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  • ACRS 1998


    Geology/Geomorphology

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    The Environmental Monitoring for Mt. Pinatubo Area in the Philippines Using Satellite Optical and SAR Data

    Genya Saito, Nobuyuki Mino, Shigeo Ogawa, Takuhico Murakami, Naoki Isitsuka, Min Cong, Marcelina M. Dumayac**, Arlene M. Evangelista*** and Hiroshi Ohkura****
    National Institute of Agro-Envoronmental Sciences, 3-1-1 Kannondai Tukuba, Japan
    **National mapping and Resource Information Authority, Fort Andres Bonifacio, 1201 Makati, Philippines
    ***Bureau of Soil and Water Management, Elliptical Rd. Corner Visayas Ave. Diliman, Quezon, Philippines
    ****National Research Institute of Earth Science and Disaster Prevention, 3-1, Tennodai, Tukuba, Japan

    Abstract
    In this paper, the authors developed the methodology of vegetation cover ratios using multiple types of optical sensor data and clarified microwave backscattering characteristics on vegetation and environments acquired by Synthetic Aperture Radar (SAR). These data are used to analyze the effects of eruption from Mt. Pinatubo, the Philippines over a time period from 1991 (eruption time) to present (1997). By this satellite image analysis, chronological changes from vegetation damage in the term of decrease rate of vegetation cover caused by volcanic ash fall and suffered area by mudflows. Through satellite image analysis, changes in vegetation damage over time is assessed from the decrease in vegetation cover to volcanic ash and mudflows.

    Introduction
    Satellite remote sensing is only one method of monitoring vegetation changes. However it is very difficult to acquire optical remote sensing data at the coast and island in Asia monsoon area, because of the cloud cover. For the reason, we cannot perform using only one optical sensor to monitor vegetation for suitable interval and long term observation. We must use multi optical sensors and/or Synthetic Aperture Radar (SAR) sensors. Mt. Pinatubo that located the northern part of Luzon Island erupted hugely on June 15, 1991, and agriculture land and first in this area were suffered much damage owing to the eruption10. We monitored this area and estimated vegetation damage by ash falling and mudflows from Mt. Pinatubo using MOS-1/MESSR, LANDSAT/TM, JERS-1/OPS as optical sensors, and JERS-1/SAR and ERS-1/SAR as macro-wave sensors.

    Optical Sensor Data
    We used MOS-1/MESSR data that were before and after Mt. Pinatubo eruption, and LANDSAT/TM and JERS-1/OPS that were after the eruption. Table 1 shows the characteristics of used optical sensors and table 2 indicates list of used optical satellite sensor data.

    Table 1 Characteristic of used optical sensors


    Table 2 List of used optical satellite sensor data

    SAR Data
    Table 3 shows characteristics of SAR instruments and Table 4 shows the list of SAR data used in this study

    SensorWavelengthIncident anglePolarizationSpatial resolutionSwath
    JERS-1L-band (1.275GHz 23.5cm)38.5HH18 m(3 looks)75 km
    ERS-1C-band (5.3 Ghz 5.66cm)23VV15 m(3 looks)100km
    Table 3 Characteristics of used SAR instruments


    Name of SenserDate(YYYY/MM/DD)OrbitTreatment Level
    JERS-1/SAR1993/03/23Descending2.1 Geometry correction
    "1995/02/25""
    ERS-1/SAR1993/08/29Ascending1.0 Raw image
    ERS-1/SAR1995/11/19Descending0 Raw signal data
    ERS-2/SAR1995/11/20"0     "
    ERS-1/SAR1996/04/21Ascending0     "
    ERS-2/SAR1996/04/22"0     "
    Table 4. List of used SAR data

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