Using SPOT data and leaf area index for rice yield estimation in Egyptian Nile delta
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Transcript of Using SPOT data and leaf area index for rice yield estimation in Egyptian Nile delta
The Egyptian Journal of Remote Sensing and Space Sciences (2011) 14, 81–89
National Authority for Remote Sensing and Space Sciences
The Egyptian Journal of Remote Sensing and Space
Sciences
www.elsevier.com/locate/ejrswww.sciencedirect.com
ORIGINAL ARTICLE
Using SPOT data and leaf area index for rice
yield estimation in Egyptian Nile delta
M. Aboelghar a,*, S. Arafat a, M. Abo Yousef b, M. El-Shirbeny a, S. Naeem b,
A. Massoud a, N. Saleh a
a National Authority for Remote Sensing and Space Sciences (NARSS), P.O. Box 1564, Alf Maskan, Cairo, Egyptb Rice Research Center, Agricultural Research Center (ARC),Giza, Egypt
Received 20 June 2011; revised 8 September 2011; accepted 21 September 2011Available online 22 October 2011
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KEYWORDS
SPOT;
Leaf area index;
Vegetation Indices;
Statistical models
Corresponding author. Ad
nsing and Space Sciences (N
64 Alf Maskan, El-Nozha E
-mail addresses: mohamed
rss.sci.eg (M. Aboelghar).
10-9823 � 2011 National Au
iences. Production and hosti
er review under responsibili
nsing and Space Sciences.
i:10.1016/j.ejrs.2011.09.002
Production and h
dress: Na
ARSS),
l-Gedida,
.aboelgha
thority f
ng by Els
ty of Na
osting by E
Abstract The objective of the current work is to generate statistical empirical rice yield estimation
models under the local conditions of the Egyptian Nile delta. The methodology is based on regress-
ing measured yield with satellite derived spectral information or leaf area index (LAI). LAI field
measurements and spectral information from SPOT data collected during two crop seasons are
examined against measured yield to generate the yield models. Near-infrared and red bands, six veg-
etation indices and LAI of 100 points are used as the main inputs for the modeling process while 20
points of the same are used for validation process. Nine models are generated and tested against the
observed yield. Comparing the generated models show relatively higher superiority of (LAI-yield)
and (infrared-yield) models over the rest of the models with (0.061) and (0.090) as a standard error
of estimate and (0.945) and (0.883) as coefficient of determinations between modeled and observed
yield. The models are applicable a month before harvest for similar regions with same conditions.� 2011 National Authority for Remote Sensing and Space Sciences.
Production and hosting by Elsevier B.V. All rights reserved.
tional Authority for Remote
23 Joseph Tito St., P.O. Box,
Cairo, Egypt.
[email protected], maboelghar@
or Remote Sensing and Space
evier B.V. All rights reserved.
tional Authority for Remote
lsevier
1. Introduction
Accurate and timely assessment of crop yield is an essential pro-cess to ensure the adequacy of a nation’s food supply. It providespolicy makers, governmental agencies and commodity traders
with the necessary information to better manage harvest, stor-age, import/export, transportation and marketing activities.The sooner this information is available, the lower the economic
risk, the greater the efficiency and the increased return on invest-ments Salazar et al., 2007). Synoptic observation and repetitivecoverage of the satellite remote sensing data is considered to bean effective methodology for real-time crop monitoring and
crop yield prediction on both local and regional scales. Spectralempirical modeling of such data is an important approach for
Figure 1 Location map of Sakha area.
