Results 41 to 50 of about 591 (94)
The flood of Januruy 8, 1993 is the largest flood preserved in the paleoflood record for Tonto Creek, and probably was the largest flood in the past three hundred years on Tonto Creek.
Fuller, J.E. +2 more
core +4 more sources
Fluviomorphic trajectories for dryland ephemeral stream channels following extreme flash floods
Aerial photographs enable evolutionary trajectory analyses of ephemeral streams. The geometric braiding index reaches the pre‐flood state the fastest, that is, in circa 15–24 years. Junction‐node density and stream‐link area recover in 25 years after extraordinary floods, but the spatial distribution of the channel forms takes 30–35 years to recover ...
Eliisa Lotsari +3 more
wiley +1 more source
Bank erosion and erosion processes from dendrogeomorphology in southern U.S. prairie streams
Abstract Streambank erosion processes influence the amount of soil material contributed to rivers and sedimentation rates in receiving reservoirs. However, the amount of data on bank erosion rates is limited both in range and extent affecting planning for mitigation and watershed management.
Joseph D. White +5 more
wiley +1 more source
Study region: Norway Study focus: Numerous geological traces provide evidence for the existence, size and catastrophic drainage of the Early Holocene glacial lake Nedre Glomsjø in southern Norway.
Katherine R. Aurand +3 more
doaj +1 more source
Challenges in the attribution of river flood events
Drivers of river floods change through time. Global warming, and associated changes in temperature and precipitation, often overlap with changes in the hydrology, such as land‐cover change, construction of levees and large‐scale irrigation. This poses a special challenge to the attribution of flood events.
Paolo Scussolini +10 more
wiley +1 more source
Study region: Six flood-plain sites in five Southeastern U.S. river basins, from expansive Lower Mississippi to the smaller White, Pascagoula, Altamaha, and Suwannee.
Mahsa Mirzakhani +5 more
doaj +1 more source
Outburst floods records in the Yigong River since holocene, southeastern Tibet
Background Paleofloods are critical geomorphic driving forces shaping the landform evolution of the Tibetan Plateau margin. Although paleoflood investigations have been conducted in the Yarlung Tsangpo River, including documented sedimentary records in ...
Chaohua Wu +6 more
doaj +1 more source
基于对近年来汉江上游古洪水水文学研究成果的整理和分析,结合文献记载和气候背景分析,对汉江上游5个沉积剖面记录的北宋时期古洪水事件进行了文献考证.研究结果表明,北宋时期为洪水频发期;洪水灾害的影响范围、灾情的严重性以及洪痕沉积规律等表明,汉江上游5个沉积剖面记录的古洪水事件可能是北宋太平兴国七年(982年)六月的一次特大洪水事件.依据树轮、冰芯、石笋等气候代用性指标及历史文献记载,北宋太平兴国七年(982年)正处于北宋980年代气候突变时期,此次古洪水事件可能是对当时气候异常多变的瞬时响应 ...
WANGGuangpeng(王光朋) +4 more
doaj +1 more source
An improved method for detecting event layers in lake sediment archives
Flood frequency and magnitude are expected to increase under future climate scenarios, yet long-term records of flood variability remain sparse beyond the instrumental period.
Jan Magne Cederstrøm +3 more
doaj +1 more source
In this chapter, we discuss recent developments in paleoflood hydrology that are specific to the collection of high-resolution records from alluvial settings.
SE Munoz (17232583) +3 more
core +5 more sources

