  Extreme space weather events occur during intervals of strong solar wind
electric fields. Curiously during these intervals, their impact on measures of
the Earth's response, like the polar cap index, is not as high as expected.
Theorists have put forward a host of explanations for this saturation effect,
but there is no consensus. Here we show that the saturation is merely a
perception created by uncertainty in the solar wind measurements, especially in
the measurement times. Correcting for the uncertainty reveals that extreme
space weather events elicit a ~300% larger impact than previously thought.
Furthermore, they point to a surprisingly general result relevant to any
correlation study: uncertainty in the measurement time can cause a system's
linear response to be perceived as non-linear.
