Land Use‐Dependent Preferential Flow Paths Affect Hydrological Response of Steep Tropical Lowland Catchments With Saprolitic Soils

Author:

Cheng Yanyan12,Ogden Fred L.134,Zhu Jianting1ORCID,Bretfeld Mario4ORCID

Affiliation:

1. Department of Civil and Architectural Engineering University of Wyoming Laramie WY USA

2. Now at Atmospheric Sciences and Global Change Division Pacific Northwest National Laboratory Richland WA USA

3. U.S. National Water Center NOAA/NWS/Office of Water Prediction Tuscaloosa AL USA

4. Smithsonian Tropical Research Institute Ancón Panama

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference68 articles.

1. Arcement G. J. &Schneider V. R.(1989).Guide for selecting Manning's roughness coefficients for natural channels and flood plains United States Geological Survey Water‐Supply Paper 2339 (pp.1–38). Denver CO.

2. Proxy global assessment of land degradation

3. The impact of forest regeneration on streamflow in 12 mesoscale humid tropical catchments

4. Global patterns in base flow index and recession based on streamflow observations from 3394 catchments

5. Bernstein L. BoschP. CanzianiO. ChenZ. ChristR. &RiahiK.(2008).IPCC 2007: Climate change 2007—Synthesis report. IPCC.

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