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1.

The tree-limit altitudes of Norway spruce (Picea abies) and Scots pine (Pinus sylvestris) from 180 sites (within an area of 95?km?×?165?km) in the southern Scandes were correlated with the geographical variables latitude, longitude and distance to the sea. The results were compared with a similar investigation of the tree-limit of mountain birch (Betula pubescens Ehrh. ssp. tortuosa (Ledeb.) Nyman) in the same area. The three tree-limit altitudes showed good negative correlation with latitude, poor correlation with longitude and good positive correlation with the distance to the sea, suggesting that on a regional scale the altitudes are controlled by macroclimate. At some sites, local topoclimatic features, some of which were partially aspect-dependent, may cause deviations in the regional pattern of tree-limit altitude that is set primarily by summer temperature. Tree-limit responses to potential future climate warming will probably differ substantially in magnitude from site to site in relation to local topography and associated ecological constraints.  相似文献   

2.
《The Journal of geography》2012,111(5):250-256
Abstract

In this study, pairs of students in fifth and seventh grade generated and answered questions based on maps. More than 90 percent of the questions they generated made sense with reference to the map on which they were based. Each of these questions was coded in terms of both its informational content (symbols, latitude and longitude, and scale) and the process by which a map user obtains the information from the map (map reading, map interpreting, map inferring). Results indicated that students most often generated three types of questions, which together accounted for more than 80 percent of all the questions: 1) read symbol, 2) infer latitude and longitude, and 3) interpret scale. Qualitatively, the questions were analyzed for what they revealed about student confusion about map content. Problems with all three aspects of map content were common among both fifth- and seventh-grade students. The problem-posing technique proved useful for evaluating student's knowledge.  相似文献   

3.
4.
极区位于高纬度地区,极区航海图投影采用墨卡托投影时,图上极区附近变形较大,在极点处变形达到无穷大;采用极球面投影时,图上恒向线不是直线;心射切面投影不是正形投影,不能直接在图上量取方位和距离;兰伯特正形投影图上,经度是由角度表示,而不是真的经度;采用横轴墨卡托投影时,几乎所有的经线以及纬线在图上为曲线。以上常用的海图投影不利于船舶在极区安全航行,也不利于航海人员进行海图作业。针对此问题,将构建的伪经纬线网与经纬线网进行转换,通过Matlab得到基于伪经纬线网的横轴墨卡托投影图,此图具有类似于墨卡托海图的特点,图上极区变形失真小,图上伪经纬线的特点可方便极区海图作业。  相似文献   

5.

“It is not our desire to change needle and thread in women's hands into astrolabes and globes; neither do we consider it necessary that a woman should retreat to a room papered with maps and ornamented with globes ‥. Their high moral standards allow them, in our view, to possess wide knowledge of geography, on condition that they do not attempt, through use of terms too coarse for a lady, to appear too eager a group of geographers. I am certainly willing to let them use such words as climate, zones, and so forth; but I do not want them to scare me stiff quoting longitude and latitude at me. Let them speak as much as they want about what they read in travelers'tales, and I will listen with pleasure ‥. But I certainly do not want to see the day when a woman's knowledge of the earth equals that of men!'”(1)  相似文献   

