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Assessing the impact of climate change on sediment discharge using a large ensemble rainfall dataset in Pekerebetsu River basin, Hokkaido 气候变化对北海道北列别河流域输沙量的影响
3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-09-04 DOI: 10.1186/s40645-023-00580-0
Riho Kido, Takuya Inoue, Misako Hatono, Kazuki Yamanoi
Abstract Increased rainfall associated with climate change can increase sediment discharge. The supply of fine sediment from slope failures inhibits bed armoring of mountain rivers and increases sediment discharge to the downstream reaches. Floods without slope failures lead to bed erosion and armoring and may ultimately decrease sediment discharge. Thus, it is important to consider sediment discharge from slope failure and bed erosion as factors affecting sediment production. Climate change affects not only the rainfall amount, but also the temporal rainfall pattern; consequently, the pattern affects the sediment production factors and the amount of sediment discharge. However, changes in sediment discharge due to climate change based on sediment production sources have not yet been clarified. In this study, we statistically analyzed 1200 results simulated using a physics-based sediment runoff model to assess the impact of changes in temporal rainfall patterns on sediment discharge and sediment production sources in the Pekerebetsu River Basin. In the simulations, we used the rainfall predicted in d4PDF (Database for policy decision-making for future climate change), a large ensemble climate simulation database at 5 km and 20 km resolutions. Our results showed that the climate-driven increase in sediment discharge was considerably larger than that of rainfall. An increase in short-term heavy rainfall increased the supply of fine sediments from slope failure. This resulted in the suppression of bed armoring and a large increase in sediment discharge. Thus, the increase in sediment discharge is not only caused by an increase in rainfall but also by changes in temporal rainfall patterns and sediment production factors. The sediment discharge calculated for the 20 km resolution climate projection was nearly one order of magnitude smaller than that for the 5 km resolution. This suggests that the 20 km resolution climate projections do not adequately represent orographic rainfall in the mountains and thus, do not adequately reproduce extreme sediment discharge events. An increased sediment supply causes bed aggradation and decreases the river conveyance capacity of the downstream channel. The model developed in this study will contribute to flood risk analysis and flood control planning for increased rainfall due to climate change.
与气候变化相关的降雨增加可增加泥沙流量。坡面破坏带来的细泥沙抑制了山地河流的河床盔甲化,增加了向下游的输沙量。没有边坡破坏的洪水会导致河床侵蚀和装甲化,并可能最终减少泥沙流量。因此,考虑坡面失稳和河床侵蚀的输沙量是影响产沙的重要因素。气候变化不仅影响降水量,而且影响降水的时间格局;因此,这种模式影响了产沙因子和输沙量。然而,基于产沙源的气候变化引起的输沙量变化尚未得到澄清。在这项研究中,我们统计分析了1200个基于物理的泥沙径流模型模拟结果,以评估时间降雨模式变化对佩克列别苏河流域输沙和产沙源的影响。在模拟中,我们使用了d4PDF(未来气候变化政策决策数据库)中预测的降雨量,d4PDF是一个5公里和20公里分辨率的大型集合气候模拟数据库。结果表明,气候驱动的输沙量增加明显大于降雨。短期强降雨的增加增加了边坡破坏带来的细沉积物的供给。这就抑制了河床的铠装作用,并大大增加了输沙量。因此,输沙量的增加不仅是由降雨的增加引起的,而且还与时间降雨模式和产沙因子的变化有关。20 km分辨率气候预估的输沙量比5 km分辨率气候预估的输沙量小近一个数量级。这表明,20公里分辨率的气候预估不能充分代表山区的地形降雨,因此不能充分再现极端沉积物排放事件。泥沙供给的增加导致河床淤积,降低下游河道的输水能力。本研究建立的模型将有助于气候变化导致降雨增加的洪水风险分析和防洪规划。
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引用次数: 0
Space and atmospheric physics on Svalbard: a case for continued incoherent scatter radar measurements under the cusp and in the polar cap boundary region 斯瓦尔巴群岛的空间和大气物理学:在尖端和极帽边界区域持续进行非相干散射雷达测量的情况
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-09-04 DOI: 10.1186/s40645-023-00585-9
L. Baddeley, Dag Lorentzen, Stein Haaland, E. Heino, Ingrid Mann, Wojciech Miloch, K. Oksavik, N. Partamies, Andres Spicher, Juha Vierinen
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引用次数: 0
Sensitivity of slip distribution on tsunami trace heights and geological evidences: a case study of the 2011 Tohoku-Oki earthquake 滑动分布对海啸迹线高度的敏感性及地质证据——以2011年东北大地震为例
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-08-25 DOI: 10.1186/s40645-023-00582-y
S. Kusumoto, K. Imai, T. Hori, D. Sugawara, K. Satake
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引用次数: 0
Foreland basin unconformity, Western Himalaya, Pakistan: timing gap, regional correlation and tectonic implications 巴基斯坦喜马拉雅西部前陆盆地不整合:时间差距、区域相关性和构造意义
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-08-24 DOI: 10.1186/s40645-023-00584-w
M. Qasim, Z. Rehman, L. Ding, J. Tanoli, W. Abbas, Muhammad Jamil, Z. Bhatti, M. Umar
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引用次数: 0
The nature of the Pacific plate as subduction inputs to the northeastern Japan arc and its implication for subduction zone processes 太平洋板块作为日本东北弧俯冲输入的性质及其对俯冲带过程的启示
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-08-22 DOI: 10.1186/s40645-023-00578-8
G. Fujie, S. Kodaira, K. Obana, Y. Yamamoto, T. Isse, Tomoaki Yamada, T. No, Y. Nakamura, S. Miura
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引用次数: 1
Marine inundation history during the last 3000 years at Lake Kogare-ike, a coastal lake on the Pacific coast of central Japan 过去3000年日本中部太平洋沿岸的一个沿海湖泊高湖的海洋淹没历史
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-08-21 DOI: 10.1186/s40645-023-00577-9
Y. Shimada, Y. Sawai, D. Matsumoto, K. Tanigawa, Kazumi Ito, T. Tamura, Y. Namegaya, M. Shishikura, S. Fujino
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引用次数: 0
Recent global nonhydrostatic modeling approach without using a cumulus parameterization to understand the mechanisms underlying cloud changes due to global warming 最近的全球非静力建模方法没有使用积云参数化来了解全球变暖导致的云变化的潜在机制
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-08-18 DOI: 10.1186/s40645-023-00583-x
A. Noda, Tomoki Ohno, C. Kodama, Ying-Wen Chen, N. Kuba, T. Seiki, Y. Yamada, M. Satoh
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引用次数: 0
K-feldspar enrichment in the Pacific pelagic sediments before Miocene 中新世以前太平洋远洋沉积物中钾长石的富集
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-08-14 DOI: 10.1186/s40645-023-00581-z
Y. Usui, T. Yamazaki
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引用次数: 0
Incoming plate structure at the Japan Trench subduction zone revealed in densely spaced reflection seismic profiles 密集反射地震剖面揭示了日本海沟俯冲带的传入板块结构
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-08-08 DOI: 10.1186/s40645-023-00579-7
Y. Nakamura, S. Kodaira, G. Fujie, M. Yamashita, K. Obana, S. Miura
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引用次数: 1
Progress in modeling the Tohoku-oki megathrust earthquake cycle and associated crustal deformation processes 东北-崎大逆冲地震旋回模拟及相关地壳变形过程研究进展
IF 3.9 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2023-07-31 DOI: 10.1186/s40645-023-00575-x
Bunichiro Shibazaki
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引用次数: 0
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Progress in Earth and Planetary Science
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