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Assessing the role of Mediterranean evergreen oaks canopy cover in land surface albedo and temperature using a remote sensing-based approach

机译:使用基于遥感的方法评估地中海常绿橡树冠层在陆地表面反照率和温度中的作用

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Modifications in vegetation cover can have an impact on the climate through changes in biogeochemical and biogeophysical processes. In this paper, the tree canopy cover percentage of a savannah-like ecosystem (montadoldehesa) was estimated at Landsat pixel level for 2011, and the role of different canopy cover percentages on land surface albedo (LSA) and land surface temperature (LST) were analysed. A modelling procedure using a SGB machine-learning algorithm and Landsat 5-TM spectral bands and derived vegetation indices as explanatory variables, showed that the estimation of montado canopy cover was obtained with good agreement (R-2 = 78.4%). Overall, montado canopy cover estimations showed that low canopy cover class (MT_1) is the most representative with 50.63% of total montado area. MODIS LSA and LST products were used to investigate the magnitude of differences in mean annual LSA and LST values between contrasting montado canopy cover percentages. As a result, it was found a significant statistical relationship between montado canopy cover percentage and mean annual surface albedo (R2 = 0.866, p < 0.001) and surface temperature (R-2 = 0.942, p < 0.001). The comparisons between the four contrasting montado canopy cover classes showed marked differences in LSA (chi(2) = 192.17, df = 3, p < 0.001) and LST (chi(2) = 318.18, df = 3, p < 0.001). The highest montado canopy cover percentage (MT_4) generally had lower albedo than lowest canopy cover class, presenting a difference of -11.2% in mean annual albedo values. It was also showed that MT_4 and MT _3 are the cooler canopy cover classes, and MT_2 and MT_1 the warmer, where MT_1 class had a difference of 3.42 degrees C compared with MT_4 class. Overall, this research highlighted the role that potential changes in montado canopy cover may play in local land surface albedo and temperature variations, as an increase in these two biogeophysical parameters may potentially bring about, in the long term, local/regional climatic changes moving towards greater aridity. (C) 2016 Elsevier Ltd. All rights reserved.
机译:植被覆盖的变化可能通过生物地球化学和生物地球物理过程的变化而对气候产生影响。在本文中,以2011年Landsat像素水平估算了类似大草原的生态系统(montadoldehesa)的树冠覆盖率,并且不同冠层覆盖率对地表反照率(LSA)和地表温度(LST)的作用分别为分析。使用SGB机器学习算法并以Landsat 5-TM谱带和导出的植被指数作为解释变量的建模过程表明,获得的蒙塔多冠层覆盖率估算值具有良好的一致性(R-2 = 78.4%)。总体而言,蒙塔多的天篷覆盖率估计值表明,低蒙盖级别(MT_1)最有代表性,占蒙塔多总面积的50.63%。 MODIS LSA和LST产品用于调查蒙大拿州不同冠层覆盖率之间的年均LSA和LST值差异的幅度。结果,发现蒙大纳树冠覆盖率与年平均地表反照率(R2 = 0.866,p <0.001)和地表温度(R-2 = 0.942,p <0.001)之间存在显着的统计关系。蒙塔多遮盖物的四个对比等级之间的比较显示LSA(chi(2)= 192.17,df = 3,p <0.001)和LST(chi(2)= 318.18,df = 3,p <0.001)有显着差异。蒙大拿州最高冠层覆盖率(MT_4)的反照率通常低于最低冠层覆盖率,这意味着年平均反照率值相差-11.2%。还表明,MT_4和MT _3是凉爽的树冠覆盖类别,MT_2和MT_1是温暖的树冠覆盖类别,其中MT_1和MT_4的类别相差3.42摄氏度。总的来说,这项研究强调了蒙大拿州冠层覆盖的潜在变化可能在局部地表反照率和温度变化中发挥的作用,因为从长远来看,这两个生物地球物理参数的增加可能潜在地导致局部/区域气候变化向更大的干旱。 (C)2016 Elsevier Ltd.保留所有权利。

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