skip to main content
Idioma:

On the Optimal Spatial Design for Groundwater Level Monitoring Networks

Ohmer, M. ; Liesch, T. ; Goldscheider, N.

Water resources research, 2019-11, Vol.55 (11), p.9454-9473 [Periódico revisado por pares]

Washington: John Wiley & Sons, Inc

Texto completo disponível

Citações Citado por
  • Título:
    On the Optimal Spatial Design for Groundwater Level Monitoring Networks
  • Autor: Ohmer, M. ; Liesch, T. ; Goldscheider, N.
  • Assuntos: Errors ; Geostatistics ; Groundwater ; Groundwater flow ; Groundwater flow models ; groundwater level monitoring network ; Groundwater levels ; Hydrogeology ; Hydrologic data ; low‐discrepancy ; Monitoring ; Observation wells ; Root-mean-square errors ; Sampling ; sampling design ; Sampling designs ; spatial optimization ; Statistical methods ; Statistics ; Water flow ; Water monitoring ; Water table ; Wells
  • É parte de: Water resources research, 2019-11, Vol.55 (11), p.9454-9473
  • Descrição: Effective groundwater monitoring networks are important, as systematic data collected at observation wells provide a crucial understanding of the dynamics of hydrogeological systems as well as the basis for many other applications. This study investigates the influence of six groundwater level monitoring network (GLMN) sampling designs (random, grid, spatial coverage, and geostatistical) with varying densities on the accuracy of spatially interpolated groundwater surfaces. To obtain spatially continuous prediction errors (in contrast to point cross‐validation errors), we used nine potentiometric groundwater surfaces from three regional MODFLOW groundwater flow models with different resolutions as a priori references. To assess the suitability of frequently‐used cross‐validation error statistics (MAE, RMSE, RMSSE, ASE, and NSE), we compared them with the actual prediction errors (APE). Additionally, we defined upper and lower thresholds for an appropriate spatial density of monitoring wells. Below the lower threshold, the observation density appears insufficient, and additional wells lead to a significant improvement of the results. Above the upper threshold, additional wells lead to only minor and inefficient improvements. According to the APE, systematic sampling lead to the best results but is often not suited for GLMN due to its nonprogressive characteristic. Geostatistical and spatial coverage sampling are considerable alternatives, which are in contrast progressive and allow evenly spaced and, in the case of spatial coverage sampling, yet reproducible coverage with accurate results. We found that the global cross‐validation error statistics are not suitable to compare the performance of different sampling designs, although they allow rough conclusions about the quality of the GLMN. Key Points A new low‐discrepancy method (R2 method) for an extensible groundwater level monitoring network design is proposed We define a range of groundwater level monitoring network densities with an optimized information/cost ratio We show that global cross‐validation error parameters are not suitable for the comparative assessment of different sampling designs
  • Editor: Washington: John Wiley & Sons, Inc
  • Idioma: Inglês
Voltar para lista de resultados

  • Realização: ABCD-USP USP   Logos de Redes Sociais: Freepik

Buscando em bases de dados remotas. Favor aguardar.