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）)

In line with the Paris Agreement, the Taiwanese government declared a 'net-zero by 2050' policy to counter the ongoing global warming trend caused by anthropogenic activities. The policy was also in line with similar moves around the world, so scientists around the world have created climate models that predict changes in the climate due to foreseeable changes in CO2 and the resulting changes in sea levels.
The session aims to synthesize a 'deep time' perspective of sediment generation and coastline change from mountain to sea. The session calls for the sharing of new methods and new data that reveal sediment generation, transportation, and deposition in short time-scale or in response to large-scale climate change, such as the large and rapid temperature change after the last glaciation. The aim is to better predict the geological response to current climate change. Studies or implementations on facilities or instruments for sediment analyses are also welcome for submission.