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Solar irradiation retrieval in Cameroon from Meteosat satellite imagery using the Heliosat_2 method

机译:使用Heliosat_2方法从Meteosat卫星影像中获取喀麦隆的太阳辐射

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The radiation climate of Cameroon is not well known. Measurements of global and diffuse incident solar irradiations were carried out from 1982 to 1987 in ten meteorological stations throughout the country using Eppley PSP pyranometers. The distance between two neighboring stations was about 200 km. This ambitious program of collecting solar radiation data throughout the Cameroon territory was abruptly stopped in 1987 because the maintenance of the pyranometers network together with the monthly field data collection became too cumbersome and costly. It therefore became necessary to look for a valuable tool to retrieve incident solar irradiation from low cost satellite imagery such as the geostationary Meteosat satellite data. In this work we use a method referred to as Heliosat_2, well documented in [12, 13], and developed by Wald and his co-workers Rigollier and Lefèvre. This method, which uses known models of physical processes in atmospheric optics, consists of first calculating the atmospheric cloud index for each pixel from images acquired in the visible band of the Meteosat sensor. The cloud index is then related to the pixel clear sky index defined as the ratio of the observed irradiation to the clear sky irradiation that should be observed at the pixel site at that instant. The computation of the clear sky irradiation is done by solving the radiative transfer equation in a cloud free atmosphere as documented in the European Solar Radiation Atlas (ESRA 2000). We have performed calculations of incident solar irradiations over the Cameroon territory using 5 km resolution Meteosat imagery of the year 1997 available from the Modeling and Remote Sensing Group of the Ecole des Mines de Paris based at Sophia Antipolis. A real advantage with the Heliosat method is that we can calculate the incident solar radiation for contiguous pixels. To assess the performances of the method for African sites we have compared the solar irradiation values derived from Meteosat data using the Heliosat_2 method to ground measurements available in Yaoundé (3°52’ N ; 11°32’ E) and Garoua (9°20’ N ; 13°23’ E). We observed that the accuracy of the Heliosat method is very satisfactory for the monthly variations of the daily solar irradiations in sahelian sites, while in forest sites the variations of the retrieved irradiations do not fit the measurements. The accuracy of the Heliosat_2 method could be greatly improved if the method was implemented using all the “high resolution” Meteosat data received every half an hour in a day; the computations of the daily irradiations might therefore be more accurate.
机译:喀麦隆的辐射气候尚不清楚。 1982年至1987年,使用Eppley PSP太阳总辐射计在全国10个气象站进行了全球太阳辐射和漫射太阳辐射的测量。两个相邻站点之间的距离约为200公里。这项雄心勃勃的计划在整个喀麦隆领土范围内收集太阳辐射数据,该计划于1987年被突然终止,因为总辐射表网络的维护以及每月现场数据的收集变得过于繁琐和昂贵。因此,有必要寻找一种有价值的工具,以从低成本卫星图像(如对地静止气象卫星数据)中检索入射的太阳辐射。在这项工作中,我们使用一种称为Heliosat_2的方法,该方法在[12,13]中有充分记载,并且由Wald及其同事Rigollier和Lefèvre开发。该方法使用大气光学中的物理过程的已知模型,该方法包括首先根据在Meteosat传感器可见带中获取的图像为每个像素计算大气云指数。然后将云指数与像素晴空指数相关联,该像素晴空指数定义为在该瞬间在像素位置处应观察到的观测辐射与晴空辐射的比率。如欧洲太阳辐射图集(ESRA 2000)所述,通过求解无云大气中的辐射传递方程,可以计算出晴朗的天空辐射。我们使用位于索菲亚安提波利斯的巴黎矿业学院的建模和遥感小组提供的5公里分辨率的1997年Meteosat影像对喀麦隆领土上的太阳入射辐射进行了计算。 Heliosat方法的真正优势在于我们可以计算连续像素的入射太阳辐射。为了评估该方法在非洲站点的性能,我们将使用Heliosat_2方法从Meteosat数据得出的太阳辐射值与Yaoundé(北纬3°52'; E 11°32')和Garoua(9°20)的地面测量值进行了比较。 'N; 13°23'E)。我们观察到,Heliosat方法的准确度对于萨赫勒地区每日日照的月变化非常令人满意,而在森林地区中,所取回的辐照的变化与测量结果不符。如果使用一天中每半小时接收到的所有“高分辨率” Meteosat数据来实现该方法,则可以大大提高Heliosat_2方法的准确性;因此,每日辐射的计算可能会更准确。

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