全文获取类型
收费全文 | 128篇 |
免费 | 6篇 |
专业分类
测绘学 | 4篇 |
地球物理 | 14篇 |
地质学 | 62篇 |
海洋学 | 13篇 |
天文学 | 34篇 |
自然地理 | 7篇 |
出版年
2021年 | 2篇 |
2020年 | 1篇 |
2019年 | 4篇 |
2018年 | 5篇 |
2017年 | 3篇 |
2016年 | 6篇 |
2015年 | 8篇 |
2014年 | 2篇 |
2013年 | 8篇 |
2012年 | 5篇 |
2011年 | 8篇 |
2010年 | 2篇 |
2009年 | 10篇 |
2008年 | 7篇 |
2007年 | 5篇 |
2006年 | 3篇 |
2005年 | 5篇 |
2004年 | 5篇 |
2003年 | 5篇 |
2002年 | 6篇 |
2001年 | 2篇 |
2000年 | 2篇 |
1999年 | 5篇 |
1998年 | 4篇 |
1997年 | 1篇 |
1996年 | 2篇 |
1995年 | 4篇 |
1994年 | 2篇 |
1993年 | 2篇 |
1992年 | 1篇 |
1990年 | 1篇 |
1989年 | 2篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1986年 | 1篇 |
1982年 | 1篇 |
1980年 | 1篇 |
1957年 | 1篇 |
排序方式: 共有134条查询结果,搜索用时 0 毫秒
1.
Della Vecchia A. Ferrazzoli P. Wigneron J.-P. Grant J.P. 《Geoscience and Remote Sensing Letters, IEEE》2007,4(4):508-512
This letter describes recent advances in modeling forest emissivity at L-band. The formulation is based on a previously developed discrete model and includes a new representation of forest litter. Comparisons with multitemporal radiometric data collected in the framework of the ldquoBray 2004rdquo experiment, which was carried out within Les Landes forest, are shown and discussed. Input variables are given by using detailed ground measurements. In general, the model reproduces both absolute values and temporal variations of measured brightness temperature. The contribution of the litter to overall emission was found to be important. 相似文献
2.
In recent years many fuller ship hull forms have been designed and constructed in various shipbuilding countries, but the data available for the development of the fuller forms are inadequate from the point of view of preliminary ship design. In this paper the authors describe how they have systematically tested vessel forms of block coefficients ranging from 0.80 to 0.90. The analysis and presentation of the test results have been made in such a manner that designers can produce hull forms like those of tankers and other bulk carriers quickly and reliably. 相似文献
3.
Castagnoli G. Cini Bonino G. Della Monica P. Taricco C. Bernasconi S.M. 《Solar physics》1999,188(1):191-202
In this paper we present the 18O profile of Globigerinoides ruber measured in the GT90/3 shallow water Ionian sea core, dated with high precision. The 18O profile covers the period 1200–1900 AD, with a resolution of 3.87 years. This long record of 700 years of 18O allows us to identify the imprint of the solar cycle in a climatic record. In fact, the spectral analysis of the time series performed with different methods shows a dominant periodicity of about 11 years with an amplitude of 0.07. The signal is in opposition to the sunspot number cycle. This component is identified at a high significance level by Monte Carlo Singular Spectrum Analysis (MC-SSA). 相似文献
4.
Tommaso Maccacaro Roberto Della Ceca Valentina Braito Alessandro Caccianiga Paola Severgnini Anna Wolter 《Astrophysics and Space Science》2004,294(1-2):89-94
We present here some initial results from the ongoing XMM-Newton bright serendipitous survey. The survey is aimed at selecting
and spectroscopically identifying a large and statistically representative sample of bright (f
x ≳ 7× 10−14 c.g.s) serendipitous X-ray sources in the 0.5–4.5 keV energy band (BSS) and a complementary (smaller) sample in the 4.5–7.5
keV energy band (HBSS).
