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A Review of some Recent Radiation Fog Prediction Studies and the Results of Integrating a Simple Numerical Model to Predict Radiation Fog over Brunei

机译:近期一些关于辐射雾的预测研究综述以及整合简单数值模型预测文莱辐射雾的结果

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— Several radiation fog studies with emphasis on numerical simulation and prediction are reviewed. One of the earliest attempts started with a given surface diurnal variation of temperature and water vapor, and concluded by forecasting the onset of saturation at various levels; thus fog, by examining the spread of temperature and moisture in the vertical. The one-dimensional (1-D) models are still popular. Some of the recent numerical simulations use more than 100 levels in the vertical and treat various kinds of vegetation, aerosols, and soils with moisture contents. Some also employ a mesoscale model in conjunction with a 1-D model to consider the advective effects. In the following a simple 1-D numerical model was used to predict the onset of fog at Brunei, based on a desktop computer and routine surface observations of dry bulb temperature (T), dewpoint temperature (T d ), and wind speed at 1800 Local Time (LT). Optimism exists in improved predictions of fog and stratus as 1-D models incorporate many physical processes, and mesoscale models continue to improve in predicting advection and cloud cover.
机译:—回顾了一些辐射雾研究,重点是数值模拟和预测。最早的尝试之一是从给定的地面温度和水蒸气的昼夜变化开始,并通过预测各种水平的饱和开始而得出结论。通过检查垂直方向上的温度和湿度的分布来确定雾气。一维(1-D)模型仍然很流行。最近的一些数值模拟在垂直方向上使用了100多个水平,并处理了各种具有水分含量的植被,气溶胶和土壤。有些人还采用中尺度模型和一维模型来考虑对流效应。以下基于台式计算机和干球温度(T),露点温度(T d )和常规温度的常规表面观测,使用简单的一维数值模型来预测文莱的起雾。风速为1800当地时间(LT)。由于一维模型包含了许多物理过程,因此对雾和地层的改进预测中存在乐观主义,而中尺度模型在对流和云层覆盖的预测中也不断提高。

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