Applying vegetation indices to detect high water table zones in humid warm-temperate regions using satellite remote sensing

被引:7
作者
Koide, Kaoru [1 ]
Koike, Katsuaki [2 ]
机构
[1] Japan Atom Energy Agcy, Geol Isolat Res & Dev Directorate, Gifu 5096132, Japan
[2] Kyoto Univ, Grad Sch Engn, Dept Urban Management, Kyoto 6158540, Japan
来源
INTERNATIONAL JOURNAL OF APPLIED EARTH OBSERVATION AND GEOINFORMATION | 2012年 / 19卷
关键词
AgbNDVI; Geobotany; Groundwater discharge; Reflectance spectra; Segmentation analysis; SPOT HRV; LEAF-AREA INDEX; CONIFER ECOSYSTEMS; FOREST; CLASSIFICATION; REFLECTANCE; DISCHARGE; HARDWOOD;
D O I
10.1016/j.jag.2012.03.017
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
This study developed a geobotanical remote sensing method for detecting high water table zones using differences in the conditions of forest trees induced by groundwater supply in a humid warm-temperate region. A new vegetation index (VI) termed added green band NDVI (AgbNDVI) was proposed to discriminate the differences. The AgbNDVI proved to be more sensitive to water stress on green vegetation than existing VIs, such as SAVI and EVI2, and possessed a strong linear correlation with the vegetation fraction. To validate a proposed vegetation index method, a 23 km(2) study area was selected in the Tono region of Gifu prefecture, central Japan. The AgbNDVI values were calculated from atmospheric corrected SPOT HRV data. To correctly extract high VI points, the influence factors on forest tree growth were identified using the AgbNDVI values, DEM and forest type data; the study area was then divided into 555 domains chosen from a combination of the influence factors and forest types. Thresholds for extracting high VI points were defined for each domain based on histograms of AgbNDVI values. By superimposing the high VI points on topographic and geologic maps, most high VI points are clearly located on either concave or convex slopes, and are found to be proximal to geologic boundaries particularly the boundary between the Pliocene gravel layer and the Cretaceous granite, which should act as a groundwater flow path. In addition, field investigations support the correctness of the high VI points, because they are located around groundwater seeps and in high water table zones where the growth increments and biomass of trees are greater than at low VI points. (c) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:88 / 103
页数:16
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