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Observed regional climatic changes over Ontario, Canada, in response to global warming

机译:观测到加拿大安大略省响应全球变暖的区域气候变化

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Human-induced climatic changes are not expected to be uniform across the globe due to the regional variations in topography, land cover/land use, economic development and so on. Investigating the regional effects of climate change is thus of great concern for decision makers and resource managers to develop scientifically informed policies and strategies against the changing climate. In the present study, regional climatology over Ontario, Canada, and its temporal trends in the past century are analysed based on the historical observations at the gauged stations, aiming to investigate how the local climate has been affected by human-induced global warming. The analysis shows that the annual mean temperature over Ontario varies mainly between 1.6 and 7 degrees C with a median of 3.8 degrees C, while its annual total precipitation usually ranges between 836 and 1004mm with a median of 896mm. Further correlation analysis suggests that no or negligible correlations between total precipitation and mean temperature are found at the vast majority of stations (accounting for over 80% of the total), except for summer when significant negative correlations (with a correlation co-efficient varying between -0.7 and -0.2) are reported at over 54% stations. As for the temporal trends, significant warming trends are detected throughout the province and the overall trend in annual mean temperature varies largely between 0.01 and 0.02 degrees Cyear(-1). Increasing trends in annual rainfall (by 1-3mmyear(-1)) and total precipitation (by 1-4mmyear(-1)) are detected at the vast majority of gauged stations, but no significant trends in annual snowfall are identified at most of the stations. The results of this study can help better understand the regional climate of Ontario and provide important references for developing future climate scenarios that can be used for impact studies.
机译:由于地形,土地覆盖/土地利用,经济发展等方面的区域差异,预计人为导致的气候变化在全球范围内并不统一。因此,对气候变化的区域影响进行调查对于决策者和资源管理者制定针对气候变化的科学知情的政策和策略非常重要。在本研究中,根据对定站的历史观测,分析了加拿大安大略省的区域气候学及其过去一个世纪的时间趋势,旨在调查人为引起的全球变暖如何影响当地气候。分析表明,安大略省的年平均气温主要在1.6至7摄氏度之间变化,中位数为3.8摄氏度,而其年总降水量通常在836至1004毫米之间,中位数为896毫米。进一步的相关分析表明,除夏季显着负相关(相关系数之间存在显着负相关)的夏季外,绝大多数台站(占总站数的80%以上)没有发现总降水量与平均温度之间的相关关系或微不足道。 -0.7和-0.2)在超过54%的电台上报告。至于时间趋势,在全省范围内都发现了明显的变暖趋势,年平均气温的总体趋势在0.01至0.02 Cyear(-1)之间变化很大。在绝大多数测站上都发现了年降水量(1-3mmyear(-1)和总降水量(1-4mmyear(-1))的增加趋势,但是在大多数降雪站没有发现年降雪的明显趋势。车站。这项研究的结果可以帮助更好地了解安大略的区域气候,并为开发可用于影响研究的未来气候情景提供重要参考。

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