A conference paper presented at ModelCARE 2002, 4th International Conference on Calibration and Reliability in Groundwater Modelling, Prague, Czech Republic, 17-29 June 2002.The dynamic response of piezometric head at any location in an aquifer to time variation of regional land surface recharge and abstraction can be expressed as a linear system comprising only a few conceptual water storages. Model structure and parameters are related to aquifer characteristics and spatial pattern of recharge by the eigenvalues and eigenfunctions of a general analytical solution to the linearised Boussinesq equation. The model is implemented as a stochastic ARMA difference equation, independently for each location. This modelling approach is demonstrated ...
Oral presentation at the Groundwater/Surface Water Interaction Workshop, during the New Zealand Hydr...
A new multi-scale groundwater modelling methodology is presented to simulate pumped water levels in ...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Increasing abstraction of groundwater for irrigated agriculture on the Central Canterbury Plains of ...
Conference paper presented at the MODSIM03, International Congress on Modelling and Simulation, held...
Abstract: Short-term management of groundwater resources, especially during droughts, can be assiste...
Low-land alluvial gravel aquifers are formed from, and tend to be recharged, by rivers. These interc...
Abstract: Short-term management of groundwater resources, especially during droughts, can be assiste...
This report addresses an issue of groundwater management that was identified by regional council sta...
The purpose of the report is to advance the technical understanding of the groundwater system and in...
Increasing abstraction of groundwater for irrigated agriculture on the Central Canterbury Plains of ...
The objective of this study is to improve the simulation of deep groundwater levels by time se- ries...
Oral presentation at New Zealand Hydrological Society & Meteorological Society of New Zealand Joint ...
Large‐scale groundwater models are required to estimate groundwater availability and to inform water...
This presentation introduces model concepts and terms, demonstrates some models, develops critical a...
Oral presentation at the Groundwater/Surface Water Interaction Workshop, during the New Zealand Hydr...
A new multi-scale groundwater modelling methodology is presented to simulate pumped water levels in ...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...
Increasing abstraction of groundwater for irrigated agriculture on the Central Canterbury Plains of ...
Conference paper presented at the MODSIM03, International Congress on Modelling and Simulation, held...
Abstract: Short-term management of groundwater resources, especially during droughts, can be assiste...
Low-land alluvial gravel aquifers are formed from, and tend to be recharged, by rivers. These interc...
Abstract: Short-term management of groundwater resources, especially during droughts, can be assiste...
This report addresses an issue of groundwater management that was identified by regional council sta...
The purpose of the report is to advance the technical understanding of the groundwater system and in...
Increasing abstraction of groundwater for irrigated agriculture on the Central Canterbury Plains of ...
The objective of this study is to improve the simulation of deep groundwater levels by time se- ries...
Oral presentation at New Zealand Hydrological Society & Meteorological Society of New Zealand Joint ...
Large‐scale groundwater models are required to estimate groundwater availability and to inform water...
This presentation introduces model concepts and terms, demonstrates some models, develops critical a...
Oral presentation at the Groundwater/Surface Water Interaction Workshop, during the New Zealand Hydr...
A new multi-scale groundwater modelling methodology is presented to simulate pumped water levels in ...
Groundwater recharge is the main forcing of regional groundwater flow. In traditional partial‐differ...