Estimation of leaf area index and canopy openness in broad-leaved forest using an airborne laser scanner in comparison with high-resolution near-infrared digital photography

2008 ◽  
Vol 4 (1) ◽  
pp. 47-55 ◽  
Author(s):  
Takeshi Sasaki ◽  
Junichi Imanishi ◽  
Keiko Ioki ◽  
Yukihiro Morimoto ◽  
Katsunori Kitada
2012 ◽  
Vol 270 ◽  
pp. 54-65 ◽  
Author(s):  
Alicia Peduzzi ◽  
Randolph H. Wynne ◽  
Thomas R. Fox ◽  
Ross F. Nelson ◽  
Valerie A. Thomas

2004 ◽  
Vol 124 (3-4) ◽  
pp. 269-275 ◽  
Author(s):  
David Riaño ◽  
Fernando Valladares ◽  
Sonia Condés ◽  
Emilio Chuvieco

2016 ◽  
Vol 187 ◽  
pp. 267-280 ◽  
Author(s):  
Eva Marino ◽  
Pedro Ranz ◽  
José Luis Tomé ◽  
Miguel Ángel Noriega ◽  
Jessica Esteban ◽  
...  

1991 ◽  
Vol 21 (7) ◽  
pp. 1127-1132 ◽  
Author(s):  
N. J. Smith ◽  
G. A. Borstad ◽  
D. A. Hill ◽  
R. C. Kerr

Techniques are developed to estimate stand leaf area index using high-resolution airborne spectral imagery. Leaf area index on 8 m radius plots was found to be strongly related to the normalized ratio of wavelengths in the red (674–687 nm) and near infrared (751–755 nm) part of the spectrum. Data from 17 stands were used. Leaf area index estimates included both the overstory (Douglas-fir, Pseudotsugamenziesii Mirb. (Franco)) and the understory (salal, Gaultheriashallon Pursh) over a range of stem densities.


2008 ◽  
Vol 148 (6-7) ◽  
pp. 1136-1146 ◽  
Author(s):  
Kenlo Nishida Nasahara ◽  
Hiroyuki Muraoka ◽  
Shin Nagai ◽  
Hiroaki Mikami

Water ◽  
2021 ◽  
Vol 13 (13) ◽  
pp. 1864
Author(s):  
Peter Mewis

The effect of vegetation in hydraulic computations can be significant. This effect is important for flood computations. Today, the necessary terrain information for flood computations is obtained by airborne laser scanning techniques. The quality and density of the airborne laser scanning information allows for more extensive use of these data in flow computations. In this paper, known methods are improved and combined into a new simple and objective procedure to estimate the hydraulic resistance of vegetation on the flow in the field. State-of-the-art airborne laser scanner information is explored to estimate the vegetation density. The laser scanning information provides the base for the calculation of the vegetation density parameter ωp using the Beer–Lambert law. In a second step, the vegetation density is employed in a flow model to appropriately account for vegetation resistance. The use of this vegetation parameter is superior to the common method of accounting for the vegetation resistance in the bed resistance parameter for bed roughness. The proposed procedure utilizes newly available information and is demonstrated in an example. The obtained values fit very well with the values obtained in the literature. Moreover, the obtained information is very detailed. In the results, the effect of vegetation is estimated objectively without the assignment of typical values. Moreover, a more structured flow field is computed with the flood around denser vegetation, such as groups of bushes. A further thorough study based on observed flow resistance is needed.


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