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Uncertainty estimation of end-member mixing using generalized likelihood uncertainty estimation (GLUE), applied in a lowland catchment

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Uncertainty estimation of end-member mixing using generalized likelihood uncertainty estimation (GLUE), applied in a lowland catchment. / Delsman, Joost R.; Essink, Gualbert H. P. Oude; Beven, Keith J. et al.
In: Water Resources Research, Vol. 49, No. 8, 08.2013, p. 4792-4806.

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Delsman JR, Essink GHPO, Beven KJ, Stuyfzand PJ. Uncertainty estimation of end-member mixing using generalized likelihood uncertainty estimation (GLUE), applied in a lowland catchment. Water Resources Research. 2013 Aug;49(8):4792-4806. doi: 10.1002/wrcr.20341

Author

Delsman, Joost R. ; Essink, Gualbert H. P. Oude ; Beven, Keith J. et al. / Uncertainty estimation of end-member mixing using generalized likelihood uncertainty estimation (GLUE), applied in a lowland catchment. In: Water Resources Research. 2013 ; Vol. 49, No. 8. pp. 4792-4806.

Bibtex

@article{86b197d77fa84de68081656150fb1088,
title = "Uncertainty estimation of end-member mixing using generalized likelihood uncertainty estimation (GLUE), applied in a lowland catchment",
abstract = "End-member mixing models have been widely used to separate the different components of a hydrograph, but their effectiveness suffers from uncertainty in both the identification of end-members and spatiotemporal variation in end-member concentrations. In this paper, we outline a procedure, based on the generalized likelihood uncertainty estimation (GLUE) framework, to more inclusively evaluate uncertainty in mixing models than existing approaches. We apply this procedure, referred to as G-EMMA, to a yearlong chemical data set from the heavily impacted agricultural Lissertocht catchment, Netherlands, and compare its results to the traditional end-member mixing analysis (EMMA). While the traditional approach appears unable to adequately deal with the large spatial variation in one of the end-members, the G-EMMA procedure successfully identified, with varying uncertainty, contributions of five different end-members to the stream. Our results suggest that the concentration distribution of effective end-members, that is, the flux-weighted input of an end-member to the stream, can differ markedly from that inferred from sampling of water stored in the catchment. Results also show that the uncertainty arising from identifying the correct end-members may alter calculated end-member contributions by up to 30%, stressing the importance of including the identification of end-members in the uncertainty assessment.",
keywords = "end-member mixing, lowland hydrology, hydrograph separation, GLUE, MODELING STREAMWATER CHEMISTRY, HYDROGRAPH SEPARATIONS, GROUNDWATER-FLOW, HYDROLOGICAL PATHWAYS, MOUNTAINOUS CATCHMENT, HEADWATER CATCHMENT, WATER CHEMISTRY, STORM RUNOFF, TRACER, IDENTIFICATION",
author = "Delsman, {Joost R.} and Essink, {Gualbert H. P. Oude} and Beven, {Keith J.} and Stuyfzand, {Pieter J.}",
note = "{\textcopyright}2013. American Geophysical Union. All Rights Reserved.",
year = "2013",
month = aug,
doi = "10.1002/wrcr.20341",
language = "English",
volume = "49",
pages = "4792--4806",
journal = "Water Resources Research",
issn = "0043-1397",
publisher = "AMER GEOPHYSICAL UNION",
number = "8",

}

RIS

TY - JOUR

T1 - Uncertainty estimation of end-member mixing using generalized likelihood uncertainty estimation (GLUE), applied in a lowland catchment

AU - Delsman, Joost R.

AU - Essink, Gualbert H. P. Oude

AU - Beven, Keith J.

AU - Stuyfzand, Pieter J.

N1 - ©2013. American Geophysical Union. All Rights Reserved.

PY - 2013/8

Y1 - 2013/8

N2 - End-member mixing models have been widely used to separate the different components of a hydrograph, but their effectiveness suffers from uncertainty in both the identification of end-members and spatiotemporal variation in end-member concentrations. In this paper, we outline a procedure, based on the generalized likelihood uncertainty estimation (GLUE) framework, to more inclusively evaluate uncertainty in mixing models than existing approaches. We apply this procedure, referred to as G-EMMA, to a yearlong chemical data set from the heavily impacted agricultural Lissertocht catchment, Netherlands, and compare its results to the traditional end-member mixing analysis (EMMA). While the traditional approach appears unable to adequately deal with the large spatial variation in one of the end-members, the G-EMMA procedure successfully identified, with varying uncertainty, contributions of five different end-members to the stream. Our results suggest that the concentration distribution of effective end-members, that is, the flux-weighted input of an end-member to the stream, can differ markedly from that inferred from sampling of water stored in the catchment. Results also show that the uncertainty arising from identifying the correct end-members may alter calculated end-member contributions by up to 30%, stressing the importance of including the identification of end-members in the uncertainty assessment.

AB - End-member mixing models have been widely used to separate the different components of a hydrograph, but their effectiveness suffers from uncertainty in both the identification of end-members and spatiotemporal variation in end-member concentrations. In this paper, we outline a procedure, based on the generalized likelihood uncertainty estimation (GLUE) framework, to more inclusively evaluate uncertainty in mixing models than existing approaches. We apply this procedure, referred to as G-EMMA, to a yearlong chemical data set from the heavily impacted agricultural Lissertocht catchment, Netherlands, and compare its results to the traditional end-member mixing analysis (EMMA). While the traditional approach appears unable to adequately deal with the large spatial variation in one of the end-members, the G-EMMA procedure successfully identified, with varying uncertainty, contributions of five different end-members to the stream. Our results suggest that the concentration distribution of effective end-members, that is, the flux-weighted input of an end-member to the stream, can differ markedly from that inferred from sampling of water stored in the catchment. Results also show that the uncertainty arising from identifying the correct end-members may alter calculated end-member contributions by up to 30%, stressing the importance of including the identification of end-members in the uncertainty assessment.

KW - end-member mixing

KW - lowland hydrology

KW - hydrograph separation

KW - GLUE

KW - MODELING STREAMWATER CHEMISTRY

KW - HYDROGRAPH SEPARATIONS

KW - GROUNDWATER-FLOW

KW - HYDROLOGICAL PATHWAYS

KW - MOUNTAINOUS CATCHMENT

KW - HEADWATER CATCHMENT

KW - WATER CHEMISTRY

KW - STORM RUNOFF

KW - TRACER

KW - IDENTIFICATION

U2 - 10.1002/wrcr.20341

DO - 10.1002/wrcr.20341

M3 - Journal article

VL - 49

SP - 4792

EP - 4806

JO - Water Resources Research

JF - Water Resources Research

SN - 0043-1397

IS - 8

ER -