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101.
John Davis Jakeman Ole M. Nielsen Kristy Van Putten Richard Mleczko David Burbidge Nick Horspool 《Ocean Dynamics》2010,60(5):1115-1138
This paper presents a framework and data for spatially distributed assessment of tsunami inundation models. Our associated
validation test is based upon the 2004 Indian Ocean tsunami, which affords a uniquely large amount of observational data for
events of this kind. Specifically, we use eyewitness accounts to assess onshore flow depths and speeds as well as a detailed
inundation survey of Patong City, Thailand to compare modelled and observed inundation. Model predictions matched well the
detailed inundation survey as well as altimetry data from the JASON satellite, eyewitness accounts of wave front arrival times
and onshore flow speeds. Important buildings and other structures were incorporated into the underlying elevation model and
are shown to have a large influence on inundation extent. 相似文献
102.
Spatial patterns of frequent floods in Switzerland 总被引:1,自引:1,他引:0
This study investigates the spatial dependence of high and extreme streamflows in Switzerland across different scales. First, using 56 runoff time series from Swiss rivers, we determined the average length of high-streamflow events for different levels of extremeness. Second, a dependence measure that expressed the probability that streamflow peaks would meet or exceed streamflow peaks at a conditioning site was used to describe and map the spatial extent of joint streamflow-peak occurrences across Switzerland. Third, we analysed the spatial patterns of jointly occurring high streamflows using cluster analysis to identify groups that react similarly in terms of flood frequency at different sites. The results indicate that, on a coarse scale, high and extreme streamflows are asymptotically independent in the main Swiss basins. Additionally, mesoscale tributaries in the main basins show distinct flood regions across river systems. 相似文献
103.
Peter Rasmussen George Pantopoulos Jørn B. Jensen Jesper Olsen Hans Røy Ole Bennike 《Boreas: An International Journal of Quaternary Research》2020,49(1):108-128
Holocene sedimentation patterns and environmental development in Aarhus Bay, Denmark, were reconstructed based on proxy analyses of two sediment cores (M1 and M5). Together, the two cores offer an opportunity to examine the history of the area during the past c. 10 000 years. The investigation consisted of acoustic mapping and multi-proxy analyses of the sediment cores including macrofossils, sediment physical properties, sediment accumulation rates, grain size, and X-ray fluorescence elemental counts. Radiocarbon dating of the two sediment successions revealed that they cover the periods c. 10 000–3700 cal. a BP (M1) and c. 4400 cal. a BP to the present (M5). The data from the M1 site indicate the presence of a near-shore lake environment between c. 10 000 and 9000 cal. a BP. The first intrusion of marine water into the area is dated to c. 9000 cal. a BP. In the following c. 1300 years, brackish-water conditions prevailed in the area characterized by a mixture of taxa from marine, limnic and terrestrial habitats, reflecting a shallow estuarine environment. Around 7700 cal. a BP full marine conditions were established, accompanied by a marked increase in sedimentation rates. The changes to full marine conditions and higher sedimentation rates are probably due to a significant sea-level rise leading to flooding of former land areas and intensified erosion. A subsequent distinct decrease in sedimentation rates around 6350 cal. a BP is presumably linked to a previously documented sea-level drop about this time. Continuous sedimentation ceased around 3700 cal. a BP in the central part of the bay, most probably due to a major sea-level lowering involving widespread erosion. In the eastern and deeper part of the bay, sedimentation continued until today. Fully marine conditions prevailed there for at least the last 4400 years. 相似文献
104.
105.
The outer coast of Finnmark in northern Norway is where the former Fennoscandian and Barents Sea ice sheets coalesced. This key area for isostatic modelling and deglaciation history of the ice sheets has abundant raised shorelines, but only a few existing radiocarbon dates constrain their chronology. Here we present three Holocene sea level curves based on radiocarbon dated deposits from isolation basins at the outermost coast of Finnmark; located at the islands Sørøya and Rolvsøya and at the Nordkinn peninsula. We analysed animal and plant remains in the basin deposits to identify the transitions between marine and lacustrine sediments. Terrestrial plant fragments from these transitions were then radiocarbon dated. Radiocarbon dated mollusk shells and marine macroalgae from the lowermost deposits in several basins suggest that the first land at the outer coast became ice free around 14,600 cal yr BP. We find that the gradients of the shorelines are much lower than elsewhere along the Norwegian coast because of substantial uplift of the Barents Sea. Also, the anomalously high elevation of the marine limit in the region can be attributed to uplift of the adjacent seafloor. After the Younger Dryas the coast emerged 1.6–1.0 cm per year until about 9500–9000 cal yr BP. Between 9000 and 7000 cal yr BP relative sea level rose 2–4 m and several of the studied lakes became submerged. At the outermost locality Rolvsøya, relative sea level was stable at the transgression highstand for more than 3000 years, between ca 8000 and 5000 cal yr BP. Deposits in five of the studied lakes were disturbed by the Storegga tsunami ca 8200–8100 cal yr BP. 相似文献
106.
J. Ole Kaven Stephen H. Hickman Nicholas C. Davatzes Ovunc Mutlu 《Computational Geosciences》2012,16(3):613-624
Frictional sliding on quasi-statically deforming faults and fractures can be modeled efficiently using a linear complementarity
formulation. We review the formulation in two dimensions and expand the formulation to three-dimensional problems including
problems of orthotropic friction. This formulation accurately reproduces analytical solutions to static Coulomb friction sliding
problems. The formulation accounts for opening displacements that can occur near regions of non-planarity even under large
confining pressures. Such problems are difficult to solve owing to the coupling of relative displacements and tractions; thus,
many geomechanical problems tend to neglect these effects. Simple test cases highlight the importance of including friction
and allowing for opening when solving quasi-static fault mechanics models. These results also underscore the importance of
considering the effects of non-planarity in modeling processes associated with crustal faulting. 相似文献
107.
108.
Studies of lake sediments on Sejerø in southern Kattegat indicate a treeless arctic environment with the dwarf shrub Salix polaris, herbs and wetland mosses. The mean July temperature was around 8 to 10°C. An AMS radiocarbon age determination of a Salix twig yielded an age of around 36 000 14C yr BP, which is in accordance with previous conventional dating of bulk sediment samples. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
109.
110.
A stratigraphic analysis of late Palaeocene sands of the Søgne Basin and the western part of the Norwegian–Danish Basin shows that the sand bodies are of differenct ages. The geographic distribution of the sand deposits shows that they are related to underlying Mesozoic structures suggesting a controlling effect of Tertiary tectonics on the deposition of sand during the late Palaeocene. However, the structural setting of various sand bodies varies from reactivation of older faults and reactivation of salt structures. The local character of the structures active during the late Palaeocene introduces minor depressions with no lateral connection. The sand bodies, which are interpreted as having been deposited in these depressions, are thus in general separate bodies with no lateral connection. The Fennoscandian shield and eroded Mesozoic sediments along the Fennoscandian Border Zone are suggested as source area for the late Palaeocene sand deposits. 相似文献