A generalization of local transit-time dissipation theory to coherent elect
rostatic wave packets with nonzero mean wave number is presented. The conne
ction between Landau damping and transit time damping is derived in a conci
se, mathematically rigorous manner, settling a longstanding controversy. It
is shown that transit time dissipation involves both Landau-type resonant
damping and nonresonant damping. For small wave packets with nonzero mean w
ave number or asymmetric incident particle distributions, the nonresonant d
amping can dominate over Landaudamping. In the opposite extreme of infinite
ly large, constant-amplitude wave packets, the nonresonant part of transit
time dissipation vanishes, and only Landau damping remains. All the analyti
cal results presented are verified independently by numerical test-particle
calculations. (C) 1999 American Institute of Physics. [S1070-664X(99)00709
-0].