マイクロ波リモートセンシング - Pandhito Panji Foundation

Chiba University
研究紹介
Research introductions
ヨサファット テトォコ スリ スマンティヨ
Josaphat Tetuko Sri Sumantyo
千葉大学大学院自然科学研究科像科学専攻
Graduate School of Science and Technology, Chiba University
クラカトア山島群
Situation map
Sumatera
island
Lampung bay
N
SAR mosaic
Indonesia
Lampung
Legundi island
Sertung island
Krakatau
volcano
complex
Panjang island
Rakata island
Banten
Panaitan island
Java island
0
15 km
Volcanoes in Indonesia : 129 volcanoes
Sumatera : 12 Java : 21 Bali : 2
Nusa Tenggara : 20 Banda sea : 9
North Sulawesi : 6
Sangihe : 5
Halmahera : 5
Krakatau volcano complex (ESDM, Indonesia)
歴史:クラカトア山島群の誕生
②
①
Panjang
Rakata
③
Panjang
caldera
before 1883
Danan
Perbuwatan
Sertung
after gigantic eruption with the
lost of volcano dome in 60,000
years ago
ancient Krakatau 60,000
years ago
Rakata
sertung
growing up of Rakata, Danan
and Perbuwatan volcanoes
17th century
North
④
Panjang
Rakata
⑤
Panjang
Danan
Perbuwatan
Sertung
Rakata, Danan and Perbuwatan
volcanoes activities stopped in
1681.
Rakata
⑥
Panjang
caldera
after 1883
Sertung
paroxymal explotion of Danan
and Perbuwatan volcanoes on
August 27, 1883 → 36,417
people killed and swept 295
villages
Rakata
Anak krakatau
Sertung
Krakatau volcano complex
growing slowly nowadays and
always create spectacular history
…
歴史:クラカトア山島群の誕生
350
Height [meter asl]
300
Anak Krakatau
250
200
150
100
50
0
1930
1952
1953
1968
1973
Observation year
Photographs : ESDM, Indonesia
1983
1996
合成開口レーダ画像生成過程
Range
JERS-1 satellite
range compressed
image
North
Azimuth
raw data
North
sensor illumination
azimuth compressed image
rotated image
合成開口レーダ画像生成過程
North
North
Sertung island
Panjang island
Anak Krakatau island
Rakata island
Full scene of JERS-1 SAR 19980731
Subset of JERS-1 SAR 19980731
クラカトア山島群地質図とSAR画像の関係
N
Panjang island
Sertung island
Anak Krakatau island
Rakata island
JERS-1 SAR 19980731
N
Map legend
Lav Lavas in 1963, 1972, 1975, 1980
Sertung island
Panjang island
Pca1 Pyroclastic airfall layer of ash,
scoriaeous lapilli, sand exposed in 1982.
Pca2 Pyroclastic airfall layer of ash,
scoreae, lapilli, sand exposed in 1956.
Smd Material deposit of the rock such as silt,
sand or block size, andesites, basaltic
andesite, and obsidian fragments
Hal
Hyperstene augite andesite lava
Anak Krakatau island
Rakata island
Pf 1883 Pyroclastic flow
Bal
Basaltic lava
Roc1 Rock distribution
Roc2 Estimated rock distribution
Landsat TM 19920518
クラカトア山島群地質図とSAR画像の関係
N
N
Panjang island
Sertung island
Panjang island
Sertung island
Anak Krakatau island
Rakata island
JERS-1 SAR 19980731
Anak Krakatau island
Rakata island
Landsat TM 19920518
Geological cross section
クラカトア火山活動
19941105
North
19961122
19941105
19980913
19961122
19980913
0
2 km
composited SAR images
後方散乱係数の見方
A
B
2000m
1500m
Rakata
island
Sertung island
1000m
Bal
Hal
Pf 1883
Pf 1883
Sea level
500m
Hal
0m
sigma-null o [dB]
A
0
B
1994
1996
1998
-5
-10
-15
-20
0
50
A
100
B
後方散乱係数の見方
C
D
Sertung island
Anak Krakatau island
Hal
Lav 1972/1973
Pf 1883
Pca2 Pca1
1000m
Panjang
island
Hal
Pca2
750m
Pf 1883
Smd
250m
Sea level
Sea level
0m
C
sigma-null o [dB]
500m
D
0
1994
1996
1998
-5
-10
-15
-20
0
50
C
100
D
後方散乱係数の見方
F
E
1000m
Panjang island
750m
Anak Krakatau island
Pca2
Lav 1972/1973
Pca1
Hal
Pca2
Pf 1883
500m
Smd
250m
Sea level
0m
sigma-null o [dB]
E
0
F
1994
1996
1998
-5
-10
-15
-20
0
50
E
100
F
後方散乱係数と火山活動の関係
#1
sigma-null o [dB]
0
-5
-10 5 dB 4 dB
-15
-20
19941105
19961122
19980913
1994
1996
1998
後方散乱係数と火山活動の関係
#2
sigma-null o [dB]
0
-5
-10
-15
-20
19941105
19961122
19980913
1994
1996
1998
後方散乱係数と火山活動の関係
1994
#3
sigma-null o [dB]
0
-5
-10
-15
-20
19941105
19961122
19980913
5 dB
7 dB
1996
1998
後方散乱係数と火山活動の関係
#4
sigma-null o [dB]
0
-5
-10 3 dB
-15
-20
19941105
19961122
19980913
1994
5 dB
1996
1998
後方散乱係数と火山活動の関係
Backscattering coefficient of each soil type
Pf 1883
-8 dB
Pca1
-10 dB
Pca2
-6 dB
Lav 1972/1973
-10 dB
Hal
-12 dB
Smd
-9 dB
Sea surface
-16 dB
Radar respons / backscattering coefficient of new lava around Anak
Krakatau Volcano
Northern area : 5 ~ 7 dB increased
Western area : 4 ~ 5 dB increased
North-eastern area : 3 ~ 5 dB increased