Staff Publications

Staff Publications

  • external user (warningwarning)
  • Log in as
  • language uk
  • About

    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

    We have a manual that explains all the features 

Record number 345616
Title Propagation and spatial distribution of drought in a groundwater catchment
Author(s) Peters, E.; Bier, G.; Lanen, H.A.J. van; Torfs, P.J.J.F.
Source Journal of Hydrology 321 (2006)1-4. - ISSN 0022-1694 - p. 257 - 275.
DOI https://doi.org/10.1016/j.jhydrol.2005.08.004
Department(s) Soil Physics, Ecohydrology and Groundwater Management
Hydrology and Quantitative Water Management
WIMEK
Publication type Refereed Article in a scientific journal
Publication year 2006
Keyword(s) discharge - recharge - level - uk - aquifer - shallow - flow
Abstract Natural droughts are usually caused by a period of lower than average precipitation. The resulting shortage in precipitation propagates through the hydrological system causing drought in the different segments of the hydrological system (unsaturated zone, saturated groundwater, surface water). To analyse the propagation and spatial distribution of the drought in the groundwater system, drought is analysed simultaneously in simulated recharge, hydraulic heads and groundwater discharge for a groundwater catchment (Pang, UK). The recharge and hydraulic heads are simulated and analysed spatially. The groundwater discharge is analysed in four reaches along the stream. Comparison of droughts in the recharge and heads shows that the droughts are greatly attenuated and delayed in the groundwater system. Comparison of the droughts in the heads and the discharge shows the opposite effect, so that the droughts in the discharge resemble more the droughts in the recharge than those in the hydraulic heads. The faster response in the groundwater discharge compared to the hydraulic heads is probably caused by the non-linear relationship between groundwater storage and discharge. Thus in the recharge and in the discharge, there are many short droughts, whereas in the hydraulic head fewer, more severe droughts occur. It is likely that these results hold not only for the Pang catchment but also generally for catchments with a large groundwater system and a non-linear groundwater discharge relationship. The spatial distribution of the droughts in the hydraulic heads shows that short droughts are more severe near the streams, as they are attenuated further away. Long periods of below average recharge have relatively more effect near the groundwater divide. The spatial distribution of the droughts in the groundwater discharge is such that upstream the droughts are more attenuated than downstream.
Comments
There are no comments yet. You can post the first one!
Post a comment
 
Please log in to use this service. Login as Wageningen University & Research user or guest user in upper right hand corner of this page.