82 M. Aboelghar et al.
crop yield estimation. This approach has the advantage of beingsimple with all the required data either readily available on a re-gional or global scale or easy to collect (Prasad et al., 2007). The
basis of this modeling process is generating statistical relation-ships between spectral variables and crop yield or estimatingcrop yield through measurable bio-physical parameters that
are highly correlated with crop canopy vigor and structureand hence, correlated with the spectral characteristics of thecrops. The normalized difference vegetation index (NDVI) is
known to be able to respond to changes in the amount of greenbiomass, chlorophyll content, and canopy water stress. It iseffective in predicting surface properties when the vegetation
canopy is not too dense or too sparse (Liang, 2004). The rela-tionship between NDVI and production has been confirmedby various field experiments (Prince and Justice, 1991; Rasmus-sen, 1992). It has a direct strong correlation with leaf area index
(LAI), biomass and vegetation cover (Tucker, 1979; Holbenet al., 1980; (Ahlrichs and Bauer, 1983; Nemani and Running,1989; Wiegand et al., 1990). These parameters drive the crop
production, and are largely influenced by variations in soil fertil-ity (Hinzman et al., 1986), soil moisture (Daughtry et al., 1980;Teng, 1990), planting date (Crist, 1984) and crop density (Aase
and Siddoway, 1981). They are also related to the crop yieldassuming the absence of significant stresses during the head-ing/filling stages (Hartfield, 1983; Wiegand and Richardson,
1990). The general drawback of most methods using statisticalrelationships between vegetation indices (VI), leaf area index(LAI) and crop yield is that they have a strong empirical charac-
ter (Groten, 1993; Sharma et al., 1993). Nomodels unless devel-oped and tested locally are suitable for local use (Shresthan andNaikaset, 2003). Therefore, the main objective of the currentstudy is to use SPOT satellite imagery and LAI field measure-
0
10
20
30
40
50
60
70
80
May-08
Jun-08
Jul-08 Aug-08
Sep-08
Oct-08
Nov-08
Dec-08
Jan-09
Feb-09
Mar-09
Apr-09
May-09
Jun-09
Jul-09 Aug-09
Sep-09
Average Air temp Average RH%
Figure 2 The recorded air temperature and relative humidity of Sakha region.
Table 1 The average air temperature and relative humidity
during the two rice seasons of 2008 and 2009.
Date Average air temp. Average RH%
May-08 20 67
Jun-08 24 66
Jul-08 24 68
Aug-08 25 70
Sep-08 24 63
May-09 21 59
Jun-09 26 63
Jul-09 27 65
Aug-09 26 66
Sep-09 26 62
Using SPOT data and leaf area index for rice yield estimation in Egyptian Nile delta 83
ments to generate statistical rice yield estimation models under
the local conditions of the Nile delta, north Egypt.
2. Materials and methods
Two SPOT4 (HRVIR) images with 20 m spatial resolution,26 days temporal resolution and four spectral bands: band 1– green (0.50–0.59 lm), band 2 – red (0.61–0.68 lm), band 3
– near infrared (0.78–0.89 lm) and band 4 – shortwave infra-red (1.58–1.75 lm) acquired during the rice seasons in Augustof 2008 and 2009, are used in the current study. Vegetation
indices are calculated from green, red and near-infrared bandsand used in the current observation. Observed crop yield aswell as leaf area index (LAI) field measurements have been
gathered throughout the same rice seasons. Then, all the previ-ous parameters are used as inputs for the models. The follow-ing sub-sections explain the applied methods to collect these
inputs.
2.1. Study area and satellite data pre-processing
The study took place in a leading rice producing area inKafr El-Sheikh Governorate (Sakha region), north Egypt. It is part ofthe Egyptian Nile delta that is characterized by extensive rice
cultivation. It is located between 31�0604000 and 31�060000 Northand 30�5403000 and 30�5506000 East (Fig. 1). The total area ofthe observation site is 24,000 m2 (2.4 ha), 1.2 ha are cultivated
by the variety (Sakha 102) while the rest is cultivated by (Sakha104). These two varieties are the most common Egyptian ricelocal varieties in the Nile delta. Both the varieties are Egyptianshort-grain varieties with national average yield 9.1–9.6 ton/ha�1, blast-resistant, early maturing, need 125 days from sowingtill harvest, with high milling output (72%). The highest andlowest air temperature is observed with the highest is during
the month of August while the lowest is during the month ofApril. The maximum relative humidity is around 82% whilethe lowest is about 43%. Fig. 2 and Table 1 show the monthly
average of air temperature and relative humidity during thetwo rice seasons of 2008 and 2009 from May to September.The source of the meteorological data is the meteorological sta-
tion of Sakha experimental agricultural research station. Thesoil type in the study area is heavy clay soil. Two SPOT4 imageryof the test site acquired in (August 24, 2008 andAugust 23, 2009)(K111/J287) during the rice seasons are used. Geometric
transformation is carried out using selected ground control
points (GCPs) to (Lat/Long) projection system. The root meansquare (RMS) error below half pixel (0.5) is accepted with thefirst-degree polynomial and nearest neighbor resembling algo-rithm technique.
