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Estimation of daily average near-surface air temperature using MODIS and AIRS data

机译:使用MODIS和AIRS数据估算每日平均近地表气温

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The near-surface air temperature is an essential climatic variable wildly used in studies of meteorology, climate, and environmental health. Numerous studies have developed approaches to estimate near-surface air temperature from remote sensing data for clear sky conditions, but efforts to estimate air temperature for cloudy sky conditions and daily average air temperature using remote sensing data still few. The current study introduces an approach to estimate daily average near-surface air temperature using the estimated daily maximum and minimum air temperatures with the help of time series of the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Atmospheric Infrared Sounder (AIRS) observations. The daily maximum temperatures of clear sky pixels are estimated from three MODIS products data using a linear regression model as expressed in [1], and the AIRS standard surface air temperature products data are used to fill the cloudy sky pixels for the images after a downscaling process. The retrieved land surface temperatures (LST) from Aqua MODIS night-overpass observations are used as the daily minimum air temperatures for the clear sky pixels, and the cloudy sky pixels are also filled by AIRS standard surface air temperature products data. Thus, the daily average near-surface air temperature can be estimated according to the diurnal variation of near-surface air temperature. This method was validated using field observed air temperature data of 176 ground meteorological stations in August 2013. The mean absolute error (MAE) and the root mean square error (RMSE) are 1.2 °C and 1.6 °C. The strength of the proposed methodology is that it can obtain reasonable near-surface air temperature data from remote sensing data, so it is useful in regions with sparse ground stations.
机译:近地表气温是气象,气候和环境健康研究中广泛使用的重要气候变量。许多研究已经开发出用于从晴朗的天空条件下的遥感数据估计近地表气温的方法,但是使用遥感数据来估计多云的天空条件下的气温和每日平均气温的工作仍然很少。当前的研究引入了一种方法,该方法借助中分辨率成像光谱仪(MODIS)和大气红外测深仪(AIRS)观测值的时间序列,利用估计的每日最高和最低气温来估计每日平均近地表气温。使用[1]中表示的线性回归模型,从三个MODIS产品数据中估算出晴空像素的每日最高温度,并使用AIRS标准地表气温产品数据对缩小后的图像填充多云的天空像素。处理。从Aqua MODIS夜间立交观测得到的地面温度(LST)被用作晴朗天空像素的每日最低气温,而多云天空像素也被AIRS标准地面气温产品数据填充。因此,可以根据近地表气温的日变化来估计日平均近地表气温。该方法已使用2013年8月的176个地面气象站的实地观察到的气温数据进行了验证。平均绝对误差(MAE)和均方根误差(RMSE)为1.2°C和1.6°C。该方法的优势在于可以从遥感数据中获取合理的近地表气温数据,因此在地面站稀少的地区很有用。

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