Temperature and dissolved oxygen trends in English estuaries over the past 30 years

IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY Estuarine Coastal and Shelf Science Pub Date : 2024-07-26 DOI:10.1016/j.ecss.2024.108892
Alec M. Hutchings, Caitlin S. de Vries, Nick R. Hayes, Harriet G. Orr
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Abstract

Water temperature and dissolved oxygen are two important parameters which affect the ecosystem functions which estuaries provide. As such, we need to understand the long-term change of these parameters in English estuaries to better understand those areas which may be vulnerable in the present and future. Detecting these trends in monitoring data is difficult however, since temporally and spatially heterogeneous sampling has the potential to obscure any long-term component of change. In this study, we use a generalized additive model (GAM) approach to isolate the inter-annual change of water temperature and dissolved oxygen in spot sampled monitoring data across English estuaries. This technique can account for the potentially non-linear variability caused by temporal and spatial variations in sampling throughout the day and year. We find that water temperature in all modelled estuaries has warmed, with an average warming of 0.037 °C/yr between 1990 and 2022, in line with temperature change in rivers and the sea surface around England. For the same period, dissolved oxygen has increased for roughly half of modelled estuaries and decreased for the other half. The variation across English estuaries in these two conditions is best explained by the geographical location of an estuary. Many of the estuaries warming at the greatest rate are those where sea surface temperature increase has also been greatest. We suggest the observed distribution of changes in dissolved oxygen can be explained by three processes: (1) temperature driven change, (2) dissolved oxygen improvement (e.g., reduced nutrient inputs through wastewater management regulation) and (3) changes in the number of primary productivity-induced super saturation events. This study provides a comprehensive look at temperature and dissolved oxygen change across English estuaries over the past ∼30 years, which may provide information on the processes behind how these water quality parameters have changed and will continue to do so.

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过去 30 年英国河口的温度和溶解氧趋势
水温和溶解氧是影响河口生态系统功能的两个重要参数。因此,我们需要了解这些参数在英格兰河口的长期变化情况,以便更好地了解目前和未来可能出现问题的区域。然而,要从监测数据中发现这些趋势并不容易,因为时间和空间上的异质性取样有可能会掩盖任何长期变化因素。在本研究中,我们采用广义加法模型(GAM)方法,从英格兰河口的定点采样监测数据中分离出水温和溶解氧的年际变化。这种技术可以解释因全天和全年采样的时间和空间变化而造成的潜在非线性变化。我们发现,所有建模河口的水温都有所升高,1990 年至 2022 年间平均升高 0.037 ℃/年,与英格兰各地河流和海面的温度变化一致。同期,大约一半的模拟河口溶解氧增加,另一半河口溶解氧减少。英国各河口在这两个条件上的差异,最好用河口的地理位置来解释。许多变暖速度最快的河口也是海面温度上升最快的河口。我们认为,观察到的溶解氧变化分布可以用三个过程来解释:(1) 温度驱动的变化,(2) 溶解氧的改善(如通过废水管理条例减少营养物质的输入),(3) 初级生产力引起的超饱和事件数量的变化。这项研究全面考察了英国河口在过去 30 年间的温度和溶解氧变化,可为了解这些水质参数的变化过程提供信息。
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来源期刊
CiteScore
5.60
自引率
7.10%
发文量
374
审稿时长
9 months
期刊介绍: Estuarine, Coastal and Shelf Science is an international multidisciplinary journal devoted to the analysis of saline water phenomena ranging from the outer edge of the continental shelf to the upper limits of the tidal zone. The journal provides a unique forum, unifying the multidisciplinary approaches to the study of the oceanography of estuaries, coastal zones, and continental shelf seas. It features original research papers, review papers and short communications treating such disciplines as zoology, botany, geology, sedimentology, physical oceanography.
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