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Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic

Research output: Contribution to Journal/Magazine › Journal article › peer-review

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Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic. / Kulasova, Alena; Beven, Keith J.; Blazkova, Sarka D. et al.
In: Journal of Hydrology and Hydromechanics, Vol. 62, No. 2, 06.2014, p. 160-168.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Kulasova, A, Beven, KJ, Blazkova, SD, Rezacova, D & Cajthaml, J 2014, 'Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic', Journal of Hydrology and Hydromechanics, vol. 62, no. 2, pp. 160-168. https://doi.org/10.2478/johh-2014-0002

APA

Kulasova, A., Beven, K. J., Blazkova, S. D., Rezacova, D., & Cajthaml, J. (2014). Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic. Journal of Hydrology and Hydromechanics, 62(2), 160-168. https://doi.org/10.2478/johh-2014-0002

Vancouver

Kulasova A, Beven KJ, Blazkova SD, Rezacova D, Cajthaml J. Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic. Journal of Hydrology and Hydromechanics. 2014 Jun;62(2):160-168. doi: 10.2478/johh-2014-0002

Author

Kulasova, Alena ; Beven, Keith J. ; Blazkova, Sarka D. et al. / Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic. In: Journal of Hydrology and Hydromechanics. 2014 ; Vol. 62, No. 2. pp. 160-168.

Bibtex

@article{072e8669512f41c58600a6f6d6aa75f3,
title = "Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic",
abstract = "Understanding and modelling the processes of flood runoff generation is still a challenge in catchment hydrology. In particular, there are issues about how best to represent the effects of the antecedent state of saturation of a catchment on runoff formation and flood hydrographs. This paper reports on the experience of mapping saturated areas using measured water table by piezometers and more qualitative assessments of the state of the moisture at soil surface or immediately under it to provide information that can usefully condition model predictions. Vegetation patterns can also provide useful indicators of runoff source areas, but integrated over much longer periods of time. In this way, it might be more likely that models will get the right predictions for the right reasons.",
keywords = "Mapping variable source areas, Boot method, Piezometers, Vegetation mapping., RESEARCH CATCHMENT VALLCEBRE, SOIL-MOISTURE PATTERNS, PLYNLIMON CATCHMENTS, EASTERN PYRENEES, MID-WALES, WATER, RUNOFF, TOPMODEL, FLOW, HILLSLOPE",
author = "Alena Kulasova and Beven, {Keith J.} and Blazkova, {Sarka D.} and Daniela Rezacova and Jiri Cajthaml",
note = "This content is open access. (CC BY-NC-ND 3.0)",
year = "2014",
month = jun,
doi = "10.2478/johh-2014-0002",
language = "English",
volume = "62",
pages = "160--168",
journal = "Journal of Hydrology and Hydromechanics",
publisher = "Slovak Academy of Sciences",
number = "2",

}

RIS

TY - JOUR

T1 - Comparison of saturated areas mapping methods in the Jizera Mountains, Czech Republic

AU - Kulasova, Alena

AU - Beven, Keith J.

AU - Blazkova, Sarka D.

AU - Rezacova, Daniela

AU - Cajthaml, Jiri

N1 - This content is open access. (CC BY-NC-ND 3.0)

PY - 2014/6

Y1 - 2014/6

N2 - Understanding and modelling the processes of flood runoff generation is still a challenge in catchment hydrology. In particular, there are issues about how best to represent the effects of the antecedent state of saturation of a catchment on runoff formation and flood hydrographs. This paper reports on the experience of mapping saturated areas using measured water table by piezometers and more qualitative assessments of the state of the moisture at soil surface or immediately under it to provide information that can usefully condition model predictions. Vegetation patterns can also provide useful indicators of runoff source areas, but integrated over much longer periods of time. In this way, it might be more likely that models will get the right predictions for the right reasons.

AB - Understanding and modelling the processes of flood runoff generation is still a challenge in catchment hydrology. In particular, there are issues about how best to represent the effects of the antecedent state of saturation of a catchment on runoff formation and flood hydrographs. This paper reports on the experience of mapping saturated areas using measured water table by piezometers and more qualitative assessments of the state of the moisture at soil surface or immediately under it to provide information that can usefully condition model predictions. Vegetation patterns can also provide useful indicators of runoff source areas, but integrated over much longer periods of time. In this way, it might be more likely that models will get the right predictions for the right reasons.

KW - Mapping variable source areas

KW - Boot method

KW - Piezometers

KW - Vegetation mapping.

KW - RESEARCH CATCHMENT VALLCEBRE

KW - SOIL-MOISTURE PATTERNS

KW - PLYNLIMON CATCHMENTS

KW - EASTERN PYRENEES

KW - MID-WALES

KW - WATER

KW - RUNOFF

KW - TOPMODEL

KW - FLOW

KW - HILLSLOPE

U2 - 10.2478/johh-2014-0002

DO - 10.2478/johh-2014-0002

M3 - Journal article

VL - 62

SP - 160

EP - 168

JO - Journal of Hydrology and Hydromechanics

JF - Journal of Hydrology and Hydromechanics

IS - 2

ER -