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101.
At Beijing Observatory both astrometric and gravimetric observations are available to study the non-tidal variations in the deflections of the vertical (or non-tidal plumbline variations, PLVs). From repeated gravimetric observations performed in a network around the observatory, the PLVs at Beijing Observatory during the period 1987.0–1996.0 have been calculated. After comparison with the observational residuals (which also contain the PLV components) of the photoelectric astrolabe located at the observatory, the accuracy of the obtained PLV results has been examined. It is shown that, due to the asymmetry of the gravimetric network, the qualities of the two different PLV components are not equal. The longitude component of the PLV at Beijing has been determined successfully, to be of the order of 0.05, with a contribution of about 0.02 in the inter-annual time scale. The result for the latitude PLV component is not good enough to draw a conclusion. Although both techniques are able to measure the PLV, the result of the determination depends very much on the availability of observational data. 相似文献
102.
M. Burša S. Kenyon J. Kouba Z. Šíma V. Vatrt V. Vítek M. Vojtíšková 《Studia Geophysica et Geodaetica》2005,49(1):13-22
Estimates of the second tesseral torque due to the variations in the radial space position of the mean ocean surface as monitored by TOPEX/POSEIDON altimeter system are derived. The magnitude of the studied torque may be compared to the tidal torque and to the tesseral torque caused by deformations due to the Earths rotation. However, such torque estimates strongly depend on the thickness of the ocean surface layer adopted in the spherical model of which the dynamics is believed to be responsible for the derived torque. The dependence on the thickness is discussed. 相似文献
103.
M.J. Broom 《Estuarine, Coastal and Shelf Science》1982,15(2):135-150
An assessment of community composition and the functional roles of the dominant species has been carried out in two intertidal areas of Malaysian mudflat dominated by natural populations of the arcid bivalve mollusc Anadara granosa.In addition to A. granosa, organisms of numerical importance are the venerid bivalve Pelecyora trigona, the neogastropod Plicarcularia leptospira, the mesogastropods Stenothyra glabrata and Cerithidea cingulata and the hermit crab Diogenes sp. The mesogastropod Natica maculosa and the neogastropod Thais carinifera may be of some importance to community organization but they are not numerically dominant. Annelids are conspicuous by their absence.The following trophic roles are ascribed to specific members of the community: A. granosa—facultative surface deposit feeder; P. trigona—suspension feeder; P. leptospira—scavenger; C. cingulata—deposit feeder/grazer; S. glabrata—deposit feeder/grazer; N. maculosa—predator; T. carinifera—predator; Diogenes sp.—scavenger/predator. S. glabrata is of particular interest because it appears to fill the niche occupied by mud snails of the genus Hydrobia in temperate mudflat systems.There is evidence of seasonality on the mudflats which points to a spawning of certain forms triggered by the major annual salinity depression at the time of the onset of the north-east monsoon in October/November. Concentrations of benthic chlorophyll a show no obvious signs of a seasonal fluctuation and the seasonality of the primary consumers is not thought to be related to food abundance. However there is some evidence of seasonality of reproduction in N. maculosa which preys on the seasonally reproducing bivalves. 相似文献
104.
Based on the meteorological data of 20 stations in the Hengduan Mountains region during 1961-2009, the annual and seasonal variation of potential evapotranspiration was analyzed in combination with the Penman-Monteith model. With the method of Spline interpolation under ArcGIS, the spatial distribution of potential evapotranspiration was presented to research the regional difference, and the correlation analysis was used to discuss the dominant factor affecting the potential evapotranspiration. The results indicated that the an-nual potential evapotranspiration showed a decreasing tendency since the 1960s, especially from the 1980s to 1990s, while it showed an increasing tendency since 2000. Regional potential evapotranspiration showed a rate of -0.17 mm a?1. Potential evapotranspiration in north, middle and south of the Hengduan Mountains exhibited decreasing trends over the studied period, and its regional trend was on the decline from southwest to northeast. 相似文献
105.
106.