6.
川渝地区气温随地形、经度和纬度的变化(英文)   总被引:4,自引:1,他引:3  
Using the daily temperature data of 95 meteorological stations from Si-chuan-Chongqing Region and its surrounding areas, this paper adopted these methods (e.g., linear regression, trend coefficient, geographical statistics, gray relational analysis and spatial analysis functions of GIS) to analyze the relations of temperature variability with topography, latitude and longitude. Moreover, the rank of gray correlation between temperature variability and elevation, longitude, latitude, topographic position and surface roughness also was measured. These results indicated: (1) The elevation affected temperature variability most obviously, followed by latitude, and longitude. The slope of the linear regression between temperature change rate and elevation, latitude and longitude was 0.4142, 0.0293 and -0.3270, respectively. (2) The rank of gray correlation between temperature change rate and geographic factors was elevation > latitude > surface roughness > topographic position > longitude. The gray correla-tion degree between temperature change rate and elevation was 0.865, followed by latitude with 0.796, and longitude with 0.671. (3) The rate of temperature change enhanced with the increase of elevation. Especially, the warming trend was significant in the plateau and mountain areas of western Sichuan, and mountain and valley areas of southwestern Sichuan (with the warming rate of 0.74℃/10a during the 1990s). However, there was a weak warming trend in Sichuan Basin and its surrounding low mountain and hilly areas. (4) The effects of latitude on temperature change rate presented the specific regulation, which the warming rate of low-latitude areas was more significant than that of high-latitude areas. However, they were consistent with the regulation that the increasing of low temperature controlled most of the warming trend, due to the effects of terrain and elevation on annual mean temperature. (5) Ba-sically, temperature variability along longitude direction resulted from the regular change of elevation along longitude. It was suggested that, in Sichuan-Chongqing Region, special features of temperature variability largely depended on the terrain complexity (e.g., undulations, mutations and roughness). The elevation level controlled only high or low annual mean temperature and the range of temperature change rate in the macro sense.  相似文献   

7.
邹斌  解思梅  郝春江  陆军  尹涛 《极地研究》2000,12(4):291-300
船载卫星遥感图象处理系统是针对南极考察气象航线预报、冰区航行的海冰预报和导航需要而研制的船陆两用多功能软件系统。采用了最新的 DEL PHI可视化软件开发工具 ,开发了用于 WINDOWS98环境下的 32位的程序 ,并针对接收系统开发了 WINDOWS设备驱动程序 ,提高了在 WIND0 WS98多任务环境下 ,接收程序的实时性和可靠性 ;采用面向对象的程序开发方法和开放式的体系结构 ,便于功能的更新和提高 ;采用 SGP4/SDP4轨道模式及两行元素的轨道参数计算出卫星星下点的位置 ,实现了在 1 A图象上计算逐点经纬度的快速动态定位和图象显示的功能 ;采用迭代法利用电子地图网格数据 ,在接收的卫星云图上迭代套上地形及海岸线。组成了适合船陆两用的多功能快速灵活的图象处理系统 ,可以在 1~ 2分钟瞬间内完成一幅图的定位套网格和套地形线的工作。解决了南极海冰监测和冰缝、水道预报的难点。可以使图象上下滚动、左右移动、任意放大、缩小和剪取 ;可以随着鼠标的移动显示出图上任意一点的经纬度 ;能够在图上标出任意目标物 ,如船位、站位、岛屿等等 ;能够方便地在图上画出航线 ,直观地判断船所处的位置和航线周围的气象和海洋环境状况 ;解决了在茫茫海洋和冰区中航行找不到参照物时的困惑 :能够输出任意大小的 2 4位真  相似文献   

8.
中国高山林线的分布高度与气候的关系   总被引:26,自引:0,他引:26  
王襄平  张玲  方精云 《地理学报》2004,59(6):871-879
通过研究我国高山林线的分布高度沿纬度、经度的变化格局,和对高山林线处的温度和基带降水等气候指标的分析,对我国高山林线分布高度与气候因子的关系进行探讨。结果表明:(1) 我国高山林线高度表现出明显的纬向和经向变化,总体趋势是:在北纬30o以北,高山林线高度随纬度升高而下降,下降速率为112 m/度左右;在30oN以南,则表现出较大的东西部差异:在东部,高山林线高度变化不明显,西部则随纬度增加呈上升趋势。在相似的纬度上,高山林线高度呈现出从东向西升高的趋势。高山林线在藏东南的洛隆、丁青、工布江达一带 (约29o~32oN,94o~96oE) 达到4 600 m,为世界最高林线高度,并以此为中心向四周降低。(2) 影响高山林线高度的主导气候因子为生长季温度条件。我国高山林线高度的温度指标为年生物温度3.5 oC,温暖指数14.2 oC·月,生长季平均温度8.2 oC。该指标相应海拔高度的地理差异,导致了我国高山林线高度的纬向、经向变化,和从沿海到内陆林线高度的差异。(3) 降水对高山林线高度有显著影响。在中高纬度地区,相同纬度上干旱区域的高山林线高于较湿润区域,降水量是通过温度间接作用于林线高度的。  相似文献   

