首页> 外文会议>International Geoscience and Remote Sensing Symposium >MODELING CANOPY INTERCEPTION OF PICEA CRASSIFOLIA FOREST IN QILIAN MOUNTAINS USING QUICKBIRD SATELLITE DATA
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MODELING CANOPY INTERCEPTION OF PICEA CRASSIFOLIA FOREST IN QILIAN MOUNTAINS USING QUICKBIRD SATELLITE DATA

机译:利用Quician山脉使用Quickbird卫星数据模拟冠层冠覆盖森林

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Canopy interception of rainfall plays an important role in hydrologic cycling and water balance of ecosystems in arid and semi-arid regions. At present, most research focuses on the characteristics of interception at the stand or plot scale. Studies of canopy interception at the river basin or landscape scale based on RS and GIS are lacking because the factors influencing canopy interception such as precipitation, vegetation are difficult to model spatially. A semi-theoretical and semi-empirical model of canopy interception was improved based on investigation in the study area. Considering the important influence of canopy structure, LAI was introduced to the model. After parameters in the model were spatialized using remote sensing data and GIS, the spatial distribution of canopy interception was estimated in the study area (i.e. Pailugou catchment). The results show that the amount of canopy interception in Pailugou catchment is between 97.9 mm and 236.6 mm and the mean interception amount is 161.8 mm. The minimum interception appears at the lower altitude area and the maximum interception presents at the higher altitude area. The interception percentage of Picea crassifolia forest is between 27.92% and 58.00%, which increases with increasing altitude and the maximum appears at 3100m, then decreases along with the increase of altitude.
机译:降雨的冠层截留在干旱和半干旱地区的生态系统的水文循环和水平中起着重要作用。目前,大多数研究重点介绍拦截在立场或绘图规模上的特征。基于RS和GIS的河流域或横向规模的树冠拦截研究缺乏,因为影响冠层截取如降水,植被,植被难以在空间上模型。基于研究区的调查,改进了冠层拦截的半理论和半实证模型。考虑到冠层结构的重要影响,莱被引入模型。使用遥感数据和GIS时,模型中的参数进行了空间化之后,研究区(即佩加鲁沟集水区)估计了顶篷拦截的空间分布。结果表明,斐济集水区的冠层拦截量在97.9毫米和236.6毫米之间,平均截取量为161.8毫米。最小拦截出现在较低的高度区域和较高高度区域的最大拦截呈现。 PICEA Crassifolia森林的截取百分比介于27.92%和58.00%之间,随着海拔高度的增加而增加,并且最大值在3100米处出现,随后随着高度的增加而降低。

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