions, such as the thermal expansion of ocean water” says Prof. Axel Timmermann, co-author of the study and Director of the IBS Center for Climate Physics.
Ice sheets respond to oceanic and climatic warming in postponed and often unpredictable methods. Formerly, scientists have highlighted the value of subsurface ocean melting as a crucial procedure, which can trigger runaway effects in the significant marine-based ice sheets in Antarctica. “However, according to our supercomputer simulations, the efficiency of these procedures might have been overstated in current studies,” states Prof. June Yi Lee from the IBS Center for Climate Physics and Pusan National University and co-author of the study. “We see that sea ice and climatic circulation modifications around Antarctica also play a vital function in managing the amount of ice sheet melting with effects for international water level forecasts,” she adds.
The research study highlights the requirement to establish more complex earth system models, which catch the various environment parts, as well as their interactions. New observational programs are needed to constrain the representation of physical processes in earth system designs, particularly from highly active regions, such as Pine Island glacier in Antarctica.
” One of the crucial difficulties in replicating ice sheets is that even small procedures can play an essential role in the large-scale reaction of an ice sheet and for the matching sea-level forecasts. Not only do we have to include the coupling of all elements, as we performed in our present research study, however we likewise need to imitate the characteristics at the highest possible spatial resolution utilizing a few of the fastest supercomputers,” sums up Axel Timmermann.
Reference: “Future sea-level forecasts with a paired atmosphere-ocean-ice-sheet design” 14 February 2023, Nature Communications.DOI: 10.1038/ s41467-023-36051-9.
