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Comparative study of atmospheric water vapor budget associated with precipitation in Central US and eastern Mediterranean

机译:美国中部和地中海东部与降水相关的大气水汽收支比较研究

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Water vapor budget (WVB) analysis is a powerful tool for studying processesleading to precipitation (P), since the linkages among atmospheric dynamics,water vapor fields, surface conditions, and P are constrained by themoisture continuity equation. This paper compares WVB calculations over theUS Midwest (MW), the US Southern Great Plains (SGP), and the easternMediterranean Sea (EM) during their seasons of maximum P. Despite theinter-regional differences in time of year, size of region, and surfacecharacteristics, the WVBs over these regions have common features. First,the change in precipitable water (dPW) is highly correlated with themoisture flux divergence (MFD) and not evaporation (E), implying thatatmospheric humidity is affected more by the large-scale atmosphericcirculation than land-atmosphere interactions. Second, P is positivelycorrelated with moisture inflow (IF/A). However, a pronounced differenceexists between the North American and the Mediterranean study regions withrespect to the processes associated with increased P. For the MW and theSGP, increased P is associated with moisture flux convergence (−MFD) due toincreased IF/A. In contrast, increased P over the EM is not associated with−MFD, since both the outflow (OF/A) and IF/A increase at similar rates.Recycling ratio (R) estimates were calculated for each region using anequation previously developed. The moisture recycling methodology involvesthe externally advected versus locally evaporated contributions to P beingexpressed in terms of a "bulk" formulation in which IF/A and OF/A aredefined at the boundaries of the study area. Due to its scale dependence, Rcannot be directly compared among the different regions, and a normalizationprocedure was developed for this comparative study. Its results suggest thenormalized R ranges between 12-25% for the study regions, with the valuefor the oceanic EM being somewhat larger than over the continental MW andSGP.
机译:水蒸气收支(WVB)分析是研究导致降水(P)的过程的强大工具,因为大气动力学,水蒸气场,地表条件和P之间的联系受湿度连续性方程约束。本文比较了美国中西部(MW),美国南部大平原(SGP)和东部地中海(EM)在最大P季节内的WVB计算。尽管每年时间,区域大小和区域之间存在区域间差异,在表面特征上,这些区域上的WVB具有共同的特征。首先,可降水量(dPW)的变化与水分通量散度(MFD)高度相关,而与蒸发量(E)高度相关,这意味着大气湿度受大规模大气环流的影响大于与陆地-大气相互作用的影响。其次,P与水分流入(IF / A )呈正相关。但是,在北美和地中海研究地区之间,与磷增加有关的过程之间存在明显差异。对于中分子量和标准GP,由于IF / 增加,磷增加与水分通量收敛(-MFD)有关。 / i>。相反,由于流出量(OF / A )和IF / A 都以相似的速率增加,因此EM上方的P增加与-MFD不相关。使用先前开发的等式,计算每个区域的回收率(Ri)。水分循环利用方法涉及以P的形式表示外部对P和局部蒸发对P的贡献,其中IF / A 和OF / A 被定义为学习区。由于其规模依赖性,不能在不同区域之间直接比较 R ,因此为该比较研究开发了归一化程序。其结果表明,研究区域的标准化 R 范围在12%至25%之间,海洋EM的值略大于大陆MW和SGP的值。

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