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Robust method predicts beginning of new climate in Arctic based on warming, wetting and sea ice loss

A robust method to determine the beginning of a new climate
This photo shows a glacier on Svalbard. This island is a “hotspot” for climate change, where warming is very rapid. The study describes a very high change in surface air temperature (TAS), but also a high variability, which affects the “Time of Emergence.” Credit: Richard Bintanja, University of Groningen

When does “anomalous weather” become “a new climate”? The moment that variations in a specific climate variable turn into the new normal is termed Time of Emergence (ToE). Scientists from the University of Groningen and the Royal Netherlands Meteorological Institute (KNMI) have developed a method to predict the time of emergence in various Arctic regions, based on warming, wetting, and sea ice melting.

The ToE for temperature and sea ice is in the near future, i.e. somewhere before 2050, whereas the amount of rainfall will enter a new climate state at the end of the century. The results were published in the journal Scientific Reports on 12 April.

The scientists have used 14 and fed them with various greenhouse gas emission scenarios and aerosol amounts to reconstruct the past and predict future Arctic climate changes. The ToE was defined as the time when the values for a climate variable have been higher than 97.5% of the historical values for ten consecutive years.

The results show that, even though the Arctic is rapidly warming, ToE for temperature and sea ice cover has generally not yet been reached. This is mainly due to the extremely high natural variability in these Arctic variables.

A robust method to determine the beginning of a new climate
This figure shows multi-model estimates of the seasonal Arctic Time of Emergence (ToE) for (a) surface temperature, (b) sea ice thickness, (c) sea ice cover, (d) rainfall and (e) total precipitation. The values are the median ToE. Credit: Scientific Reports

Most sensitive predictor for climate change

There are large regional differences. For example, sea ice thickness has already reached a new climate state in the central Arctic region, as there is a relatively small variability in year-to-year thickness. This makes sea ice the most sensitive predictor for .

“We were excited to see that we were able to estimate ToE in a consistent and robust way,” says Richard Bintanja, University of Groningen Professor of Climate and Environmental Change and corresponding author of the study. The new predictions for ToE will help local Arctic inhabitants to adapt to the new Arctic climate. “The next step is to apply these insights in society, policy, and ecology.”

More information:
Nicoleta Tsakali et al, The time of emergence of Arctic warming, wetting and sea ice melting, Scientific Reports (2025). DOI: 10.1038/s41598-025-96607-1

Citation:
Robust method predicts beginning of new climate in Arctic based on warming, wetting and sea ice loss (2025, May 6)
retrieved 6 May 2025
from https://phys.org/news/2025-05-robust-method-climate-arctic-based.html

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