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排序方式: 共有289条查询结果,搜索用时 46 毫秒
41.
Nobuyuki YagiMichael L. Clark Lee G. AndersonRagnar Arnason Rebecca Metzner 《Marine Policy》2012,36(1):241-245
ITQs have not yet been introduced by the Government of Japan. In coastal areas, fishery cooperative associations have traditionally played an important role in managing fisheries through self-imposed rules and peer-monitoring systems. Recently, however, the economic competitiveness of Japanese fisheries in the international market is being questioned. In this paper, a detailed examination of the pros and cons of the current system in Japan is compared to the current fishery management measures of Iceland and the United States, where attaining economically or biologically efficient outcomes may be prioritized in making fisheries management decisions. For many coastal fisheries in Japan, maintaining a management scheme in which stakeholders play an active role in determining fisheries measures seems more relevant if their priority is to maintain the stability of coastal communities and equity of stakeholders. Intensive dialog among stakeholders would be necessary to identify shared objectives of their fishery operations and to make decisions to establish specific steps toward the goal of increasing economic efficiency, environmental sustainability, or stability of communities and equity of stakeholders. 相似文献
42.
Grilli Stéphan T. Shelby Mike Kimmoun Olivier Dupont Guillaume Nicolsky Dmitry Ma Gangfeng Kirby James T. Shi Fengyan 《Natural Hazards》2017,86(1):353-391
Natural Hazards - We perform numerical simulations to assess how coastal tsunami hazard from submarine mass failures (SMFs) is affected by slide kinematics and rheology. Two types of two-layer SMF... 相似文献
43.
Katharine A. Smith Elizabeth W. North Fengyan Shi Shih-Nan Chen Raleigh R. Hood Evamaria W. Koch Roger I. E. Newell 《Estuaries and Coasts》2009,32(4):748-757
Seagrass beds have declined in Chesapeake Bay, USA as well as worldwide over the past century. Increased seston concentrations,
which decrease light penetration, are likely one of the main causes of the decline in Chesapeake Bay. It has been hypothesized
that dense populations of suspension-feeding bivalves, such as eastern oysters (Crassostrea virginica), may filter sufficient seston from the water to reduce light attenuation and enhance seagrass growth. Furthermore, eastern
oyster populations can form large three-dimensional reef-like structures that may act like breakwaters by attenuating waves,
thus decreasing sediment resuspension. We developed a quasi-three-dimensional Seagrass-Waves-Oysters-Light-Seston (SWOLS)
model to investigate whether oyster reefs and breakwaters could improve seagrass growth by reducing seston concentrations.
Seagrass growth potential (SGP), a parameter controlled by resuspension-induced turbidity, was calculated in simulations in
which wave height, oyster abundance, and reef/breakwater configuration were varied. Wave height was the dominant factor influencing
SGP, with higher waves increasing sediment resuspension and decreasing SGP. Submerged breakwaters parallel with the shoreline
improved SGP in the presence of 0.2 and 0.4 m waves when sediment resuspension was dominated by wave action, while submerged
groins perpendicular to the shoreline improved SGP under lower wave heights (0.05 and 0.1 m) when resuspension was dominated
by along-shore tidal currents. Oyster-feeding activity did not affect SGP, due to the oysters’ distance from the seagrass
bed and reduced oyster filtration rates under either low or high sediment concentrations. Although the current implementation
of the SWOLS model has simplified geometry, the model does demonstrate that the interaction between oyster filtration and
along-shore circulation, and between man-made structures and wave heights, should be considered when managing seagrass habitats,
planning seagrass restoration projects, and choosing the most suitable methods to protect shorelines from erosion. 相似文献
44.
Pablo Huq 《Estuaries and Coasts》2009,32(4):709-719
This investigation examines the influence of the Kelvin number (K) and fractional depth (h/D) on bulge formation from buoyant outflows from an estuary or strait perpendicular to the coastline. Here K = W/R is the ratio of the width (W) at the mouth of the estuary to the deformation radius (R), and h and D are the buoyant layer and ambient ocean depths, respectively. Measurements of velocity and lateral shear (≈ relative vorticity
ζ) at the baymouth are reported for experiments on a flat-bottomed rotating turntable. The form of the velocity profile across
the mouth depends on the value of K. The buoyant outflow flows across the entire width of the estuary for narrow estuaries (i.e., K ≤ 1). In contrast, for wide estuaries (K > 2), dense oceanic water inflows on the left and the buoyant waters outflow on the right (looking seaward). Velocity profiles
of the inflowing oceanic waters are laterally uniform with velocities (V/C ≈ −0.4), whereas velocity profiles of the outflowing buoyant waters are laterally sheared with peak velocities of V/C ≈ 1.0 at the right hand exit. The flow pathways when bulges form comprises an anticyclonic turn offshore of the mouth and
a downshelf propagating coastal current. Anticyclonic bulges form for surface-advected outflows h/D < 0.25. Anticyclonic bulges do not form for sufficiently large magnitudes of non-dimensional relative vorticity ζ/f (>0.4), and an additional flow pathway is that buoyant waters recirculate back cyclonically into the estuary at the left-hand
(upshelf) side of the estuary. The offshore extent of buoyant waters associated with this cyclonic recirculation can be as
large as 7R. 相似文献
45.