2.2. Generation of estimator variables of crop yield
The observation points included most of variations in fieldconditions and crop production parameters, so that the modelcould be used with different crop production conditions that
are presented in the current study area. Based on a grid systemdesigned by the research team, the study area is divided into 60parcels; 30 parcels are cultivated by each variety and each par-cel (20 · 20 m) that represents a single SPOT pixel is fixed as
one plot of measurements (Fig. 3). The location of the centersquare meter of each plot is recorded using global positioningsystem (GPS). Within each parcel, five LAI measurements are
collected and the average is recorded. At the end of each riceseason, a harvester is used to measure the yield of each parceland the average of yield (kg/m2) is calculated. Finally, the
whole dataset is completed as: 60 points for each rice seasonof (rice yield, LAI measurements, spectral variables includingred and near-infrared bands represented as digital numbers
and six vegetation indices). The data of the two years are com-bined in one dataset and regression analysis between observedyield and each individual variable is performed. One hundredpoints from the two seasons are randomly chosen for modeling
Figure 3 Gridding system for field measurements and data collection.
84 M. Aboelghar et al.
process while 20 points from the two seasons are used to val-idate the models.
LAI-2000 plant canopy analyzer is used to measure LAI foreach point during the two seasons. This device calculates LAI
and other canopy structure attributes from radiation measure-ments made with a (fish-eye) optical sensor (148� field-of-view). Measurements made above the canopy and below
the canopy are used to determine canopy light interception atfive angles, fromwhich LAI is computed using amodel of radio-active transfer in vegetative canopy.Measurements are made by
positioning the optical sensor and pressing a button; data areautomatically logged into the control unit for storage and LAIcalculations. Multiple below-canopy readings and the fish-eyefield-of-view assure that LAI calculations are based on a large
sample of the foliage canopy. After collecting above and be-low-canopy measurements, the control unit performs all calcu-lations and the results are available for immediate on-site
inspection.Six vegetation indices are tested in the current study; nor-
malized difference vegetation index (NDVI), soil adjusted veg-
etation index (SAVI), green vegetation index (GVI), infraredpercentage vegetation Index (IPVI), ratio vegetation index(RVI) and difference vegetation Index (DVI). NDVI is deter-
mined using the red (R) and near-infrared (NIR) bands of agiven image (Rouse et al., 1973) and is expressed as follows:
NDVI ¼ qir � qr
qir þ qr
ð1Þ
where qr and qir are spectral reflectance from the red and NIR-band images, respectively. The green vegetation index (GVI) is
determined using
GVI ¼qir � qg
qir þ qg
ð2Þ
where qg and qir are spectral reflectance from the Green and
NIR-band images, respectively (Panda et al., 2010). Soiladjusted vegetation index (SAVI) is determined as
SAVI ¼ qir � qr
qir þ qr þ L
� �� ð1þ LÞ ð3Þ
where qr and qir are spectral reflectance from the red andNIR-band images, respectively and L is an optimal adjustmentfactor. Huete (1988) defined the optimal adjustment factor of
L = 0.25 to be considered for higher vegetation density inthe field, L = 0.5 for intermediate vegetation density, andL = 1 for the low vegetation density. He suggested that SAVI
