“…Not all active regions that are productive at other wavelengths produce noise storms, and the non-radio signatures are often scant (Willson, 2005;Iwai et al, 2012;Li et al, 2017), unlike Type II and III bursts, which have obvious associations with CMEs and flares (Cairns et al, 2003;Reid and Ratcliffe, 2014). There is general agreement that both the burst and continuum components of noise storms are produced by plasma emission, largely due to their often high circular polarizations (Aschwanden, 1986;Mugundhan et al, 2018), but what accelerates the electrons is still debated. Small-scale reconnection events (Benz and Wentzel, 1981) or weak shocks associated with upwardpropagating waves (Spicer, Benz, and Huba, 1982) are the two leading ideas, and recent work has favored persistent interchange reconnection between open and closed fields at the boundaries of active regions (Del Zanna et al, 2011;Mandrini et al, 2015) or reconnection driven by moving magnetic features (Bentley et al, 2000;Li et al, 2017).…”