Almost all engineering evacuation models define the objective as minimizing the time required to clear the region or total
travel time, thus making an implicit assumption that who will or should evacuate is known. Conservatively evacuating everyone
who may be affected may be the best strategy for a given storm, but there is a growing recognition that in some places that
strategy is no longer viable and in any case, may not be the best alternative by itself. Here, we introduce a new bi-level
optimization that reframes the decision more broadly. The upper level develops an evacuation plan that describes, as a hurricane
approaches, who should stay and who should leave and when, so as to minimize both risk and travel time. The lower level is
a dynamic user equilibrium (DUE) traffic assignment model. The model includes four novel features: (1) it refocuses the decision
on the objectives of minimizing both risk and travel time; (2) it allows direct comparison of more alternatives, including
for the first time, sheltering-in-place; (3) it uses a hurricane-scenario-based analysis that explicitly represents the critically
important uncertainty in hurricane track, intensity, and speed; and (4) it includes a new DUE algorithm that is efficient
enough for full-scale hurricane evacuation applications. The model can be used both to provide an evacuation plan and to evaluate
a plan’s performance in terms of risk and travel time, assuming the plan is implemented and a specified hurricane scenario
then actually occurs. We demonstrate the model with a full-scale case study for Eastern North Carolina. 相似文献
46.
Isabella M. Angelini Michael Garstang Robert E. Davis Bruce Hayden David R. Fitzjarrald David R. Legates Steven Greco Stephen Macko Vickie Connors 《Theoretical and Applied Climatology》2011,105(1-2):243-261
Recent studies suggest that vegetation can drive large-scale atmospheric circulations and substantially influence the hydrologic cycle. We present observational evidence to quantify the extent of coupling between vegetation and the overlying atmosphere. Within the context of vegetation–atmospheric interactions, we reanalyze existing climatological data from springtime leaf emergence, emissivity, dew point temperatures, and historical records of precipitation and forest coverage. We construct new rainfall transects based on a robust global climatology. Using isotopic analysis of precipitation, we find that rain in Amazonia comes primarily from large-scale weather systems coupling interior regions to the ocean and is not directly driven by local evaporation. We find that changes in vegetative cover and state influence the temperature and moisture content of the surface and atmospheric boundary layer but are not reflected in observable precipitation changes. This analysis reaffirms the view that changes in precipitation over continental reaches are a product of complex processes only partly influenced but not controlled by local water sources or vegetation. 相似文献
47.
Triaxial shear testing of polished slickensided surfaces 总被引:1,自引:1,他引:0
Christopher L. Meehan Binod Tiwari Thomas L. Brandon J. Michael Duncan 《Landslides》2011,8(4):449-458
A series of consolidated-drained triaxial tests were performed on precut and polished clay specimens to measure their drained
residual strength. Two soils were tested during this research program: Rancho Solano Clay and San Francisco Bay Mud. Specimens
were tested using a specially modified triaxial compression device which was developed to minimize the effects of end-platen
restraint on the measured strengths. Special attention was paid to the influence of changing specimen area and membrane effects
during the test. Triaxial test results were compared with baseline measurements of drained residual shear strength that were
made for each of the clay soils using Bromhead ring shear tests and polished-specimen direct shear tests. Residual strength
values measured in the triaxial device were higher than the drained residual strengths measured in the Bromhead ring shear
apparatus and the direct shear device, indicating that this test approach is more challenging than the use of direct shear
tests conducted on polished slickensided surfaces. Comparison of single stage and multistage triaxial test data indicates
that multistage triaxial testing may work well for specimens that fail along a well-defined plane, provided that careful attention
is given to the effects of end platen restraint, membrane restraint, and changes in specimen area during shear. 相似文献
48.
Lide Jiang Xiao-Hai Yan Yu-Heng Tseng Laurence C. Breaker 《Estuarine, Coastal and Shelf Science》2011
The responses of coastal upwelling to different magnitudes of wind stress over a narrow and a wide shelf are studied using a 3-D primitive equation numerical model. The results show that the position of the upwelling front depends on both the strength and the duration of the wind forcing. The comparison between different shelf widths shows that wide shelf will limit the cold water intrusion, so that the corresponding decrease in sea surface temperature is less compared to narrow shelves. Besides, the difference between hydrostatic and nonhydrostatic model results shows that nonhydrostatic effects will enhance the growth of surface meandering, and can be more pronounced near steep fronts. Although difference does exist, our results show that the nonhydrostatic effects are very small at least in this idealized study case. 相似文献
49.
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