# References ## GRLP papers The model, its correction, and its published extensions and applications. All are open access (CC-BY). Source-grounded notes on each — governing equations, parameters, and how they map to the code — are in `docs/literature/README.md` in the repository. - **Wickert, A. D. and Schildgen, T. F. (2019).** Long-profile evolution of transport-limited gravel-bed rivers. *Earth Surface Dynamics*, **7**, 17–43. [doi:10.5194/esurf-7-17-2019](https://doi.org/10.5194/esurf-7-17-2019). *The foundational paper — defines the model.* - **Wickert, A. D. and Schildgen, T. F. (2020).** Corrigendum to "Long-profile evolution of transport-limited gravel-bed rivers." *Earth Surface Dynamics*, **7**, 17–43. [doi:10.5194/esurf-7-17-2019-corrigendum](https://doi.org/10.5194/esurf-7-17-2019-corrigendum). *Removes the valley-width-derivative term; corrected code is GRLP v1.4.1.* - **McNab, F., Schildgen, T. F., Turowski, J. M., and Wickert, A. D. (2023).** Diverse responses of alluvial rivers to periodic environmental change. *Geophysical Research Letters*, **50**, e2023GL103075. [doi:10.1029/2023GL103075](https://doi.org/10.1029/2023GL103075). *Gain/lag linearization and equilibration timescale.* - **McNab, F., Schildgen, T. F., Turowski, J. M., and Wickert, A. D. (2025).** Influence of network geometry on long-term morphodynamics of alluvial rivers. *Earth Surface Dynamics*, **13**, 1059–1092. [doi:10.5194/esurf-13-1059-2025](https://doi.org/10.5194/esurf-13-1059-2025). *Extends GRLP to drainage networks.* - **Ruby, A., McNab, F., Schildgen, T. F., Wickert, A. D., and Fernandes, V. M. (2026).** How sediment supply, sea-level, and glacial isostatic oscillations drive alluvial river long-profile evolution and terrace formation. *AGU Advances*, **7**, e2025AV002035. [doi:10.1029/2025AV002035](https://doi.org/10.1029/2025AV002035). *Río Santa Cruz application; shelf-coupled base-level forcing.* ## Selected supporting literature Cited by the model derivation for its physics and closures. - **Parker, G. (1978).** Self-formed straight rivers with equilibrium banks and mobile bed. Part 2. The gravel river. *Journal of Fluid Mechanics*, **89**, 127–146. *Equilibrium-width (near-threshold) channel.* - **Wong, M. and Parker, G. (2006).** Reanalysis and correction of bed-load relation of Meyer-Peter and Müller using their own database. *Journal of Hydraulic Engineering*, **132**, 1159–1168. *Bed-load transport coefficient.* - **Meyer-Peter, E. and Müller, R. (1948).** Formulas for bed-load transport. *Proc. 2nd Meeting IAHR*, 39–64. - **Paola, C., Heller, P. L., and Angevine, C. L. (1992).** The large-scale dynamics of grain-size variation in alluvial basins, 1: Theory. *Basin Research*, **4**, 73–90. *Diffusive basin-filling; equilibration time.* - **Blom, A., Arkesteijn, L., Chavarrías, V., and Viparelli, E. (2017).** The equilibrium alluvial river under variable flow and its channel-forming discharge. *JGR Earth Surface*, **122**, 1924–1948. - **Shreve, R. L. (1966).** Statistical law of stream numbers. *Journal of Geology*, **74**, 17–37; and **Shreve, R. L. (1974).** Variation of mainstream length with basin area in river networks. *Water Resources Research*, **10**, 1167–1177. *Random network topology.* - **Hack, J. T. (1957).** Studies of longitudinal stream profiles in Virginia and Maryland. *USGS Professional Paper* 294-B. - **Kennett, J. P. (1982).** *Marine Geology.* Prentice-Hall. *Continental-shelf gradient used for shelf-coupled base level.*