The “stabilized” sea level in late Holocene
ID:3802 View Protection:ATTENDEE Updated Time:2024-04-14 12:35:21 Hits:1905 Invited speech

Start Time:2024-05-19 16:29(Asia/Shanghai)

Duration:15min

Session:S20 主题20、城市海岸带与陆海统筹 » S20-3主题20、城市海岸带与陆海统筹 专题20.4、专题20.6、专题20.7(19日下午,4F观海厅2)

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Abstract
In the context of climate change, understanding the magnitude and rate of sea level rise is crucial for predicting and adapt with climate change. Geological records indicate that sea levels have fluctuated by hundreds of meters in the past, with rates up to 4 meters per century. Nonetheless, exceptionally steady sea levels throughout the last few millennia have been seen, contributing to the rise of human civilization and coastal megacities. In this study, we perform geological evidence, numerical simulations, and ancient literature, to show that the “stabilized” sea levels observed over the past few thousand years are not common and likely caused by the transition between rising and falling sea levels. Furthermore, we have found that sea level changes lag climate changes by millennia. Recognizing these facts are of particularly important for planning future adaptation strategy.
Keywords
sea level rise,Mid-late Holocene
Speaker
杨虎
研究员 南方海洋科学与工程广东省实验室(珠海)

Submission Author
杨虎 南方海洋科学与工程广东省实验室(珠海)
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Important Date
  • Conference Date

    May 17

    2024

    to

    May 20

    2024

  • Mar 31 2024

    Draft paper submission deadline

  • Mar 31 2024

    Contribution Submission Deadline

  • May 20 2024

    Registration deadline

Sponsored By
青年地学论坛理事会
Organized By
厦门大学近海海洋环境科学国家重点实验室
中国科学院城市环境研究所
自然资源部第三海洋研究所
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