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Assessing the feasibility of increasing spatial resolution of remotely sensed image using HNN super-resolution mapping combined with a forward model

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VNƯ Jo u rn al o f Science, E a rth Sciences 28 (2012) 264-275


<b>Assessing the feasibility o f increasing spatial resolution o f </b>


<b>remotely sensed image using HNN super-resolution mapping </b>



<b>combined with a forward model</b>



<b>Nguyen Quang Minh*</b>



<i>Faculty o f Surveying and Mapping, Hanoi University o f M ining and Geology</i>


Received 03 September 2012


Revised 24 September 2012; accepted 15 October 2012


A bstract. Spatial resolution o f land covers from remotely sensed images can be increased using
super-resolution m apping techniques for soft-classified land cover proportions. A further
development o f super-resolution mapping techniques is downscaling the original remotely sensed
image usmg super-resolution mapping techniques with a forward model. In this paper, the model
for increasing spatial resolution o f remote sensing multispectral image is tested with real SPO T 5
imagery for an area in Bac Giang Province, Vietnam in order to evaluate the feasibility o f
application o f this model to the real imagery. The soft-classified land cover proportions obtained
using a fuzzy c-means classification are then used as input data for a Hopfield neural netw ork
(HNN) to predict the m ultispecừal images at sub-pixel spatial resolution. Visually, the resulted
image is compared with a SPOT 5 panchromatic image acquired at the same time with the
multispecừal data. The predicted image is apparently sharper than the original coarse spatial
resolution image.


<i>Keywords: Hopfield neural network optimisation, soft classification, image downscaling, forward </i>


model.



<b>1. Introduction </b> m apping such as E lad a n d F e u e r [1], T ipping


and B ishop [2]. A lthough w idely applied in
Spatial resolution o f im age and photos can im age processing, these approaches are hardly


be increased by the super-resolution algorithm s. applicable for super-resolution o f rem otely


In the im age processing context, im age super- sensed m ultispectral (M S) im agery because o f


resolution com m only refers to the process o f the lack o f a sequence o f im ages o f the scene at


using a set o f cross-correlated coarse spatial the same or sim ilar tim es. The only feasible


resolution im ages o f the sam e scene to obtain a application o f the super-resolution approaches


single higher spatial resolution im age. T here are using im age sequences is for hyperspectral


num erous studies on such super-resolution im agery [3]. F or o ther com m on m ultispectral


rem otely sensed im agery, only few m ethods for


* Tel-84-982721243 in cre asin g th e sp a tia l re so lu tio n to sub-pixel
E-mail:


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<i>N.Q. Mirth / V N U Journal of Science, Earth Sciences 28 (2012) 264-275</i> 265


level have been proposed such as a Point


Spread Function-derived convolution filter [4],



segm entation technique [5], and geostatistical


m ethod [6],


Sub-pixel spatial resolution land cover


m aps can be predicted using super-resolution


m apping techniques. The input data for super­


resolution m apping are com m only the land


cover proportions estim ated by soft-


classification [7], T here is a list o f super­


resolution m apping techniques have been


inừoduced including spatial dependence


m axim isation [8], linear optim isation


techniques [9], H opfield neural netw ork (H NN )


optim isation [10], tw o-point histogram


optim isation [1 1], genetic algorithm s [12] and


feed-forw ard neural netw orks [13], The



supplem entary data are also supplied to H N N to


produce m ore accurate sub-pixel land cover


m aps such as m ultiple sub-pixel shifted im age


[14], fused and panchrom atic (PA N ) im agery


[15,16]. These latter approaches produce a


synthetic M S or PA N im age as an interm ediate


step for super-resolution m apping based on a


forw ard m odel and then these im ages are


com pared w ith the predicted and observed MS


or PAN im ages to produce an accurate sub­


pixel image classification.


The creation o f the predicted M S an d then


PA N im age b y a forw ard m odel suggested a


possibility to im plem ent a super-resolution for


the M S image. A m ethod for increasing the



spatial resolution o f the original M S image IS


inừoduced by N guyen Q uang M inh et al [17].


T he new m odel is based on the H NN super­


resolution m apping technique from


unsupervised soft-classification com bined w ith


a forw ard m odel using local end-m em ber


spectra [15,16]. T he m ethod is exam ined w ith a


degraded rem ote sensing im age and both visual


and statistical evaluations show n a good result.


