Topography z(x,y) or parameters describing a topographic surface; rate coefficients; switches for activating options and choosing between alternative transport/erosion formulas. Uses a formatted text file for input of parameters.
Other input format
Describe output parameters
Outputs include grids of surface elevation, drainage area, gradient, stratigraphy, drainage direction, Voronoi cell areas, sediment texture; data on mesh configuration; total landscape volume and change in volume at each storm (time step); list of storm durations, timing, and intensities.
Other output format
Pre-processing software needed?
Describe pre-processing software
Post-processing software needed?
Describe post-processing software
An extensive library of Matlab scripts provides visualization and post-processing capabilities. A few scripts also exist for IDL, and it is possible to process the output to generate lists of points for input to ArcGIS. In addition, a post-processing program called CHILD2VTK is available to convert output into VTK format for use in visualization programs such as ParaView.
Visualization software needed?
If above answer is yes
ESRI, IDL, Matlab
Other visualization software
Describe processes represented by the model
Basic processes include runoff generation, water erosion and sediment transport, and gravitational erosion and sediment transport. Depending on the application, the user can apply a vegetation-growth module, various tectonic functions, and other options.
Describe key physical parameters and equations
Too many to list here -- see Tucker et al. (2001a), the CHILD Users Guide, and other documents listed in the bibliography.
Describe length scale and resolution constraints
In principle, the model can address spatial scales ranging from gullies and small (~1km2) catchments to mountain ranges, as long as setup and parameters are chosen appropriately. Resolutions greater than about 10,000 nodes normally require significant computation time.
Describe time scale and resolution constraints
The steady flow assumption used by most (not all) hydrology sub-models restricts time scale to periods significantly longer than a single storm. The model has been mostly used to address time scales relevant to significant topographic evolution, though in the case of rapidly changing landscapes (e.g., gully networks) this can be as short as decades.
Describe any numerical limitations and issues
The fluvial sediment transport equations are quasi-diffusive and typically have orders of magnitude spatial variations in rate coefficient (reflecting differences in water discharge), which makes the system of equations stiff. Small time steps are typically required, which can lead to long compute times for large meshes.
Describe available calibration data sets
The model has been benchmarked against analytical solutions for simple cases, such as fluvial slope-area scaling and parabolic to parabolic-planar hillslope form under uniform erosion, materials, and climate. Testing and calibration of some of the individual components (e.g., linear and nonlinear soil creep, stream-power fluvial erosion law, etc.) have been reported in the literature (for a review, see Tucker and Hancock, 2010). Testing of the full coupled model using natural experiments (Tucker, 2009) is ongoing.
Upload calibration data sets if available:
Describe available test data sets
Upload test data sets if available:
Describe ideal data for testing
See Tucker (2009)
Do you have current or future plans for collaborating with other researchers?
Channel-Hillslope Integrated Landscape Development (CHILD) Model
CHILD was originally developed in 1997 by Nicole Gasparini, Stephen Lancaster, and Greg Tucker, in a research group directed by Rafael Bras at the Department of Civil and Environmental Engineering at MIT. Development and use of CHILD continues, with contributions by (among others) Mikael Attal (Edinburgh), Patrick Bogaart (Wageningen), Quintijn Clevis (Oxford), Daniel Collins (Wisconsin), Arnaud Desitter (Oxford), Homero Flores (MIT), Erkan Istanbulluoglu (Nebraska), Scott Miller (Syracuse), Vanessa Teles (IFP), and the original developers.
Fault block uplift and subsidence
Simulation of a pair of normal-fault blocks separated by a vertical fault. The lower left edge is fixed through time, and represents a shallow shelf just below sea level. The inner block of the landscape rises at a steady rate, while the outer block subsides. Initially, the relief and erosion rate are small, and the subsiding basin is underfilled. Notice the progradation of a fan-delta complex. As relief and sediment flux increase, the fan deltas reach the shallow shelf and the basin becomes filled (or "over-filled" as they say, meaning that there is more than enough sediment to keep filling the basin as it continues to subside).
