首页> 外文会议>International Conference on Frontiers of Sensors Technologies >Estimation of daily average near-surface air temperature using MODIS and AIRS data
【24h】

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

机译:使用MODIS和AIRS数据估计每日平均近表面空气温度

获取原文

摘要

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:近表面空气温度是在气象,气候和环境健康研究中使用的基本气候变量。许多研究已经开发了估计近视空气温度的方法,从遥感数据估计清晰的天空条件,但努力估算多云的天空条件和每日平均空气温度的努力,使用遥感数据仍然很少。目前的研究介绍了一种方法来借助估计的每日最大和最小空气温度借助中等分辨率成像分光镜(MODIS)和大气红外发声器(空气)观察的时间序列来估计每日平均近表面空气温度。使用线性回归模型的三种Modis产品数据估计清晰天空像素的每日最大温度,如[1]中所示,且航空公司标准表面空气温度产品数据用于在缩减后填充图像的多云天空像素过程。来自Aqua Modis夜总会观测的检索到的陆地表面温度(LST)用作清晰天空像素的日常气温,并且多云的天空像素也被烟囱标准表面空气温度产品数据填充。因此,可以根据近表面空气温度的昼夜变化来估计每日平均近表面空气温度。 2013年8月使用176个地面气象站的现场观测到的空气温度数据验证了该方法。平均绝对误差(MAE)和根均方误差(RMSE)为1.2°C和1.6°C。所提出的方法的强度是它可以从遥感数据获得合理的近表面空气温度数据,因此它在具有稀疏地面站的区域中是有用的。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号