Estimating threshold-exceeding probability maps of environmental variables with Markov chain random fields

被引:9
作者
Li, Weidong [1 ,2 ,3 ]
Zhang, Chuanrong [2 ,3 ]
Dey, Dipak K. [4 ]
Wang, Shanqin [1 ]
机构
[1] Huazhong Agr Univ, Coll Resources & Environm, Wuhan 430070, Peoples R China
[2] Univ Connecticut, Dept Geog, Storrs, CT 06269 USA
[3] Univ Connecticut, Ctr Environm Sci & Engn, Storrs, CT 06269 USA
[4] Univ Connecticut, Dept Stat, Storrs, CT 06269 USA
关键词
Environmental evaluation; Geostatistics; Spatial uncertainty; Transiogram; SEQUENTIAL INDICATOR SIMULATION; REGIME SHIFTS; UNCERTAINTY ASSESSMENT; SPATIAL-DISTRIBUTION; CONTAMINATION; PREDICTION; ALGORITHM; SOILS; RISK;
D O I
10.1007/s00477-010-0389-9
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Estimating and mapping spatial uncertainty of environmental variables is crucial for environmental evaluation and decision making. For a continuous spatial variable, estimation of spatial uncertainty may be conducted in the form of estimating the probability of (not) exceeding a threshold value. In this paper, we introduced a Markov chain geostatistical approach for estimating threshold-exceeding probabilities. The differences of this approach compared to the conventional indicator approach lie with its nonlinear estimators-Markov chain random field models and its incorporation of interclass dependencies through transiograms. We estimated threshold-exceeding probability maps of clay layer thickness through simulation (i.e., using a number of realizations simulated by Markov chain sequential simulation) and interpolation (i.e., direct conditional probability estimation using only the indicator values of sample data), respectively. To evaluate the approach, we also estimated those probability maps using sequential indicator simulation and indicator kriging interpolation. Our results show that (i) the Markov chain approach provides an effective alternative for spatial uncertainty assessment of environmental spatial variables and the probability maps from this approach are more reasonable than those from conventional indicator geostatistics, and (ii) the probability maps estimated through sequential simulation are more realistic than those through interpolation because the latter display some uneven transitions caused by spatial structures of the sample data.
引用
收藏
页码:1113 / 1126
页数:14
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