Evolution of river valley landscape, stratigraphy, and geoarchaeology
Scenario 1: Steady Aggradation
Scenario 2: Pomme de Terre River incision/aggradation history
Scenario 3: incision/aggradation history based on oxygen isotope curve
Overview and general
Tucker, G.E., Gasparini, N.M, Bras, R.L., and Lancaster, S.L., 1999. A 3D Computer Simulation Model of Drainage Basin and Floodplain Evolution: Theory and Applications, Technical report prepared for U.S. Army Corps of Engineers Construction Engineering Research Laboratory. (View/edit entry)
Tucker, G.E., Lancaster, S.T., Gasparini, N.M., and Bras, R.L., 2001. The Channel-Hillslope Integrated Landscape Development (CHILD) Model, in Landscape Erosion and Evolution Modeling, edited by R.S. Harmon and W.W. Doe III, Kluwer Academic/Plenum Publishers, pp. 349-388. (View/edit entry)
Tucker, G.E., Lancaster, S.T., Gasparini, N.M., Bras, R.L., and Rybarczyk, S.M., 2001. An Object-Oriented Framework for Hydrologic and Geomorphic Modeling Using Triangulated Irregular Networks, Computers and Geosciences, 27(8), pp. 959-973., 10.1016/S0098-3004(00)00134-5 (View/edit entry)
Attal, M., Cowie, P.A., Whittaker, A.C., Hobley, D., Tucker, G.E., and Roberts, G.P. (2011) Testing fluvial erosion models using the transient response of bedrock rivers to tectonic forcing in the Apennines, Italy, Journal of Geophysical Research, 116, F02005., 10.1029/2010JF001875 (View/edit entry)
Attal, M., Tucker, G.E., Whittaker, A.C., Cowie, P.A., and Roberts, G.P. (2008) Modeling fluvial incision and transient landscape evolution: Influence of dynamic channel adjustment. Journal of Geophysical Research - Earth Surface, v. 113, F03013, 10.1029/2007JF000893 (View/edit entry)
Bogaart, P.W., Tucker, G.E., and de Vries, J.J. (2003) Channel network morphology and sediment dynamics under alternating periglacial and temperate regimes: A numerical simulation study: Geomorphology, vol. 54, no. 3/4, p. 257-277., 10.1016/S0169-555X(02)00360-4 (View/edit entry)
Bras, R.L., Tucker, G.E., and Teles, V.T. (2003) Six myths about mathematical modeling in geomorphology: in Prediction in Geomorphology, edited by P. Wilcock and R. Iverson, American Geophysical Union, pp. 63-79. (View/edit entry)
Clevis, Q., Tucker, G.E., Lock, G., Lancaster, S.T., Gasparini, N.M., and Desitter, A. (2006) A simple algorithm for the mapping of TIN data onto a static grid: applied to the stratigraphic simulation of river meander deposits Computers and Geosciences, v. 32, p. 749-766., 10.1016/j.cageo.2005.05.012 (View/edit entry)
Clevis, Q., Tucker, G.E., Lock, G., Lancaster, S.T., Gasparini, N.M., Desitter, A., and Bras, R.L. (2006) Geoarchaeological simulation of meandering river deposits and settlement distributions; a three-dimensional approach. Geoarchaeology, v. 21, no. 8, p. 843-874., 10.1002/gea.20142 (View/edit entry)
Collins, D., Bras, R., and Tucker, G.E. (2004) Modeling the effects of vegetation-erosion coupling on landscape evolution: Journal of Geophysical Research - Earth Surface, v. 109, no. F3, F03004., 10.1029/2003JF000028 (View/edit entry)
Crosby, B.T., Whipple, K.X., Gasparini, N.M., and Wobus, C.W. (2007) Formation of Fluvial Hanging Valleys: Theory and Simulation, Journal of Geophysical Research, 112., 10.1029/2006JF000566 (View/edit entry)
Fleurant, C., Tucker, G.E., and Viles, H.A. (2008) Modelling cockpit karst landforms. In: Gallagher, K., Jones, S.J., and Wainwright, J., eds., Landscape Evolution: Denudation, Climate and Tectonics over Different Time and Space Scales. Geological Society of London Special Publication 296. (View/edit entry)
Flores-Cervantes, J.H., Istanbulluoglu, E., and R.L. Bras (2006) Development of gullies on the landscape: A model of headcut retreat resulting from plunge pool erosion, Journal of Geophysical Research - Earth Surface, 111, Issue F1., 10.1029/2004JF000226 (View/edit entry)
Gasparini, N. M., K. X. Whipple, and R. L. Bras (2007), Predictions of steady state and transient landscape morphology using sediment-flux-dependent river incision models, Journal of Geophysical Research, 112., 10.1029/2006JF000567 (View/edit entry)
Gasparini, N.M., Bras, R.L., and Tucker, G.E. (2008) Numerical predictions of the sensitivity of grain size and channel slope to an increase in precipitation. In: Rice, S.P., Roy, A.G., and Rhoads, B.L., eds., River Confluences, Tributaries and the Fluvial Network, John Wiley & Sons. (View/edit entry)
