日本地球惑星科学連合2024年大会

講演情報

[E] 口頭発表

セッション記号 H (地球人間圏科学) » H-QR 第四紀学

[H-QR04] Deep time perspective on the geological response to climate change

2024年5月28日(火) 10:45 〜 12:00 303 (幕張メッセ国際会議場)

コンビーナ:Wang Liang-Chi(National Chung Cheng University, Taiwan)、Yu Neng-Ti(National Tsing Hua University)、鹿島 薫(島根大学エスチュアリー研究センター/国立中正大学地球環境科学系(台湾))、岡崎 裕典(九州大学大学院理学研究院地球惑星科学部門)、Chairperson:Neng-Ti Yu(National Tsing Hua University)、鹿島 薫(島根大学エスチュアリー研究センター/国立中正大学地球環境科学系(台湾))

10:45 〜 11:00

[HQR04-06] The relationship of river suspended sediment delivery and NDVI of the Tsengwen River basin

★Invited Papers

*CHIA-HUNG JEN1、 Chien-min Chu2 (1.National Kaohsiung Normal University、2.Chinese Culture University)

キーワード:River suspended sediment delivery, NDVI, Tsengwen River

In this study, we try to build the relationship between catchment scale suspended sediment delivery and NDVI of the Tsengwen River, southwestern Taiwan. The suspended sediment delivery is collected and processed by the Water Resource Agency, MOA of Taiwan by using daily river discharge and monthly suspended sediment concentrations. We first construct the annual rating curve equation of the daily river discharge and monthly suspended sediment concentrations, then use this equation to obtain daily suspended sediment from the daily river discharge data. By the way, the river sediment delivery could be obtained from the daily river discharge data. Then we try to obtain the catchment scale NDVI data from the seasonal Landsat images. Each of the 30 m raster cells could have the NDVI value, and then the average catchment scale NDVI value could also be calculated to build the average for the construction of the relationship of river suspended sediment delivery and NDVI of the Tsengwen River basin. The results show that the two have mid negative correlation. It implies that catchment vegetation cover could affect the suspended sediment output.