人口总量及其空间分布特征与经济发展关系的动力学研究   总被引：5，自引：3，他引：2  

陈楠  林宗坚 《测绘科学》2006,31(4):14-16

建立了人口—经济系统的微分方程组模型,并在方程中引入人口空间分布与经济发展协调的因子η,通过分析模型的稳定性特征得出以下结论:人口经济系统是复杂的非线性关系;人口的过于快速增长会使经济总量趋向于零;如果η>1并且较高,则人口经济系统发展稳定时,经济总量会高些,也即人口数量稳定在同样水平时,会因为空间分布的不同而有不同的经济产出。说明在控制人口数量的同时必须重视人口空间分布的问题。  相似文献   

区域蒸散发量的遥感模型方法研究   总被引：5，自引：0，他引：5  

乔平林  张继贤  王翠华  燕琴  刘正军 《测绘科学》2006,31(3):45-46,61

蒸散是水资源管理的一个重要参数。与传统的蒸散计算方法相比,利用遥感进行蒸散研究具有快速、准确、大区域尺度及地图可视化显示等特点。本文通过研究,提出了基于能量平衡方法遥感反演蒸散发的计算模型,指出了模型参数的求解方法,建立了基于MOD IS遥感数据的大区域蒸散发遥感反演技术方法。通过对石羊河流域进行试验,反演误差基本小于10%,并且具有进一步推广的技术前景。  相似文献   

A universal nutrient application strategy for the bioremediation of oil-polluted beaches   总被引：2，自引：0，他引：2  

Li H  Zhao Q  Boufadel MC  Venosa AD 《Marine pollution bulletin》2007,54(8):1146-1161

Biostimulation by nutrient application is a viable technology for restoring oil-contaminated beaches. Maximizing the nutrient residence time is key for achieving a rapid cost-effective cleanup. We considered the nutrient injection strategy through a perforated pipe at the high tide line and we simulated numerically beach hydraulics, which allowed us to estimate the optimal injection flow rate of nutrient solution. Our results indicate that the optimal application is one that starts following the falling high tide and lasts for half tidal cycle. The saturated wet-front of the nutrient solution on the beach surface would move seaward with the same speed of the falling tide keeping a constant distance with the tide line. The numerical results were generalized to beaches of wide ranges of hydraulic and tidal properties using a novel dimensionless formulation for water flow and solute transport in porous media. Nomographs were presented to provide the flow rate based on four parameters: The beach slope and hydraulic conductivity, and tidal amplitude and period.  相似文献   

Accuracy of the linearized standard balance and asymmetric balance systems in a shallow-water numerical model     

Ingo Slch  J. Dominique Mller  Lloyd J. Shapiro 《Dynamics of Atmospheres and Oceans》2007,44(2):77-103

A numerical evaluation of the accuracy of the standard balance equations (BE) and the asymmetric balance equations (AB) in strong vortex applications is presented. Linearized equations for the evolution of disturbances on a symmetric hurricane-like vortex in a shallow-water model are used to compare forecasts using the AB and BE formulations with benchmark primitive equation forecasts. The validity of the BE and AB models is formally determined by the square of the Froude number, F², and the square of the local Rossby number for disturbances with azimuthal wavenumber n, , respectively. The numerical experiments demonstrate that accurate results can be achieved with BE and AB in situations where F² and , respectively, are not necessarily small. When the divergence of the asymmetric disturbance is not much smaller than its vorticity, and the azimuthal wavenumber of the disturbance is low, the AB system proves to be a useful alternative to BE.  相似文献   

Influence of upper air conditions on the Patagonia icefields   总被引：1，自引：1，他引：0  

L.A. Rasmussen  H. Conway  C.F. Raymond 《Global and Planetary Change》2007,59(1-4):203

Upper-air conditions archived in the NCEP-NCAR Reanalysis have been used to investigate changes in precipitation and snowfall over the Patagonia icefields during 1960–99. Apparently, whereas total precipitation has not changed, warming has caused a decrease in the amount falling as snow. Precipitation at a site is taken to be proportional to the product of the relative humidity and the component of the wind in a particular critical direction, both at 850 hPa ( 1400 m) at a point over the ocean to the west of the icefields; whether it falls as rain or snow is assumed to depend on whether the temperature at the elevation of the site is above or below + 2 °C. The critical direction is assumed to be 270°, which is perpendicular to the north–south trending Andes and is also the prevailing wind direction in this zone of strong westerlies. Because of the scarcity of precipitation records on or near the icefields, the constant of proportionality cannot be determined, so the investigation is limited to examining relative changes in those upper air variables. Warming at 850 hPa has been 0.5 °C over the 40 years, both winter and summer, with the effects that it has: (1) shifted from snow to rain 5% of the precipitation, the total of which has changed little, and (2) increased annual melt in the ablation areas by 0.5 m w.e. The icefields have been losing mass since at least 1870, so this 40-year trend represents only an acceleration of the longer-term trend of adjusting to climate change since the Little Ice Age.  相似文献   

