Realistic forecasting of groundwater level, based on the eigenstructure of aquifer dynamics

被引:49
作者
Bidwell, VJ [1 ]
机构
[1] Lincoln Environm, Canterbury 8152, New Zealand
关键词
groundwater forecasting; aquifer dynamics; eigenvalue; ARMAX;
D O I
10.1016/j.matcom.2005.02.023
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Short-term management of groundwater resources, especially during droughts, can be assisted by forecasts of groundwater levels. Such forecasts need to account for the dynamic response of the aquifer to likely recharge scenarios and recent but unknown abstractions. This paper describes a method for formulating ARMAX forecast equations from a linear system description based on the eigenvalues and eigenvectors (eigenstructure) of aquifer dynamics. For the piezometric response of a heterogeneous aquifer to a fixed spatial distribution of land surface recharge, with time-varying magnitude, only a few eigenvalues are significant. The resulting model is demonstrated with monthly values of land surface recharge and groundwater level data from a 2000 km(2) alluvial aquifer in Canterbury, New Zealand. (c) 2005 IMACS. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:12 / 20
页数:9
相关论文
共 7 条
[1]   Ground water drought management by a feedforward control method [J].
Ahn, H .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 2000, 36 (03) :501-510
[2]  
BIDWELL VJ, 2002, P 4 INT C CAL REL GR, V46, P92
[3]  
BIDWELL VJ, 1991, NZ J HYDROLOGY, V30, P16
[4]  
BOX GEP, 1970, TIME SERIES ANAL FOR
[5]   AN EIGENVALUE NUMERICAL TECHNIQUE FOR SOLVING UNSTEADY LINEAR GROUNDWATER MODELS CONTINUOUSLY IN TIME [J].
SAHUQUILLO, A .
WATER RESOURCES RESEARCH, 1983, 19 (01) :87-93
[6]   COMPARISON OF UNIVARIATE AND TRANSFER-FUNCTION MODELS OF GROUNDWATER FLUCTUATIONS [J].
TANKERSLEY, CD ;
GRAHAM, WD ;
HATFIELD, K .
WATER RESOURCES RESEARCH, 1993, 29 (10) :3517-3533
[7]  
Young P., 1984, RECURSIVE ESTIMATION