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Landscapes on the edge: River intermittency in a warming world 边缘景观:变暖世界中的河流间歇
IF 5.8 1区 地球科学 Q1 GEOLOGY Pub Date : 2024-07-01 DOI: 10.1130/g52043.1
Jonah S. McLeod, Alexander C. Whittaker, Rebecca E. Bell, Gary J. Hampson, Stephen E. Watkins, Sam A.S. Brooke, Nahin Rezwan, Joel Hook, Jesse R. Zondervan, Vamsi Ganti, Sinéad J. Lyster
Sediment transport in rivers is not steady through time. Highly intermittent river systems, which only transport bedload during the most significant flow events, are particularly sensitive to changes in climate and precipitation patterns. People and landscapes can be vulnerable to fluvial processes, and quantifying river intermittency is critical for assessing landscape response to projected changes in precipitation extremes due to climate change. We generated new constraints on recent to modern fluvial intermittency factors—the frequency at which bedload is mobilized in a river—based on field measurements in the Corinth Rift, Greece, and Holocene sediment accumulation rates. Results reveal some of the lowest documented intermittency factors to date, showing Mediterranean rivers can transport an entire annual sediment load in a rare storm event. Coupling intermittency calculations with historical flood and precipitation data indicates these rivers transport bedload during one storm every ~4 yr, associated with rainfall >50 mm/d, and subsequent floods; this hydroclimate is typical across the Mediterranean region. Furthermore, climate models predict precipitation extremes will increase across Europe, and the frequency of events that surpass thresholds of sediment transport will increase significantly, potentially causing sediment loads to double by 2100 CE. As the area of arid land likely to host intermittent rivers also increases, sensitive landscapes are on the edge of significant geomorphic change, driven by global warming.
河流中的沉积物迁移在时间上并不稳定。间歇性很强的河流系统只在最重要的水流事件期间输送泥沙,因此对气候和降水模式的变化特别敏感。人类和地貌都很容易受到河流过程的影响,量化河流的间歇性对于评估地貌对气候变化导致的极端降水变化的响应至关重要。我们根据在希腊科林斯裂谷的实地测量结果和全新世沉积物累积率,对近代至现代的河流间歇因子--河床负荷在河流中的移动频率--提出了新的约束条件。结果表明,这是迄今为止有据可查的最低间歇系数,表明地中海河流可以在一次罕见的风暴事件中运走全年的泥沙量。将间歇性计算与历史洪水和降水数据相结合,表明这些河流在每隔约 4 年的一次暴风雨期间(降雨量大于 50 毫米/天)以及随后的洪水中输送泥沙;这种水文气候在整个地中海地区都很典型。此外,据气候模型预测,整个欧洲的极端降水量将增加,超过泥沙输运阈值的事件频率将显著增加,到公元 2100 年,可能导致泥沙负荷增加一倍。随着可能形成间歇性河流的干旱土地面积的增加,敏感的地貌正处于全球变暖导致的重大地貌变化的边缘。
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引用次数: 0
Turbidity currents regulate the transport and settling of microplastics in a deep-sea submarine canyon 浊流调节深海海底峡谷中微塑料的迁移和沉降
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-06-04 DOI: 10.1130/g52116.1
Xiaodong Zhang, Zhifei Liu, Daoji Li, Yulong Zhao, Yanwei Zhang
Microplastics are widely distributed in deep oceans, with some of the highest concentrations reported in submarine canyons, which are thought to be closely related to turbidity currents. However, the turbidity current role in microplastic transport and deposition is poorly understood. Here, we present temporal variation in microplastic abundance and settling flux from sediment trap observations on the levee of Gaoping Canyon, offshore Taiwan, where turbidity currents occur frequently. The results showed that relatively high microplastic abundance and flux were consistent with the increases of near-bottom suspended sediment concentration caused by turbidity currents. The microplastics, dominated by polypropylene (59%) and polyethylene (21%), were probably derived from Taiwan coastal resuspension and river input and then transported into the submarine canyon by typhoon- or earthquake-triggered turbidity currents. During the turbidity currents, the average microplastic abundance and flux was 4137 particles per kilogram and 40.11 particles per square meter per day, respectively, showing an increase of 49% and 270%, respectively, compared to non−turbidity current periods. The total microplastic flux during the turbidity currents accounted for ∼76% of annual flux. Our study highlights turbidity currents to be the major hydrodynamic process in regulating microplastic transport and settling in a submarine canyon.
