在热带印度洋的表面叶绿素和pCO2的时空变化及其使用CMIP6模型的长期趋势
Sachiko Mohanty1, Biswarup Bhattacharya1, Charu Singh1
1Indian Institute of Remote Sensing, ISRO, Dehradun 248001, Uttarakhand, India.
The Science of the total environment
|November 4, 2023
概括
全球气候变化影响印度洋生物地质化学. 升高的溶解无机碳推动了海洋酸化,南部地区受到影响最大.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 生物地质化学生物地质化学
背景情况:
- 海洋温度和二氧化碳水平的上升对全球海洋生物地质化学有重大影响.
- 印度洋 (IO) 是研究这些气候变化影响的关键区域.
研究的目的:
- 研究印度洋中叶绿素和二氧化碳 (pCO2) 部分压力的时空分布.
- 在模拟这些生物地球化学参数时评估气候模型的性能.
- 确定印度洋pCO2趋势的关键驱动因素.
主要方法:
- 利用卫星数据,现场观测和来自11个合模型相互比较项目第6阶段 (CMIP6) 模型的模拟.
- 评估了和pCO2分布的模型偏差,特别是在阿拉伯海.
- 使用多模型手段分析了pCO2的年度循环和分解的pCO2趋势.
主要成果:
- 大多数CMIP6模型在西南季风期间在索马里地区附近的叶绿素中表现出负偏差.
- 在CESM和CanESM5模型中,热带IO的偏差相对较低.
- 增加的溶解无机碳被确定为主要的驱动因素 (约. 70%) 的pCO2趋势,度和温度起到次要作用.
结论:
- 南部的IO和阿拉伯海最容易受到由溶解无机碳驱动的pCO2变化的影响.
- 模型模拟提供了气候变化下的IO生物地球化学性质变化的洞察力.
- 建议进一步改进模型,以更好地代表海洋生物地质化学.
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