Extended Data Fig. 8: Trend differences arising from trend calculation methods: the role of ensemble size.
From: Emergence of Southern Hemisphere stratospheric circulation changes in response to ozone recovery
SH ND zonal-mean temperature trend shown in each panel is the difference between using the linear trend (for example, as in Extended Data Fig. 6a) and differencing the climatologies (for example, as in Extended Data Fig. 6b) for the average of 1 ≤ n ≤ 9 ensemble members (the difference for n = 10 is shown in Extended Data Fig. 6c).
