Arctic summer sea ice loss will accelerate in coming decades

The Arctic sea ice (ASI) is expected to decrease with further global warming. However, considerable uncertainty remains regarding the temperature range that would lead to a completely ice-free Arctic. Here, we combine satellite data and a large suite of models from the latest phase of the Coupled Mo...

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Bibliographic Details
Published in:Environmental research letters Vol. 19; no. 7; pp. 074032 - 74038
Main Authors: Poltronieri, Anna, Bochow, Nils, Olson Aksamit, Nikolas, Boers, Niklas, Kristen Jakobsen, Per, Rypdal, Martin
Format: Journal Article
Language:English
Published: Bristol IOP Publishing 01-07-2024
IOS Press
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Summary:The Arctic sea ice (ASI) is expected to decrease with further global warming. However, considerable uncertainty remains regarding the temperature range that would lead to a completely ice-free Arctic. Here, we combine satellite data and a large suite of models from the latest phase of the Coupled Model Intercomparison Project (CMIP6) to develop an empirical, observation-based projection of the September ASI area for increasing global mean surface temperature (GMST) values. This projection harnesses two simple linear relationships that are statistically supported by both observations and model data. First, we show that the September ASI area is linearly proportional to the area inside a specific northern hemisphere January-September mean temperature contour Tc. Second, we use observational data to show how zonally averaged temperatures have followed a positive linear trend relative to the GMST, consistent with Arctic amplification. To ensure the reliability of these observations throughout the rest of the century, we validate this trend by employing the CMIP6 ensemble Combining these two linear relationships, we show that the September ASI area decrease will accelerate with respect to the GMST increase. Our analysis of observations and CMIP6 model data suggests a complete loss of the September ASI (area below 10 6 km 2 ) for global warming between 1.5°C and 2.2°C above pre-industrial GMST levels.
Bibliography:ERL-118027.R1
Environmental Research Letters
ISSN:1748-9326
1748-9326
DOI:10.1088/1748-9326/ad5194