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首页> 外文期刊>Journal of hydrometeorology >Quantifying the strength of soil moisture-precipitation coupling and its sensitivity to changes in surface water budget
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Quantifying the strength of soil moisture-precipitation coupling and its sensitivity to changes in surface water budget

机译:量化土壤水分-降水耦合的强度及其对地表水收支变化的敏感性

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This paper presents a new index to quantify the strength of soil moisture-precipitation coupling in AGCMs and explores how the soil moisture-precipitation coupling in Community Atmosphere Model version 3 (CAM3)-Community Land Model version 3 (CAM3-CLM3) responds to parameterization-induced surface water budget changes. Specifically, this study (a) compares the regions of strong coupling identified by the newly proposed index and the index currently used in the Global Land-Atmosphere Coupling Experiment (GLACE); (b) examines how the surface water budget changes influence the strength of soil moisture-precipitation coupling as measured by the two indexes, respectively; and (c) examines how these changes influence the memory of the coupled land-atmosphere system as measured by the correlation between soil moisture and subsequent precipitation. The new index and the GLACE index are consistent in identifying central North America and West Africa as major regions of strong coupling during June August (JJA). However, in some areas of western Europe and of subtropical South America where the GLACE index is low, the new index suggests a modest significant coupling during JJA. In response to the surface water budget changes that presumably favor a stronger soil moisture-precipitation coupling, the new index increases, but the GLACE index decreases in a majority of the regions of modest-to-strong coupling, although both show some mixed response. Changes in the land-atmosphere system memory suggest an increase of coupling strength, consistent with results from the new index. The strong dependence of the GLACE index on the relative importance of atmospheric internal variability is identified as a potential cause for the differences between the two indexes. The two indexes emphasize different aspects of soil moisture - precipitation coupling, and one might be more suitable than the other depending on the purpose of individual studies.
机译:本文提出了一个新的指标来量化AGCM中土壤水分-降水耦合的强度,并探讨了社区大气模型版本3(CAM3)-社区土地模型3(CAM3-CLM3)中的土壤水分-降水耦合如何响应参数化引起的地表水预算变化。具体而言,这项研究(a)比较了新提出的指数和全球陆地-大气耦合实验(GLACE)中当前使用的指数确定的强耦合区域; (b)考察地表水收支的变化如何分别通过两个指标来衡量对土壤水分-降水耦合强度的影响; (c)研究这些变化如何影响耦合的陆地-大气系统的记忆,这是通过土壤水分和随后的降水之间的相关性来衡量的。新的指数和GLACE指数一致地确定了北美中部和西非为8月(JJA)期间强耦合的主要区域。但是,在GLACE指数较低的西欧和亚热带南美地区,新指数表明在JJA期间存在适度的显着耦合。响应于可能有利于更强土壤水分-降水耦合的地表水收支变化,新指数增加,但是在大多数中等至强耦合区域中,GLACE指数下降,尽管两者均表现出一些混合响应。陆地-大气系统记忆的变化表明耦合强度的增加,与新指标的结果一致。 GLACE指数对大气内部变化的相对重要性的强烈依赖性被确定为这两个指数之间差异的潜在原因。两项指标强调了土壤水分的不同方面-降水耦合,根据个人研究的目的,其中一项可能比另一项更适合。

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