Emergence time of CO2-forced European summer climate trends
Médéric St-Pierre, Joakim Kjellsson, Wonsun Park, Leonard F. Borchert, Mojib Latif

TL;DR
The study finds that rising CO2 levels will significantly impact European summer climate trends, particularly in terms of temperature and soil moisture, within a few decades.
Contribution
The study provides new insights into the time of emergence of CO2-forced climate trends in Europe using a large ensemble of simulations.
Findings
Near-surface temperature trends emerge within 20–40 years under increasing CO2.
Soil moisture trends emerge after 30 years in the Mediterranean and 70 years in Western Europe.
Extreme dry summers become more severe in a 4xCO2 climate, impacting agriculture.
Abstract
This study investigates the time of emergence (ToE) of European summer climate trends in a warming world. We use a large ensemble of simulations performed with the Kiel Climate Model, in which atmospheric CO2 levels increase by 1% per year starting from pre-industrial concentration. The ToE for near-surface temperature, soil moisture, and the hydrological cycle highlights a relatively fast (20–40 years) emergence of near-surface temperature trends, while precipitation trends remain within the range of natural variability until the end of the 140-year-long simulation when CO2 levels quadruple. Soil moisture trends emerge after approximately 30 years in parts of the Mediterranean region, whereas in Western and Central Europe, they only emerge in the west after about 70 years when CO2 concentrations have doubled. Although many CO2-forced climate trends are not emerging over Europe, a…
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Taxonomy
TopicsClimate variability and models · Climate Change and Environmental Impact · Science and Climate Studies
