Articles | Volume 24, issue 3
https://doi.org/10.5194/npg-24-569-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.Quantifying the changes of soil surface microroughness due to rainfall impact on a smooth surface
Related subject area
Subject: Scaling, multifractals, turbulence, complex systems, self-organized criticality | Topic: Climate, atmosphere, ocean, hydrology, cryosphere, biosphere
Brief communication: Climate science as a social process – history, climatic determinism, Mertonian norms and post-normality
Characteristics of intrinsic non-stationarity and its effect on eddy-covariance measurements of CO2 fluxes
Fractional relaxation noises, motions and the fractional energy balance equation
How many modes are needed to predict climate bifurcations? Lessons from an experiment
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Allmaras, R. R., Burwell, R. E., Larson, W. E., and Holt, R. F.: Total porosity and random roughness of the interrow zone as influenced by tillage, USDA Conservation Re. Rep. 7, USDA, Washington, D.C., 16 pp., 1966.
Bertuzzi, P., Rauws, G., and Courault, D.: Testing roughness indices to estimate soil surface roughness changes due to simulated rainfall, Soil Till. Res., 17, 87–99, https://doi.org/10.1016/0167-1987(90)90008-2, 1990.
Burrough, P. A.: Multiscale sources of spatial variation in soil. I. The application of fractal concepts to nested levels of soil variation, J. Soil Sci., 34, 577–597, https://doi.org/10.1111/j.1365-2389.1983.tb01057.x, 1983.