National Centre for Epidemiology and Population Health, Research School of Population Health, Australian National University , Building 62, Acton, Canberra, Australia 2602.
Department of Pediatric Infectious Diseases, Institute of Tropical Medicine, Nagasaki University , 1-12-4, Sakamoto, Nagasaki, Japan 852-8523.
Environ Sci Technol. 2017 Jul 18;51(14):8119-8127. doi: 10.1021/acs.est.6b05146. Epub 2017 Jun 26.
The Indian Ocean Dipole (IOD) is a global climate phenomenon that influences the spread of human infectious diseases through climate extremes including droughts and floods. The Dipole Mode Index (DMI), which measures the strength of the IOD, is one of the main indicators of rainfall variability across Australia. Using an ecological, time-series approach we examined the short-term and nonlinear relationship between the DMI and weekly cryptosporidiosis reported from 2001 to 2012 across the temperate, subtropical, and tropical climate zones in Australia, controlling for season, long-term trends, and cryptosporidiosis counts from the past week. The association of DMI with cryptosporidiosis was nonlinear and varied in the short term and by climatic zone. Including cryptosporidiosis counts from the previous week improved model fit in all three zones and modified the DMI-disease relationship in the subtropical and temperate regions. In the temperate zone, a 0.1 unit increase in an extreme positive DMI was associated with a higher risk of reported cryptosporidiosis [Relative Risk (RR) 1.23 (95% confidence interval (CI), 1.00-1.52)], compared to the risk associated with mean DMI. This methodology shows the potential for quantifying the short-term and nonlinear response of infections like cryptosporidiosis with climate variability. These findings also suggest that future models that account for lagged disease effects may better represent the time varying environmental exposure-disease relationship. The expected increases in the frequency of positive DMI events will likely result in decreased rainfall across temperate Australia, with potential implications for public health.
印度洋偶极子(IOD)是一种全球气候现象,通过干旱和洪水等气候极端事件影响人类传染病的传播。IOD 的衡量指标偶极子模态指数(DMI)是澳大利亚各地降雨变化的主要指标之一。我们采用生态时间序列方法,研究了 2001 年至 2012 年期间澳大利亚温带、亚热带和热带气候区每周报告的隐孢子虫病与 DMI 之间的短期和非线性关系,控制了季节、长期趋势以及上周的隐孢子虫病病例数。DMI 与隐孢子虫病之间的关联是非线性的,并且在短期内和气候区之间存在差异。在所有三个区域中,包括上周的隐孢子虫病病例数都可以提高模型拟合度,并改变亚热带和温带地区的 DMI-疾病关系。在温带地区,与平均 DMI 相关的风险相比,极端正 DMI 增加 0.1 个单位与报告的隐孢子虫病风险增加相关[相对风险 (RR) 1.23(95%置信区间 (CI),1.00-1.52)]。这种方法显示了量化感染(如隐孢子虫病)与气候变化之间短期和非线性反应的潜力。这些发现还表明,未来考虑疾病滞后效应的模型可能会更好地代表不断变化的环境暴露-疾病关系。预计阳性 DMI 事件的频率增加将导致澳大利亚温带地区降雨量减少,这可能对公共卫生产生影响。