南部-比利牛斯 阿基坦 普瓦图-夏朗德 利穆赞 奥弗涅 朗格多克-鲁西永 普罗旺斯-阿尔卑斯-蓝色海岸 罗纳-阿尔卑斯 勃艮第 弗朗什-孔泰 阿尔萨斯 洛林 香槟-阿登 法兰西岛 中央 卢瓦尔河地区 布列塔尼半岛 下诺曼底 Haute-Normandie 皮卡第 北部-加来海峡
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都卜勒雷達
The precipitation-radar images show only qualitative information on precipitation.The radar images are based on non-processed raw data. Their quality is limited to non-quantitative information, since radar is only an indirect method of measuring precipitation, based on reflectivity. Quantitative information from radar measurements is obtained by comparing the data with conventional precipitation measurements. However, real-time measurements aren't possible yet. This so-called quasi-calibrated data is neither produced regularly nor updated. For different technical reasons radar information is still incomplete and patchy. The spatial resolution of the precipitation radar image is 4 km x 4 km and the temporal resolution is 15 minutes. Based on the magnitude of radar reflection seven different intensities of precipitation were distinguished.
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