H ow ever, there still exist som e concerns about


the feasibility o f the m odel because it is not


tested in a m ore com plicated landscape w ith


different kinds o f land cover features w hich are


varying in sizes and shapes as well as specfral


characteristics. This paper, therefore, is to



im plem ent the test o f the algorithm in a


com plicated landscape.


<b>2. G eneral m odel</b>


T he proposed m odel is an extension o f the


super-resolution m apping approach based on


H N N optim isation. T he prediction o f a MS


im age at the sub-pixel spatial resolution is


based on a forw ard m odel w ith local specfra as


w as used in N guyen et al., 2006 [15], In


addition to the goal functions and the


proportion con sừ ain t o f the H N N for super-


resolution m apping, a reflectance constraint is


used to retain the brighừiess values o f the


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266 <i>N.Q. M in h / V N U Journal of Science, Earth Sciences 28 (2012) 264-275</i>


<b>Spatial </b> <b>SR MS image (2 0 m)</b>


<b>convolution</b>


Figure 1. General model for super-resolution MS imagery prediction.


<b>Synthetic MS </b>
<b>image (4 0 m )</b>


Figure 1 presents the H N N sub-pixel MS


im age prediction algorithm . T he procedure is as


follow s: From the M S im ages at the original


M S spatial resolution, land cover area


proportion images are predicted using a soft-
classifier. A set o f local end-m em ber specừ a


v a lu e s is calc u la te d b a se d o n th e e stim a te d land


cover proportions and the original M S image.


L and cover proportions are then used to


constrain the H N N for super-resolution


m apping w ith a zoom factor z to produce the


land cover map at the sub-pixel spatial



resolution. From the super-resolution land


cover m ap at the first iteration, an estim ated MS


im age (at the sub-pixel spatial resolution) is


then produced using a forw ard m odel and the


estim ated local end-m em ber spectra. The


estim ated M S image is then convolved spatially


to create a synthetic M S im age at the coarse


spatial resolution o f the original image.


Follow ing a com parison o f the observed and


synthetic M S im ages, an error value is


produced to retain the brightness value o f the


pixels o f the original M S image. The process is


repeated until the energy function o f the HNN


is m inim ised and the synthetic M S im age is


generated.



A dem onsfration o f the algorithm for an


image o f 2x2 pixels can be d escn bed in Figure


2. Firstly, the soft-classification predicts land


cover proportion as in Figure lb from the MS


specừal im age as in Figure la. There are two


land covers in this im age called Class A and


Class B. From the land cover proportions in


Figure lb , the land cover classes at sub-pixel


level are predicted as in Figure Ic w here a pixel


is divided into 4 x 4 sub-pixels and the 2x2


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<i>N.Q. M in h Ị V N U Journal of Science, Earth Sciences 28 (20Ĩ2) 264-275</i> 267


land cover image o f Class A and Class B. The


brightness o f the new 16x16 pixels image is


predicted using end-m em ber spectra (standard


brightness for the C lass A and B in this area o f



the image). For exam ple, the brightness o f the


pure pixel o f Class A is 35 and Class B is 50


and it is possible to produce a new spectra!


image by assigning all the sub-pixels belonging


to Class A the brightness value o f 35 and the


sub-pixels o f C lass B the brighừiess value o f 50


as in Figure Id.


100% land
coverA


50% land
c o v erA
50% land
c o v er B


62.5% land
cover A
37.5% land
cover B
100% land
coverB
(b)



Figure 1. Creation o f !6><16 pixels image from 2x2 pixels image.


<i>2.Ỉ. </i> <i>Soft-classification f o r super-resolution </i>
<i>m apping o f M S im agery</i>


Soft-classification is an intennediate step in


the sub-pixel M S im age predictio n process. The


prediction o f the M S im age based on super­


resolution m apping requires land cover


proportions w hich are obtained from soft-


classi fication as input data. C onventionally,


there m ust be a set o f training data for m ost o f


the soft-classifiers. A ccordingly, it is necessary


to have som e prior infom iation about the


specừal distribution o f land cover classes in the


M S bands, although training data are not


alw ays available for the im age. A nd som etim es,


there is a requirem ent o f increasing the spatial



resolution o f the im age w itho ut concerning the


lan d cover classes in the im age scene. In these


cases, the algorithm can be im plem ented w ith


unsupervised soft-classified land cover


proportions such as fuzzy c-means classifier [18].


