Figure 1From: Decreased Sun-Earth energy-coupling efficiency starting from 2006 Decade averages of geomagnetic responses to the solar wind input. Hourly values of geomagnetic (a) Dst, (b) Kp, and (c) AL indices, and (d) probability of Kp ≥4 are averaged and plotted against the modified Akasofu’s epsilon \(\epsilon ' = (4\pi /\mu _{0})\cdot \text {V}_{\textit {SW}}\cdot \text {B}_{\text {tan}}^{2}\cdot \text {sin}^{4}(\theta _{c}/2) =(4\pi /\mu _{0}) \cdot V_{\textit {SW}}\cdot (\text {B}_{\text {tan}} -\text {B}_{Z})^{2}/4\). The total energy input is estimated by multiplying square of l 0= 7 to 10 R E , i.e., about 3 to 5 ×109 km 2. Data are divided into five 10-year periods as indicated by the legend (purple lines, blue lines, dark blue lines, orange circles, and red crosses, which approximately correspond to solar cycles #20 to 24, respectively). Green pluses near the horizontal axis denote the estimated statistical errors (\(\sigma /\sqrt {(n-1)}\) where n is the number of data point and σ is the standard deviation). Representative values for each ε ′ bin is obtained by logarithmic averaging. (e) Hourly values of geomagnetic Dst index are averaged and plotted against the solar wind proton density N P .Back to article page