9.
山体效应是地理地带性之外,在大尺度上影响垂直带分布的主要因素,山体基面高度则是山体效应的第一影响因子。青藏高原及其周边地区,雪线呈现出中心高、周围低,与山体基面高度相一致的环状分布模式。为分析山体基面高度对雪线分布的影响,本文共收集青藏高原及周边地区雪线数据142个,采用纬度、经度和基面高度为自变量的三元一次方程拟合研究区雪线分布,计算各自的标准回归系数和相对贡献率,再将基面高度划分成5个子集(0~1000 m、1001~2000 m、2001~3000 m、3001~4000 m和4001~5000 m),分析基面高度不同的山地对雪线的影响差异。结果表明:① 在青藏高原,纬度、经度和基面高度对雪线高度分布的相对贡献率分别为51.49%、16.31%和32.20%;② 随着基面高度的增高,各子集模型的决定系数虽有逐渐降低的趋势,但仍保持在较高的值域(R2=0.895~0.668),说明模型的有效性;③ 随基面高度的抬升,纬度和山体基面高度对雪线分布高度的相对贡献率分别表现出降低(92.6%~48.99%,R2=0.855)和增大(3.33%~31.76%,R2=0.582)的趋势,表明基面高度越高,其对雪线分布高度的影响越大。  相似文献   

10.
气候变化下的祁连山地区近40 年多年冻土分布变化模拟   总被引:4,自引:1,他引:3  
冻土是一种对气候变化极为敏感的土体介质,故气候的变化过程能反映和模拟冻土的分布及变化趋势。基于高程-响应模型,运用高分辨率的高程数据(DEM)、经度数据(Longitude)、纬度数据(Latitude)、年平均气温数据(MAAT)和气温垂直递减率数据(VLRT)对祁连山地区近40 年的多年冻土分布状况进行了数值模拟。分析表明:① 该高程-响应模型模拟的冻土范围和变化趋势与相关研究所引入逻辑回归模型的模拟结果基本一致。② 该模型模拟的1970s、1980s、1990s,2000s 的祁连山地区冻土分布面积分别为9.75×104 km2、9.35×104 km2、8.85×104 km2、7.66×104 km2。在这40 年中,冻土的分布范围呈现出明显减少的趋势。③ 从1970s 到1980s、1980s 到1990s、1990s 到2000s 三个时间段内,冻土分布范围的退缩速率分别为4.1%、5.3%、13.4%,其呈现逐渐增速的趋势,1990s 到2000s 出现了跳跃式增长。本研究可为分析长时间序列祁连山地区的多年冻土变化提供科学参考依据。  相似文献   

11.
Spatial distribution changes in major crops can reveal important information about cropping systems. Here, a new centroid method that applies physics and mathematics to spatial pattern analysis in agriculture is proposed to quantitatively describe the historical centroids of rice, maize and wheat in China from 1949 to 2014. The geographical centroids of the rice area moved 413.39 km in a 34.32° northeasterly (latitude 3.08°N, longitude 2.10°E) direction at a speed of 6.36 km/year from central Hunan province to Hubei province, while the geographical centroids of rice production moved 509.26 km in the direction of 45.44° northeasterly (latitude 3.22°N, longitude 3.27°E) at a speed of 7.83 km/year from central Hunan province to Henan province. The geographical centroids of the maize area and production moved 307.15 km in the direction of 34.33° northeasterly (latitude 2.29°N, longitude 1.56°E) and 308.16 km in the direction of 30.79° northeasterly (latitude 2.39°N, longitude 1.42°E), respectively. However, the geographical centroids of the wheat area and production were randomly distributed along the border of Shanxi and Henan provinces. We divided the wheat into spring wheat and winter wheat and found that the geographical centroids of the spring wheat area and production were distributed within Inner Mongolia, while the geographical centroids of winter wheat were distributed in Shanxi and Henan provinces. We found that the hotspots of crop cultivation area and production do not always change concordantly at a larger, regional scale, suggesting that the changing amplitude and rate of each crops’ yield differ between different regions in China. Thus, relevant adaptation measures should be taken at a regional level to prevent production damage in those with increasing area but decreasing production.  相似文献   

