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Joe M. Osborne, James A. Screen, and Mat Collins

; Semenov and Latif 2015 ). But can this state dependence actually be a help rather than a hindrance? For example, we know that certain background ocean–atmosphere states, while not strictly predictable, vary on (multi-) decadal time scales. Two dominant patterns of ocean–atmosphere variability in the Northern Hemisphere midlatitudes are the Pacific decadal oscillation (PDO) and the Atlantic multidecadal oscillation (AMO). Recently, Screen and Francis (2016) showed that Arctic warming is enhanced for

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James Williams, Bruno Tremblay, Robert Newton, and Richard Allard

1.5 m was observed from repeated submarine transects between the coast of Alaska and the North Pole. The decrease in sea ice draft is attributed primarily to sea ice dynamics with thermodynamics playing a less influential role ( Tucker et al. 2001 ). The particular dynamical mechanisms leading to the reduction in thickness are an anomalously weak Beaufort Gyre, a broad Transpolar Drift Stream, and high export of multiyear ice (MYI) associated with a positive Arctic Oscillation (AO) index in the

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Yongjia Lu, Wenshou Tian, Jiankai Zhang, Jinlong Huang, Ruhua Zhang, Tao Wang, and Mian Xu

1. Introduction The Arctic Oscillation (AO), also called the northern annular mode (NAM), shows a deep and nearly barotropic structure, extending from the troposphere to the stratosphere, and is closely associated with the stratospheric polar vortex (e.g., Thompson and Wallace 1998 ; Baldwin and Dunkerton 1999 , 2001 ; Mukougawa and Hirooka 2004 ; Luo et al. 2012 ; Cheng and Tan 2019 ). Overall, there is a possibility that stratospheric NAM signals can extend downward into the troposphere

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Hengchun Ye, Eric J. Fetzer, Ali Behrangi, Sun Wong, Bjorn H. Lambrigtsen, Crysti Y. Wang, Judah Cohen, and Brandi L. Gamelin

circulation on Arctic climate variability, represented by the Arctic Oscillation (AO; Thompson and Wallace 1998 ), which describes the fluctuation of atmospheric pressure differences between the central Arctic and the two weaker centers at about 45°N over the Atlantic and Pacific basins. A regional study over western Siberia suggested a large influence of the AO on air temperature and a lesser influence on precipitation during winter ( Frey and Smith 2003 ). Thus, to understand the association between

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Mitchell Bushuk, Dimitrios Giannakis, and Andrew J. Majda

between the Bering Sea and Sea of Okhotsk ( Deser et al. 2000 ). Regression of sea level pressure (SLP) onto the corresponding principal component (PC) yields a spatial pattern that closely resembles the Arctic Oscillation (AO; Thompson and Wallace 1998 ), the leading pattern of SLP variability north of 20°N. Deser et al. (2000) observe a connection between the low-frequency (interannual to decadal) variability of the atmosphere and the low-frequency variability of sea ice. In particular, they find

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Masashi Kohma, Seiya Nishizawa, and Shigeo Yoden

maximum phase. Asymmetry of the time variations of SSW and VI events is characterized by the difference in the acceleration process of the stratospheric westerly wind: deceleration due to wave driving can be rapid, while acceleration associated with radiative cooling is generally more gradual. As for the slow variations in the Northern Hemisphere troposphere, the Arctic Oscillation (AO) is one of the well-known slow variations. The term was coined by Thompson and Wallace (1998) as the leading

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Thomas Jung and Michael Hilmer

1. Introduction The North Atlantic oscillation (NAO)—a phenomenon that is well known for many decades—is the dominant mode of North Atlantic atmospheric variability and describes the simultaneous strengthening and weakening of the Azores high and Icelandic low (e.g., Defant 1924 ; Walker 1924 ; Cayan 1992 ; Hurrell 1995 ). Recently, the link between the NAO and Arctic sea ice export through Fram Strait during wintertime has attracted increasing scientific interest (e.g., Kwok and Rothrock

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Hae-Jeong Kim and Joong-Bae Ahn

1. Introduction The Arctic Oscillation (AO), characterized by oscillation of atmospheric pressure between the Arctic and the midlatitudes, is one of the most dominant patterns of hemispheric scale variability in the Northern Hemisphere ( Thompson and Wallace 2000 ). Numerous studies have revealed the impacts of the AO on the boreal winter climate over the middle and high latitudes of North America, Europe, and East Asia (e.g., Higgins et al. 2002 ; Kolstad et al. 2010 ; Park et al. 2011

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Wolfgang Buermann, Benjamin Lintner, and Céline Bonfils

winter Arctic Oscillation. Using simple correlation analysis, the June precipitation index is observed to project similar spatial patterns onto the late winter/early spring surface temperature and soil moisture proxy fields as the boreal winter AO. We next describe the results of a technique—canonical correlation analysis (CCA)—that isolates coupled patterns of variability between two fields. The CCA framework represents a valuable tool for understanding how the development of anomalous, early

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Thomas L. Delworth and Keith W. Dixon

1. Introduction The dominant pattern of atmospheric variability during winter over the extratropical Northern Hemisphere (NH) is referred to as the Arctic oscillation (AO) ( Thompson and Wallace 1998 , 2000 ) and is characterized by a redistribution of mass between the polar latitudes and midlatitudes. A positive phase of the AO corresponds to reduced sea level pressure over the Arctic and increased westerly winds at midlatitudes. The largest changes in midlatitudes associated with the AO

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