(L = 0.5) successfully minimized the effect of soil variations ingreen vegetation compared to NDVI. Based on our observa-tions, we considered canopy cover of the rice crop in the field
as high dense during the satellite images acquisition time in2008 and 2009. Thus, 0.25 is used as the (L) factor using theHuete strategy of selecting the (L) factor, which is also sup-
ported by Thiam and Eastmen (1999). IPVI is the infrared per-centage vegetation index which was first described by Crippen(1990). He found that the subtraction of the red in the numer-ator as is done with SAVI to be irrelevant, and proposed this
index as a way of improving calculation speed. It is restrictedto values between 0 and 1 and eliminates the conceptualstrangeness of negative values for vegetation indices. It is cal-
culated as explained in the following equation:
IPVI ¼ NIR
NIRþ Rð4Þ
Using SPOT data and leaf area index for rice yield estimation in Egyptian Nile delta 85
RVI is the ratio vegetation index which is first described by
Jordan (1969). It is used to eliminate various albedo effects andit is calculated as shown in the following equation:
RVI ¼ NIR
Redð5Þ
DVI is the difference vegetation index, which is describedby Richardson and Everitt (1992) as follows:
DVI ¼ NIR�Red ð6Þ
All VI values and LAI are considered for the regressionanalysis and integrated yield prediction models of the two riceseasons are produced. The explanatory power of the indepen-
dent variables in the model and eventual prediction accuracyof the generated models can be assessed with statistical param-eters such as standard error of estimate (SEE), (t) test, andcoefficient of determination (R2).
3. Results and discussion
Nine statistical yield prediction models are produced. Figs. 4–12 show the trendline and the correlation coefficients for allgenerated models. Basically, linear regression is the best model
that represents the relation between observed yield and eachindividual estimator. It is found that the coefficient of determi-nation (R2) of all models is around (0.8) except for (GVI-yield)
model that showed relatively low ones. The models are exam-ined and the relative superiority over the generated models isdecided through computing Standard Error of Estimate
(SEE) and (t) test and the squared coefficient of determinationsbetween modeled and observed yield (R2). Table 2 shows thegenerated models and the validation results and Figs. 13–21show the trendline and the squared coefficient of determina-
tion between observed and modeled yield.The main objective of the current study is to generate rice
yield prediction models for the most common rice local varie-
ties in the Egyptian Nile delta (Sakha 102) and (Sakha 104).The data of the two seasons were combined in one dataset,part of this dataset was used to generate the models while
the other part was used to validate these models. The idea ofcombining the two rice seasons of the two varieties in one data-set is to generate applicable rice yield prediction models that
could be applied through satellite remote sensing data withacceptable accuracy. The first step of yield prediction is to iso-late the investigate crop from the other land cover types. Clas-sifying different crop types in Egyptian Nile delta is still
problematic and classifying different crop varieties within the
Table 2 The generated models and the validation results.
Variable Regression equation
NIR Yield = 0.0129IR�0.236Red Yield = �0.0923R+ 3.5717
NDVI Yield = 2.3606NDVI�0.2713RVI Yield = 0.2522RVI + 0.1131
IPVI Yield = 4.721IPVI�2.632DVI Yield = 0.0116DVI + 0.21
GVI Yield = 1.3675GVI + 0.468
SAVI Yield = 1.8899SAVI�0.2697
LAI Yield = 0.2846LAI�0.0764*Yield kg/m2.
