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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Quantitative scenarios for future hydrologic extremes in the US Southern Great Plains
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Quantitative scenarios for future hydrologic extremes in the US Southern Great Plains

机译:美国南部大平原未来水文极端的定量情景

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摘要

Decision-makers using climate projection information are often faced with the problem of data breadth, complexity, and uncertainty, which complicates the translation of climate science products in addressing management challenges. Recently, the concept of climate scenario planning attempts to simplify climate information by developing a series of plausible future storylines. In some cases, however, these storylines lack quantitative detail on extremes that may be useful to decision-makers. Here, we analyse a large suite of statistically downscaled climate projections from two methods to develop quantitative projections for hydrologic extremes (heavy precipitation and drought) across Oklahoma and Texas in the United States. Downscaled projections are grouped into four specific temperature/precipitation scenarios, including Warm/Wet, Hot/Dry, Central Tendency, and the full multi-model ensemble average. The region is split into three sub-domains spanning the region's west-east precipitation gradient, and projections are examined throughout the mid- and late-21st century, using two emissions scenarios (mid-range and high). Most scenarios project increased frequency and duration of moderate or greater drought across the whole domain, with the high-emissions Hot/Dry projections showing the most severe examples. The Warm/Wet scenario also increases the frequency of dry months, particularly in the Southern High Plains, but does not discernably alter duration, and retains a similar frequency of pluvial (wet) periods. The mid-range projections generally retain similar evolutions among scenarios, but they reduce drought intensity and project no change in drought/pluvial frequency with the Warm/Wet scenario. Notably, the occurrence of intense precipitation increases across all scenarios and emissions categories and does not significantly differ between any of the scenarios, including Hot/Dry versus Warm/Wet. Some observed differences in extreme precipitation magnitudes between
机译:使用气候投影信息的决策者通常面临数据广度,复杂性和不确定性的问题,这使气候科学产品翻译在解决管理挑战中。最近,气候情景计划的概念试图通过开发一系列合理的未来故事情节来简化气候信息。然而,在某些情况下,这些故事列表缺乏对决策者可能有用的极端情况的定量细节。在这里,我们分析了两种统计上较低的气候投影,从两种方法中开发了在俄克拉荷马州和德克萨斯州的水文极端(重沉淀和干旱)的定量投影。将次要投影分为四个特定的温度/降水场景,包括暖/湿,热/干,中央趋势和全多模型集合平均值。该地区分为三个跨越该地区的西部降水梯度的子域,并在21世纪中期和21世纪中期进行预测,使用两个排放场景(中档和高)。大多数情景项目跨越整个领域的中等或更大干旱的频率和持续时间增加,具有高排放热/干投影,显示最严重的例子。温暖/湿式场景还增加了干燥的月份的频率,特别是在南部高平原中,但不能明确地改变持续时间,并保留类似的普华(湿)时段的频率。中档投影通常会在场景之间保持类似的演变,但它们会降低干旱强度和项目,没有温暖/潮湿场景的干旱/潜伏频率的变化。值得注意的是,在所有场景和排放类别中发生强烈降水量的发生,并且在任何情景之间没有显着差异,包括热/干与湿/湿。一些观察到的极端降水量之间的差异

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