地中海、红海和阿拉伯海上空的海气二氧化碳交换

IF 2.6 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES
Mona Zarghamipour, Hossein Malakooti, Mohammad Hadi Bordbar
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引用次数: 0

摘要

人为温室气体排放正在重塑海洋二氧化碳吸收模式。这项研究的重点是受人为气候变化影响较大的阿拉伯海、红海和地中海等重要区域,旨在揭示海气二氧化碳交换动态的复杂性。了解这些过程对于预测气候变化和评估海洋生态系统的健康状况至关重要。在此背景下,我们结合基于观测的数据(Oc_v2020)和气候模式模拟的多模式集合,探索了从 1982 年到 2019 年这些地区海气二氧化碳通量(FCO2)的时空变化。我们对模型输出采用了贝叶斯模型平均法,从而更好地反映了模拟的二氧化碳通量。总体而言,气候模式似乎低估了阿拉伯海西部的 FCO2。我们推测,模型失效的原因是垂直水流速度的负偏差以及模型对沿岸上升流过程中碳释放的不真实表示。我们的研究结果表明,红海、阿拉伯海和地中海中部地区的二氧化碳源已经减少,其趋势分别为-0.494±0.009、-1.350±0.001 和-0.329±0.074 gCm-2 year-1 decade-1。与此相反,整个西地中海的二氧化碳吸收汇增强,趋势为- 0.793 ± 0.086 gCm-2 year-1 decade-1。总体而言,水温变化被认为是造成海面二氧化碳分压(pCO2)的主要因素。但阿拉伯海是个例外,在那里,非热效应发挥了主要作用。我们的研究结果表明,二氧化碳通量的变化伴随着海面二氧化碳分压的区域变化。在整个北阿拉伯海,FCO2 也与海面风的变化相关,这可能是由于风驱动的上升流的变化造成的。总之,我们的研究加深了对区域海气二氧化碳交换动力学的理解,强调了在有强烈季节性上升流的地区改进模式代表性的必要性。阿拉伯海的显著变化突出表明,迫切需要对该地区进行科学管理,以减轻人类引起的全球变暖的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Air–Sea CO2 Exchange Over the Mediterranean Sea, the Red Sea and the Arabian Sea

Anthropogenic greenhouse gas emissions are reshaping oceanic CO2 uptake patterns. This study focuses on the crucial regions of the Arabian Sea, Red Sea, and Mediterranean Sea which are highly affected by human-caused climate change, aiming to unravel the complexities of air–sea CO2 exchange dynamics. Understanding these processes is essential for predicting climate changes and assessing the health of marine ecosystems. In this context, a combination of observation-based data (Oc_v2020), and a multi-model ensemble of climate model simulations, were employed to explore the spatial and temporal variations in air–sea CO2 flux (FCO2) over these areas from 1982 to 2019. We implemented the Bayesian Model Averaging approach on the model outputs, resulting in a better representation of simulated CO2 flux. Overall, climate models seem to underestimate the FCO2 over the western Arabian Sea. We speculate that this model failure is attributed to the negative biased in vertical water velocity and the unrealistically representation of carbon release during coastal upwelling processes in the model. Our findings suggest that CO2 source across the Red Sea, the Arabian Sea, and the central region of the Mediterranean Sea has been reduced with a trend of − 0.494 ± 0.009, − 1.350 ± 0.001, and − 0.329 ± 0.074 gCm−2 year−1 decade−1, respectively. In contrast, the CO2 sink across the Western Mediterranean has been enhanced with a trend of − 0.793 ± 0.086 gCm−2 year−1 decade−1. In general, change in the water temperature was recognized as the major contributor to the sea surface partial pressure of CO2 (pCO2). The exception was found in the Arabian Sea, where non-thermal effects play the major role. Our results show that the CO2 flux variation is accompanied by regional changes in the sea surface pCO2. Across the North Arabian Sea, FCO2 is also correlated with the surface wind variability, which is likely due to the changes in wind-driven upwelling. In conclusion, our study advances the understanding of regional air–sea CO2 exchange dynamics, emphasizing the need for improved model representation in areas with intense seasonal upwelling. The prominent changes in the Arabian Sea, underscore the immediate necessity for science-based management in this region to mitigate the impacts of human-induced global warming.

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来源期刊
CiteScore
5.40
自引率
0.00%
发文量
104
审稿时长
1.7 months
期刊介绍: International Journal of Environmental Research is a multidisciplinary journal concerned with all aspects of environment. In pursuit of these, environmentalist disciplines are invited to contribute their knowledge and experience. International Journal of Environmental Research publishes original research papers, research notes and reviews across the broad field of environment. These include but are not limited to environmental science, environmental engineering, environmental management and planning and environmental design, urban and regional landscape design and natural disaster management. Thus high quality research papers or reviews dealing with any aspect of environment are welcomed. Papers may be theoretical, interpretative or experimental.
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