Title: Russia land cover mapping from VGT S10 data
1Russia land cover mapping from VGT S-10 data
Global Land Cover 2000
Sergey Bartalev International Forest Institute,
Moscow, Russia Visiting Scientist in the JRC of
the European Commission, Ispra, Italy
Global Vegetation Monitoring Unit
2Geographical extent of the study and used
SPOT4-VGT data
Global Land Cover 2000
Type of products used SPOT 4-VGT S10 products
including spectral and angular data Geographical
extent 420N - 750N and 50E -1800E with
particular attention to Russian territory and the
boreal zone of Eurasia Time window from end of
March 1999 until beginning of November 1999
Global Vegetation Monitoring Unit
3Distribution of the forest in the World
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Boreal and Temperate Zone
World
Global Vegetation Monitoring Unit
4The key elements being taken into consideration
to design the land cover mapping method
- requirements of users and particularly at
national level - the satellite data properties allow to
distinguish the land cover types - regional environment peculiar properties
- availability of auxiliary (non satellite) data
- practical realizability due to existing
technical and other limitation -
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Global Vegetation Monitoring Unit
5The main options and obstacles to classify the
land cover types with SPOT4-VGT data
- Options
- spectral properties the land cover types
- spectral-phenological changes of the land cover
- the angular anisotropy of reflected radiation of
land cover - Obstacles
- presents of the pixels contaminated by
clouds/shadow and snow - presents of the pixels contaminated MIR defective
detectors - Sun/View directional dependence of spectral
response - dependence of phenological changes both from time
of observation and geographical location
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Global Vegetation Monitoring Unit
6Relation between main options and obstacles to
classify the land cover types with SPOT4-VGT data
Spectral features (single image)
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Contamination by clouds, snow and MIR defective
detectors
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7Separability of main land cover types with
spectral signatures derived from single S-10
SPOT4-VGT image
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Global Vegetation Monitoring Unit
8Separability of different species forest with
spectral signatures derived from single S-10
SPOT4-VGT image
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Global Vegetation Monitoring Unit
9Steps of the satellite data pre-processing
- Producing the mask of contaminated pixels related
to snow, clouds and MIR channel defective
detectors with the following steps procedure - detection of utterly contaminated pixels with
pre-specified thresholds - detection of slightly contaminated pixels with
pixel-by-pixel adaptive thresholds derived from
time series of data - Hot-spot factor normalization of spectral
reflectance with BRDF model (subsidiary and
optional step) - Producing the seasonally optimised composites of
spectral channels - Producing of the spectral-angular parameters with
two options are considered - statistics of Sun-Earth-Sensor relative angular
parameters derived under condition of maximum
NDVI pixels selection - BRDF model derived parameters estimation
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10Clouds and Snow spectral properties. Normalised
Different Snow Indexes NDSI
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NDSI (CH1-CH4) / (CH1CH4)
From Hall et al., 1998 "Algorithm Theoretical
Basis Document (ATBD) for the MODIS Snow-, Lake
Ice- and Sea Ice-Mapping Algorithms. Version 4.0"
Global Vegetation Monitoring Unit
11Detection of the contaminated pixels
- Step 1 Detection of the pixels utterly
contaminated by snow and clouds with
pre-specified thresholds - Snow/Ice Cs (?, t) 1 ? ??R1 (?, t) gt 0.1
AND NDSI (?, t) gt 0.1 - Clouds Cc (?, t) 1 ? ? ? R1 (?, t) gt
0.1 AND - 0.1 lt NDSI (?, t) lt 0.1 - where
- ? - geographical co-ordinates t - fixed time of
observation (decade) - Ri ( i1?4) - reflectance in the channel i NDSI
- snow indexes - Cs - set of snow detected pixels Cc - set of
clouds detected pixels - CP1 ? Cs U Cc - set of contaminated pixels
at the 1st step - Steps 2?J Detection of the defective detectors
and slightly contaminated by snow/clouds pixels
with adaptive thresholds derived from time series
of data - CP'j (?, t) 1 ? t ? R4 (?, t) ? Mj (R4 (?) ?
