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Abstract

In the article titled "Background Radiance Estimation for Gas Plume Quantification for Airborne Hyperspectral Thermal Imaging" [1], there are some errors in Figures 2(b), 10, 15, and 16. In Figure 2(b), the emissivity of "slate stone shingle" is absent. Moreover, the emissivities of some materials have been misnamed. In Figure 10, there is a confusion between the curves of the methods CB and SB. In Figures 15 and 16 the curves' order in the legend has been modified. The corrected figures are shown as follows. (Figure Presented).
Corrigendum
Corrigendum to (Background Radiance
Estimation for Gas Plume Quantification for
Airborne Hyperspectral Thermal Imaging)
Ramzi Idoughi,1,2 Thomas H. G. Vidal,1Pierre-Yves Foucher,1
Marc-André Gagnon,3and Xavier Briottet1
1ONERA, e French Aerospace Lab, DOTA, 2 Avenue Edouard Belin, 31400 Toulouse, France
2Institut Sup´
erieur de l’A´
eronautiqueetdelEspace(ISAE),Toulouse,France
3Telops Inc., 100-2600 St-Jean-Baptiste Avenue, Qu´
ebec, QC, Canada G2E 6J5
Correspondence should be addressed to Pierre-Yves Foucher; pierre-yves.foucher@onera.fr
Received  August ; Accepted  August 
Copyright ©  Ramzi Idoughi et al. is is an open access article distributed under the Creative Commons Attribution License,
which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
In the article titled “Background Radiance Estimation for
Gas Plume Quantication for Airborne Hyperspectral
ermal Imaging” [], there are some errors in Figures
(b), , , and . In Figure (b), the emissivity of “slate
stone shingle” is absent. Moreover, the emissivities of
some materials have been misnamed. In Figure ,
there is a confusion between the curves of the methods
CBandSB.InFiguresandthecurves’order
in the legend has been modied. e corrected gures
are shown as follows.
285
290
295
300
(K)
305
310
320
315
(a)
0
0.2
0.4
0.6
0.8
1
Emissivity
900 1000 1100 1200 1300800
Wavenumber (cm−1)
Brown sandy loam
Asphalt
Bare red brick
Olive green paint
Aluminum
Concrete paving
Copper
Slate stone shingle
Oxidized galvanized steel
Green grass
(b)
F : Ground parameters simulation. (a) Ground temperature map. (b) Emissivity spectra of materials present in the synthetic scene.
Hindawi Publishing Corporation
Journal of Spectroscopy
Volume 2016, Article ID 4616050, 4 pages
http://dx.doi.org/10.1155/2016/4616050
Journal of Spectroscopy
Lon
Lbkg
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
2
4
6
8
10
12
14
Radiance (𝜇W/sr/cm2/cm−1 )
900 1000 1100 1200 1300 1400800
Wavenumber (cm−1)
(a)
Lon
Lbkg
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
2
4
6
8
10
12
14
16
Radiance (𝜇W/sr/cm2/cm−1 )
900 1000 1100 1200800 14001300
Wavenumber (cm−1)
(b)
Lon
Lbkg
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
0
2
4
6
8
10
12
Radiance (𝜇W/sr/cm2/cm−1 )
900 1000 1100 1200 1300 1400
800
Wavenumber (cm−1)
(c)
Lon
Lbkg
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
0
2
4
6
8
10
12
14
Radiance (𝜇W/sr/cm2/cm−1 )
900 1000 1100 1200 1300 1400800
Wavenumber (cm−1)
(d)
F : Comparison of background radiance estimation methods, for four dierent pixels through the plume. e red curves stand for the
on-plume radiances; the dashed green ones are the real background radiances. e cyan, blue, and magenta curves represent, respectively, the
background radiance estimated by the SB, CB, and CSB methods. (a) Results for pixel  (brown sandy loam), (b) results for pixel  (asphalt),
(c) results for pixel  (aluminum), and (d) results for pixel  (copper).
Journal of Spectroscopy
900 950 1000 1050 1100 1150 1200 1250 1300850
Wavenumber (cm−1)
4
6
8
10
12
14
16
Radiance (𝜇W/sr/cm2/cm−1 )
Lon
⟨Loff
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
(a)
4
6
8
10
12
14
16
Radiance (𝜇W/sr/cm2/cm−1 )
900 950 1000 1050 1100 1150 1200 1250 1300850
Wavenumber (cm−1)
Lon
⟨Loff
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
(b)
4
6
8
10
12
14
16
18
Radiance (𝜇W/sr/cm2/cm−1 )
900 950 1000 1050 1100 1150 1200 1250 1300
850
Wavenumber (cm−1)
Lon
⟨Loff
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
(c)
F : Comparison of background radiance estimation methods, for three dierent pixels through the plume. e red curves stand
for the on-plume radiances; the dashed green ones are the expected background radiances. e cyan, blue, and magenta curves represent,
respectively, the background radiance estimated by the SB, CB, and CSB methods. (a) Results for pixel , (b) results for pixel , and (c) results
for pixel .
12
12.5
13
13.5
14
14.5
15
15.5
16
Radiance (𝜇W/sr/cm2/cm−1 )
Lon
⟨Loff
̃
LSB
bkg
̃
LCB
bkg
̃
LCSB
bkg
100
20 30 40 50 60 70 80 90
100
x
Plume detected
F : Comparison of dierent radiances at the ethylene absorptive band (950.4cm−1), along a horizontal cross section containing some
plume-present pixels. e red curve stands for the on-plume radiances; the green dashed one is the expected background radiances. e cyan,
blue, and magenta curves represent, respectively, the background radiances estimated by the SB, CB, and CSB methods.
Journal of Spectroscopy
References
[] R. Idoughi, T. H. G. Vidal, P. Foucher, M. Gagnon, and X. Briot-
tet, “Background radiance estimation for gas plume quanti-
cation for airborne hyperspectral thermal imaging,Jour-
nal of Spectroscopy, vol. , Article ID ,  pages,
.
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