全文获取类型
收费全文 | 75332篇 |
免费 | 1090篇 |
国内免费 | 523篇 |
专业分类
测绘学 | 1717篇 |
大气科学 | 4989篇 |
地球物理 | 15050篇 |
地质学 | 26693篇 |
海洋学 | 6595篇 |
天文学 | 17523篇 |
综合类 | 178篇 |
自然地理 | 4200篇 |
出版年
2021年 | 739篇 |
2020年 | 843篇 |
2019年 | 910篇 |
2018年 | 1807篇 |
2017年 | 1736篇 |
2016年 | 2024篇 |
2015年 | 1116篇 |
2014年 | 1978篇 |
2013年 | 3693篇 |
2012年 | 2236篇 |
2011年 | 2993篇 |
2010年 | 2686篇 |
2009年 | 3552篇 |
2008年 | 3067篇 |
2007年 | 3118篇 |
2006年 | 2913篇 |
2005年 | 2109篇 |
2004年 | 2119篇 |
2003年 | 2088篇 |
2002年 | 1924篇 |
2001年 | 1703篇 |
2000年 | 1595篇 |
1999年 | 1378篇 |
1998年 | 1425篇 |
1997年 | 1384篇 |
1996年 | 1170篇 |
1995年 | 1180篇 |
1994年 | 1030篇 |
1993年 | 921篇 |
1992年 | 851篇 |
1991年 | 868篇 |
1990年 | 953篇 |
1989年 | 830篇 |
1988年 | 764篇 |
1987年 | 932篇 |
1986年 | 845篇 |
1985年 | 1042篇 |
1984年 | 1157篇 |
1983年 | 1128篇 |
1982年 | 1003篇 |
1981年 | 977篇 |
1980年 | 866篇 |
1979年 | 807篇 |
1978年 | 804篇 |
1977年 | 778篇 |
1976年 | 706篇 |
1975年 | 720篇 |
1974年 | 686篇 |
1973年 | 745篇 |
1972年 | 466篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
431.
432.
433.
A study was conducted in Lakshadweep islands to determine the feasibility of using Indian Remote Sensing (IRS) satellites for detecting changes in the seagrass from other coastal features. IRS ID and IRS P6 LISS III having spatial resolution of 23.5 m with lower cost compared to all other contemporary satellites with the same spatial resolution have not been widely used for monitoring the changes in seagrass cover. In this context, the present study attempted to explore the effectiveness of LISS III data for mapping seagrasses and to inform the international community about the usefulness of these low-cost imageries for coastal resource monitoring. Supervised classification and change detection studies found a significant decrease in seagrass cover of 73.03 ha in the Lakshadweep group of islands. An overall accuracy of 67.5% was obtained for the change maps, and seagrass cover and its changes vary at different islands. 相似文献
434.
Rémy Thibaud Géraldine Del Mondo Thierry Garlan Ariane Mascret Christophe Carpentier 《Transactions in GIS》2013,17(5):742-762
Defining a model for the representation and the analysis of spatio‐temporal dynamics remains an open domain in geographical information sciences. In this article we investigate a spatio‐temporal graph‐based model dedicated to managing and extracting sets of geographical entities related in space and time. The approach is based on spatial and temporal local relations between neighboring entities during consecutive times. The model allows us to extract sets of connected entities distant in time and space over long periods and large spaces. From GIS concepts and qualitative reasoning on space and time, we combine the graph model with a dedicated spatial database. It includes information on geometry and geomorphometric parameters, and on spatial and temporal relations. This allows us to extend classical measurements of spatial parameters, with comparisons of entities linked by complex relations in space and time. As a case study, we show how the model suggests an efficient representation of dunes dynamics on a nautical chart for safe navigation. 相似文献
435.
AbstractThis paper describes some results of an attempt to design and to write a general purpose computer program which can be used to produce quality maps of discrete data by the person who has had no training in computer programming. In the first section, the variety of the maps this program can produce is illustrated; in the second section, some of the principles involved in such map production are discussed; in the third section, the input arrangements for using the program are described and, finally, the role of such programs in teaching and research in the years ahead is discussed. 相似文献
436.
Abstract The Arc of the Geodesic.—In the first part of this paper a method was given for computing the azimuth of a geodesic. The method gives the convergence of the geodesic correctly up to the second power of e the eccentricity. The formula (9), however, also depends on the assumption that σ, the arc-length of the geodesic, can be obtained with sufficient accuracy from the Supplemental Dalby Theorem, that is to say, by a purely spherical computation. It is, therefore, needful to show that this supposition is justifiable; a means must in fact be indicated for verifying the assumption. 相似文献
437.
AbstractFor the sake of the junior reader we may repeat an old and simple investigation. Let us suppose that the paper on which a map is printed undergoes a regular expansion p in one direction, say the X direction, and another regular expansion q in the Y direction, perpendicular to the former; it is required to know the effect of these expansions on the area of any parcel on the map. Note that, so far as the mathematics are affected, X and Y are not necessarily parallel to the margins of the sheet; we shall take them here as axes of any rectangular coordinate system. The symbols p and q are regarded as ratios, so that 100p and 100p represent the percentage expansions; if the paper contracts instead of expanding, no more is necessary than to change the sign. 相似文献
438.
AbstractI. Introduction.—Map projection is a branch of applied mathematics which owes much to J. H. Lambert (v. this Review, i, 2, 91). In his “Beyträge zum Gebrauche der Mathematik und deren Anwendung” (Berlin, 1772) he arrived at a form of projection whereof the Transverse Mercator is a special case, and pointed out that this special case is adapted to a country of great extent in latitude but of small longitudinal width. Germain (“Traité des Projections”, Paris, 1865) described it as the Projection cylindrique orthomorphe de Lambert, but he also introduced the name Projection de Mercator transverse or renversée; he shows that Lambert's treatment of the projection was remarkably simple. 相似文献
439.
AbstractIn the second part of the paper on this subject in the last issue (30, 483) the references to the relative angular and linear closures are rather misleading. Mr Clendinning points out that the probable angular error at a station must be considered; the mean error is clearly different. 相似文献
440.
Abstract“A Well-Defined mountain, though miles inland and never visited by the surveyors, will often prove the very keystone of a chart which cannot be regularly and theoretically triangulated” (“Hydrographic Surveying”, by Rear-Adm. Sir Wm J. L. Wharton, K.C.B., and Rear-Adm. Mostyn Field, F.R.S. 3rd Ed. 1909, p. 128). To many the reasons prohibiting the occupation of inland stations may be unknown; it may suffice to state that, in the past, British hydrographers have mapped many coastal waters where penetration of the land was at least inadvisable. Since the charts so made were in general sold to the world, seamen of all nations have benefited from the surveys. 相似文献