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首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >On an improvement of UV index forecast: UV index diagnosis and forecast for Belsk, Poland, in Spring/Summer 1999
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On an improvement of UV index forecast: UV index diagnosis and forecast for Belsk, Poland, in Spring/Summer 1999

机译:关于紫外线指数预报的改进:1999年春季/夏季波兰贝尔斯克的紫外线指数诊断和预报

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摘要

A forecast of the UV index for the following day is presented. The standard approach to the UV index modelling is applied, i.e., the clear-sky UV index is multiplied by the UV cloud transmission factor. The input to the clear-sky model (tropospheric ultraviolet and visible-TUV model, Madronich, in: M. Tevini (Ed.), Environmental Effects of Ultraviolet Radiation, Lewis Publisher, Boca Raton, 1993, p. 17) consists of the total ozone forecast (by a regression model using the observed and forecasted meteorological variables taken as the initial values of aviation (AVN) global model and their 24-hour forecasts, respectively) and aerosols optical depth (AOD) forecast (assumed persistence). The cloud transmission factor forecast is inferred from the 24-h AVN model run for the total (Sun + sky) solar irradiance at noon. The model is validated comparing the UV index forecasts with the observed values, which are derived from the daily pattern of the UV erythemal irradiance taken at Belsk (52°N, 21°E), Poland, by means of the UV Biometer Solar model 501A for the period May-September 1999. Eighty[one percent and 92% of all forecasts fall into ±1 and ±2 index unit range, respectively. Underestimation of UV index occurs only in 15%. Thus, the model gives a high security in Sun protection for the public. It is found that in ~35% of all cases a more accurate forecast of AOD is needed to estimate the daily maximum of clear-sky irradiance with the error not exceeding 5%. The assumption of the persistence of the cloud characteristics appears as an alternative to the 24-h forecast of the cloud transmission factor in the case when the AVN prognoses are not available.
机译:给出了第二天紫外线指数的预测。应用了紫外线指数建模的标准方法,即,将晴空紫外线指数乘以紫外线云透射因子。晴空模型的输入(对流层紫外线和可见-TUV模型,Madronich,见:M。Tevini(编辑),《紫外线辐射的环境影响》,Lewis Publisher,Boca Raton,1993,第17页)。臭氧总量预测(通过将观测和预测的气象变量分别用作航空(AVN)全球模型的初始值和其24小时预报的回归模型)和气溶胶光学深度(AOD)预报(假定的持久性)。云传输因子预测是根据针对中午的总(太阳+天空)太阳辐照度运行的24小时AVN模型得出的。通过将紫外线指数预测值与观测值进行比较,验证了该模型的有效性,该值是根据紫外线生物计量仪太阳能模型501A从波兰Belsk(52°N,21°E)拍摄的紫外线红斑日照的每日模式得出的在1999年5月至9月期间。所有预测的百分之八十[%]和[92%]分别落入±1和±2指数单位范围。紫外线指数的低估仅发生在15%。因此,该模型为公众提供了高度的防晒保护。发现在所有情况的约35%中,需要更准确的AOD预测来估计晴空辐射的日最大值,且误差不超过5%。在没有AVN预测的情况下,假设云特征的持久性似乎可以替代24小时的云传输因子预测。

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