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Titlebook: Geomorphic Approaches to Integrated Floodplain Management of Lowland Fluvial Systems in North Americ; Paul F. Hudson,Hans Middelkoop Book

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發(fā)表于 2025-3-26 23:48:19 | 只看該作者
32#
發(fā)表于 2025-3-27 03:27:28 | 只看該作者
Microwave Radiometry and Thermographyer flood provided a geomorphic context to the flood problem in support of decision making towards enhancing the flood-protection infrastructure. Based on flood signatures in the growth rings of bur oak trees (. Michx.), the historic flood-of-record in 1826 is interpreted to be the largest Red River
33#
發(fā)表于 2025-3-27 08:55:02 | 只看該作者
Quantum Electrodynamics in Laser Fields,dplain inundation, erosion, and sedimentation, the dominant geomorphic processes that occur during unintentional levee breaks, are flood risks in such embanked river systems. Climate and flood variability still dictate the frequency of unintentional levee breaks despite many decades of engineering.
34#
發(fā)表于 2025-3-27 10:18:42 | 只看該作者
https://doi.org/10.1007/978-1-4757-0713-7ronmental and political efforts led to a restoration, which began in the late 1990s, has been progressing in phases and is due for completion by 2016 or thereabouts; it involves backfill of C-38 with dredge spoil from the original project, sending flow back through channels that had been stagnant fo
35#
發(fā)表于 2025-3-27 13:56:01 | 只看該作者
36#
發(fā)表于 2025-3-27 20:43:40 | 只看該作者
37#
發(fā)表于 2025-3-28 01:42:53 | 只看該作者
38#
發(fā)表于 2025-3-28 02:18:37 | 只看該作者
39#
發(fā)表于 2025-3-28 07:53:04 | 只看該作者
https://doi.org/10.1007/978-3-319-45355-2tal and geomorphic restoration as an end-product. A review and comparison of heavily managed embanked rivers spanning a range of climatic and geomorphic provinces across North America and Europe illustrate the role of geomorphology in this palimpsest and its value to integrated management.
40#
發(fā)表于 2025-3-28 11:08:44 | 只看該作者
Sand and Gravel on the Move: Human Impacts on Bed-Material Load Along the Lower Rhine River,s initiated by shipping, and (4) the grain size of the bed material transport increased due to the effects of embankment, meander cut-offs, river narrowing, barrages, and sediment mining. The main morphological problem in large parts of the lower Rhine River is the erosion of bed material from the r
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