12.
Summary. The latitude of the Sq ( H ) focus along the 0° longitude meridian in the northern hemisphere has been determined for all the quiet days, as determined from the aa indices, for the sunspot minimum years 1963–64–65. It is shown that: (a) most of the large variability of the focus latitude is due to the effect of a superposed northward magnetic field that is present on AQDs and which tends to move the apparent focus latitude poleward in the northern hemisphere, and (b) a smaller equatorward motion is caused by the negative AQD events that occur in the 0830–1330 LT range. When these two classes of days are removed from the data set, the focus latitude is found to be completely contained within the range 36°-48° for the months March-October
with an average value of 41.5 ± 2.3, whilst in winter the range is larger with an average value of 36.7 ± 3.4. However, since the magnitude of the superposed northward field is longitude-dependent, it may be present even on days not classed as AQDs. It is shown that much of the variability in the focus latitude of the normal days along the 0° longitude meridian is caused by variations in the amplitude of the superposed northward field.  相似文献   

13.
Estimation of soil organic carbon reservoir in China   总被引:6,自引:0,他引:6  
1 IntroductionResearch on global change has aroused many scientists' attention to the balance, storage and spatial distribution of carbon in the terrestrial ecosystem. The carbon stored in soil is 2.5-3 times as much as that stored in plants[1,2], so the distribution and conversion of carbon in humus has become one of the global research foci on organic carbon at present[3]. Organic carbon and nitrogen contents in soils are not only important components of soils but also the most important eco…  相似文献   

14.
Abstract

Attempts have been made by different organizations in India to organize data in order to develop a suitable information system. These attempts were oriented towards specific uses, such as natural resources, data management, thematic mapping and the like. In some attempts software has been developed for some specific purpose. It is not an easy task to develop an information system for a country such as India. Its extent in latitude and longitude is well above average. There are federal and state agencies for the collection of data and the preparation of maps. The geographical information concerning India is available from the following sources: the administrative areas of states, union territories, districts, sub-districts and villages; survey sheets; remote sensing images; aerial photographs; and thematic base maps of the National Atlas and Thematic Mapping Organisation. There are other map series available which have been used for socio-economic mapping. By the end of 1987 the Indian Remote Sensing Satellite will be launched and then remotely-sensed data will be readily available. Considering the geographical bases available in the country, five levels can be identified for developing an information system for India. Some of the thematic maps at 1:1000 000 scale can be used for initiating such a geographical information system.  相似文献   

15.
"We report on a project that converted subnational population data to a raster of cells on the earth. We note that studies using satellites as collection devices yield results indexed by latitude and longitude. Thus it makes sense to assemble the terrestrial arrangement of people in a compatible manner. This alternative is explored here, using latitude/longitude quadrilaterals as bins for population information.... The results to date of putting world boundary coordinates together with estimates of the number of people are described. The estimated 1994 population of 219 countries, subdivided into 19,032 polygons, has been assigned to over six million five minute by five minute quadrilaterals covering the world."  相似文献   

16.
姚永慧  张百平  谭靖  韩芳 《地理研究》2009,28(6):1633-1643
长江上游包括青藏高原东南部、秦巴山地、四川盆地与云贵高原部分地区,在地理、地貌、气候、生物多样性方面都表现得极为复杂和丰富多彩,在世界山地中也占有举足轻重的位置。特别是复杂多样的山地垂直带谱更是欧亚大陆乃至世界山地垂直带研究中至关重要的组成部分。在地学信息图谱和数字山地垂直带体系的基础上,本文系统地收集和分析了长江上游共50个山地垂直带谱所体现的空间规律,河源区、横断山区、秦巴山区及贵州高原的垂直带谱类型多样并各具特色,且在经度和纬度方向又具有统一的分布规律,如雪线、林线、针叶林及阔叶林等的分布界线变化规律比较符合二次曲线规律,验证了大陆尺度上山地垂直带二次曲线模式假说。另外,山地垂直带分布规律又具有尺度效应,中小尺度上地形的影响作用表现得极为显著。  相似文献   

