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Errors in climate model daily precipitation and temperature output: time invariance and implications for bias correction

机译:气候模式每日降水量和温度输出的误差:时间不变性及其对偏差校正的影响

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When correcting for biases in general circulation model (GCM) output, for example when statistically downscaling for regional and local impacts studies, a common assumption is that the GCM biases can be characterized by comparing model simulations and observations for a historical period. We demonstrate some complications in this assumption, with GCM biases varying between mean and extreme values and for different sets of historical years. Daily precipitation and maximum and minimum temperature from late 20th century simulations by four GCMs over the United States were compared to gridded observations. Using random years from the historical record we select a "base" set and a 10 yr independent "projected" set. We compare differences in biases between these sets at median and extreme percentiles. On average a base set with as few as 4 randomly-selected years is often adequate to characterize the biases in daily GCM precipitation and temperature, at both median and extreme values; 12 yr provided higher confidence that bias correction would be successful. This suggests that some of the GCM bias is time invariant. When characterizing bias with a set of consecutive years, the set must be long enough to accommodate regional low frequency variability, since the bias also exhibits this variability. Newer climate models included in the Intergovernmental Panel on Climate Change fifth assessment will allow extending this study for a longer observational period and to finer scales.
机译:在校正一般循环模型(GCM)输出中的偏差时,例如在对区域和局部影响研究进行统计缩减时,通常的假设是,可以通过比较历史时期的模型模拟和观察结果来表征GCM偏差。我们证明了这种假设的一些复杂性,GCM偏差在平均值和极值之间以及不同的历史年份之间变化。将美国四个GCM在20世纪末进行的模拟得出的每日降水量和最高和最低温度与网格观测结果进行了比较。使用历史记录中的随机年份,我们选择一个“基准”集和一个10年独立的“预计”集。我们在中位数和极端百分位数之间比较这些集合之间的偏差差异。平均而言,只有4个随机选择年份的基本集通常足以表征每日GCM降水量和温度的偏差(中值和极值)。 12年为偏倚校正将成功提供了更高的信心。这表明某些GCM偏差是时间不变的。当用一组连续的年份来描述偏差时,该组必须足够长以适应区域低频变化,因为该偏差也表现出这种变化。政府间气候变化专门委员会第五次评估中包括的较新的气候模型将使这项研究的观察期更长,规模更小。

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