Predicting Coral Reef Carbonate Chemistry Through Statistical Modeling: Constraining Nearshore Residence Time Around Guam

IF 1.7 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Aquatic Geochemistry Pub Date : 2023-03-01 DOI:10.1007/s10498-023-09411-6
Heidi K. Hirsh, Thomas A. Oliver, Hannah C. Barkley, Johanna L. K. Wren, Stephen G. Monismith, Derek P. Manzello, Ian C. Enochs
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Abstract

To accurately predict the impacts of ocean acidification on shallow-water ecosystems, we must account for the biogeochemical impact of local benthic communities, as well as the connectivity between offshore and onshore water masses. Estimation of residence time can help quantify this connectivity and determine the degree to which the benthos can influence the chemistry of the overlying water column. We present estimates of nearshore residence time for Guam and utilize these estimates to model the effects of benthic ecosystem metabolism on the coral reef carbonate system. Control volume and particle tracking approaches were used to estimate nearshore residence time. These estimates were paired with observed patterns in the reef carbonate system around Guam using water samples collected by NOAA’s National Coral Reef Monitoring Program. Model performance results suggest that when considering the effects of benthic metabolism on the carbonate system, it is paramount to represent the contact time of the water volume with the benthos. Even coarse estimates of residence time significantly increase model skill. We observed the highest predictive skill in models including control volume derived estimates of residence time, but only when those estimates were included as an interaction with benthic composition. This work shows that not only is residence time critically important to better predict biogeochemical variability in coral reef environments, but that even coarse hydrodynamic models can provide useful residence time estimates at management relevant, whole-ecosystem scales.

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通过统计模型预测珊瑚礁碳酸盐化学:限制关岛附近的近岸停留时间
为了准确预测海洋酸化对浅水生态系统的影响,我们必须考虑到当地底栖生物群落的生物地球化学影响,以及近海和陆上水体之间的连通性。对停留时间的估计可以帮助量化这种连通性,并确定底栖生物对上覆水柱化学的影响程度。我们提出了关岛近岸停留时间的估计值,并利用这些估计值来模拟底栖生态系统代谢对珊瑚礁碳酸盐系统的影响。采用控制体积和粒子跟踪方法估计近岸停留时间。这些估计与使用美国国家海洋和大气管理局国家珊瑚礁监测计划收集的水样在关岛周围珊瑚礁碳酸盐系统中观察到的模式相匹配。模型性能结果表明,在考虑底栖生物代谢对碳酸盐系统的影响时,最重要的是表征水量与底栖生物的接触时间。即使对停留时间的粗略估计也能显著提高模型技能。我们观察到,包括控制体积推导的停留时间估计值在内的模型的预测能力最高,但只有当这些估计值被包括为与底栖生物组成的相互作用时。这项工作表明,停留时间不仅对更好地预测珊瑚礁环境中的生物地球化学变异性至关重要,而且即使是粗糙的水动力学模型也可以在管理相关的整个生态系统尺度上提供有用的停留时间估计。
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来源期刊
Aquatic Geochemistry
Aquatic Geochemistry 地学-地球化学与地球物理
CiteScore
4.30
自引率
0.00%
发文量
6
审稿时长
1 months
期刊介绍: We publish original studies relating to the geochemistry of natural waters and their interactions with rocks and minerals under near Earth-surface conditions. Coverage includes theoretical, experimental, and modeling papers dealing with this subject area, as well as papers presenting observations of natural systems that stress major processes. The journal also presents `letter''-type papers for rapid publication and a limited number of review-type papers on topics of particularly broad interest or current major controversy.
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