使用Anderson-Ⅱ型9级撞击采样器测量了南京市鼓楼商业区、江北工业区、钟山风景区和宁六高速公路交通源春、夏、秋三季的大气气溶胶质量浓度。分析结果表明:南京市PM2.1和PM10的质量浓度存在明显的季节变化,秋季>春季>夏季;ρPM10春季为167.47 μg/m3,夏季为 85.99 μg/m3,秋季为238.99 μg/m3;ρPM2.1春季为59.66 μg/m3,夏季为42.80 μg/m3,秋季为100.15 μg/m3。不同季节中ρPM10和ρPM2.1均存在较好的相关性,夏季相关性最好,相关系数为0.952;秋季次之,相关系数为0.783;春季相对较差,相关系数为0.613。城市不同功能区之间ρPM2.1和ρPM10的质量浓度值差异很大,交通源>工业区>商业区>风景区。城市不同功能区的质量浓度谱分布基本一致,均为双峰型分布,峰值分别位于0.43~0.65 μm/m3和9.0~10.0 μm/m3。南京市春、夏、秋三个季节大气粒子质量浓度谱为双峰分布,粒子主要集中在0.43~3.3 μm/m3的粒径段。江北工业区ρPM10和ρPM2.1质量浓度的相关系数为0.814,略高于鼓楼商业区的0.797。 相似文献
107.
介绍了由德国Geo++研究的直接在野外进行的绝对校准方法,该方法可以消除多路径效应,测得和方位角相关的PCV.经过进一步的研究,该校正过程高效准确且可以实时提供校正结果。简单列举了AOAD/M—T类型天线的相对和绝对PCV的结果,对PCV的改正精度要求做了简单介绍。 相似文献
108.
选取新疆北疆20个站1961-2006年积雪及稳定积雪日数、最大积雪深度资料,同时选择冬季降水量和气温稳定通过0℃以下的日数作为积雪的影响因子,分析了46 a来北疆积雪的变化趋势。结果表明:46 a来最大积雪深度呈显著增加趋势,平均年增长0.8%,其变化与冬季降水量增加有关,呈正相关;积雪日数和稳定积雪日数也呈稍增加趋势,增加主要发生在1960-1980年代,1990年代以来有所减少,其变化与气温稳定通过0℃以下的日数呈显著正相关。 相似文献
109.
江苏夏季气温异常的时空变化特征 总被引:7,自引:4,他引:3
利用中国160气象观测站1951-2005 年和江苏省59气象观测站1961-2004年的月平均气温资料, 在分析江苏气温变化的季节-年际变化特征的基础上, 重点分析了江苏夏季气温的年际、年代际变化的时间和空间特征.发现:江苏夏季气温1970s到1990s前期基本上处在一个偏凉期,1960s及1990s中后期以后基本上处在一个偏热期;江苏夏季气温异常存在显著的准6 a、准9 a的年际周期和以16 a为中心的年代际周期;江苏夏季气温趋势自西北向东南呈现正负正的位相分布特点,即江苏西北部和东南部地区夏季气温呈现升高的趋势,其它地区呈现降低的趋势. 相似文献
110.
Variations of Terrestrial Water Storage in the Yangtze River Basin under Climate Change Scenarios 下载免费PDF全文
In this study, the water balance-based Precipitation-Evapotranspiration-Runoff (PER) method combined with the land surface model Variable Infiltration Capacity (VIC) was used to estimate the spatiotemporal variations of terrestrial water storage (TWS) for two periods, 1982–2005 (baseline) and 2071–2100, under future climate scenarios A2 and B2 in the Yangtze River basin. The results show that the estimated TWS during the baseline period and under the two future climate scenarios have similar seasonal amplitudes of 60–70 mm. The higher values of TWS appear in June during the baseline period and under the B2 scenario, whereas the TWS under A2 shows two peaks in response to the related precipitation pattern. It also shows that the TWS is recharged from February to June during the baseline period, but it is replenished from March to June under the A2 and B2 scenarios. An analysis of the standard derivation of seasonal and interannual TWS time series under the three scenarios demonstrates that the seasonal TWS of the southeastern part of the Yangtze River basin varies remarkably and that the southeastern and central parts of the basin have higher variations in interannual TWS. With respect to the first mode of the Empirical Orthogonal Function (EOF), the inverse-phase change in seasonal TWS mainly appears across the Guizhou-Sichuan-Shaanxi belt, and the entire basin generally represents a synchronous change in interannual TWS. As a whole, the TWS under A2 presents a larger seasonal variation whereas that under B2 displays a greater interannual variation. These results imply that climate change could trigger severe disasters in the southeastern and central parts of the basin. 相似文献