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首页> 外文期刊>Bulletin of the American Meteorological Society >Influence of choice of time period on global surface temperature trend estimates.
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Influence of choice of time period on global surface temperature trend estimates.

机译:时间段的选择对全球表面温度趋势估计的影响。

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摘要

Annual global surface temperature and global land surface temperature trends are calculated for all possible periods of the historical record between 1850 and 2009. Two-dimensional parameter diagrams show the critical influence of the choice of start and end years on the calculated trend and associated temperature changes and suggest time scales required to establish robust trends. The largest trends and associated temperature changes are all positive and have occurred over periods ending in recent years. Substantial positive changes also occurred from the early twentieth century until the mid-1940s. The continents exhibit greater long-term warming than the global average overall, but less warming in the early part of the century (segments ending in the 1940s). The recent period of short-term cooling beginning in the late 1990s is neither statistically significant nor unusual in the context of trend variability in the full historical record. Global-mean and land surface temperature changes for periods ending in recent years and longer than about 90 years are extremely unlikely to have occurred by chance. In contrast, short-term trends over less than a few decades are generally not statistically significant. This implies significant contributions of decadal variability to trends estimated over such short time periods.Digital Object Identifier http://dx.doi.org/10.1175/2010BAMS3030.1
机译:计算了1850年至2009年之间历史记录的所有可能期间的年度全球地表温度和全球地表温度趋势。二维参数图显示了选择开始和结束年份对计算趋势和相关温度变化的关键影响并建议建立稳固趋势所需的时间范围。最大的趋势和相关的温度变化都是正的,并且发生在最近几年结束的时期内。从20世纪初到1940年代中期,也发生了重大的积极变化。各大洲的长期变暖幅度高于全球平均水平,但在本世纪初变暖幅度较小(段于1940年代结束)。从整个历史记录的趋势变化来看,1990年代后期开始的近期短期降温既没有统计学意义,也没有异常。在最近几年结束的超过90年的全球平均和陆地表面温度变化极不可能是偶然发生的。相反,少于几十年的短期趋势通常在统计上并不显着。这意味着十年间的可变性对如此短的时间段内估计的趋势做出了重大贡献。数字对象标识符http://dx.doi.org/10.1175/2010BAMS3030.1

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