same crop type is almost not possible under the current agri-
cultural conditions in Egyptian Nile delta using available satel-lite imagery. The models were generated using two seasons andtwo varieties to cover all possible minimal variations and to benot limited to the conditions of one season. It is expected that
these models could be applicable in future through any type ofhigh resolution satellite data. The generated models could beapplied to predict the yield of these two common rice varieties
under normal agricultural practices and common environmen-tal conditions in Egyptian Nile delta. Concerning the results ofthe models, it is found that the statistical relationship between
middle infrared, green bands and yield showed low accuracy,so, these two variables are excluded from further analysis.Among the rest of the examined variables, LAI is the best esti-
mator that gave the highest (R2) and the lowest (SEE). The cal-culated yields from all variables are comparable except for(GVI) that showed lowest validation result. This may be be-cause of the calculation of (GVI) as a ratio between green band
and (IR) and as mentioned above that green band showed rel-atively low correlation with yield. Among spectral variables,(IR) band is the best estimator with the highest validation re-
sult. The calculated (t) is less than the tabeled (t) with all vari-ables that reflects insignificant difference between modeled andobserved yields. (Table 1). Among the three statistical method
that are used to validate the generated models. SEE and R2 aremore powerful than (t) test method for showing the differencein prediction ability among the generated models.
The generated models are site specific and limited to the
area and environment as well as to the date of the experiment.Following the rice growing circle, milking stage (when waterycontent of the grain turn to thick milky ones) is selected as the
best crop growing stage that is closely related to LAI and riceyield. This assumption is proved by the author after one-sea-son experiment during rice season of 2007 using LAI measure-
ments that were gathered using (LAI-2000 plant canopyanalyzer device) and NDVI measurements that were gatheredfrom SPOT data and gathered also using (PlantPen NDVI
300 m) device (Aboelghar et al., 2010). NDVI-meter measuresNDVI comparing the reflected light at two distinct wave-lengths, 660 and 740 nm. NDVI data collected by NDVI-meterduring different growing stages of rice were examined against
the yield and against LAI. It is found that the NDVI of themilking stage of rice is the most correlated growing stage toyield and LAI. This is consistent with other results from the lit-
erature (Murthy et al., 1996; Labus et al., 2002; Royo et al.,2003). The models are produced under the common soil, cli-matic and crop conditions of Egyptian Nile delta and could
R2 SEE t values
0.883 0.090 0.454
0.720 0.123 �0.0940.850 0.099 0.381
0.823 0.098 0.307
0.850 0.099 0.372
0.874 0.090 0.506
0.786 0.210 0.037
0.850 0.099 0.369
0.945 0.061 �0.419
y = -0.0923x + 3.5717
R2 = 0.8004
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0 5 10 15 20 25 30 35 40Red
Yie
ld K
g/m
2
Figure 5 Rice yield statistical modeling using red band.
y = 2.3606x - 0.2713
R2 = 0.8298
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.100 0.200 0.300 0.400 0.500 0.600 0.700 0.800
NDVI
Yie
ld K
g/m
2
Figure 6 Rice yield statistical modeling using NDVI.
Yie
ld K
g/m
2
y = 4.7213x - 2.632
R2 = 0.8298
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.100 0.200 0.300 0.400 0.500 0.600 0.700 0.800 0.900
IPVI
Figure 8 Rice yield statistical modeling using IPVI.
y = 0.0116x + 0.21
R2 = 0.8676
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 20.000 40.000 60.000 80.000 100.000 120.000
DVI
Yie
ld K
g/m
2
Figure 9 Rice yield statistical modeling using DVI.
y = 0.2846x - 0.0764
R2 = 0.82
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0 1 2 3 4 5 6
LAI
Yie
ld K
g/m
2
Figure 10 Rice yield statistical modeling using LAI.
y = 0.0129x - 0.2355
R2 = 0.8512
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0 20 40 60 80 100 120 140
Infrared
Yie
ld k
g/ m
2
Figure 4 Rice yield statistical modeling using near-infrared
band.
Yie
ld K
g/m
2
y = 0.2522x + 0.1131
R2 = 0.8824
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 1.000 2.000 3.000 4.000 5.000 6.000
RVI
Figure 7 Rice yield statistical modeling using RVI.
y = 1.3675x + 0.468
R2 = 0.3189
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.050 0.100 0.150 0.200 0.250 0.300 0.350 0.400 0.450 0.500
GVI
Yie
ld K
g/m
2
Figure 11 Rice yield statistical modeling using GVI.
