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Rainfall-induced runoff and subsurface stormflow at the hillslope scale. / Rumynin, Vyacheslav G.

Theory and Applications of Transport in Porous Media. Springer Nature, 2015. p. 51-81 (Theory and Applications of Transport in Porous Media; Vol. 26).

Research output: Chapter in Book/Report/Conference proceeding › Chapter › Research › peer-review

Harvard

Rumynin, VG 2015, Rainfall-induced runoff and subsurface stormflow at the hillslope scale. in Theory and Applications of Transport in Porous Media. Theory and Applications of Transport in Porous Media, vol. 26, Springer Nature, pp. 51-81. https://doi.org/10.1007/978-3-319-21801-4_2

APA

Rumynin, V. G. (2015). Rainfall-induced runoff and subsurface stormflow at the hillslope scale. In Theory and Applications of Transport in Porous Media (pp. 51-81). (Theory and Applications of Transport in Porous Media; Vol. 26). Springer Nature. https://doi.org/10.1007/978-3-319-21801-4_2

Vancouver

Rumynin VG. Rainfall-induced runoff and subsurface stormflow at the hillslope scale. In Theory and Applications of Transport in Porous Media. Springer Nature. 2015. p. 51-81. (Theory and Applications of Transport in Porous Media). https://doi.org/10.1007/978-3-319-21801-4_2

Author

Rumynin, Vyacheslav G. / Rainfall-induced runoff and subsurface stormflow at the hillslope scale. Theory and Applications of Transport in Porous Media. Springer Nature, 2015. pp. 51-81 (Theory and Applications of Transport in Porous Media).

BibTeX

@inbook{422fe303442f485189ab911e8b71ad75,
title = "Rainfall-induced runoff and subsurface stormflow at the hillslope scale",
abstract = "Surface runoff (or overland flow), which is generated by the precipitation that falls within a drainage area (catchment, watershed), is governed by several factors and processes, including rainfall rate and duration, the characteristics of infiltration (capillary imbibition and gravity-driven) and the temperature regime of soil, landscape surface characteristics, vegetation type, and some others. Hillslopes are regarded as a basic element of catchments, therefore the mathematical and physical description of the hydrological processes that occur at the hillslope scale is the first step to designing more general hydrological models describing hydrological response at catchment/watershed scale.",
author = "Rumynin, {Vyacheslav G.}",
year = "2015",
month = jan,
day = "1",
doi = "10.1007/978-3-319-21801-4_2",
language = "English",
series = "Theory and Applications of Transport in Porous Media",
publisher = "Springer Nature",
pages = "51--81",
booktitle = "Theory and Applications of Transport in Porous Media",
address = "Germany",

}

RIS

TY - CHAP

T1 - Rainfall-induced runoff and subsurface stormflow at the hillslope scale

AU - Rumynin, Vyacheslav G.

PY - 2015/1/1

Y1 - 2015/1/1

N2 - Surface runoff (or overland flow), which is generated by the precipitation that falls within a drainage area (catchment, watershed), is governed by several factors and processes, including rainfall rate and duration, the characteristics of infiltration (capillary imbibition and gravity-driven) and the temperature regime of soil, landscape surface characteristics, vegetation type, and some others. Hillslopes are regarded as a basic element of catchments, therefore the mathematical and physical description of the hydrological processes that occur at the hillslope scale is the first step to designing more general hydrological models describing hydrological response at catchment/watershed scale.

AB - Surface runoff (or overland flow), which is generated by the precipitation that falls within a drainage area (catchment, watershed), is governed by several factors and processes, including rainfall rate and duration, the characteristics of infiltration (capillary imbibition and gravity-driven) and the temperature regime of soil, landscape surface characteristics, vegetation type, and some others. Hillslopes are regarded as a basic element of catchments, therefore the mathematical and physical description of the hydrological processes that occur at the hillslope scale is the first step to designing more general hydrological models describing hydrological response at catchment/watershed scale.

UR - http://www.scopus.com/inward/record.url?scp=85007246322&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-21801-4_2

DO - 10.1007/978-3-319-21801-4_2

M3 - Chapter

AN - SCOPUS:85007246322

T3 - Theory and Applications of Transport in Porous Media

SP - 51

EP - 81

BT - Theory and Applications of Transport in Porous Media

PB - Springer Nature

ER -

ID: 42323266