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首页> 外文期刊>Journal of Hydrology >Exploring stochastic climate uncertainty in space and time using a gridded hourly weather generator
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Exploring stochastic climate uncertainty in space and time using a gridded hourly weather generator

机译:使用网格小时天气发生器探索空间和时间的随机气候不确定性

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Exploring the effects of climate change on the hydrological response at the local scale requires climate data at high spatial and temporal resolutions. This is best achieved by generating downscaled ensembles of future climate variables derived from climate models. For this purpose we present a methodology to re-parameterize the AWE-GEN-2d model (Advanced WEather GENerator for a two-dimensional grid). The model simulates key meteorological variables needed by hydrological models and is particularly suitable to explore the effects of stochastic (natural) climatic uncertainty, which is fundamental for hydrological applications, especially at sub-kilometer and hourly scales. Factors of change for different climate statistics are calculated from climate model simulations of present and future climates and subsequently applied to the statistics derived from observations to re-parameterize AWE-GEN-2d. The model abilities in generating an ensemble of future climate variables for the transient period 2020-2089 is presented with examples of precipitation and near-surface air temperature fields from hourly to multi-annual scales for a small mountainous region in the Swiss Alps. The stochastic uncertainty is examined for present and future periods and for spatial scales from the RCM scale (12-km, daily) to 2-km demonstrating the potential use of AWE-GEN-2d outputs. At the RCM scale, model results yield a small increase in annual precipitation (4%) which is within the stochastic uncertainty range for present and future periods (7%). At the fine scale of 2-km, the increase in annual precipitation can exceed the stochastic uncertainty, but for less than 10% of the domain area. On the contrary, changes in annual near-surface air temperature exceed stochastic uncertainty both at the RCM and finer scales. Stochastic climate uncertainty was concluded to be very similar when comparing present and future periods and 12-km and 2-km scales. The benefits of using AWE-GEN-2d in hydrologica
机译:探索气候变化对当地水文响应的影响需要高空间和时间分辨率的气候数据。通过产生从气候模型的未来气候变量的次要集合来实现这一目标。为此目的,我们提出了一种方法来重新参数化AWE-GEN-2D模型(用于二维网格的高级天气发生器)。该模型模拟水文模型所需的关键气象变量,特别适用于探索随机(自然)气候不确定性的影响,这是水文应用的基础,特别是在亚千米和每小时尺度。改变为不同的气候统计的因子是从当前和未来的气候的气候模式模拟计算,并且随后施加到从观测衍生重新参数AWE-GEN-2d中的统计信息。产生瞬态期202089的未来气候变量的集合的模型能力,提出了从小到瑞士阿尔卑斯山区小山区的多年尺度的沉淀和近表面空气温度场的实例。随机不确定性被检查为现在和未来的时间,以及从RCM秤(每日12公里)的空间秤到2公里,展示了AWE-GEN-2D输出的潜在使用。在RCM规模,模型结果产生的年降水量小(4%),其在目前和未来期间的随机不确定性范围内(7%)。在2公里的细度下,年降水量的增加可能超过随机性的不确定性,但占域区域的10%。相反,年度近表面空气温度的变化在RCM和更精细的尺度上超过随机不确定性。在比较现在和未来时期和12公里和2公里的秤时,结论时,随机气候不确定性得出结论是非常相似的。在水中武器中使用AWE-GEN-2D的好处

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