A record-breaking low ice cover over the Great Lakes during winter 2011/2012: combined effects of a strong positive NAO and La Nina

作者：Bai Xuezhi; Wang Jia^*; Austin Jay; Schwab David J; Assel Raymond; Clites Anne; Bratton John F; Colton Marie; Lenters John; Lofgren Brent; Wohlleben Trudy; Helfrich Sean; Vanderploeg Henry; Luo Lin; Leshkevich George

来源：Climate Dynamics, 2015, 44(5-6): 1187-1213.

DOI：10.1007/s00382-014-2225-2

• Great Lakes ice cover
• Ice growth
• Surface heat budget
• NAO
• La Nina
• ENSO

A record-breaking low ice cover occurred in the North American Great Lakes during winter 2011/2012, in conjunction with a strong positive Arctic Oscillation/ North Atlantic Oscillation (+AO/NAO) and a La Nina event. Large-scale atmosphere circulation in the Pacific/ North America (PNA) region reflected a combined signal of La Nina and +NAO. Surface heat flux analysis shows that sensible heat flux contributed most to the net surface heat flux anomaly. Surface air temperature is the dominant factor governing the interannual variability of Great Lakes ice cover. Neither La Nina nor +NAO alone can be responsible for the extreme warmth; the typical mid-latitude response to La Nina events is a negative PNA pattern, which does not have a significant impact on Great Lakes winter climate; the positive phase of NAO is usually associated with moderate warming. When the two occurred simultaneously, the combined effects of La Nina and +NAO resulted in a negative East Pacific pattern with a negative center over Alaska/Western Canada, a positive center in the eastern North Pacific (north of Hawaii), and an enhanced positive center over the eastern and southern United States. The overall pattern prohibited the movement of the Arctic air mass into mid-latitudes and enhanced southerly flow and warm advection from the Gulf of Mexico over the eastern United States and Great Lakes region, leading to the record-breaking low ice cover. It is another climatic pattern that can induce extreme warming in the Great Lakes region in addition to strong El Nino events. A very similar event occurred in the winter of 1999/2000. This extreme warm winter and spring in 2012 had significant impacts on the physical environment, as well as counterintuitive effects on phytoplankton abundance.

• 出版日期2015-3