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Comparative study of the relationship between regional climate factors and local weather in Western Pacific countries

机译:西太平洋国家区域气候因素与当地天气之间关系的比较研究

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Many studies have reported that climate change affects the local weather. However, there are still considerable uncertainties, since the results depended on the various regional characteristics, time scales, and statistical models. The purpose of this study is to examine how regional climates such as El Nino-Southern oscillation and Indian Ocean Dipole can influence the local weather, and to compare the patterns between some countries in Western Pacific. Monthly data for regional climate and local weather, such as NINO3, DMI (dipole mode index), maximum temperature, and rainfall, were derived from Regional Office of Western Pacific, concerning 21 regions or cities in Mongolia, South Korea, Japan, Papua New Guinea (PNG), Laos, and Cambodia. We defined the four seasons in former three countries, but wet and dry seasons in latter countries. Generalized linear models with interaction between season and other explanatory variables (climate or weather) were used to estimate NINO3 and DMI effects on maximum temperature or rainfall. Also, the moving average lag structures of NINO3 and DMI were applied in the model. The significant NINO3 and DMI effects on rainfall were mostly shown in summer (Mongolia, Korea, and Japan) or all season (Laos and PNG), but the direction varied region to region. With respect to maximum temperature, NINO3 and DMI effects were relatively consistent within the country, but varied on season. For instance, the effects in summer (negative on NINO3, positive on DMI) were in contrast with other seasons in Mongolia, Korea, and Japan, in addition NINO3 effect of PNG was negative in wet season, but positive in dry season. Meanwhile, the lagged effects of NINO3 and DMI on rainfall and temperature were mixed from long and short lags in most countries, whereas only short-term effect was dominant in PNG. Local weather was not only influenced by regional climate factors, but the patterns varied on season, time scale, and locations. These results would be able to support understanding the relationship between weather and health problems.
机译:许多研究报告说,气候变化会影响当地的天气。但是,由于结果取决于各种地区特征,时间范围和统计模型,因此仍然存在很大的不确定性。这项研究的目的是研究诸如厄尔尼诺-南方涛动和印度洋偶极子之类的区域气候如何影响当地天气,并比较西太平洋一些国家之间的模式。 NINO3,DMI(偶极子模式指数),最高温度和降雨量等区域气候和局部天气的月度数据来自西太平洋区域办事处,涉及蒙古,韩国,日本,巴布亚新几内的21个地区或城市几内亚(PNG),老挝和柬埔寨。我们在前三个国家定义了四个季节,而在后三个国家定义了干湿两季。使用具有季节和其他解释变量(气候或天气)之间相互作用的广义线性模型来估计NINO3和DMI对最高温度或降雨量的影响。此外,在模型中应用了NINO3和DMI的移动平均滞后结构。 NINO3和DMI对降雨的显着影响主要表现在夏季(蒙古,韩国和日本)或整个季节(老挝和PNG),但方向因地区而异。关于最高温度,NINO3和DMI的影响在国内相对稳定,但随季节而变化。例如,夏季的影响(对NINO3的影响为负,对DMI的影响为正)与蒙古,韩国和日本的其他季节相反,此外,PNG的NINO3效果在雨季为负,而在旱季为正。同时,在大多数国家中,NINO3和DMI对降雨和温度的滞后效应混合了长时滞和短时滞,而PNG中只有短期效应占主导地位。当地的天气不仅受区域气候因素的影响,而且模式在季节,时间尺度和位置上也各不相同。这些结果将有助于理解天气和健康问题之间的关系。

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