All Stories

  1. Stronger Arctic amplification from anthropogenic aerosols than from greenhouse gases
  2. Robust Polar Amplification in Ice-Free Climates Relies on Ocean Heat Transport and Cloud Radiative Effects
  3. Comparing the impacts of ozone-depleting substances and carbon dioxide on Arctic sea ice loss
  4. The Montreal Protocol is delaying the occurrence of the first ice-free Arctic summer
  5. Large Contribution of Ozone‐Depleting Substances to Global and Arctic Warming in the Late 20th Century
  6. Spurious Climate Impacts in Coupled Sea Ice Loss Simulations
  7. Modeled Interannual Variability of Arctic Sea Ice Cover is within Observational Uncertainty
  8. Robust Anthropogenic Signal Identified in the Seasonal Cycle of Tropospheric Temperature
  9. Separating the Influences of Low-Latitude Warming and Sea Ice Loss on Northern Hemisphere Climate Change
  10. Stronger Arctic amplification from ozone-depleting substances than from carbon dioxide
  11. The Recent Emergence of Arctic Amplification
  12. Are Multi‐Decadal Fluctuations in Arctic and Antarctic Surface Temperatures a Forced Response to Anthropogenic Emissions or Part of Internal Climate Variability?
  13. Modeling the breakup of tabular icebergs
  14. Distinguishing the impacts of ozone and ozone-depleting substances on the recent increase in Antarctic surface mass balance
  15. Robust Arctic warming caused by projected Antarctic sea ice loss
  16. Tropical climate responses to projected Arctic and Antarctic sea-ice loss
  17. Substantial twentieth-century Arctic warming caused by ozone-depleting substances
  18. Nonuniform Contribution of Internal Variability to Recent Arctic Sea Ice Loss
  19. Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate
  20. The Role of Internal Variability in Twenty‐First‐Century Projections of the Seasonal Cycle of Northern Hemisphere Surface Temperature
  21. Contrasting the Antarctic and Arctic Atmospheric Responses to Projected Sea Ice Loss in the Late Twenty-First Century
  22. Robust response of the Amundsen Sea Low to stratospheric ozone depletion
  23. Troposphere-stratosphere dynamical coupling in the southern high latitudes and its linkage to the Amundsen Sea