This work explores the proposition that magnetic field resonances modu
late the transport of particle and magnetic flux in the earth's magnet
otail. Coordinated high- and low-altitude measurements during a substo
rm show periodic variations of magnetic field, plasma density and flow
bursts in the magnetotail with frequencies that correlate well with t
hose of magnetic field oscillations at geosynchronous altitude and pul
sations measured by ground-based stations. The pulsations' frequency i
s in the Pc 5 range. The example presented here occurred during the su
bstorm period of May 19-20, 1996, that was chosen as the first ISTP/GG
S campaign for the groundbased and theory investigations. There appear
s to be a resonance between modes sustained by the near-Earth magnetic
field and compressional and flapping pulsations that can be sustained
by the magnetotail.