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Showing 1–15 of 15 results
Advanced filters: Author: Kyle C. Armour Clear advanced filters

  • The spatial pattern of climate change is uncertain. Analyses of a simple model suggest that uncertainty in tropical feedbacks induces a global response, but the impact of uncertainty in polar feedbacks tends to be limited to the region.

    • Gerard H. Roe
    • Nicole Feldl
    • Dargan M. W. Frierson
    Research
    Nature Geoscience
    Volume: 8, P: 135-139

  • Unlike the Arctic, the Southern Ocean has shown little warming. An analysis of observations and numerical simulations suggests that Southern Ocean warming patterns are shaped by meridional overturning more than surface heating.

    • Kyle C. Armour
    • John Marshall
    • Emily R. Newsom
    Research
    Nature Geoscience
    Volume: 9, P: 549-554

  • Thermoregulatory platforms that combine the advantages of passive and active thermal management systems have remained elusive. Here, the authors draw inspiration from the static infrared-reflecting space blanket and dynamic color-changing squid skin to develop a composite material that addresses this challenge.

    • Erica M. Leung
    • Melvin Colorado Escobar
    • Alon A. Gorodetsky
    ResearchOpen Access
    Nature Communications
    Volume: 10, P: 1-10

  • Recent observations of Earth's energy budget indicate low climate sensitivity. Research now shows that these estimates should be revised upward, resolving an apparent mismatch with climate models and implying a warmer future.

    • Kyle C. Armour
    News & Views
    Nature Climate Change
    Volume: 6, P: 896-897

  • The relative roles of local and remote processes in determining equatorial warming are still debated. Model simulations show that coupled feedbacks strongly damp the equatorial surface temperature response to local equatorial forcing, while amplifying the response to remote off-equatorial forcing.

    • Malte F. Stuecker
    • Axel Timmermann
    • Michiya Hayashi
    Research
    Nature Climate Change
    Volume: 10, P: 124-129

  • Model simulations with CO2 forcing prescribed in discrete geographical regions reveal that polar amplification arises primarily due to local lapse-rate feedback, with ice-albedo and Planck feedbacks playing subsidiary roles.

    • Malte F. Stuecker
    • Cecilia M. Bitz
    • Fei-Fei Jin
    Research
    Nature Climate Change
    Volume: 8, P: 1076-1081

  • Estimating the magnitude of radiative and non-radiative feedbacks is key for understanding the climate dynamics of polar regions. Here the authors propose an inclusive methodology to quantify the influence of all those feedbacks, stimulating more systematic analyses in observational and model ensembles.

    • Hugues Goosse
    • Jennifer E. Kay
    • Martin Vancoppenolle
    ReviewsOpen Access
    Nature Communications
    Volume: 9, P: 1-13