about
Observed and simulated temperature extremes during the recent warming hiatusLocal biomass burning is a dominant cause of the observed precipitation reduction in southern Africa.Humid heat waves at different warming levels.Top ten European heatwaves since 1950 and their occurrence in the coming decadesSlow and fast responses of mean and extreme precipitation to different forcing in CMIP5 simulationsClimate emergencies do not justify engineering the climateDependence of Present and Future European Temperature Extremes on the Location of Atmospheric BlockingDynamical response of Mediterranean precipitation to greenhouse gases and aerosolsPDRMIP: A Precipitation Driver and Response Model Intercomparison Project—Protocol and Preliminary ResultsThe Geoengineering Model Intercomparison Project Phase 6 (GeoMIP6): simulation design and preliminary resultsMagnitude of extreme heat waves in present climate and their projection in a warming worldPercentile indices for assessing changes in heavy precipitation eventsNew vigour involving statisticians to overcome ensemble fatigueMediterranean Precipitation Response to Greenhouse Gases and AerosolsAerosol effect on climate extremes in Europe under different future scenariosA multimodel examination of climate extremes in an idealized geoengineering experimentConsistency of Temperature and Precipitation Extremes across Various Global Gridded In Situ and Reanalysis Datasets*Evaluating model-simulated variability in temperature extremes using modified percentile indicesExtreme Cold Winter Temperatures in Europe under the Influence of North Atlantic Atmospheric BlockingThe Changing Seasonality of Extreme Daily PrecipitationFrequency of extreme precipitation increases extensively with event rareness under global warming
P50
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P50
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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Jana Sillmann
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P106
P1153
23101759100
P31
P496
0000-0002-0219-5345