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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Trends of surface solar radiation in unforced CMIP5 simulations
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Trends of surface solar radiation in unforced CMIP5 simulations

机译:趋势在非受迫性表面太阳辐射CMIP5模拟

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We consider decadal scale trends of annual mean all-sky surface solar radiation (SSR) that occur solely because of internal variability of the climate system. We give statistical estimates of their magnitude and probability of occurrence. The estimates are based on 43 preindustrial control (piControl) experiments of the Coupled Model Intercomparison Project phase 5 (CMIP5). Trends are found to depend strongly on geographical region and on whether they are quantified in absolute units or relative to the long-term mean SSR. We find it to be sufficient to provide one map for absolute and one for relative trends, as approximate analytical relations are shown to hold between trends of different length and likelihood and the standard deviation of the underlying SSR time series. We estimate that a positive trend over 30 years and with 25 chance of occurrence (75th percentile of all possible trends) has a magnitude between 0.15 and 1.7 W/m2/decade or 0.11 and 1.4 of long-term mean SSR per decade, depending on geographical location. Comparison with present-day observations and intermodel spread suggests an average uncertainty of these estimates of about 30. Intermodel spread suggests that regional uncertainties can be up to about 3 times larger or smaller. We give examples of how these results may be used to obtain statistical estimates of how (un)likely it is that observed SSR trends or part thereof are due to internal variability alone.
机译:我们考虑年平均的年代际尺度的趋势全天表面太阳辐射(SSR)发生仅仅因为内部的变化气候系统。他们的大小和发生概率。估计是基于43工业化前的控制(piControl)耦合的实验模型相互比较项目阶段5 (CMIP5)。趋势是强烈依赖地理区域和是否量化的绝对或相对于单位长期代表苏维埃社会主义共和国。提供一个绝对的地图,一个用于相对趋势近似分析趋势之间的关系所持有不同的长度和可能性和标准偏差的底层SSR时间序列。超过30年,估计一个积极的趋势有25%的几率发生(第75百分位0.15之间的所有可能的趋势)级和1.7 W / m2 /十年的长期或0.11和1.4%平均每十年SSR,取决于地理的位置。观察和intermodel传播提出了一个平均这些估计的不确定性30%。不确定性可以约3倍或更小。可用于获得的统计估计(联合国)可能是如何观察SSR趋势还是部分是由于内部的变化一个人。

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