17.
为了解决传统球面格网与经纬度坐标在转换效率或精度上存在的问题,提出一种新的转换算法.在分析球面退化四叉树格网(DQG)的剖分原理及其编码规则的基础上,给出DQG单元的行列定义规则,并设计了一套地址码与经纬度之间快速坐标转换的详细算法;将该算法与QTM行列逼近法、ZOT投影法及ETP投影法进行效率对比实验,结果表明:对于100万个DQG格网单元,其转换算法的平均耗时量为上述传统算法的53%、39%和7%,且避免了QTM行列逼近法出现的半格网误差现象,精度较高.  相似文献   

18.
Summary. From a study of 'abnormal quiet days' (AQDs) along the 0° meridian between 14 and 60° N, it was found (Butcher & Brown) that the minimum in H at stations on the poleward side of the Sq ( H ) focus was formed by a small negative substorm event when the normal Sq ( H ) amplitude was reduced by a superposed northward field.
In this paper we consider both the AQD event and the superposed northward field as a function of longitude and also consider in more detail the latitude variation of the superposed northward field. From such a study it is concluded that: (1) the AQD event is definitely due to a small magnetospheric substorm event; (2) the superposed northward field varies smoothly with longitude falling to zero some 110° from the longitude of its maximum amplitude; (3) the superposed northward field has a variation with geomagnetic latitude tending to zero near 20° and 70°N with a maximum near 55° N in summer and 35° N in winter; (4) there is some evidence that the effect of the IMF penetrates into the mid-latitude E-region and its effect is latitude-dependent. Although the evidence supports the suggestion that the currents responsible for the superposed northward field flow in the E-region no suggestion as to the origin of the driving force of the currents is forthcoming.  相似文献   

19.
A new context for active tectonic zone recognition is proposed on the basis of the exporting energy of the terrain features at continental scale. Toward this end, elevation, latitude, and longitude decorrelation stretch of multi-temporal moderate resolution imaging spectroradiometer (MODIS) monthly average land surface temperature (LST) imagery (MYD11C3) is applied in a study area extending from Red Sea to Indian Ocean and from Persian Gulf to Black Sea and Caspian Sea. Multiple linear regression analysis of principal components images (principal components analysis (PCAs)) quantified the variance explained by elevation, latitude, and longitude. Selective variance reduction reconstructed the multi-temporal LST imagery from the residual images and selected PCAs by taking into account the portion of variance that is not related to elevation, latitude, and longitude. The reconstructed imagery presents the magnitude the standardized LST value per pixel deviates from the elevation, latitude, and longitude predicted one, whereas a positive LST anomaly is defined as a region that presents positive reconstructed LST value throughout the year. Clustering of the reconstructed standardized imagery mapped a great positive LST anomaly of tectonic origin that occupies the greatest in elevation and most massive areas, forming three regions: (a) the Himalayan Belt along the Pakistan, Afghanistan borders, and the Eastern Alpine zone (Makhran Ranges and Zagros Ranges), (b) the coastal zone (along the Red Sea) of the Arabian Shield, and (c) the Oman Mountains Province along the Persian Gulf. The method will allow the classification of terrain objects (e.g. mountains, basins) on the basis of both the exporting energy (reconstructed LST) and geomorphometry.  相似文献   

20.
基于GIS的定位观测数据空间化   总被引:20,自引:3,他引:17  
属性数据空间化是当前GIS领域的前沿问题之一。在对中国624个气象站多年平均气温数据空间化过程中,通过使用30秒分辨率的数字高程数据,把气温分解为受经纬度、海拔高度影响的规律性成分和受其它因素影响的非规律性成分两部分,并分别用多元回归和反距离权重内插方法对二者实施空间化,最后将空间化结果进行合成得到基于栅格的中国多年平均气温分布数据。该数据既能反映气温在空间上的宏观变化,又能反映气温在局部地区的微观变化。该方法可供其它类型观测数据空间化、特别是在观测站点稀疏的情况下参考和借鉴。  相似文献   

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