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首页> 外文期刊>International journal of sustainable development and planning >RELATIONSHIP BETWEEN EL NINO SOUTHERN OSCILLATION INDEX AND RAINFALL (QUEENSLAND, AUSTRALIA)
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RELATIONSHIP BETWEEN EL NINO SOUTHERN OSCILLATION INDEX AND RAINFALL (QUEENSLAND, AUSTRALIA)

机译:EL NINO南方涛动指数与降雨之间的关系(澳大利亚昆士兰州)

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This paper explores the relationship between El Nino Southern Oscillation Index (SOI) and rainfall in South East Queensland. Several statistical models of the SOI and rainfall data are analysed including interactions. The results of the analyses show that although the SOI and rainfall can be predicted for short terms using time series analysis methods, mean squared error (MSE) and Their s U showed that in comparison to persistence model forecasts may not be significantly better. Although the short term predictions may be worse, this does not mean that these cannot be used; rather, it shows that for different fitting and forecast periods, models can fail in predicting ahead. In fact weather forecasts can predict the short term rainfall well - but cannot predict monthly precipitation for two or three or more months ahead. In climate predictions the limit of predictability is reached when the standardised MSE reaches the climate variance (=1). All the rainfall models used in this study show an MSE well below 1, i.e. the models did not reach the limit of predictability.
机译:本文探讨了厄尔尼诺南部涛动指数(SOI)与昆士兰东南部降雨之间的关系。分析了SOI和降雨数据的几种统计模型,包括相互作用。分析结果表明,尽管可以使用时间序列分析方法对SOI和降雨量进行短期预测,但均方误差(MSE)和他们的s U表明,与持久性模型相比,预测可能不会更好。尽管短期预测可能更糟,但这并不意味着不能使用这些预测。相反,它表明对于不同的拟合和预测周期,模型可能无法提前进行预测。实际上,天气预报可以很好地预测短期降雨-但无法预测未来两三个月或三个月以上的月降水量。在气候预测中,当标准MSE达到气候变化(= 1)时,可预测性达到极限。本研究中使用的所有降雨模型均显示MSE远低于1,即该模型未达到可预测性的极限。

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