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The influence of climate variability effects on groundwater time series in the lower central plains of Thailand

Author(s)
Taweesin, Korrakoch
Seeboonruang, Uma
Saraphirom, Phayom
Date Issued
March 8, 2018
Type
Article
DOI
10.3390/w10030290
Abstract
This research studies the relationship between the climate index and the groundwater level of the lower Chao Phraya basin, in order to forecast the groundwater level in the studied area by using Autoregressive IntegratedMoving Average with Explanatory (ARIMAX). The combination of 6 climate indices-Dipole Mode Index, Indian Summer Monsoon Index, Multivariate ENSO Index, Sea Surface Temperature NINO4, Southern Oscillation Index and theWestern North PacificMonsoon Index-were used, along with the groundwater level data from 14 stations during the period 1980-2011 to develop the forecastmodel and verify itwith the data of 2012.The first stepwas correlation of the ARIMAmodel with Autocorrelation Function and Partial Autocorrelation Function. The possible model was then selected using BIC statistics. Diagnostic Checking was done to consider the white noise characteristic of estimated residuals by using the statistics of Box and Ljung (Q-statistic). If the selected models were found to be proper, then the Granger Causality Test of the leading parameters or the climate index would be performed as the next step. The results show that there is a relationship between the groundwater level and the climate index. The model could be used to forecast effectively the average RMSE value at 0.6. The last step was to develop theMODFLOWfor a conceptualmodel and synthesize groundwater levels in the study area, which covers around 43,000 km2 and has 8 layers of groundwater, with Bangkok clay on the top. All other boundary values were set to be steady. The calibration was done using the data of 325 observed wells. The normalized RMS value was 9.705%. The results were verified by the data using ARIMAX over the same time periods. To conclude, the simulated results of the monthly groundwater level in 2012 of the wells have a confidence interval of around 95%, which is near the result from the ARIMAX model. The advantages of the ARIMAX model include high accuracy, no requirement for a large amount of data and inexpensive implementation. It is one of the effective tools for the groundwater prediction.
Citation
Water Switzerland, 10(3), 2018
Subjects

ARIMAX model

Climate variability

Correlogram

Groundwater fluctuati...

Time series

Metrics
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