用于拟合源和受体数据集的自回归大气色散模型

M. Mulholland
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引用次数: 5

摘要

本文提出了一种对不同位置的排放和浓度进行递归预测的方法,该方法符合大气色散模型,但与同一点的观测值有最小二乘偏差。作为副产品,该技术在每个时间步上产生浓度分布网格。这种稳健的程序使有争议的数据合理化,并充分利用不完整的源或受体观察记录。因此,在通过剩余观测记录的程序步骤中,可以在线估计几个未知的源率。利用伪谱法的子网格自适应,将精确的平流扩散解表述为每个时间步长的线性变换。利用第0、第1和第2垂直集中力矩,将其扩展到垂直维度,只允许均匀的风廓线,但在水平方向上风场和扩散系数逐渐变化。然后,一个离散的Kaiman滤波器提供所有源速率的最佳估计,构成状态向量,以最小化任何源和受体观察的偏差。该算法已在东德兰士瓦高原90公里× 90公里的区域应用,包括9个SO2源和8个探测器。有迹象表明,该方法将是解释此类数据集的有价值的辅助手段。
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An autoregressive atmospheric dispersion model for fitting combined source and receptor data sets

A method is developed for recursive prediction of emissions and concentrations at various positions, which obey an atmospheric dispersion model, yet have a least squares deviation from observations at the same points. As a by-product, the technique yields a concentration distribution grid on each time-step. This robust procedure rationalizes data which are in dispute, and makes optimal use of incomplete source or receptor observation records. Thus several unknown source-rates may be estimated on-line as the procedure steps through the remaining observation records. An accurate advection-diffusion solution is formulated as a linear transformation for each time-step, using a sub-grid adaptation of the pseudospectral method. This is extended to the vertical dimension using the zeroth, first and second vertical moments of concentration, allowing only uniform wind profiles, but gradual wind-field and diffusivity variations in the horizontal. A discrete Kaiman filter then provides optimal estimates of all source rates, constituting the state vector, to minimize deviations from any source and receptor observations. The algorithm has been applied in a 90 km × 90 km region of the Eastern Transvaal Highveld, including nine SO2 sources and eight detectors. Indications are that the method will be a valuable aid in interpreting such data sets.

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