JpGU-AGU Joint Meeting 2017

講演情報

[EJ] 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-TT57] [EJ] 合成開口レーダー

2017年5月24日(水) 10:45 〜 12:15 201A (国際会議場 2F)

コンビーナ:宮城 洋介(防災科学技術研究所)、小林 祥子(玉川大学)、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)、森下 遊(国土交通省国土地理院)、座長:宮城 洋介(防災科学技術研究所)、座長:森下 遊(国土地理院)

12:00 〜 12:15

[STT57-06] JICA-JAXA熱帯林早期警戒システム(JJ-FAST)のための、PALSAR-2/ScanSARを使った早期森林伐採検出手法(アドバンスト)の検討 3 – 南米での時系列解析結果 –

*渡辺 学1コヤマ クリスティアン1林 真智2三好 寛2島田 政信1,2 (1.東京電機大学 理工学部、2.JAXA)

キーワード:森林監視、ALOS-2、多偏波

Time series PALSAR-2/ScanSAR data were used for detecting early-stage deforestation. The data were taken 9 times/year, following ALOS-2 systematic observation strategy [1], and it covers global areas, including major tropical forest in the world. By using this data, JICA and JAXA launched a service, “JICA-JAXA Forest Early Warning System in the Tropics (JJ-FAST)” in November 2016 [1]. The system is on the web, and is freely accessible from a smartphone or other devices. Decrease of Gamma0HV are observed after deforestation, and current algorithm uses HV polarization data and two data taken in different timing. HH polarization, and time series data will be used for the future operation. Time series data obtained in South America with HH and HV polarizations were used, and compared it to the Landsat data to clarify the ability to detect the early-stage deforestation, where fallen trees were left on the ground. The Sigma0HH value increased by 1.2 dB in areas undergoing the early stages of deforestation. The detection timing is almost same as that using the optical sensor. On the other hand, the Sigma0HV value decreased by 3.2 dB for late-stage deforestation areas, where fallen trees were removed. The detection timing is about a few month after the detection of deforestation by Sigma0HH, or optical sensor. Many errors of the deforestation detection were observed at wet forest areas. Temporal variations of Gamma0 were observed for the area, which induces the deforestation detection errors. The variations of Gamma0 shows some correlation with precipitation for both HH and HV polarization [3], and flooding, variation of moisture for soil and trees may be the possible cause for the Gamma0 variation.

[1] ALOS-2 systematic observation strategy,
http://www.eorc.jaxa.jp/ALOS/en/top/obs_top.htm Accessed February 16, 2017
[2] JJ-FAST, http://www.eorc.jaxa.jp/jjfast/jj_index.html, February 16, 2017
[3] Manabu Watanabe, et al., Multi-temporal Fluctuations in L-band Backscatter from a Japanese Forest, IEEE Trans. Geosci. Remote Sensing, 53(11), 5799-5813, 2015