Plasmoids in the Earth's magnetotail were studied statistically, using
low energy particle (LEP) and magnetic field (MGF) data from the Geot
ail spacecraft. Their evolution along the tail axis from X-GSM' = -16
to -210 R-E was investigated with 824 plasmoid events. Their dependenc
e on Y-GSM' was studied as well to derive the three-dimensional struct
ure of the plasmoids. (The coordinates are aberrated to remove the ave
rage effects of the orbital velocity of the Earth about the Sun.) We d
efined a plasmoid as a structure with rotating magnetic fields and enh
anced total pressure. In the near tail (X-GSM' greater than or equal t
o -50 R-E), there was a tendency for the plasmoids to be observed in t
he premidnight sector around the tail axis (\Y-GSM' - 3\ less than or
equal to 10 R-E), while they were observed widely (\Y-GSM'\ less than
or equal to 20 R-E) in the middle tail (-50 > X-GSM' greater than or e
qual to -100 R-E) and in the distant tail (-100 R-E > X-GSM'). The pla
smoids expanded in the +/-Y-GSM' direction with typical velocities of
+/-130 +/- 100 km/s in the near tail. This strongly supports the view
that plasmoids are initially formed at the near-Earth neutral line whi
ch has a limited extent in the Y-GSM' direction. The plasmoids acceler
ated in the downtail direction from 400 +/- 200 km/s to 700 +/- 300 km
/s from the near to the middle tail. Then, it is suggested that they d
ecelerated to 600 +/- 200 km/s as they traveled to the distant tail. T
he ion temperature inside plasmoids was 4.5 +/- 2 keV in the near and
middle tail, and then rapidly decreased to 2 +/- 1 keV from the middle
to the distant tail region. The ion temperature in the distant tail w
as 2 times higher than the values deduced previously. Typical plasmoid
dimensions were estimated to be 10 R-E (length) x 40 R-E (width) x 10
R-E (height) in the middle and distant tail. The energy carried by ea
ch plasmoid was similar to 2 x 10(14) J in the middle tail, half of wh
ich was lost from the middle to the distant tail. Inside plasmoids,the
thermal energy flux exceeded the bulk energy flux and Poynting flux.
The energy released tailward in the course of a substorm was estimated
to be roughly 10(15) J.