The edges dissolution approximation method is described in Carnegie et al.
This approximation requires that the dissolution coefficients are known, that
the formation model is being fit to cross-sectional data conditional on those
dissolution coefficients, and that the terms in the dissolution model are a
subset of those in the formation model. Under certain additional conditions,
the formation coefficients of a STERGM model are approximately equal to the
coefficients of that same model fit to the observed cross-sectional data as
an ERGM, minus the corresponding coefficients in the dissolution model. The
approximation thus estimates this ERGM (which is typically much faster than
estimating a STERGM) and subtracts the dissolution coefficients.
The conditions under which this approximation best hold are when there are
few relational changes from one time step to another; i.e. when either
average relational durations are long, or density is low, or both.
Conveniently, these are the same conditions under which STERGM estimation is
slowest. Note that the same approximation is also used to obtain starting
values for the STERGM estimate when the latter is being conducted. The
estimation does not allow for calculation of standard errors, p-values, or
likelihood for the formation model; thus, this approach is of most use when
the main goal of estimation is to drive dynamic network simulations rather
than to conduct inference on the formation model. The user is strongly
encouraged to examine the behavior of the resulting simulations to confirm
that the approximation is adequate for their purposes. For an example, see
the vignette for the package tergm
.
It has recently been found that subtracting a modified version of the
dissolution coefficients from the formation coefficients provides a more
principled approximation, and this is now the form of the approximation
applied by netest
. (The modified values subtracted from the formation
coefficients are equivalent to the (crude) dissolution coefficients with
their target durations increased by 1.)