INTERFEROMETRIC COHERENCE MEASUREMENTS OF
TROPICAL, TEMPERATE AND BOREAL FORESTS
| Adrian Luckman and John
Baker |
Remote Sensing Applications Development
Unit, British National Space Centre Monks Wood, Abbots
Ripton, Huntingdon, Cambridgeshire, UK, PE17 2LS
A.Luckman nerc.ac.uk
|
ABSTRACT
- The relationship between forest biomass
density and interferometric coherence was
investigated using SAR image pairs acquired as part
of the ERS tandem mission. Temperate, boreal and
tropical forest test sites were imaged although so
far results are available only from Corsican Pine
stands at Thetford Forest in the UK.
- Interferograms were generated for a variety
of repeat-pass image pairs including four 1-day
pairs, one 35-day pair and one 315 day pair.
Corresponding coherence maps were produced and
registered to a database containing information about
the distribution of stands of Corsican Pine with a
variety of biomass densities estimated from their
age. The relationships between the estimated biomass
density and both the backscattering coefficient and
the coherence were derived from this database.
- The 1-day repeat coherence shows a useful
dependence on biomass density up to around 100 tonnes
/ hectare and this dependence is stronger than that
between backscattering coefficient and biomass
density. The coherence in the forest areas over
longer timescales is uniformly low. However, it
remains high in urban areas even after 315 days.
- Keywords: Forest, interferometry, ERS-Tandem,
biomass density
1. INTRODUCTION
- ERS SAR remote sensing has the important advantages of
radiometric stability, long-term support and relative
independence from atmospheric conditions. However, for
forest monitoring purposes, C-band data is not ideal
because in general the backscattering coefficient of
forests at this wavelength is poorly related to their
biophysical characteristics. SAR interferometry is
expected to provide improved capability for forest
applications by making use of the additional information
carried in the phase differences and in the coherence (g)
between repeat-pass image pairs [Refs. 1 and 2]. The
coherence is expected to decrease with forest density
because there is more opportunity for small changes in
scattering characteristics over time when more scatterers
are present. Over time scattering characteristics might
be affected by moisture, wind or growth. Also, the
interferometric phase difference between clearings and
adjacent forest canopies may allow tree height to be
inferred.
- This paper describes the preliminary findings of the ESA
ERS Tandem project AOT.UK316 which aims to investigate
the relationship between interferometric coherence and
biomass density and to use the extra information derived
from repeat-pass interferometry to assess forest
characteristics at several established forest test sites.
These include a temperate plantation at Thetford in the
UK, a boreal forest test site at Siggefora in Sweden and
tropical forest test sites at Tapajós and Manaus in
Brazil.
- Preliminary work suggests that 1-day interferometric
coherence is very low over the tropical forest test sites
but carries useful information at the temperate and
boreal forests sites. As most data so far has been
received and processed for the temperate forest site at
Thetford, this paper describes the preliminary results
from interferometric processing carried out at that site.
2. TEST SITE, FIELD AND IMAGE DATA
Thetford Forest is a predominantly coniferous plantation first
developed in the 1930s on heath and low grade agricultural land
in East Anglia. It consists mainly of Scots and Corsican Pine
stands and includes a large range of ages of Corsican Pine from 3
years to 60 years.
Fieldwork had been carried out to measure the biomass density
of Corsican Pine stands of a range of ages. This data was used to
characterize the relationship between stand age and biomass
density and hence to allow the biomass density to be estimated
within a much larger set of forest stands. Plantation stocking
maps provided by the UK Forestry Commission (now Forest
Enterprise) were digitized to determine the location of forest
stands of different ages of Corsican Pine within a geocoded
database at a resolution of 10m.
Image data consists of four ERS Tandem image pairs from August
1995 and April, May and June 1996. This dataset allowed
repeat-pass interferometry to be investigated over many time
delays including 1, 35, 70, 244, 279 and 315 days.
3. IMAGE PROCESSING
- Interferometric processing was carried out using the
ESRIN/POLIMI ISAR software which proved to be effective
though cumbersome.
- All 8 images were co-registered to sub-pixel accuracy
using the most recent image as a reference.
Interferograms and optimized coherence maps were derived
for the subset of the possible combinations of image
pairs which were considered of most interest. The ones
examined in this paper include all four possible 1-day
repeat pairs, one of the possible 35-day repeat pairs and
the maximum 315-day repeat pair.
- The complex SAR images were detected and averaged to form
6-look amplitude products. These were calibrated (taking
into account only the K-factor for this preliminary
analysis) and registered to a geocoded database
containing the forest stand information. The coherence
maps were also registered to this same database.
- The relationships between the estimated biomass density
and both the backscattering coefficient (s0)
and the coherence were derived from the database using
the digitized forest stand map. In each case average
values were calculated over image areas of at least 150
pixels representing homogeneous forest stands of at least
1.5 ha.
