Research articles

Filter By:

Article Type
Year
  • The stability of climatic conditions since the Last Glacial Maximum has contributed to current global patterns of species richness. Changes in patterns of climate stability this century reveal areas where climate change could reduce biodiversity, with largest losses in past climatic safe havens.

    • Stuart C. Brown
    • Tom M. L. Wigley
    • Damien A. Fordham
    Letter
  • Ozone forms in the atmosphere when other anthropogenically emitted gases react with sunlight and negatively impacts terrestrial gross primary productivity (GPP). Reducing emissions of ozone precursors by 50%, particularly in the road transportation and energy sectors, could increase GPP by 750 TgC yr–1.

    • Nadine Unger
    • Yiqi Zheng
    • Kandice L. Harper
    Letter
  • The rapid growth of climate change research presents challenges for IPCC assessments and their stated aim of being comprehensive, objective and transparent. Here the authors use topic modelling to map the climate change literature, and assess how well it is represented in IPCC reports.

    • Max W. Callaghan
    • Jan C. Minx
    • Piers M. Forster
    Letter
  • Arctic warming is attributed to GHGs and feedbacks, but the specific contribution of ozone-depleting substances (ODS)—also potent GHGs—has never been quantified. Here, model simulations suggest ODS contributed 0.8°C of Arctic warming and led to considerable sea-ice loss during the period 1955–2005. [This summary has been amended to reflect the addendum published 28 January 2020]

    • L. M. Polvani
    • M. Previdi
    • K. L. Smith
    Letter
  • 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
    Letter
  • Detection and attribution typically aims to find long-term climate signals in internal, often short-term variability. Here, common methods are extended to high-frequency temperature and humidity data, detecting instantaneous, global-scale climate change since 1999 for any year and 2012 for any day.

    • Sebastian Sippel
    • Nicolai Meinshausen
    • Reto Knutti
    Letter