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Sensitivity Analysis of Atmospheric Dispersion Simulations by FLEXPART to the WRF-Simulated Meteorological Predictions in a Coastal Environment

机译:FLEXPART对WRF模拟的沿海天气预报的大气弥散模拟的敏感性分析

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In this study the sensitivity of the atmospheric dispersion model FLEXPART-WRF to the meteorological data inputs simulated by the mesoscale model ARW in the Kalpakkam coastal environment is examined. High-resolution simulations are conducted with ARW using four alternative planetary boundary layer parameterizations (YSU, MYNN, ACM2 and BL) for a typical period 14-22 Sep 2010 characterized with wide variability in atmospheric flow conditions at the coastal site. Observations generated through a field meteorological experiment are used to study the model sensitivity. Wind field, mixed layer depth, temperature and friction velocity are considered as parameters to evaluate dispersion uncertainty from FLEXPART. Results indicate that the simulated dispersion patterns are influenced by meteorological model forecasts using various boundary layer physics options. It has been found that the ensemble mean of all the meteorological members is closer to the observations than the individual cases. Of the various members the YSU and MYNN are found to give best meteorological simulations in the ensemble. The computed dispersion with various meteorological members indicate that ACM2 and BL simulate highest and least diffusivities leading to widely spread plume in the case of ACM2 and relatively narrow plume with BL, respectively. The ensemble mean of all the simulations is found to yield a better representation of the plume under various possible atmospheric conditions. The meteorological members YSU and MYNN are found to give minimum variance and fractional bias with respect to the ensemble. The minimum uncertainty in tracer concentration estimates due to meteorological uncertainty is -30 to 30 % obtained with MYNN. The results demonstrate that the dispersion model results are sensitive to the mesoscale model meteorological simulations.
机译:在这项研究中,考察了卡尔帕卡姆沿海环境中大气扩散模型FLEXPART-WRF对中尺度模型ARW模拟的气象数据输入的敏感性。在2010年9月14日至22日的典型时​​间段内,使用四个替代行星边界层参数化设置(YSU,MYNN,ACM2和BL),使用ARW进行了高分辨率模拟,其特征是沿海站点的大气流动条件存在较大差异。通过现场气象实验产生的观测值用于研究模型的敏感性。风场,混合层深度,温度和摩擦速度被视为评估FLEXPART色散不确定性的参数。结果表明,使用各种边界层物理方法,模拟的色散模式受气象模型预测的影响。已经发现,与个别情况相比,所有气象成员的集合平均数更接近观测值。在各个成员中,YSU和MYNN在集合中可提供最佳的气象模拟。计算得出的具有各种气象成员的色散表明,ACM2和BL模拟最高和最小扩散率,分别导致在ACM2情况下烟羽广泛散布和带有BL的相对狭窄烟羽。在所有可能的大气条件下,所有模拟的集合均值可以更好地表示羽状流。发现气象成员YSU和MYNN相对于整体具有最小的方差和分数偏差。由于气象不确定性,示踪剂浓度估计值的最小不确定性为MYNN获得的-30%至30%。结果表明,色散模型结果对中尺度模型的气象模拟很敏感。

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