86 M. Aboelghar et al.
be applied under similar conditions. The applicability of themodels with high accuracy is limited to the experiment date
and the type of the used satellite data. Precautions should be
taken when using these empirical relationships for otherspace-borne or air-borne sensors because of NDVI differencebetween sensors is often substantial (Spanner et al., 1994 and(Kim et al., 2010). Generation of new models might be neces-
y = 1.242x - 0.2879
R2 = 0.8499
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (NDVI)
Obs
erve
d yi
eld
Figure 15 Correlation between observed yield and NDVI based
model.
y = 0.8778x + 0.1363
R2 = 0.7203
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (R)
Obs
erve
d yi
eld
Figure 14 Correlation between observed yield and red based
model.
y = 1.8899x - 0.2697
R2 = 0.8299
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.100 0.200 0.300 0.400 0.500 0.600 0.700 0.800 0.900 1.000
SAVI
Yie
ld K
g/m
2
Figure 12 Rice yield statistical modeling using SAVI.
y = 1.2021x - 0.2504
R2 = 0.883
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (IR)
Obs
erve
d yi
eld
Figure 13 Correlation between observed yield and near infrared
based model.
y = 0.9738x + 0.0079
R2 = 0.8225
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (RVI)
Obs
erve
d yi
eld
Figure 16 Correlation between observed yield and RVI based
model.
y = 1.2422x - 0.2874
R2 = 0.8499
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (IPVI)
Obs
erve
d yi
eld
Figure 17 Correlation between observed yield and IPVI based
model.
y = 1.135x - 0.181
R2 = 0.8742
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (DVI)
Ob
serv
ed y
ield
Figure 18 Correlation between observed yield and DVI based
model.
y = 1.0681x - 0.0429
R2 = 0.9453
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (LAI)
Obs
erve
d yi
eldj
Figure 19 Correlation between observed yield and LAI based
model.
Using SPOT data and leaf area index for rice yield estimation in Egyptian Nile delta 87
y = 10.681x - 10.373
R2 = 0.7855
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
1.030 1.040 1.050 1.060 1.070 1.080 1.090 1.100 1.110
Predicted yield (GVI)
Obs
erve
d yi
eld
Figure 20 Correlation between observed yield and GVI based
model.
y = 1.2421x - 0.2871
R2 = 0.8501
0.000
0.200
0.400
0.600
0.800
1.000
1.200
1.400
1.600
0.000 0.200 0.400 0.600 0.800 1.000 1.200 1.400 1.600
Predicted yield (SAVI)
Ob
serv
ed y
ield
Figure 21 Correlation between observed yield and SAVI based
model.
88 M. Aboelghar et al.
sary to estimate rice yield in middle Egypt region that has dif-ferent conditions.
4. Conclusion
A combined dataset through two rice seasons of the year 2008
and 2009 is used to produce statistical empirical rice yield pre-diction in a test site in Egyptian Nile delta. The planting dateswere May 24, 2008 and May 23, 2009. Various yield models
containing different number of predictor variables are gener-ated. The basic idea is the simpler the model, the easier andquicker will be the estimation process as fewer variables are ta-ken into account for data collection and computation process.
The spectral variables considered in the current study are redand near-infrared bands either alone or in the form of vegeta-tion indices and LAI as a bio-physical parameter that is related
to crop yield. LAI and infrared models showed higher accu-racy over the rest of the models as shown by the statisticalanalysis. The generated LAI and IR based models could be ap-
plied yearly to predict rice yield in Egyptian Nile delta and canbe also applied for rice yield estimation in any rice producingarea with similar conditions as the study area more than amonth before harvest. Similar studies could be also the basis
for a yield prediction and early warning system for the othermain crops of the country. The available satellite imagery dur-ing crop seasons and multi-temporal measurements of LAI
and infrared using field devices in selected sites of each cropcould be the main sources for the inputs of the models. Apply-ing the generated models on satellite imagery will produce
yield maps for the main crops month/s before harvest.
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