基流分割在水文计算中的应用——确定泉水流量     

夏凡  许伟林  蒋南杰 《城市地质》2010,5(2):42-44

本文运用基流分割法确定鱼卡盆地泉水流量,联合水量平衡法还原鱼卡河上站流量系列资料,为鱼卡盆地水资源评价奠定了基础。  相似文献   

Lower Hybrid Wave Electron Heating in the Fast Solar Wind     

J. Martin Laming 《Astrophysics and Space Science》2005,298(1-2):385-388

We discuss electron–ion equilibration by lower hybrid waves in the fast solar wind, and its observed effects upon element charge state distributions.  相似文献   

基于地表能量平衡的厦门岛城市功能区人为热排放分析   总被引：2，自引：0，他引：2  

刘嘉慧  赵小锋  林剑艺 《地球信息科学学报》2018,20(7):1026-1036

人为热排放不仅是城市热岛形成的重要因子,而且是与能源消耗密切相关的指标,对其大小和变化特征进行分析有利于减缓城市热岛与节能减排。本文以厦门岛为研究区,利用2009年多时相的Landsat TM影像和地表能量平衡模型反演出不同季节的人为热排放,在此基础上结合IKONOS影像解译的城市功能区,分析不同类型城市功能区人为热排放的时空变化特征。结果表明：不同类型城市功能区的人为热排放均在夏季达到最大,春季最小;工业区的人为热排放一直高于其他类型的城市功能区;工业区人为热排放高值区主要集中厦门岛西部传统的重点工业区,交通区人为热排放高值区的空间分布与厦门岛“三纵四横”的交通干线分布格局相吻合,居住区人为热排放高值区主要集中在旧城区,商业及公共设施区人为热排放高值区主要集中在单体建筑大的商圈和公共设施;总体上厦门岛西部的人为热排放比东部要高。这种时空分布的差异性与用地类型、人口数量与经济发展程度密切相关,而且建筑物的密度、高度和下垫面的材料通过影响其他地表通量来改变人为热排放的大小。通过分析不同城市功能区人为热排放的时空变化特征,可以从更微观的角度理解城市热环境和能源利用现状,为促进城市可持续发展提供理论依据。  相似文献   

环境资源与生态系统的关系   总被引：1，自引：1，他引：0  

刘立国  王洁  赵剑强 《地球科学与环境学报》2005,27(3):104-106

采用论述、图解及数学关系式的方法，较深入地分析了资源、环境与生态系统的关系。认为环境要素可分为仅产生污染型影响的环境要素；既可以产生污染型影响又可以导致资源破坏型影响的环境要素；仅产生资源破坏型影响3种类型。自然环境的优劣由组成自然环境各环境要素的环境质量状况和可作为自然环境要素的自然资源的数量多少决定。要实现环境与经济的可持续发展，应该把环境质量和资源利用同时作为衡量环境优劣的因素。  相似文献   

Towards an energy‐based runoff generation theory for tundra landscapes     

William L. Quinton  Sean K. Carey 《水文研究》2008,22(23):4649-4653

Runoff hydrology has a large historical context concerned with the mechanisms and pathways of how water is transferred to the stream network. Despite this, there has been relatively little application of runoff generation theory to cold regions, particularly the expansive treeless environments where tundra vegetation, permafrost, and organic soils predominate. Here, the hydrological cycle is heavily influenced by 1) snow storage and release, 2) permafrost and frozen ground that restricts drainage, and 3) the water holding capacity of organic soils. While previous research has adapted temperate runoff generation concepts such as variable source area, transmissivity feedback, and fill‐and‐spill, there has been no runoff generation concept developed explicitly for tundra environments. Here, we propose an energy‐based framework for delineating runoff contributing areas for tundra environments. Aerodynamic energy and roughness height control the end‐of‐winter snow water equivalent, which varies orders of magnitude across the landscape. Radiant energy in turn controls snowmelt and ground thaw rates. The combined spatial pattern of aerodynamic and radiant energy control flow pathways and the runoff contributing areas of the catchment, which are persistent on a year‐to‐year basis. While ground surface topography obviously plays an important role in the assessment of contributing areas, the close coupling of energy to the hydrological cycles in arctic and alpine tundra environments dictates a new paradigm. Copyright © 2008 John Wiley & Sons, Ltd.  相似文献