Supervised soft-classifiers could also be


<i>used, such as B ayesian, neural netw ork or k 'N N </i>


classifiers. H ow ever, the training data for these


soft-classification techniques should be


obtained from the unsupervised classifications.


In the research im plem ented by N guyen Q uang


M inh et al [17], a test for algorithm w as


im plem ented w ith a set o f degraded MS im age


and soft-classified land cover proportions w as


obtained using k-N N classification using a



fraining data set ex ừ acted from unsupervised


Interactive Self-O rganising D ata (ISO D A TA )


classifier. In this case, training data w ere


clustered in the reference image. In this


experim ent, a fuzzy c-m eans classification is


used to predict land cover proportions o f a real


SPO T im age to produce super-resolved specừ al


image o f different spatial resolutions to evaluate


the algorithm .


<i>2.2. F orw ard m odel a nd end-m em ber spectra</i>


A fter the first iteration o f the H N N


algorithm , once the sub-pixel classification is


obtained, a forw ard m odel is used to p ro duce a


sub-pixel M S im age from the sub-pixel land


cover classes. The brighừiess value (e.g.,



reflectance, radiance, digital num ber) o f a sub­


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268 <i>N.Q . M in h / V N U journal o f Science, Earth Sciences 28 (2012) 264-275</i>


<i><b>+</b></i>

(

1

)



<i>w here Ve is the output neuron o f the class e and </i>


<i>Ss e </i>is th e end-m em ber spectra o f the land cover
cla ss <i>e for a spectral band s. A s presented in </i>


N guyen et al., 2006 [15], the end-m em ber


specfra vector Ss (Ss = [5^ o f the


<i>original pixel (x,y) o f the specừ al band A’ can be </i>


e s tim a te d lo c a lly u s in g th e p re d ic te d la n d c o v e r
class proportions and the M S im age at the


original coarse spatial resolution as


S ,= iP ^ W P )~ 'w P ^ R ,, (2)


<b>where p is a m aừix o f land cover proportions wiửi</b>


<i>r ^ x -\) { y - \)</i>


<b>p =</b> <i><sub>PT</sub></i> <sub>/ T</sub>



and w is the m atrix o f w eights w ith


<b>w =</b>


<b>3. E xp erim en t condition</b>


<b>5.7. </b><i>Data</i>


T he experim ent in N guyen Q uang M inh et


al [17] is conducted in an area having many


large objects w ith linear boundaries. It m ay lead


to a concern that th e algorithm proposed in this


p aper is able to w o rk w ell only w ith some


specific landscapes. Therefore, a second data


set is used for testin g the algorithm in a m ore


com plicated landscape. This im age was


obtained in B ac G iang Province, Vietnam.


T he SPO T 5 im age used in this test was


acquired in A ug ust 2011 w ith the spatial



resolution o f 10m and four spectral bands


(Figure 2). T he test im age is registered to


W G S-1984 U TM m ap projection in Zone 48N


and the location is at 21°17’53.65"N ,
1 0 6 °H 7 .6 4 " E . T he test im age covers 1 square


kilom etre area o f 102x102 pixels. To evaluate


the results o f increasing the spatial resolution


algorithm , a 2.5m spatial resolution


panchrom atic im age acquired at the sam e time


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<i>N.Q. M in h / V N U journal of Science, Earth Sciences 28 (2012) 264-275</i> 269


_(c) „


<i>Figure 2. SPOT 5 image in Bac Giang Province, Viettiam: (a) Band 1, (b) Band 2, (c) Band 3 and (d) Band 4.</i>


<i>3.2. Soft-classification</i>


The land cover proportions are estim ated


from 10m spatial resolution SPO T 5 im age



using fuzzy c-m eans classifiers so it is not


necessary to have prior understanding about


land cover classes in the area. The soft-


classified land cover proportions o f five land


cover classes and six land cover classes are


obtained as in Figure 3c and Figure 3d,


respectively.


