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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Estimating winter trends in climatic variables in the Chic-Chocs Mountains, Canada (1970–2009)
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Estimating winter trends in climatic variables in the Chic-Chocs Mountains, Canada (1970–2009)

机译:估计加拿大Chic-Chocs山区的冬季气候变化趋势(1970-2009年)

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摘要

This paper presents an analysis of winter climate variability based on daily mean temperature and precipitation data since 1970 in the Chic-Chocs Mountain range (located in the Gaspé Peninsula, Eastern Quebec, Canada). Mountain environments are particularly sensitive to rapid climate change and are therefore good indicators of recent global warming. The main goal of this study is to demonstrate how joint probability temperature/precipitation distributions can be used to estimate winter condition changes (trends) for six meteorological stations in the study area (the altitudinal range for the stations is from 5 to 574 m). The presence and persistence of snow cover was also estimated. Previous studies have shown a lack of evidence of significant trends in snow-cover characteristics (density, depth and snow water equivalent (SWE)) from the early 1980s to the present, despite an increase in temperature over the same period. A reanalysis of these data sets in addition to the use of a combination of temperature and precipitation data categorized into four modes (warm/wet, warm/dry, cold/wet and cold/dry) was also performed. Despite this new analysis, no clear evidence of climate change could be found in the study area over the last four decades. The results revealed that patterns and trends are quite different from one station to another, but when the environment is taken into account (valley or plateau, coastal versus inland) some apparent patterns emerge.
机译:本文基于1970年以来Chic-Chocs山脉(位于加拿大魁北克东部的加斯佩半岛)的日平均温度和降水数据,对冬季气候变化进行了分析。山区环境对快速的气候变化特别敏感,因此是近期全球变暖的良好指标。这项研究的主要目的是演示如何使用联合概率温度/降水分布来估计研究区域内六个气象站的冬季条件变化(趋势)(站的海拔范围从5到574 m)。还估计了积雪的存在和持久性。以前的研究表明,尽管同期温度升高,但缺乏证据表明从1980年代初期到现在的积雪特征(密度,深度和雪水当量(SWE))有显着趋势。除了使用归类为四种模式(暖/湿,暖/干,暖/干,冷/湿和冷/干)的温度和降水数据的组合之外,还对这些数据集进行了重新分析。尽管进行了这一新的分析,但在过去的四十年中,研究区域仍未找到明确的气候变化证据。结果表明,一个站点到另一个站点的模式和趋势有很大不同,但是当考虑到环境(谷地或高原,沿海与内陆)时,就会出现一些明显的模式。

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