日本地球惑星科学連合2015年大会

講演情報

口頭発表

セッション記号 S (固体地球科学) » S-TT 計測技術・研究手法

[S-TT54] 合成開口レーダー

2015年5月25日(月) 09:00 〜 10:45 201A (2F)

コンビーナ:*山之口 勤(一般財団法人 リモート・センシング技術センター)、小林 知勝(国土交通省国土地理院)、宮城 洋介(防災科学技術研究所)、座長:山之口 勤(一般財団法人 リモート・センシング技術センター)、小林 知勝(国土交通省国土地理院)

09:45 〜 10:00

[STT54-11] ALOS-2データの氷河域研究への適用-初期解析事例-

*山之口 勤1土井 浩一郎2中村 和樹3青木 茂4 (1.(一財)リモート・センシング技術センター、2.国立極地研究所、3.日本大学、4.北海道大学低温科学研究所)

ALOS-2/ PALSAR-2 successfully launched on 24, May, 2014 and it has been collecting the data all over the world properly.The major difference between ALOS and ALOS-2 are improvement of spatial resolution, short revisit cycle, keeping short baseline and improvement of observation opportunity by left-right looking. Among them, the important improvement are short base line and short revisit cycle because it is expected to provide the high coherency between observations. It is able to observe in 14 days difference in the best case, it is almost 3 times shorter temporal difference than ALOS data.
Based on these difference, we choose two area for the comparison between ALOS-2 and ALOS data. One is Mt. El Salto, Andes region. This area has many rock glaciers and we successfully detected the movement of them. Here we would like to check whether ALOS-2 can detect these Phenomenon as ALOS data. The other target area is East Antarctic marginal zone between ice sheet and ice shelf. We already confirmed that the possibility of the extraction of grounding line by PALSAR data and how it improve using ALOS-2 data to take into the effect of short revisit cycle and short baseline. We plan to report how ALOS-2 data be useful for cryospheric study based on these two case studies.
ALOS-2/PALSAR-2 and ALOS/PALSAR data were provided by Research Announcement by JAXA PI project (PI No. P1418002)