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141.
Bernhard E. Nickel 《先进运输杂志》1988,22(2):134-153
Dramatic deteriorations in the future development of demographic and socio-economic factors having a decisive impact on public transport demand in 2000 - 2030 are predicted. How can a reasonable public transport service be maintained under these changing conditions? Depending on the entrepreneurial objectives defined individually by each public transport company a range of strategic actions must be taken in the field of offer and performance: Advancing strategies, consolidation strategies and defensive strategies are discussed with the stress laid on improving service in order to attract more ridership. 相似文献
142.
Ira Hirschman Claire Mcknight John Pucher Robert E. Paaswell Joseph Berechman 《Transportation》1995,22(2):97-113
In 1992, the authors carried out a statistical analysis of Triborough Bridge and Tunnel Authority (TBTA) crossings in New York City, to determine the impact of toll increases on traffic volumes and revenue. Using twelve years of monthly time-series data, we developed a set of multiple regression models that estimated traffic volumes on each TBTA bridge and tunnel as a function of the toll level and other explanatory variables. In most cases, the estimated toll elasticities were negative and much less than 1.0 in absolute value; the median toll elasticity for automobiles was found to be –0.10. Our finding that automobile travel demand is highly inelastic with respect to toll rates is consistent with most previous travel demand studies. 相似文献
143.
144.
Igor P. Semiletov Irina I. Pipko Irina Repina Natalia E. Shakhova 《Journal of Marine Systems》2007,66(1-4):204
Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO2) concentration and other non-CO2 radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO2 concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO2. The Arctic Ocean's role in determining regional CO2 balance has been ignored, because of its small size (only 4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO2 exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO2 because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO2; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO2 sink that also must be included in any Arctic regional CO2 budget. Both the direction and amount of CO2 transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO2 accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO2 decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO2 sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO2 ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO2 range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources. 相似文献
145.
分别采用多层次参数扫描(MLPS)算法和模拟退火粒子群优化(SAPSO)算法对并联式混合动力车逻辑门限控制策略的参数进行优化.将优化后的车辆以TEST-CITY-HWY测试循环进行仿真,并将结果与优化前的车辆的仿真结果进行对比.结果表明,经MLPS算法优化后,燃油消耗和HC与NOx排放分别下降了11.98%、6.01%和4.03%,但CO排放增加了25.18%;经SAPSO算法优化后,燃油消耗和HC、CO与NOx排放分别下降了13.61%、9.57%、27.78%和18.53%,且电池荷电状态(SOC)比MLPS优化略高.说明SAPSO算法在混合动力车控制参数优化效果上明显优于MLPS算法. 相似文献
146.
Impact of phytoplankton community size on a linked global ocean optical and ecosystem model 总被引:1,自引:0,他引:1
We isolated the effect phytoplankton cell size has on varying remote sensing reflectance spectra (Rrs(λ)) in the presence of optically active constituents by using optical and radiative transfer models linked in an offline diagnostic calculation to a global biogeochemical/ecosystem/circulation model with explicit phytoplankton size classes. Two case studies were carried out, each with several scenarios to isolate the effects of chlorophyll concentration, phytoplankton cell size, and size-varying phytoplankton absorption on Rrs(λ). The goal of the study was to determine the relative contribution of phytoplankton cell size and chlorophyll to overall Rrs(λ) and to understand where a standard band ratio algorithm (OC4) may under/overestimate chlorophyll due to Rrs(λ) being significantly affected by phytoplankton size. Phytoplankton cell size was found to contribute secondarily to Rrs(λ) variability and to amplify or dampen the seasonal cycle in Rrs(λ), driven by chlorophyll. Size and chlorophyll were found to change in phase at low to mid-latitudes, but were anti-correlated or poorly correlated at high latitudes. Phytoplankton size effects increased model calculated Rrs(443) in the subtropical ocean during local spring through early fall months in both hemispheres and decreased Rrs(443) in the Northern Hemisphere high latitude regions during local summer to fall months. This study attempts to tease apart when/where variability about the OC4 relationship may be associated with cell size variability. The OC4 algorithm may underestimate [Chl] when the fraction of microplankton is elevated, which occurs in the model simulations during local spring/summer months at high latitudes in both hemispheres. 相似文献
147.
利用计算流体力学软件FLUENT,基于三维可压缩、黏性、非定常流场数值模拟方法,建立隧道-空气-列车三维数值仿真模型.针对高海拔地区隧道空气动力学效应,研究列车以300 km/h的速度运行通过不同海拔隧道时产生的隧道内瞬变压力及车体表面瞬变压力的变化特征,分析大气压和温度等因素对瞬变压力的影响规律,得到海拔高度与瞬变压... 相似文献
148.
Waygood E. Owen D. Olsson Lars E. Taniguchi Ayako Friman Margareta 《Transportation》2020,47(4):1987-2009
Transportation - Social interaction with friends is an important contributor to children’s well-being, but how transport affects this is rarely studied. For two or more children (not of the... 相似文献
149.
杨家其 《武汉理工大学学报(交通科学与工程版)》2002,26(1):141-146
从政策选择上对如何阻止长期以来困扰国际海运业的船舶移籍问题进行探讨,基于对国内外船舶移籍现状及其发展过程的分析,深入分析了欧盟成员国在阻止船舶移籍方面所采取的政府干预与政策竞争策略,指出了中国改善船舶移籍状况的政策取向。 相似文献
150.
办公自动化系统是实现企业内部各部门之间办公信息的收集与处理、流动与共享、实现科学决策的信息系统.公文管理作为企业办公自动化系统的核心涉及到几乎所有的部门,文中在分析公文管理特点的基础上,以Petri网为描述手段,建立了企业办公自动化环境下收发文过程的Petri网模型,并利用矩阵方程对其进行了相关的分析和验证. 相似文献