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Showing 1–7 of 7 results
Advanced filters: Author: Stephan A. Fueglistaler Clear advanced filters

  • Limiting global warming to 1.5 °C will prevent tropical regions from reaching the limit of human adaptability, according to robust dynamical constraints on projected heat stress.

    • Yi Zhang
    • Isaac Held
    • Stephan Fueglistaler
    Research
    Nature Geoscience
    Volume: 14, P: 133-137

  • Stratospheric water vapour affects Earth’s radiation budget. A 19-month record of the hydrogen isotopic composition of water in the tropical stratosphere, collected through remote sensing measurements, shows a clear seasonal cycle in the isotopic composition that propagates upwards in this region, and is most likely created in the tropical tropopause layer.

    • Jörg Steinwagner
    • Stephan Fueglistaler
    • Thomas Röckmann
    Research
    Nature Geoscience
    Volume: 3, P: 262-266

  • Hydrological sensitivity describes how much precipitation changes for a given warming. Here, the authors show that the hydrological sensitivity differs between the three tropical ocean basins, which influences land rainfall changes across the tropical and mid-latitude regions.

    • Jie He
    • Kezhou Lu
    • Stephan A. Fueglistaler
    Research
    Nature Climate Change
    Volume: 14, P: 623-628

  • Ozone depletion in the Arctic stratosphere consistently disrupts surface temperature and precipitation patterns across the Northern Hemisphere, according to atmospheric chemistry–climate modelling and observations.

    • Marina Friedel
    • Gabriel Chiodo
    • Thomas Peter
    Research
    Nature Geoscience
    Volume: 15, P: 541-547

  • Deforestation in Amazonia has previously been linked to thermally driven precipitation increases. Satellite observations and model simulations now suggest a shift toward a dynamically driven hydroclimate, with enhanced rainfall seen downwind of deforested areas.

    • Jaya Khanna
    • David Medvigy
    • Robert Walko
    Research
    Nature Climate Change
    Volume: 7, P: 200-204

  • Regional projections of daily extreme precipitation are uncertain, but can be decomposed into thermodynamic and dynamic contributions to improve understanding. While thermodynamics alone uniformly increase extreme precipitation, dynamical processes introduce regional variations.

    • S. Pfahl
    • P. A. O’Gorman
    • E. M. Fischer
    Research
    Nature Climate Change
    Volume: 7, P: 423-427