Deutsch
 
Hilfe Datenschutzhinweis Impressum
  DetailsucheBrowse

Datensatz

DATENSATZ AKTIONENEXPORT

Freigegeben

Zeitschriftenartikel

Large-scale emergence of regional changes in year-to-year temperature variability by the end of the 21st century

MPG-Autoren
/persons/resource/persons198616

Olonscheck,  Dirk
School of Geosciences, Edinburgh;
Max Planck Research Group The Sea Ice in the Earth System, The Ocean in the Earth System, MPI for Meteorology, Max Planck Society;

Externe Ressourcen
Es sind keine externen Ressourcen hinterlegt
Volltexte (beschränkter Zugriff)
Für Ihren IP-Bereich sind aktuell keine Volltexte freigegeben.
Volltexte (frei zugänglich)

s41467-021-27515-x.pdf
(Verlagsversion), 10MB

Ergänzendes Material (frei zugänglich)

2021_NatureCommunications_Olonscheck.zip
(Ergänzendes Material), 12MB

Zitation

Olonscheck, D., Schurer, A. P., Lücke, L., & Hegerl, G. (2021). Large-scale emergence of regional changes in year-to-year temperature variability by the end of the 21st century. Nature Communications, 12: 7237. doi:10.1038/s41467-021-27515-x.


Zitierlink: https://hdl.handle.net/21.11116/0000-0009-74F3-2
Zusammenfassung
Global warming is expected to not only impact mean temperatures but also temperature variability, substantially altering climate extremes. Here we show that human-caused changes in internal year-to-year temperature variability are expected to emerge from the unforced range by the end of the 21st century across climate model initial-condition large ensembles forced with a strong global warming scenario. Different simulated changes in globally averaged regional temperature variability between models can be explained by a trade-off between strong increases in variability on tropical land and substantial decreases in high latitudes, both shown by most models. This latitudinal pattern of temperature variability change is consistent with loss of sea ice in high latitudes and changes in vegetation cover in the tropics. Instrumental records are broadly in line with this emerging pattern, but have data gaps in key regions. Paleoclimate proxy reconstructions support the simulated magnitude and distribution of temperature variability. Our findings strengthen the need for urgent mitigation to avoid unprecedented changes in temperature variability.