Forecasting of Dengue Disease Incident Risks Using Non-stationary Spatial of Geostatistics Model in Bone Regency Indonesia

Rahim AmranMallongi Anwar Stang
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引用次数: 8

Abstract

Background: Standard statistical models generally assume that any incident of dengue disease in one location are independent with the incidence of dengue disease in other locations. However, the independent assumption does not apply in the spread of dengue disease. The spread of dengue disease tends to occur almost simultaneously in a same area or in the adjacent area due to similar environmental factors in the area. Similar environmental factors results in their risk spatial correlation of disease spread. If spatial correlation aspects is not considered in modeling then the conclusion of the significant factors that influence on the risk of spreading disease becomes inaccurate. Objective: The purpose of this study was to make mapping the risk of dengue fever incidence in Bone Regency South Sulawesi province by region (districts) with non-stationary spatial geostatistics model. Materials and Methods: The analysis variables included are larvae density, temperature, population density, rainfall, altitude from sea level and the incidence rate of dengue fever. Results: The results showed that risk rate model of dengue in Bone Regency with stationary spatial geostatistics models are as follows: log(pi) = -0.08+0.006X1+0.02X2-0.02X3-0.04X4-0.01X5. X1 = The density of larvae, X2 = Air temperature, X3 = Population density, X4 = Rainfall and X5 = The height of the sea level. Risk rate model of dengue in Northern Bone Regency (cluster 1) with non-stationary spatial geostatistics models are as follow: log(pi) = -0.02-0.0009X1-0.17X2+0.003X3+0.22X4-0.006X5. Risk rate model of dengue in Southern Bone Regency (cluster 2) with non-stationary spatial geostatistics models are as follow: log(pi) = -0.02-0.02X1-0.01X2-0.02X3-0.02X40.03X5. Risk rate model of dengue in Western Bone Regency (cluster 3) with non-stationary spatial geostatistics models are as follow: log(pi) = -0.08-0.007X1-0.02X2-0.03X3-0.009X4-0.06X5. Conclusion: The prediction error values on the non-stationary model between (0.27-3.6) lower than stationary model with variation between (0.68-6.37).
利用非平稳空间地统计模型预测印度尼西亚骨骼摄政地区登革热事件风险
背景:标准统计模型通常假设一个地区的登革热发病率与其他地区的登革热发病率是独立的。然而,这种独立的假设并不适用于登革热的传播。由于该地区的环境因素相似,登革热的传播往往几乎同时发生在同一地区或邻近地区。相似的环境因素导致疾病传播的风险空间相关性。如果在建模中不考虑空间相关性方面,那么对影响疾病传播风险的重要因素的结论就会变得不准确。目的:采用非平稳空间地统计模型,对南苏拉威西省骨县登革热发病风险进行区(区)划分。材料与方法:蚊幼虫密度、温度、种群密度、降雨量、海拔高度和登革热发病率为分析变量。结果:用平稳空间地统计学模型建立的骨县登革热危险率模型为:log(pi) = -0.08+0.006X1+0.02X2-0.02X3-0.04X4-0.01X5。X1 =幼虫密度,X2 =气温,X3 =种群密度,X4 =降雨量,X5 =海平面高度。采用非平稳空间地统计学模型建立北骨县(聚类1)登革热风险率模型为:log(pi) = -0.02-0.0009X1-0.17X2+0.003X3+0.22X4-0.006X5。采用非平稳空间地统计学模型建立的南骨县(聚类2)登革热风险率模型为:log(pi) = -0.02-0.02 x1 -0.01 x2 -0.02 x3 -0.02 x40 - 0.03 x5。Western Bone Regency (cluster 3)登革热风险率模型采用非平稳空间地统计学模型:log(pi) = -0.08-0.007X1-0.02X2-0.03X3-0.009X4-0.06X5。结论:非平稳模型的预测误差值小于平稳模型,误差值在0.27 ~ 3.6之间,方差在0.68 ~ 6.37之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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