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The space-time correlation structure of convective rainstorms in the Lagrangian reference frame.

机译:拉格朗日参考系中对流暴雨的时空相关结构。

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This dissertation investigates the statistical nature of subsynoptic, convective rainfall using data from the Convective Initiation Downburst Experiment conducted in Denver, Colorado in 1987. Forty-six PAM network gages, mean spacing of 10.6 km, and 31 FLOWS network gages, mean spacing of 2.4 km were utilized. Both had a measurement time interval of 1 minute.; Thirteen rainfall events are isolated from the raw data and used in this study. The storms included raincells, cell clusters and small mesoscale areas. The average storm speed from the FLOWS and PAM events is 76.5 km/hr and 56.4 km/hr, respectively. The predominant direction of storm movement is at an azimuth between 90{dollar}spcirc{dollar} and 180{dollar}spcirc.{dollar}; The structure of rainstorms relative to the fixed Eulerian reference frame are examined using spatial cross-correlation. Curves of correlation coefficient versus gage separation distance are plotted for all possible pairs of stations. As expected, the correlation coefficient increases as the gage separation distance decreases and as the data time averaging interval increases.; Storm kinematics is the primary cause of data scatter and low levels of correlation for the measured Eulerian rainfall fields. An analysis in the Lagrangian reference frame, moving with the center of mass of the storm, is proposed to minimize data scatter and obtain correlations representative of the internal structure of the rainfall event. The Lagrangian transformation technique consists of three steps: (1) estimation of storm kinematics; (2) spatial interpolation of the Eulerian rainfall field and (3) construction of the Lagrangian rainfall field.; The spatial cross-correlations are then recomputed and compared to the original Eulerian spatial correlation plots. Considerable improvement is seen in the Lagrangian correlation levels with greatly reduced data scatter. For five rainstorms the minimum increase in average correlation coefficient was 0.53 while the largest increase was 1.11.; The final objective of this study was to demonstrate that stochastic generation of the Lagrangian fields was possible with a simple rainfall model. A first-order autoregressive scheme with a random component was used. Spatial correlation curves, computed from numerous realizations of Lagrangian rainfall fields generated using this model, match the correlation of the rainstorms used in model calibration.
机译:本文利用1987年在科罗拉多州丹佛市进行的对流启动Downburst实验的数据,研究了亚热带对流降雨的统计性质。46个PAM网络量规,平均间距为10.6 km,31个FLOWS网络量规,平均间距为2.4公里被利用。两者的测量时间间隔均为1分钟。从原始数据中分离出13个降雨事件,并将其用于本研究。暴风雨包括雨单元,细胞簇和中小型规模的区域。 FLOWS和PAM事件的平均风暴速度分别为76.5 km / hr和56.4 km / hr。风暴运动的主要方向是在90度和180度之间的方位角。相对于固定的欧拉参考系,暴雨的结构使用空间互相关进行了检验。对于所有可能的站对,绘制了相关系数与量规间距的关系曲线。如所期望的,相关系数随着量规间距的减小和数据时间平均间隔的增大而增大。风暴运动学是造成数据分散和相关的低水平欧拉雨场的主要原因。提出了在拉格朗日参考系中以风暴的质心为中心进行分析的方法,以最大程度地减少数据散布并获得代表降雨事件内部结构的相关性。拉格朗日变换技术包括三个步骤:(1)风暴运动学估计; (2)欧拉降雨场的空间插值;(3)拉格朗日降雨场的构建。然后重新计算空间互相关,并将其与原始欧拉空间相关图进行比较。拉格朗日相关性水平有了很大的改善,数据散布大大减少了。对于五场暴雨,平均相关系数的最小增加为0.53,最大增加为1.11。这项研究的最终目的是证明通过简单的降雨模型可以随机产生拉格朗日油田。使用具有随机分量的一阶自回归方案。通过使用此模型生成的拉格朗日降雨场的多种实现计算出的空间相关曲线与模型校准中使用的暴雨的相关性相匹配。

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