In this article we address several criticisms of Petschek-type reconne
ction models which have recently been raised by Heikkila. We discuss f
eatures of the time-dependent Petschek-type models in the context of t
he solar wind-magnetosphere interaction, and point out that such model
s can incorporate and reproduce observed features at the magnetopause,
such as plasma jets and erosion of the current sheet. We argue that s
ome of Heikkila's criticisms can be attributed to weaknesses a in the
analysis due to incomplete experimental information, rather than to fl
aws in the concept of reconnection per se; in this category we include
the question of which instability lends to the localised breakup of t
he magnetopause current sheet. Other criticisms are based on an adhere
nce to steady-state models, and cannot be sustained within the extende
d time-dependent theory. We discuss, for example, how the time-depende
nt model can provide a consistent picture of how energy from the incom
ing solar wind is transferred and converted as it enters the magnetosp
here.