Assessing the value of high-resolution isotope tracer data in the stepwise development of a lumped conceptual rainfall-runoff model

被引:56
作者
Birkel, C. [1 ,2 ]
Dunn, S. M. [1 ]
Tetzlaff, D. [2 ]
Soulsby, C. [2 ]
机构
[1] Macaulay Land Use Res Inst, Aberdeen AB15 8QH, Scotland
[2] Univ Aberdeen, Sch Geosci, No Rivers Inst, Aberdeen AB24 3UF, Scotland
关键词
stable isotopes; solute transport; models; conservative tracers; multi-criteria calibration; measurement uncertainty; sampling resolution; WATER RESIDENCE TIMES; HYDROLOGICAL PATHWAYS; MESOSCALE CATCHMENT; STREAM WATER; CALIBRATION; UNCERTAINTY; TRANSPORT; SEPARATION; DEUTERIUM; BEHAVIOR;
D O I
10.1002/hyp.7763
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
A study was undertaken in a small agricultural catchment in north east Scotland with the objective of assessing the value of high-resolution isotope data for integration within a lumped, conceptual hydrological model to improve calibration and aid evaluation. Daily samples of precipitation and stream flow, collected over a year, were analysed for deuterium using new laser spectroscopy technology. The utility of such high-resolution isotope data was evaluated in relation to the associated uncertainty which was contextualized in relation to uncertainties over hydrometric data and the influence of different sampling resolutions. The simulations were evaluated against model and data errors using auxiliary stream deuterium time series in addition to discharge. The lumped conceptual catchment isotope model (CIM) was developed and adequately reflects flow dynamics and deuterium peaks, but a simple assumption of 'good mixing' is not able to fully reproduce the daily stream deuterium dynamic. Using auxiliary data for model evaluation, however, significantly constrained acceptable behavioural parameter sets and therefore reduces the model's degree of freedom. The data indicate that isotopic variability in the stream response is not adequately captured using weekly tracer data. The input resolution of precipitation deuterium concentrations, which were much more variable, proved to be crucial. This approach has provided further assessment of the value of tracers in hydrological modelling, demonstrating their usefulness in terms of model conceptualization, development and calibration, which outweighs the additional uncertainty. Copyright (C) 2010 John Wiley & Sons, Ltd.
引用
收藏
页码:2335 / 2348
页数:14
相关论文
共 65 条
  • [1] Barnes CJ, 1996, HYDROL PROCESS, V10, P793, DOI 10.1002/(SICI)1099-1085(199606)10:6<793::AID-HYP372>3.0.CO
  • [2] 2-K
  • [3] On undermining the science?
    Beven, Keith
    [J]. HYDROLOGICAL PROCESSES, 2006, 20 (14) : 3141 - 3146
  • [4] Towards a simple dynamic process conceptualization in rainfall-runoff models using multi-criteria calibration and tracers in temperate, upland catchments
    Birkel, C.
    Tetzlaff, D.
    Dunn, S. M.
    Soulsby, C.
    [J]. HYDROLOGICAL PROCESSES, 2010, 24 (03) : 260 - 275
  • [5] Do Nash values have value? Discussion and alternate proposals
    Criss, Robert E.
    Winston, William E.
    [J]. HYDROLOGICAL PROCESSES, 2008, 22 (14) : 2723 - 2725
  • [6] A MULTISIGNAL AUTOMATIC CALIBRATION METHODOLOGY FOR HYDROCHEMICAL MODELS - A CASE-STUDY OF THE BIRKENES MODEL
    DEGROSBOIS, E
    HOOPER, RP
    CHRISTOPHERSEN, N
    [J]. WATER RESOURCES RESEARCH, 1988, 24 (08) : 1299 - 1307
  • [7] Uncertainty in river discharge observations: a quantitative analysis
    Di Baldassarre, G.
    Montanari, A.
    [J]. HYDROLOGY AND EARTH SYSTEM SCIENCES, 2009, 13 (06) : 913 - 921
  • [8] DOCHARTAIGH BEO, 2004, IR04130R BRIT GEOL S
  • [9] Conceptualization in catchment modelling: simply learning?
    Dunn, S. M.
    Freer, J.
    Weiler, M.
    Kirkby, M. J.
    Seibert, J.
    Quinn, P. F.
    Lischeid, G.
    Tetzlaff, D.
    Soulsby, C.
    [J]. HYDROLOGICAL PROCESSES, 2008, 22 (13) : 2389 - 2393
  • [10] Transit time distributions of a conceptual model: their characteristics and sensitivities
    Dunn, S. M.
    Birkel, C.
    Tetzlaff, D.
    Soulsby, C.
    [J]. HYDROLOGICAL PROCESSES, 2010, 24 (12) : 1719 - 1729