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Troutman & Karlinger 1994
Troutman, B.M. and Karlinger, M.R. (1994). Inference for a generalized Gibbsian distribution on channel networks. Water Resources Research 30: doi: 10.1029/94WR00765. issn: 0043-1397.

We introduce a two-parameter (&bgr;0 and &bgr;1) Gibbsian probability model to characterize the spatial behavior of channel networks. This model is defined for trees draining basins on a square lattice. The probability of a tree s is proportional to exp <-&bgr;0H(s,&bgr;1)>, where H(s,&bgr;1) is taken to be a summation over lattice points v in the basin of A(v,s)&bgr;1, letting A(v,s) be the area upstream from (but not including) point v. Procedures are developed for estimating the parameters given an actual network obtained, for example, from digital elevation data and for using bootstrapping to obtain confidence intervals for these estimates. We also develop several goodness of fit tests for the model. These procedures are applied to a set of data for 50 subnetworks from Willow Creek in Montana. The estimation algorithm converged successfully for 34 of these subnetworks. For these 34 subnetworks the two-parameter model gives in most cases a fit significantly better than a one-parameter model (with &bgr;1 constrained to be 1) studied in a previous paper. There is still, however, statistically significant lack of fit for as many as 13 subnetworks (depending on which test is applied). The parameter &bgr;1 averages 0.75 for the 34 subnetworks. The function H(s,&bgr;1) in the Gibbsian model may be given a statistical mechanical interpretation of ''energy'' associated with a configuration s. Other researchers have employed a similar definition of energy expenditure in drainage systems but have given physical arguments that the exponent &bgr;1 should be 0.50. We finally discuss the idea of defining ''optimal channel networks'' as those which minimize free energy in the Gibbsian model; it is shown that minimization of energy (rather than free energy) as other researchers have proposed is valid only under the assumption of a ''low temperature'' (i.e., large &bgr;0) system. Our results indicate that this assumption would not be justified for Willow Creek. We devote some discussion to the discrepancies between our approach and results and those of other researchers.

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Abstract

Keywords
Hydrology, Networks
Journal
Water Resources Research
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American Geophysical Union
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