微塑料广泛分布于深海,据报道,一些浓度最高的微塑料出现在海底峡谷,这被认为与浊流密切相关。然而,人们对浊流在微塑料迁移和沉积中的作用知之甚少。在此,我们介绍了在浊流频繁发生的台湾近海高屏峡谷堤坝上通过沉积物捕集器观测到的微塑料丰度和沉降通量的时间变化。结果表明,相对较高的微塑料丰度和通量与浊流导致的近底悬浮沉积物浓度增加相一致。这些微塑料主要是聚丙烯(59%)和聚乙烯(21%),可能来自台湾沿海的再悬浮和河流输入,然后被台风或地震引发的浊流输送到海底峡谷。在浊流期间,微塑料丰度和通量分别为平均每天每公斤 4137 粒和每平方米 40.11 粒,与非浊流期间相比,分别增加了 49% 和 270%。浊流期间的微塑料通量占全年通量的 76%。我们的研究表明,浊流是调节海底峡谷微塑料迁移和沉降的主要水动力过程。
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引用次数: 0
Fluvial response to Late Pleistocene–Holocene climate change in the Colorado River drainage, central Texas, USA: COMMENT 美国得克萨斯州中部科罗拉多河流域晚更新世-全新世气候变化的冲积响应:COMMENT
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-05-01 DOI: 10.1130/g51850c.1
Mike Blum, Dustin Sweet
Abstract not available
无摘要
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引用次数: 0
Fluvial response to Late Pleistocene–Holocene climate change in the Colorado River drainage, central Texas, USA: REPLY 美国得克萨斯州中部科罗拉多河流域晚更新世-全新世气候变化的冲积响应:REPLY
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-05-01 DOI: 10.1130/g52087y.1
E. Gabriela Gutiérrez, Daniel F. Stockli
Abstract not available
无摘要
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引用次数: 0
Ice-rafted dropstones at midlatitudes in the Cretaceous of continental, Iberia: REPLY 伊比利亚大陆白垩纪中纬度地区的冰蚀滴石:REPLY
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-04-01 DOI: 10.1130/g52152y.1
Juan Pedro Rodríguez-López, Carlos L. Liesa, Aránzazu Luzón, Arsenio Muñoz, María J. Mayayo, Julian B. Murton, Ana R. Soria
Abstract not available
无摘要
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引用次数: 0
Ice-rafted dropstones at midlatitudes in the Cretaceous of continental Iberia: COMMENT 伊比利亚大陆白垩纪中纬度地区的冰蚀滴石:评论
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-04-01 DOI: 10.1130/g52006c.1
M. Isabel Benito, I. Emma Quijada, Martín Garcia-Martín, Alejandro Pertuz, Pablo Suarez-Gonzalez, Angélica Torices, Sonia Campos-Soto
Abstract not available
无摘要
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引用次数: 0
Discovery of Permian–Triassic eclogite in northern Tibet establishes coeval subduction erosion along an ~3000-km-long arc: REPLY 在西藏北部发现的二叠纪-三叠纪蚀变岩确定了沿一条约3000公里长的弧线共生的俯冲侵蚀作用:REPLY
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-03-01 DOI: 10.1130/g52012y.1
Chen Wu, Andrew V. Zuza, Drew A. Levy, Jie Li, Lin Ding
Abstract not available
无摘要
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引用次数: 0
Boninitic melt percolation makes depleted mantle wedges rich in silica: COMMENT 褐铁矿熔体渗流使贫化的地幔楔块富含二氧化硅:评论
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-03-01 DOI: 10.1130/g51824c.1
Antoine Bénard, Dmitri A. Ionov, Oliver Nebel, Richard J. Arculus
Abstract not available
无摘要
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引用次数: 0
Boninitic melt percolation makes depleted mantle wedges rich in silica: REPLY 褐铁矿熔体渗流使贫化的地幔楔块富含二氧化硅:回复
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-03-01 DOI: 10.1130/g51951y.1
Ming Chen, Jianping Zheng, Hong-Kun Dai, Qing Xiong, Min Sun, Mikhail M. Buslov, Xiang Zhou, Jingao Liu
Abstract not available
无摘要
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引用次数: 0
Discovery of Permian–Triassic eclogite in northern Tibet establishes coeval subduction erosion along an ~3000-km-long arc: COMMENT 藏北二叠纪-三叠纪蚀变岩的发现确定了沿约 3000 公里长的弧线共生的俯冲侵蚀:COMMENT
IF 5.8 1区 地球科学 Q1 Earth and Planetary Sciences Pub Date : 2024-03-01 DOI: 10.1130/g51860c.1
Shuguang Song, Hafiz U. Rehman
Abstract not available
无摘要
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引用次数: 0
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Geology
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