Canopy foliar nitrogen retrieved from airborne hyperspectral imagery by correcting for canopy structure effects

被引:50
|
作者
Wang, Zhihui [1 ,2 ]
Skidmore, Andrew K. [1 ]
Wang, Tiejun [1 ]
Darvishzadeh, Roshanak [1 ]
Heiden, Uta [3 ]
Heurich, Marco [4 ]
Latifi, Hooman [5 ]
Hearne, John [2 ]
机构
[1] Univ Twente, Fac Geoinformat Sci & Earth Observat ITC, POB 217, NL-7500 AE Enschede, Netherlands
[2] RMIT Univ, Sch Math & Geospatial Sci, GPO Box 2476, Melbourne, Vic 3001, Australia
[3] German Aerosp Ctr DLR, German Remote Sensing Data Ctr DFD, Dept Land Surface, D-82234 Oberpfaffenhofen, Wessling, Germany
[4] Bavarian Forest Natl Pk, Freyunger Str 2, D-94481 Grafenau, Germany
[5] Univ Wurzburg, German Aerosp Ctr, Dept Remote Sensing Cooperat, Oswald Kulpe Weg 86, D-97074 Wurzburg, Germany
关键词
Foliar nitrogen; Forest canopy structure; Hyperspectral remote sensing; Essential biodiversity variables; LEAF OPTICAL-PROPERTIES; SPECTRAL INVARIANTS; AREA INDEX; CHLOROPHYLL CONTENT; WATER-CONTENT; MODEL; SPECTROSCOPY; REFLECTANCE; PROSPECT; MASS;
D O I
10.1016/j.jag.2016.09.008
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
A statistical relationship between canopy mass-based foliar nitrogen concentration (%N) and canopy bidirectional reflectance factor (BRF) has been repeatedly demonstrated. However, the interaction between leaf properties and canopy structure confounds the estimation of foliar nitrogen. The canopy scattering coefficient (the ratio of BRF and the directional area scattering factor, DASF) has recently been suggested for estimating %N as it suppresses the canopy structural effects on BRF. However, estimation of %N using the scattering coefficient has not yet been investigated for longer spectral wavelengths (>855 nm). We retrieved the canopy scattering coefficient for wavelengths between 400 and 2500 nm from airborne hyperspectral imagery, and then applied a continuous wavelet analysis (CWA) to the scattering coefficient in order to estimate %N. Predictions of %N were also made using partial least squares regression (PLSR). We found that %N can be accurately retrieved using CWA (R-2 = 0.65, RMSE = 0.33) when four wavelet features are combined, with CWA yielding a more accurate estimation than PLSR (R-2 = 0.47, RMSE = 0.41). We also found that the wavelet features most sensitive to %N variation in the visible region relate to chlorophyll absorption, while wavelet features in the shortwave infrared regions relate to protein and dry matter absorption. Our results confirm that %N can be retrieved using the scattering coefficient after correcting for canopy structural effect. With the aid of high-fidelity airborne or upcoming space-borne hyperspectral imagery, large-scale foliar nitrogen maps can be generated to improve the modeling of ecosystem processes as well as ecosystem-climate feedbacks. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:84 / 94
页数:11
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