首页> 外文期刊>Boletin Geologico y Minero >The Priestley-Taylor equation applied to pixel scale: An alternative for detailed studies of basins [La ecuación de Priestley-Taylor aplicada a nivel de píxel: Una alternativa para estudios detallados de cuencas]
【24h】

The Priestley-Taylor equation applied to pixel scale: An alternative for detailed studies of basins [La ecuación de Priestley-Taylor aplicada a nivel de píxel: Una alternativa para estudios detallados de cuencas]

机译:将Priestley-Taylor方程应用于像素尺度:对盆地进行详细研究的替代方法[将Priestley-Taylor方程应用于像素尺度:对盆地进行详细研究的替代方法]

获取原文
获取原文并翻译 | 示例
           

摘要

The estimate of potential daily evapotranspiration (LE_d) is of great interest on a local and regional scale. Currently, scale regional estimates are conducted from the combination of field data with satellite images (SI). This paper presents a methodology of simple application to estimate the LE_d on a regional scale by means of the equation of Priestley and Taylor (1972) (PT) and a model to obtain daily net radiation (Rn_d) pixel by pixel. Rn_d model was developed from local data recorded by an energy balance station (EBS) in the sub-humid pampean region of Argentina, resulting Rn_d=A.Rs↓_d.(1- albedo) + B, where A and B are two experimental parameters and Rs↓_d is daily short wave incoming radiation. Rnd model was combined with the PT equation and was applied to obtain LE_d on a pixel scale (30 m by 30 m) using the calculated albedo from a Landsat SI (TM sensor), the alpha PT parameter was set in 1.26 and ground heat flux in zero on a daily scale. LE_d maps were developed for 6 consecutive days, where LEd temporal variation is mainly regulated by the Rs↓_d and spatial variation of the albedo. Although the model proposed has not been validated with local measurement or other models, a estimation of the uncertainty in the methodology used to determine LEd was 22%, which suggests being a good alternative for its application in the pampean region of Argentina or other similar regions of the world.
机译:在局部和区域范围内,潜在的每日蒸散量(LE_d)的估计引起了人们的极大兴趣。当前,区域范围的估计是根据现场数据与卫星图像(SI)的组合进行的。本文介绍了一种简单应用的方法,即通过Priestley和Taylor(1972)(PT)方程以及一个逐像素获取每日净辐射(Rn_d)的模型来估计区域尺度的LE_d。 Rn_d模型是根据阿根廷半湿润的南美地区一个能量平衡站(EBS)记录的本地数据开发的,得出Rn_d = A.Rs↓_d。(1-反照率)+ B,其中A和B是两个实验参数和Rs↓_d是每日短波入射辐射。将Rnd模型与PT方程组合,并使用从Landsat SI(TM传感器)计算出的反照率,将其应用于像素尺度(30 m x 30 m)以获取LE_d,将alpha PT参数设置为1.26并选择地面热通量每天为零。 LE_d图连续6天绘制,其中LEd的时间变化主要受Rs↓_d和反照率的空间变化影响。尽管所提议的模型尚未通过本地测量或其他模型进行验证,但用于确定LEd的方法的不确定性估计为22%,这表明该模型可很好地替代其在阿根廷的amp邦地区或其他类似地区的应用世界的。

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