The main objective of this writing is to present a practical way to envisage the flood vulnerability in deltaic region, particularly
on the concern of sea level rise. Kuching city of Malaysia is established on banks of Sarawak River, 30 km from the sea. Therefore,
it is subjected to fluvial and tidal floods. Kuching Bay experiences the highest King Tides in Southeast Asia region. These
tide magnitudes could be a glimpse of future sea level rise. By means of modelling these tides, it provides an understanding
and preparation for the impacts of sea level rise on the flood mitigation infrastructures and the city itself. The modelling
efforts had created an illustration that a 10% rise in tide levels would result in increase of flooding areas up to 6% relative
to existing tide levels. 相似文献
A three-dimensional transportation model for suspended solids (SS) in Zhujiang (Pearl) River estuary, South China, was developed by coupling with a three-dimensional hydrodynamic model. The model was validated using hourly measured data of sediment contents during 25-26, July 1999. The results showed that modeled contents matched well with measured ones and that the modeled top layer distribution agreed with the remotely sensed image of suspended solids in summer. The modeled results showed clearly the layers of suspended solids in depth, with larger sediment contents in lower layers though in the interface between salt water and freshwater the lowest contents appeared in middle layer. In overall, the suspended solids inflow from 8 rivers,transport southwestward, and carried by strong coastal flow in Zhujiang River estuary. Contours of sediment contents in the estuary spread further to the open sea during ebb tide rather than flood tide which reflects that the suspended solids in the estuary are land sourced. 相似文献
The geodynamic setting of the Bikou volcanic group is a critical question to trace the Precambrain tectonic framework and evolution for the Yangtze plate. This study has suggested that the Bikou volcanic group is composed of several residual oceanic crust units: MORB (mid-ocean ridge basalt), Alk-OIB (alkaline ocean island basalt) and Th-OIB (tholeiitic ocean island basalt) as well as subduction-related volcanic rocks. According to field observation, those distinct rocks occurred collectively in form of tectonic contact, implying that the Bikou volcanic group was an ophiolitic mélange. Coupled with geochronological data, a perished oceanic basin at the northern margin of the Yangtze block during Neoproterozoic was tested by this ophiolitic mélange. Meanwhile, the isogeochemical data suggest that the ocean occurred in the Southern Hemisphere identical to Indian, South Atlantic and South Pacific oceans in terms of their Dupal anomalies, and the original source of the rocks could be probably mixing by EMI and EMII component caused by dehydration melting of subducting oceanic crust during subduction process. On the basis of geochemical characteristics of the studied rocks, the Bikou volcanic group could imply that a partial breakup event occurred in the northern margin of Yangtze plate during the Neoproterozoic era.
Through comprehensive research on the various geophysical and geological data acquired recently, we consider that the Chasang area in the western uplift of Qiangtang is a huge south-dipping block which is overlapped by several east-west trending blocks rather than a simple and palaeo-doming existing for a long time. The structural and geophysical features of the area, which only alone limited between Shuanghu and Rongma districts, are of no regional significance. Their development is closely related with the approximately south-north trending transform faults developed during the Mesozoic era on the east and west sides of the area and their later continuous movement. The compressing, overlapping and uplifting of the Chasang area began at the stage of reversing of the Qiangtang Basin during the Lower Cretaceous, which is in direct relation with Bangonghu-Dingqing limited ocean’s closure and the convergence of the neighboring blocks. The compression and overlapping of the area have further developed and reformed since the Eocene because of the continuing collision and pushing of the Indian Plate to the north. 相似文献
To quantify the interplay between scalar sources and sinks (Sc) and net ecosystem exchange (NEE), “forward” and “inverse” approaches have been proposed. The canonical form of forward approaches is a one-dimensional ecophysiological-radiative transfer scheme coupled to turbulent transport theory. In contrast, inverse approaches strictly rely on turbulent transport theory and mean scalar concentration as their primary input to infer Sc and NEE. While the formulation of both approaches have evolved over the past decade, no systematic comparison between them was undertaken for the same data set, and over a wide range of atmospheric conditions. Our objective is to compare the predicted Sc and NEE from these two approaches with eddy-covariance measurements. The results show that the forward method outperformed all three inverse methods for unstable and neutral conditions on short time scales (30 min) but yielded comparable results at longer time scales. Poor agreement was obtained under stable conditions for all models. Hence, for modeling event-based flux variations, forward models are preferred. Since the forward method requires detailed knowledge of ecophysiological, drag, radiative transfer and other canopy attributes, all of which are difficult to obtain on a routine basis, a symbiotic use of forward and inverse approaches is most advantageous. 相似文献
The importance of underground structures in transportation and utility networks makes their vulnerability to earthquakes a
sensitive issue. Underground facilities are usually less vulnerable to earthquakes compared to above-ground structures, but
the associated risk may be relevant, since even a low level of damage may affect the serviceability of a wide network. Seismic
analysis of tunnels close to seismogenic faults is a complex problem, which is often neglected at the design stage for the
lack of specific codes or guidelines for the design of underground structures in seismic conditions and also because, as mentioned
above, underground structures are considered less vulnerable to earthquake loading. This paper investigates the seismic response
of deep tunnels focusing on the required steps for a proper design under both static and dynamic loading. The study aims at
contributing to improve the methods currently used for the seismic analysis of underground structures. At this purpose, the
seismic response of a deep tunnel in Southern Italy has been investigated along the transversal direction. The infrastructure
is part of the railway switch line connecting Caserta to Foggia in the Southern Apennines which is one of the most active
seismic regions in Italy. The seismic response in the transversal direction has been analysed by using the pseudo-static approach
as well as through advanced numerical modeling using the spectral element method coupled with a kinematic approach for finite
fault simulations. The pseudo-static approach has been implemented using a closed-form analytical solution. The results obtained
from advanced numerical modeling and the pseudo-static method have been compared to assess their validity and limitations. 相似文献