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270 <i>N.Q. M in h / V N U Journal o f Science, Earth Sciences 28 (2012) 264-275</i>


<b>4. R esults and discussions</b>


<i>4.1. R esuits</i>


The m eth o d o f increasing the M S image


using H N N an d forw ard m odel w as applied to


super-resolve the 10m SPO T 5 M S im ages to


p red ict M S im age at spatial resolutions o f 5m


(zoom factor o f 2), 3.3m (zoom factor o f 3) and



2.5m (zoom factor o f 4). The predicted soft-


classified proportions w ere used to consừain


<i>the H N N w ith w eighting factors o f kị = 100, k: </i>


=1 0 0<i>, k i = </i>100 and 100 to predict the sub­


pixel land cover and then the M S image. The


false colours com positions using B and 1, Band


2 and B and 4 as R ed, G reen and Blue are


show n in Figure 4.


(e) ^ _ (f)


Figure 4. Super-resolution o f 10m SPOT 5 multispectral image: (a) 5m super-resolved image using 5 land cover
classes, (b) 3.3m super-resolution image using 5 land cover classes, (c) 2.5m super-resolution image using 5 land


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<i>4.2. Evaluation</i>


In the case o f degraded image as in N guyen


Q uang Minh et al. [17], the dow nscaled


imagery was com pared with the reference



m ultispectral image at finer spatial resolution to


obtain visual and qualitative evaluations. In this


experim ent, the finer m ultispectral im agery is


not available for the full assessm ent. Therefore,


the predicted m ultispectral im age at finer


resolution can be only com pared w ith 2.5m


panchrom atic im age for a visual evaluation.


The visual com parison o f the super­


resolved image from the real SPOT 5 data with


the panchrom atic im age (Figure 3b) also shows


an im provem ent in sharpness o f the results. The


objects in Figure 4(a-f) are sharpened and look


clearer that o f original im age ( r ig u r e 3a).


A lthough the landscape o f im age area is


com plicated w ith sm all and linear features such



as houses and roads, the im provem ent o f the


algorithm can be seen in the b ou ndaries o f


between the objects. Figure 5 show s the


im provem ent o f the algorithm for increasing the


spatial resolution o f M S im age using H N N with


a forw ard m odel to the original im age. The


boundaries o f ponds in the centre o f the original


M S image (Figure 5a) are blurred and


fragm ented because o f the m ixing o f the land


categories in these boundary pixels. In the


predicted M S im age using HNN and a forw ard


m odel (Figure 5b), these boundaries are clear


and look m ore sim ilar to the real ponds in


panchrom atic im age (Figure 5c).


(a) (b) (c)



Figure 5. Some land cover features in (a) original MS image (false colour composite), (b) increased resolution
MS image to 2.5m spatial resolution from 5 land cover class proportions (false colour composite)


and (c) panchromatic image.


F or sm all objects such as houses and roads,


there are few objects w hich is not clearly seen


in the original im age can be recognised in the


super-resolved image. In Figure 6a (com posite


image using Band 1, Band 2 and Band 4 o f the


original MS im age), the road is difficult to be


recognised because it is fragm ented due to the


m ixed pixels effect. U sing the H NN super


resolution m apping and then the forw ard m odel


as in Figure 6b (com posite im age u sing B and 1,


Band 2 and B and 4 o f the 2.5m spatial


resolution increased im age), it is possible to



recreate the road sim ilar to the shape o f the real


road shown in the panchrom atic im age Figure


6c.


For the sm all features such as a group o f


houses in Figure 6c, the perform ance o f the


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272 <i>N.Q. M inh / V N U Journal of Science, Earth Sciences 28 ( 2 0 W 264-275</i>


However, the new ly proposed algorithm still


show s some im provem ent in defining clear


boundaries o f these features. T his m ay be


because o f the soft-classifier cannot define the


houses as a separate class. T his problem m ay be


resolved by increasing the num ber o f classes for


fuzzy c-m eans classifier or using prior


inform ation on these classes in supervised soft-


classifiers.



Figure 6. Some land cover features such as roads and houses in (a) original image, (b) spatial resolution
increased image (false colour composite) and (c) panchrom atic image.