Gasparini, N.M., Bras, R.L., and Whipple, K.X. (2006) Numerical modeling of non-steady-state river profile evolution using a sediment-flux-dependent incision model, in Tectonics, climate and landscape evolution, S. Willett, N. Hovius, M. Brandon & D. Fisher, eds., GSA Special Paper 398, Penrose Conference Series, Geological Society of America, pp 127-141. (View/edit entry)
Gasparini, N.M., Tucker, G.E., and Bras, R.L. (2004) Network-scale dynamics of grain-size sorting: Implications for downstream fining, stream-profile concavity, and drainage basin morphology: Earth Surface Processes and Landforms, 29(4), 401-422., 10.1002/esp.1031 (View/edit entry)
Istanbulluoglu, E., Bras, R.L., Flores-Cervantes, H., and Tucker, G.E. (2005) Implications of bank failures and fluvial erosion for gully development: Field observations and modeling. Journal of Geophysical Research - Earth Surface, v. 110, no. F1, F01014., 10.1029/2004JF000145 (View/edit entry)
Lancaster, S.T., S.K. Hayes, and G.E. Grant, 2003. Effects of wood on debris flow runout in small mountain watersheds, Water Resources Research, 39(6), 1168., 10.1029/2001WR001227 (View/edit entry)
Lancaster, S.T., S.K. Hayes, and G.E. Grant (2001) Modeling sediment and wood storage and dynamics in small mountainous watersheds, in Geomorphic Processes and Riverine Habitat, J.M. Dorava, D.R. Montgomery, B.B. Palcsak, and F.A. Fitzpatrick (eds.), pp. 85-102, American Geophysical Union, Washington. Reprint (View/edit entry)
Solyom, P., and Tucker, G.E. (2004) The effect of limited storm duration on landscape evolution, drainage basin geometry and hydrograph shapes: Journal of Geophysical Research - Earth Surface, v. 109, F03012., 10.1029/2003JF00032 (View/edit entry)
Tucker, G.E. (2004) Drainage basin sensitivity to tectonic and climatic forcing: implications of a stochastic model for the role of entrainment and erosion thresholds. Earth Surface Processes and Landforms, 29, 185-205., 10.1002/esp.1020 (View/edit entry)
Tucker, G.E., and Bras, R.L. (2000) A Stochastic Approach to Modeling the Role of Rainfall Variability in Drainage Basin Evolution, Water Resources Research, 36(7), pp. 1953-1964., 10.1029/2000WR900065 (View/edit entry)
Related theory and data
Baldwin, J.A., Whipple, K.X., and Tucker, G.E. (2003) Implications of the shear-stress river incision model for the timescale of post-orogenic decay of topography: Journal of Geophysical Research. Vol. 108, No. B3., 10.1029/2001JB000550 (View/edit entry)
Lancaster, S.T., and Bras, R.L., (2002) A simple model of river meandering and its comparison to natural channels, Hydrological Processes, 16, 1-26., 10.1002/hyp.273 (View/edit entry)
Snyder, N.P., Whipple, K.X., Tucker, G.E., and Merritts, D.J. (2003) The importance of a stochastic distribution of floods and erosion thresholds in the bedrock river incision problem: Journal of Geophysical Research, vol. 108, no. B2., 10.1029/2001JB001655 (View/edit entry)
Tucker, G.E., and Whipple, K.X. (2002) Topographic outcomes predicted by stream erosion models: Sensitivity analysis and intermodel comparison, Journal of Geophysical Research, v. 107, no. B9, 2179., 10.1029/2001JB000162 (View/edit entry)
Whipple, K.X., and Tucker, G.E. (1999) Dynamics of the Stream Power River Incision Model: Implications for Height Limits of Mountain Ranges, Landscape Response Timescales and Research Needs: Journal of Geophysical Research, v. 104, p. 17,661-17,674., 10.1029/1999JB900120 (View/edit entry)
Whipple, K.X., and Tucker, G.E. (2002) Implications of sediment-flux dependent river incision models for landscape evolution: Journal of Geophysical Research, v. 107, no. B2., 10.1029/2000JB000044 (View/edit entry)
Issues and Announcements
July 6, 2010
Version R10.7 has been released! Included with this version is a set of hands-on, tutorial-style exercises that were "beta tested" at the "Summer School and Workshop on Modelling Surface Processes on Geological Timescales" in Davos, Switzerland, in June 2010. Space-time varying uplift fields can now be specified -- see the Users Guide for details.
January 29, 2009
Philippe Steer reports:
I am Philippe Steer, PhD student at Geosciences Montpellier in France.
I have encountered an error when trying to compile child:
"INT_MAX" was not declared in this scope /Code/tMesh/tMesh.cpp
Solution to this problem:
add "#include <limits.h>" at the begining of tMesh.cpp
OS: linux- Opensuse11
Computer: Dell Precision T 7400, Intel Xeon, 64 bits
compiling with gcc 4.3
I hope it will help other newbies (as I am!) in C,