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James H. Ruppert Jr., Xingchao Chen, and Fuqing Zhang

Plateau during the warm season ( Wang et al. 2004 ; Bao et al. 2011 ), and likewise for many other continental regions downstream of mountain ranges (e.g., Laing et al. 2008 ). Many studies have argued that a key driver of this phenomenon is the mountain–plains solenoidal circulation ( Carbone and Tuttle 2008 ; Huang et al. 2010 ; Sun and Zhang 2012 ; Bao and Zhang 2013 ), and the nocturnal low-level jet in the case of the United States ( Stensrud 1996 ; Trier et al. 2014 ). These mechanisms

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