CPj-1(?, t) ? 1) 2SDj (R4 (?) ? CPj-1(?, t)
? 1) - OR ? R4 (?, t) ? Mj (R4 (?) ? CPj-1(?,
t) ? 1) - 2SDj (R4 (?) ? CPj-1(?, t) ? 1) - Mj (R4 (?) and SDj (R4 (?) - mean and standard
deviation of R4 (?, t) at the step j - ? - fixed geographical co-ordinates
- CPj ? CPj-1 U CP'j - set of contaminated
pixels at the step j (j2?J)
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12Producing of the seasonal mosaics
Main zonal ecosystems of Russia
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Snow duration map derived from SPOT4-VGT S-10 data
Global Vegetation Monitoring Unit
13The seasonal composites of S-10 images
spring
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summer
autumn
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SWIR-NIR-R
14Comparison of the summer and autumn seasonal
composites of S-10 images
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summer
autumn
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NIR-SWIR-R
15Producing of the spectral-angular parameters
- Objective to investigate the possibilities to
derive from time series of SPOT4-VGT data the
parameters that are sensitive to the structure
(forest density, height and etc.) of observed
surface based on the angular anisotropy of
reflected radiation - Two options are considered
- statistical analysis of Sun-Earth-Sensor
relative angular parameters derived under
condition of maximum NDVI pixels selection - parameters derived from BRDF model
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Global Vegetation Monitoring Unit
16Averaging of Sun-Earth-Sensor relative angular
parameters from SPOT4-VGT S-10 time series
products
Color composite of M(PHA) and M(VZA) and M(SZA)
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M (?) Mj (? (?, t) ? t ? CP(?, t) ? 1) where
? - one of Sun-Earth-Sensor angular parameter t
- time of observation (decade) ? - fixed
geographical co-ordinates CP(?, t) - mask of
contaminated pixels M (?) - mean of ?
Z
SZA
N
SAA
VAA
VZA - view zenith angle SZA - Sun zenith
angle PHA - phase angle
17Comparison of Sun-Earth-Sensor time-averaged
angular parameters from SPOT4-VGT S-10 products
with forest map
Color composite of mean values of PHA and VZA and
SZ
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Z
SZA
N
Forest map
SAA
VAA
18BRDF model based approach to derive
spectral-angular parameters from time series of
S10 products
The linearized MRPV model of BRDF
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- Sun Zenith, View Zenith and Phase angles
respectively
where RNi - reflectance in the spectral channel i
normalized for the hot-spot factor
RNi A RNj B, where i and j - spectral
channels and i?j An estimations of A and B
coefficients of linear equation are considering
as parameters sensitive to surface structure
Global Vegetation Monitoring Unit
19An estimation of the linear equation coefficients
between pairs of normalized reflectances in two
channels of S10 products
An estimation of slope A and interception B with
moving time window along profiles of NIR and MIR
channels
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Maximum is R2 0.93
Global Vegetation Monitoring Unit
20Color composite of Slope and Interception values
of linear equation derived with pairs of RED-NIR
and NIR-MIR channels
RED-NIR Slope - Slope - Interception
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Z
SZA
N
SAA
VAA
NIR-MIR Slope - Slope - Interception
21An example of relationship between Slope values
of linear equation derived with NIR-MIR channels
and forest density
The forest density values are estimated in the
set of grid cells based on forest inventory data
base
Global Land Cover 2000
Z
SZA
N
SAA
VAA
Standard deviation of Slope values for each class
of forest density is estimated in range of 0.4-0.5
22Possible steps of the satellite data thematic
classification
- Eco-regional stratification
- Ecostrata-by-ecostrata unsupervised clustering of
spectral-seasonal composites 3 mosaics x RED,
NIR and MIR channels. - Two different clustering algorithm are
considering - ISODATA ERDAS
- ELBG
- Clusters labeling (if needs with additional
splitting of clusters using auxiliary
non-satellite data) into thematic classes with
using - existing forest maps and forest inventories data
- high-resolution satellite imagery
- digital elevation model and topomaps
- Splitting of forest related classes to 2-3 cover
density categories with spectral-angular
parameters derived from satellite data (have to
be investigated additionally)
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Global Vegetation Monitoring Unit
23Eco-regional stratification
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Global Vegetation Monitoring Unit
24The lessons learned from Russia land cover
mapping exercise with SPOT4-VGT data
- Pre-processing
- the procedure of contaminated pixels detection
is developed and applied with satisfactory
results - the developed multi-temporal data composting
procedure allows to produce the seasonal mosaics
that are almost free from contaminated pixels and
angular effect and gives possibility to use
phenological changes of land cover as an
additional option for thematic classification - the possibility to retrieve from
spectral-angular data an information on surface
structure has been demonstrated. An practical
benefit of spectral-angular data for land cover
mapping are limited with using S-10 product and
still have to be clarified. It is very likely
that better result can be obtained with daily
data (S-1 and P products)
Global Land Cover 2000
Global Vegetation Monitoring Unit
25The lessons learned from Russia land cover
mapping exercise with SPOT4-VGT data
- Thematic classification
- Conclusions on clustering algorithm
- the ELBG gives significantly better results then
ERDAS ISODATA algorithm when both of them are
applied at the continental level - on the eco-regional level ERDAS ISODATA
algorithm is allow to perform the clustering with
acceptable results - the ecological stratification is critical issue
to classify the forest at the level of main group
of species (for example dark and light
coniferous). Without applying any stratification
it is foreseeable to classify the coniferous,
deciduous and mixed forest. - the efficient way to integrate seasonal mosaics
into the classification procedure have to
developed - the possibility to classify the forest according
to its density is required to be investigated
additionally
Global Land Cover 2000
Global Vegetation Monitoring Unit