Heterogeneity, or messiness, is a broadly desirable characteristic of
river corridors and an indicator of many of the geomorphic processes
that sustain fluvial ecosystems. However, quantifying geomorphic
heterogeneity is complicated by a lack of consistent metrics, methods of
dividing up the river corridor into the patches that form the basis for
those metrics, and guidance on interpreting metrics. Drawing from both
geomorphic and landscape ecology concepts, we offer ideas and guidance
intended to help investigators, from researchers to restoration
practitioners, more effectively and reliably use heterogeneity to
describe river corridor processes and characteristics. We define
geomorphic heterogeneity as having both a spatial and temporal
dimension. Spatially, heterogeneity can be described by diversity, or
the evenness and richness of geomorphic units, and spatial
configuration, or the arrangement of geomorphic units relative to one
another. Temporally, heterogeneity can be described by turnover rate, or
the rate of change of geomorphic units. Interpretation of heterogeneity
metrics depends integrally on the definition of the geomorphic unit
schema on which metrics are based. Contextual information, such as
measurements of process space, disturbance frequency, and geomorphic
trajectory, can also be key to using effective measurements of
heterogeneity. Geomorphic applications of heterogeneity require
carefully defined geomorphic unit schemas that reflect processes and
characteristics of interest, robust metrics of heterogeneity whose
meaning is appropriate to the question at hand, and interpretation of
those metrics based on the context of expected geomorphic processes and
the frequency of disturbance.