Magnetosphere-ionosphere dynamics are determined by the solar wind and interplanetary magnetic field (IMF) forcing and the system's response to that forcing. Arguably, the most important quantity in the solar wind forcing is the rate of opening of magnetic flux, or the reconnetion rate, on the dayside magnetopause. For several decades, coupling functions have been used to quantify the upstream solar wind forcing. Typically, coupling functions are proportional to the product 𝐴𝐴 𝐴𝐴 𝛼𝛼 𝐵𝐵 𝛽𝛽 𝑇𝑇 sin 𝛾𝛾 (𝜃𝜃∕2) , where 𝐴𝐴 𝐴𝐴 is solar wind speed,is the IMF clock angle in the Geocentric Solar Magnetospheric (GSM) coordinate system. The exponents 𝐴𝐴 𝐴𝐴 , 𝐴𝐴 𝐴𝐴 and 𝐴𝐴 𝐴𝐴 are empirically determined, for example, by maximizing correlation between the coupling function and geomagnetic indices (Lockwood, Bently et al., 2019;Newell et al., 2007;Vasyliunas et al., 1982). Because geomagnetic disturbances on the ground are also much affected by how the magnetosphere and ionosphere responds to the upstream forcing, the interpretation of these coupling functions in terms of a dayside coupling efficiency is challenging. The coupling function presented by Milan et al. (2012) is slightly different in this regard, as it was specifically designed to predict the dayside reconnection rate in units of Weber per second, or Volt:where 𝐴𝐴 Λ = 3.3 ⋅ 10 5 m 2/3 s 1/3 . The coupling function coefficients 𝐴𝐴 𝐴𝐴𝐴 𝐴𝐴𝐴 𝐴𝐴 were in this case estimated by fitting the expansion of the open magnetic flux inside the polar cap as monitored by global Far Ultraviolet imaging of the aurora during intervals when tail reconnection was assumed to be negligible.