DISTRIBUTION OF PRECIPITABLE WATER IN SOUTHERN GREECE IN SUPPORT OF SOLAR RADIATION MODELS

N. Chrysoulakis, C. Cartalis
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引用次数: 4

Abstract

Precipitable water by reflecting the total water vapour amount in zenith direction between the surface of the earth and the top of the atmosphere is considered an important parameter for soiar radiation models. However, lack of ground data and/or radiosoundings in the examined area results in the inability to calculate precipitable water with further implications in the results of solar radiation models. The aim of this study is the estimation of the probability distribution function of the annual mean of precipitable water for Southern Greece. For the purposes of the study, radiosoundings of the National Meteorological Agency at Hellinicon station were used to obtain the daily values of water vapour for the period 1974-1995. Results were compared to measurements to show satisfactory agreement, a fact which allows their use for solar energy studies – as well as for energy budget calculations – in Southern Greece where in situ measurements are missing.
希腊南部可降水量分布,支持太阳辐射模型
反映地球表面与大气顶部之间天顶方向水汽总量的可降水量被认为是太阳辐射模式的一个重要参数。但是,由于研究地区缺乏地面数据和(或)无线电探测,因此无法计算可降水量,从而进一步影响太阳辐射模式的结果。本研究的目的是估计希腊南部年平均可降水量的概率分布函数。为了进行这项研究,使用了国家气象厅在Hellinicon站的无线电探测来获得1974-1995年期间的每日水蒸汽值。结果与测量结果进行了比较,显示出令人满意的一致性,这一事实允许它们用于太阳能研究——以及用于能源预算计算——在希腊南部,那里没有现场测量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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