information to differentiate between various forest
or other agricultural and cultural cover types.
Radar data, which utilizes the active microwave
portion of the spectrum, can provide important
additional information about terrain surfaces and
forest and agricultural plants canopies. Satellite
remote sensing often used to obtain information,
on actual land cover/land use and to monitor
changes in the regions with often cloudy
conditions such as indonesia. However, radar data
can be independent of the atmospheric conditions
and the time of the day. Therefore, data supplied
by Synthetic Aperture Radar (SAR) such as the
European Remote Sensing Satellite (ERS-1) has
potential for environmental applications. The
main objective of this research was to detect
changes in the land use of the tropical rain
forested area, including the forest land, agricultural
land and other land resources near the forest using
multi-temporal optical data (e.g., Landsat MSS and
TM and Spot XS data) and microwave (e.g. ERS-1
and JERS-1 radar data) satellite images in two
Indonesian test site (i.e. Bengkulu, South Sumatra
and Jambi, Central Sumatra).
2. MATERIALS AND METHODS
2.1 Study Areas
Two test sites were used for this research. The
first study area is located on the south west coast
of Sumatra, Indonesia. It is situated between
3°35’00" and 3°51°00" Latitude South and between
102°12°00" and 102°45°00" Longitude East. The
area lies in the Bengkulu province and covers
about 2,100 km?. In general, the topography of
this study area can be considered undulating
through rolling to mountainous. The altitude
varies from O to 1800 m asl. The settlements are
located along the main and secondary roads.
Bengkulu is one of the nine major cities in
sumatra and it is the seaport city on the south-
western coast of Sumatra. The main river in the
area is the Air-Bengkulu river. Most of the
irrigation systems are of the conventional gravity
type.
The major land use/cover classes exist in the area
are: cultivated land which consist of rain fed
agriculture land and irrigated agriculture land;
agro-forestry, which is a combination of forest
trees and crops; forest plantations; shifting
cultivation, is characterized by scattered arable
plots in the forest area which involves the
cutting/burning of the natural vegetation (forest,
scrub or grass); natural forest is consist of
highland and lowland rain forest; mixed cover of
bushes Grass/Scrub/shrubland; and urban or
settlements which include villages, towns and
cities.
The second area of study lies approximately from
316
latitude 1° 15 to 1° 45 (S) and from longitude
102° 15 to 102° 45 (E). This area is located in the
Bungotebo county, northwestern part of Jampi
province, Central Sumatra. The river Batang Har
divided the area into two part. The form of
topography in this site is relatively flat land with
a very small part of mountains. The altitude varie
between 25 to 160 m. Verstappen (1973), used the
peneplain to refer to this type of terrain. Part of
the peneplain are covered with acid volcanic tuff
particularly near the Bukit Barisan mountain
Podzolic red yellow soil type is dominant in the
study area. The land cover in this test site is
dominated by forests. Plantations of rubber, oi
palm are found in the area. Most of rubber
plantations were planted by the indigenous people
and normally located at the boundary of or inside
forest. New settlements that cause by
transmigration is located in the south and southeast
of the study area. Other agriculture cover types
like rice field also found in the area.
2.2. Data Used
For the first test site, the remote sensing data were
acquired by both passive and active systems,
Landsat-1 MSS data of 13 June 1973 were used to
classify land use in 1973 and to compare with land
use data of 1990. The spatial resolution was 80 x
80 m square and spectral bands were representing
the green, red, and two in infrared part of the
spectrum. The Landsat-5 TM data, acquired on 29
December 1990 were used to study recent land
use. The spectral bands used were blue, green,
red, NIR, two MIR, and one thermal IR. The
spatial resolution was 30 x 30 m square.
ERS-1 Synthetic Aperture Radar (SAR) data
acquired on 20 July 1993 in C-Band (5.6 cm
wavelength) and VV polarization were used. The
spatial resolution was 12.5 m with a swath width
of 100 km. The incidence angle was 23°. During
1994, two other images were acquired of the study
area. Unfortunately, because the new images wer
obtained in a different acquisition mode, there was
a significant shift from the image acquired in the
preceding year. Two JERS-1 Synthetic Aperturt
Radar data sets acquired on 6 March 1993 and 20
May 1994 were also used for the study. The data
were obtained in the L-Band (23 cm wavelength)
HH polarization and an incidence angle of 35.
The spatial resolution was 12.5 m and the swath
width was 75 km.
For the second study area the following data wer
available: Landsat-5 TM data of September 13
1993, Spot XS data of March 21, 1993, ERS!
images of October 17, 1993, June 6, 1994, and
July 7, 1994, and JERS-1 of August 16, 1993.
2.3 Method Used
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996