Influence of non-linearity in the storage-discharge relationship on discharge droughts

E. Peters, H.A.J. van Lanen

Research output: Chapter in Book/Report/Conference proceedingAbstractAcademic

Abstract

During drought, most stream flow is derived from stored sources, primarily groundwater. In many catchments the relation between groundwater storage and discharge is non-linear, for example because the aquifer is unsaturated, because of variations in the conductivity of the aquifer. In this paper it is examined whether and how non-linearity in the storage-discharge relationship increases drought duration and severity
Original languageEnglish
Title of host publicationNCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003
EditorsN. Douben, A.G. van Os
Place of Publication[S.L.]
PublisherNCR
Pages90-91
Publication statusPublished - 2004

Fingerprint

nonlinearity
drought
aquifer
groundwater
streamflow
conductivity
catchment

Keywords

  • groundwater flow
  • drought
  • water storage
  • catchment hydrology
  • usa
  • spain

Cite this

Peters, E., & van Lanen, H. A. J. (2004). Influence of non-linearity in the storage-discharge relationship on discharge droughts. In N. Douben, & A. G. van Os (Eds.), NCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003 (pp. 90-91). [S.L.]: NCR.
Peters, E. ; van Lanen, H.A.J. / Influence of non-linearity in the storage-discharge relationship on discharge droughts. NCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003. editor / N. Douben ; A.G. van Os. [S.L.] : NCR, 2004. pp. 90-91
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abstract = "During drought, most stream flow is derived from stored sources, primarily groundwater. In many catchments the relation between groundwater storage and discharge is non-linear, for example because the aquifer is unsaturated, because of variations in the conductivity of the aquifer. In this paper it is examined whether and how non-linearity in the storage-discharge relationship increases drought duration and severity",
keywords = "grondwaterstroming, droogte, wateropslag, hydrologie van stroomgebieden, vs, spanje, groundwater flow, drought, water storage, catchment hydrology, usa, spain",
author = "E. Peters and {van Lanen}, H.A.J.",
year = "2004",
language = "English",
pages = "90--91",
editor = "N. Douben and {van Os}, A.G.",
booktitle = "NCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003",
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}

Peters, E & van Lanen, HAJ 2004, Influence of non-linearity in the storage-discharge relationship on discharge droughts. in N Douben & AG van Os (eds), NCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003. NCR, [S.L.], pp. 90-91.

Influence of non-linearity in the storage-discharge relationship on discharge droughts. / Peters, E.; van Lanen, H.A.J.

NCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003. ed. / N. Douben; A.G. van Os. [S.L.] : NCR, 2004. p. 90-91.

Research output: Chapter in Book/Report/Conference proceedingAbstractAcademic

TY - CHAP

T1 - Influence of non-linearity in the storage-discharge relationship on discharge droughts

AU - Peters, E.

AU - van Lanen, H.A.J.

PY - 2004

Y1 - 2004

N2 - During drought, most stream flow is derived from stored sources, primarily groundwater. In many catchments the relation between groundwater storage and discharge is non-linear, for example because the aquifer is unsaturated, because of variations in the conductivity of the aquifer. In this paper it is examined whether and how non-linearity in the storage-discharge relationship increases drought duration and severity

AB - During drought, most stream flow is derived from stored sources, primarily groundwater. In many catchments the relation between groundwater storage and discharge is non-linear, for example because the aquifer is unsaturated, because of variations in the conductivity of the aquifer. In this paper it is examined whether and how non-linearity in the storage-discharge relationship increases drought duration and severity

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KW - droogte

KW - wateropslag

KW - hydrologie van stroomgebieden

KW - vs

KW - spanje

KW - groundwater flow

KW - drought

KW - water storage

KW - catchment hydrology

KW - usa

KW - spain

M3 - Abstract

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EP - 91

BT - NCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003

A2 - Douben, N.

A2 - van Os, A.G.

PB - NCR

CY - [S.L.]

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Peters E, van Lanen HAJ. Influence of non-linearity in the storage-discharge relationship on discharge droughts. In Douben N, van Os AG, editors, NCR-days 2003. Dealing with Floods within Constraints, November 6-8, 2003. [S.L.]: NCR. 2004. p. 90-91