首页|基于TSEB平行模型的黄土丘陵沟壑区蒸散发遥感估算

基于TSEB平行模型的黄土丘陵沟壑区蒸散发遥感估算

Retrieving Evapotranspiation of Loess Hilly-gully Region Using TSEB Parallel Model Based on Remote Sensing Image

扫码查看
复杂地形条件下和干旱半干旱植被稀疏条件下的蒸散发遥感估算一直是蒸散发区域遥感估算的难点、热点问题.针对黄土丘陵沟壑区地表起伏、覆被不均一、植被稀疏的特征,选择陕甘交界区为研究区,利用Landsat TM资料求取地表特征参数和地表能量平衡各参量,采用TSEB平行模型反演出该区域的瞬时土壤蒸发、植被蒸腾和土壤一植被总蒸散发量,经过尺度转换,得到日蒸散量;并利用附加阻抗法和FAO Penman-Monteith公式计算实际蒸散发,对TSEB平行模型法遥感估算结果进行了间接精度评价,比较验证结果表明TSEB平行模型法估算的蒸散发结果合理,精高较高.
Evapotranspiation retrievals in conditions of rugged terrain and arid/semiarid sparse vegetation are always the hotspot in estimation of regional evapotranspiration from remote sensing images. Concerning with the complex characteristics of the loess hilly-gully region, such as undulating topography, un-unique land use/covers and less vegetated land surface, etc,land surface characteristic parameters and flux was retrieved, and the instantaneous veg-etation transpiration and soil evaporation was estimated with the TSEB parallel model by using the Landsat TM da-ta for an experimental study site located on the conjuncture area of Shaanxi and Gansu where the terrain surface is very undulating with less vegetation developed, heavy soil and water loss loess plateau. And then the calculated re-sult was merged into daily evapotranspiration, also the spatial pattern of the daily evapotranspiration was analyzed.Actual evapotranspiration of the study area was calculated with the extra resistance method and Penman-Monteith equation to compare with the TSEB parallel model estimated, which suggested that the TSEB parallel model can be used for the accurate estimation of evapotranspiration in loess hilly-gully region.

EvapotranspirationTSEB modelRemote sensingLoess hilly-gully region

潘竟虎、刘春雨

展开 >

西北师范大学地理与环境科学学院,甘肃,兰州,730070

兰州大学资源环境学院,甘肃,兰州,730000

蒸散发 TSEB模型 遥感 黄土丘陵沟壑区

国家自然科学基金甘肃省自然科学基金西北师范大学知识与科技创新工程项目

409610260710RJZA104NWNU-KJCXGC-03-60

2010

遥感技术与应用
中国科学院遥感联合中心

遥感技术与应用

CSTPCDCSCD北大核心
影响因子:0.961
ISSN:1004-0323
年,卷(期):2010.25(2)
  • 10
  • 7