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A GUST-FACTOR CRITERION FOR RAPID DETERMINATION OF ATMOSPHERIC STABILITY AND MIXING HEIGHT FOR OVERWATER DISPERSION ESTIMATES

机译:快速确定大气弥散度的大气稳定性和混合高度的古斯特因子准则

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摘要

In order to estimate atmospheric pollution concentration downwind from its source, meteorological models (numerical, analytical, or graphical) are usually employed. Included in the model inputs are atmospheric stability and mixing height, which are not routinely measured in the marine environment. On the basis of relationships amongst gust factor, turbulence intensity, and stability parameter, methods are developed for rapid estimation of these two inputs. It is found that, based on the stability classification of the Offshore and Coastal Dispersion Model, when the gust factor (G, which is the ratio of peak gust to the sustained wind speed) is between 1.15 and 1.45, the stability is near-neutral. When G is less than 1.15, it is stable, and for G greater than 1.45, unstable. Using routine buoy measurements as a composite characteristic, equations for the mixing height under various stability classes are also formulated.
机译:为了从源头估算顺风而下的大气污染浓度,通常采用气象模型(数值,分析或图形)。模型输入中包括大气稳定性和混合高度,这在海洋环境中通常无法测量。基于阵风因子,湍流强度和稳定性参数之间的关系,开发了用于快速估计这两个输入的方法。根据近海和海岸扩散模型的稳定性分类,发现阵风因子(G,即阵风的峰值与持续风速之比)在1.15和1.45之间时,稳定性接近中性。当G小于1.15时,它是稳定的;对于G大于1.45时,它是不稳定的。使用常规浮标测量作为综合特征,还可以得出各种稳定性等级下的混合高度方程。

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