The interaction between solar wind, interplanetary magnetic field (IMF) and the Earth's magnetic field is dominated by the north-south (B z ) component of IMF, which is the most important driver of dayside reconnection (Dungey, 1961), and thus the energy input into the magnetosphere. The dawn-dusk (B y ) component of IMF is also known play an important role, leading, for example, to a B y -dependence of the ionospheric convection patterns (