作者: Marika M. Holland , Julienne Stroeve
DOI: 10.1029/2011GL049303
关键词: Cryosphere 、 National Snow and Ice Data Center 、 Arctic ice pack 、 Arctic sea ice decline 、 Sea ice 、 Climatology 、 Arctic 、 Environmental science 、 Effects of global warming 、 Arctic ecology
摘要: [1] Seasonal predictions of Arctic sea ice conditions often rely on statistical relationships a set predictors that have shown skill for historical conditions. However, with rapid changes occurring in the climate, it is unclear whether these will remain valid. Here, preindustrial control, present-day and 20th–21st century climate model integrations are used to assess end-of-summer extent under various changing Of importance future forecasting systems, we find variance September anomalies explained by winter-spring predictors, such as area basin thin cover, increases during transition seasonally ice-covered Arctic. In contrast, summer atmospheric circulation variability plays decreasingly important role explaining cover anomalies. These primarily related climate-dependent location