<i>4.3. D iscussions</i>


The effect o f zoom factor to spatial


resolution increasing algorithm can be seen in


Figure 8. . C om paring the im age created by


H N N using zoom factor o f 2 (Figure 4a), with


the image created w ith zoom factor o f 3 (Figure


4b) and 4 (Figure 4c), it is possible to see that


w hen the zoom factor increases, the boundaries


betw een the features are sm oother. The


boundaries betw een the ponds and the


surrounding features are fragm ented in Figure


8. a and F igure 8. b and look sm oother and


clearer in F igure 8. c.


(a) (b) (c)



Figure 8. Effect o f zoom factor to spatial resolution increasing algorithm: (a) zoom factor of 2, (b) zoom factor
o f 3 and (c) zoom factor o f 4.


In spite o f increasing the spatial resolution


o f the rem otely sensed M S im ages, the


proposed m ethod has a problem w ith pixels that


belong to the sam e class (referred to as pure


pixels in this paper). A lthough the problem can


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<i>N.Q. M in h / V N U Journal of Science, Earth Sciences 28 (2012) 264-275</i> 273


classes so there m ore m ixed pixels or dividing a


class into sub-classes so several pure pixels are


defined as m ixed pixels, there w ill still exist


pure pixels. The effect o f num ber o f land cover


classes can be seen in Figure 9.. The ponds in


Figure 9 .a apparently sm aller than those in


Figure 9.b due to som e “pure pixels” in the



boundaries w ere re-classified as m ixed pixels


w hen the num ber o f classes increased from 5 to


6. These m ixed pixels are then super-resolved


to produce different boundaries betw een the


same features in the tw o im ages.


Figure 9. (a) Result from HNN using 5 land cover classes, and (b) result from HNN using 6 land cover classes.


B ecause the H N N super-resolution m ethod


w orks only on m ixed pixels, w hich are usually


located across the border betw een different


classes, it is suggested that the m ethod is


suitable for the super-resolution o f im ages o f


large objects, for exam ple the agricultural


scenes. In these im ages, spatial variation is


hom ogeneous w ithin the land p arcels and


super-resolution based on the spatial clustering



goal functions o f the H N N can the agricultural


field boundaries or increasing the sharpness o f


linear features such as roads or canals.


As m entioned above, the use o f


unsupervised classification can reduce the


eư o rs in land cover class p roportion prediction.


Furtherm ore, the use o f unsupervised


classification facilitates the autom ation o f the


spatial resolution increasing process because


the class p roportions can b e obtained w ithout


fraining data and w ithout a fraining step.


Through the choice o f the num ber o f classes,


the user can control the effect o f the super­


resolution algorithm on the resulting sub-pixel


M S im ages. W hen the num ber o f classes is



changed, the num ber o f m ixed pixels m ay be


changed as a result.


A draw back o f the H N N super-resolution


procedure is the subjective choice o f the


param eters for the goal functions, the


proportion co n sừ ain t and the m ulti-class


constraint [15]. B y em pirical investigation, the


values o f the param eters should retain an equal


effect betw een the con sừ ain ts and the goal


functions in the optim isation process. For


exam ple, the em pirical investigation in this


paper show s th at the values o f these param eters


in this paper w ere sim ilar and around the value


o f 100. T he finding is also obtained from the


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27 4 <i>N.Q. M in h / V N U journal of Science, Earth Sciences 28 (2012) 264-275</i>



<b>5. C onclusions</b>


The approach for increasing the spatial


resolution M S im agery utilised the H N N super­


resolution m apping technique com bined w ith a


forw ard m odel is tested w ith 10 SPO T 5


rem otely sensed data. In this research, the soft-


classified land cover proportions were


estim ated using a fuzzy c-m eans classifier. The


feasibility o f the m ethod w as evaluated based


on visual com parison o f the resulted im age w ith


panchrom atic im age acquired at the sam e tim e


w ith original image. T he com parison show ed


that the proposed m ethod can generate MS


im ages w ith m ore detail features. The super­


resolved im age w as apparently sharper than the



original coarse spatial resolution im age. In


addition, the evaluation also dem onsừ ated that


w hen the zoom factor increased, the resulting


sub-pixel im ages w ere closer to the reference


image.


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