首页> 美国卫生研究院文献>The American Journal of Tropical Medicine and Hygiene >Predictive Time Series Analysis Linking Bengal Cholera with Terrestrial Water Storage Measured from Gravity Recovery and Climate Experiment Sensors
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Predictive Time Series Analysis Linking Bengal Cholera with Terrestrial Water Storage Measured from Gravity Recovery and Climate Experiment Sensors

机译:通过重力恢复和气候实验传感器测量的孟加拉霍乱与陆地储水之间的预测时间序列分析

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摘要

Outbreaks of diarrheal diseases, including cholera, are related to floods and droughts in regions where water and sanitation infrastructure are inadequate or insufficient. However, availability of data on water scarcity and abundance in transnational basins, are a prerequisite for developing cholera forecasting systems. With more than a decade of terrestrial water storage (TWS) data from the Gravity Recovery and Climate Experiment, conditions favorable for predicting cholera occurrence may now be determined. We explored lead–lag relationships between TWS in the Ganges–Brahmaputra–Meghna basin and endemic cholera in Bangladesh. Since bimodal seasonal peaks in cholera in Bangladesh occur during spring and autumn seasons, two separate logistical models between TWS and disease time series (2002–2010) were developed. TWS representing water availability showed an asymmetrical, strong association with cholera prevalence in the spring (τ = −0.53; P < 0.001) and autumn (τ = 0.45; P < 0.001) up to 6 months in advance. One unit (centimeter of water) decrease in water availability in the basin increased odds of above normal cholera by 24% (confidence interval [CI] = 20–31%; P < 0.05) in the spring, while an increase in regional water by 1 unit, through floods, increased odds of above average cholera in the autumn by 29% (CI = 22–33%; P < 0.05).
机译:腹水病(包括霍乱)的爆发与水和卫生基础设施不足或不足的地区的洪水和干旱有关。但是,获得有关跨国盆地缺水和丰度数据的能力,是发展霍乱预报系统的前提。借助重力恢复和气候实验获得的十余种陆地水存储(TWS)数据,现在可以确定有利于预测霍乱发生的条件。我们探讨了恒河-布拉马普特拉-梅格纳盆地的台风预报系统与孟加拉国地方性霍乱之间的超前-滞后关系。由于孟加拉国霍乱的双峰季节高峰发生在春季和秋季,因此在TWS和疾病时间序列(2002-2010)之间建立了两个独立的逻辑模型。表示可用水量的TWS在春季(τ= -0.53; P <0.001)和秋天(τ= 0.45; P <0.001)之前的6个月之前与霍乱流行呈非对称性强关联。在春季,流域水供应量每减少一单位(厘米水),则比正常霍乱的几率增加24%(置信区间[CI] = 20–31%; P <0.05),而区域供水量增加1个单位通过洪水使秋季霍乱高于平均水平的几率增加了29%(CI = 22-33%; P <0.05)。

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