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首页> 外文期刊>Natural Hazards and Earth System Sciences Discussions >A high resolution climatology of precipitation and deep convection over the Mediterranean region from operational satellite microwave data: development and application to the evaluation of model uncertainties
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A high resolution climatology of precipitation and deep convection over the Mediterranean region from operational satellite microwave data: development and application to the evaluation of model uncertainties

机译:来自运营卫星微波数据的地中海地区降水和深度对流的高分辨率气候学:开发和应用于模型不确定性的评估

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摘要

A new precipitation and convection dataset for the Mediterranean Basin, derived from operational satellite microwave data is documented. The dataset is derived from diagnostics that rely on brightness temperatures measured since 1999 in the water vapour absorption line (183–191 GHz). The dataset consists of twice-daily (a.m. and p.m.) and monthly maps of precipitation and convection occurrences on a 0.2° lat × 0.2° long grid for the area 25°–60° N, 10° W–50° E. The instruments used so far are the AMSU-B sensor on the NOAA-15 to -17 satellites, and the MHS sensor on the NOAA-18 and -19 and METOP-2 satellites, with precipitation and convection available separately for the different sensors. The slightly different radiometric characteristics of MHS compared to AMSU-B do not affect significantly the continuity of the dataset. Precipitation and convection data from different sensors on different satellites are remarkably consistent, with generally small biases between the instruments. When larger biases appear, they can be explained either by the drifts in the satellite orbit, scan asymmetry, or temporal aliasing from insufficiently resolving the diurnal cycle of precipitation and convection. After a description of climatological aspects of rain and deep convection occurrence, the interest of this dataset to evaluate model uncertainties for simulating a high-impact weather event and for climatic regional runs over this area is illustrated.
机译:记录了来自运营卫星微波数据的地中海盆地的新的降水和对流数据集。数据集源自诊断,依赖于自1999年以来在水蒸气吸收线(183-191GHz)以​​来测量的亮度温度。 DataSet由两次(AM和PM)和0.2°L×0.2°N,10°W-50°E.的0.2°-60°N,10°W-50°E.的每天降水和对流发生的每月降水和对流发生的每月地图。该仪器到目前为止使用的是NOAA-15至-17卫星上的AMSU-B传感器,以及NOAA-18和-19和-19和METOP-2卫星的MHS传感器,用于不同传感器的降水和对流。与AMSU-B相比,MHS的略微不同的辐射性特征不会显着影响数据集的连续性。来自不同卫星的不同传感器的降水和对流数据非常一致,仪器之间的偏差通常很小。当出现较大的偏差时,它们可以通过卫星轨道轨道,扫描不对称性或时间叠种的漂移来解释,从不充分地解析降水和对流的昼夜循环。在雨和深度对流发生的气候方面的描述之后,说明了该数据集的兴趣来评估模拟用于模拟高影响天气事件和对该区域的气候区域的模型不确定性。

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