4. PRELIMINARY RESULTS
Results are shown quantitatively in Figure 1 and qualitatively
in Figures 2 to 11.
Although much of the Thetford area is covered by forest,
strong phase fringes were developed for each of the 1-day repeat
image pairs over the whole area. In the interferograms generated
from image pairs spanning greater than 1-day, fringes were
visible only outside the forest area.
The fringes, before and after the removal of orbital effects,
for one of the 1-day repeat image pairs are shown in Figures 2
and 3. These have not been normalised but the appearance of only
one fringe over the area in Figure 3 confirms the flat nature of
this region. Ongoing work will determine if the phase difference
between clearings and adjacent forest canopies may allow tree
height to be inferred.
Figure 1 shows that there is a strong relationship between
interferometric coherence and biomass density for each of the
1-day repeat pairs but that this relationship is not significant
over time scales of 35 days or more. In each of the 1-day repeat
cases, this relationship is stronger than that between s0
and biomass density. This is partly due to the soil scattering
component which becomes significant at low biomass density values
in some images, presumable because of higher soil moisture.
There is some variability in the relationship between biomass
density and 1-day repeat coherence and future work will
investigate whether this variability is related to meteorological
or atmospheric conditions. This variability is also apparent in
Figures 4 and 5 which show the coherence maps for two of the
1-day repeat pairs. Figure 10 shows a colour composite of three
of the 1-day repeat coherence maps showing that a large amount of
extra information is available using this technique. Here the
area with lowest coherence indicates the mature stands of
Thetford Forest.
Figures 6 and 7 show coherence maps for one of the 35-day
repeat and the 315-day repeat pairs. Some coherence remains in
the towns and over the Feltwell agricultural area after a month
in the early growing season but little remains elsewhere. Over a
time scale of nearly a year, there still remains high coherence
in the urban areas and over the airfields that are characteristic
of this region. Figure 11 combines coherence maps from 1, 35 and
315 days showing the limits of coherence over 1-day in red, 35
days in yellow and long term in white.
Another source of information in the ERS data lies in the
difference in intensity between images from different dates.
Figures 8 and 9 show composites of coherence, s0 and
Ds0 for 1-day and 35-day repeat image pairs [Refs. 3
and 4]. This demonstrates that for 1-day repeat pairs, most
information is carried in the coherence while for longer time
periods more information is carried in the intensity difference
than in the coherence.


5. CONCLUSIONS AND FUTURE WORK
This study has investigated the relationship between
interferometric coherence and biomass density of Corsican Pine
stands at Thetford Forest in the UK for repeat-pass ERS SAR image
pairs over a variety of time scales.
The 1-day repeat coherence is strongly related to biomass
density although this relationship is variable with the date of
acquisition, probably because of environmental factors.
Preliminary results show the dependence to be monotonic although
noisy up to biomass densities of around 100 tonnes per hectare.
Coherence over longer time scales than 1-day is uniformly low
over forest areas. The relationship between biomass density and
1-day repeat coherence is stronger than that between biomass
density and s0 suggesting that the extra information
provided by SAR interferometry may be useful for forest
applications.
Well developed phase fringes from 1-day repeat data may allow
phase difference information to be used in the estimation of tree
height.
Future work will concentrate on determining the sources of
variability in the relationships and using the phase information
to estimate tree height. The analysis will be repeated at the
boreal forest test site at Siggefora in Sweden and further
attempts will be made to perform similar analyses of the tropical
forest test sites.
6. REFERENCES
[1] J. O. Hagberg, L. M. H. Ulander, and J. Askne,
ìRepeat-Pass SAR Interferometry Over Forested Terrain,î IEEE
Transactions on Geoscience and Remote Sensing, vol. 33, pp.
331-339, 1995.
[2] J. I. H. Askne, P. B. G. Dammert, L. M. H. Ulander, and G.
Smith, ìC-band Repeat-Pass Interferometric SAR Observations of
the Forest,î IEEE Transactions on Geoscience and Remote
Sensing, vol. 35, pp. 25-35, 1997.
[3] U. Wegmuller and C. Werner, ìSAR Interferometric
Signatures of Forest,î IEEE Transactions on Geoscience and
Remote Sensing, vol. 33, pp. 1153-1161, 1995.
[4] U. Wegmuller and C. Werner, ìRetrieval of Vegetation
Parameters with SAR Interferometry,î IEEE Transactions on
Geoscience and Remote Sensing, vol. 35, pp. 18-24, 1997.
Keywords: ESA European
Space Agency - Agence spatiale europeenne,
observation de la terre, earth observation,
satellite remote sensing,
teledetection, geophysique, altimetrie, radar,
chimique atmospherique, geophysics, altimetry, radar,
atmospheric chemistry
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