The work is partly based on observations obtained with XMM-Newton, an ESA science mission with instruments and contributors directly founded by ESA member states and the USA(NASA) and on
observations collected at TNG. The TNG telescope is operated on the island of La Palma by the Centro Galileo Galilei of the
INAF in the Spanish Observatorio del Roque de Los Muchachos of the Instituto de Astrofísica de Canarias.
On behalf of the XMM-Newton Survey Science Center. 相似文献
5.
6.
7.
Gabriella Della Penna 《Celestial Mechanics and Dynamical Astronomy》1999,75(2):103-124
A model for planetary precession is investigated using analytical and numerical techniques. A Hamiltonian function governing
the model is derived in terms of action-angle Andoyer-Déprit variables under the assumption of equatorial symmetry. As a first
approximation a simplified Hamiltonian with zero-eccentricity is considered and stability estimates are derived using KAM
theory. A validation of the analytical results is performed computing Poincaré surfaces of section for the circular and elliptical
model. We also investigate the role of the eccentricity and its connection with the appearance of resonances. Special attention
is devoted to the particular case of the Earth–Moon system.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
8.
Andrew G. Fountain & Aldo Vecchia 《Geografiska Annaler: Series A, Physical Geography》1999,81(4):563-573
Glacier mass balance is estimated for South Cascade Glacier and Maclure Glacier using a one-dimensional regression of mass balance with altitude as an alternative to the traditional approach of contouring mass balance values. One attractive feature of regression is that it can be applied to sparse data sets where contouring is not possible and can provide an objective error of the resulting estimate. Regression methods yielded mass balance values equivalent to contouring methods. The effect of the number of mass balance measurements on the final value for the glacier showed that sample sizes as small as five stakes provided reasonable estimates, although the error estimates were greater than for larger sample sizes. Different spatial patterns of measurement locations showed no appreciable influence on the final value as long as different surface altitudes were intermittently sampled over the altitude range of the glacier. Two different regression equations were examined, a quadratic, and a piecewise linear spline, and comparison of results showed little sensitivity to the type of equation. These results point to the dominant effect of the gradient of mass balance with altitude of alpine glaciers compared to transverse variations. The number of mass balance measurements required to determine the glacier balance appears to be scale invariant for small glaciers and five to ten stakes are sufficient. 相似文献
9.
Roberto Danovaro Daniela Marrale Antonio Dell'Anno Norberto Della Croce Anastasios Tselepides Mauro Fabiano 《Progress in Oceanography》2000,46(2-4)
Bacterial abundance, biomass and cell size were studied in the oligotrophic sediments of the Cretan Sea (Eastern Mediterranean), in order to investigate their response to the seasonal varying organic matter (OM) inputs. Sediment samples were collected on a seasonal basis along a transect of seven stations (ranging from 40 to 1570 m depth) using a multiple-corer. Bacterial parameters were related to changes in chloroplastic pigment equivalents (CPE), the biochemical composition (proteins, lipids, carbohydrates) of the sedimentary organic matter and the OM flux measured at a fixed station over the deep basin (1570 m depth). The sediments of the Cretan Sea represent a nutrient depleted ecosystem characterised by a poor quality organic matter. All sedimentary organic compounds were found to vary seasonally, and changes were more evident on the continental shelf than in deeper sediments. Bacterial abundance and biomass in the sediments of the Cretan Sea (ranging from 1.02 to 4.59 × 108 cells g−1 equivalent to 8.7 and 38.7 μgC g−1) were quite high and their distribution appeared to be closely related to the input of fresh organic material. Bacterial abundance and biomass were sensitive to changes in nutrient availability, which also controls the average cell size and the frequency of dividing cells. Bacterial abundance increased up to 3-fold between August '94 and February '95 in response to the increased amount of sedimentary proteins and CPE, indicating that benthic bacteria were constrained more by changes in quality rather than the quantity of the sedimentary organic material. Bacterial responses to the food inputs were clearly detectable down to 10 cm depth. The distribution of labile organic compounds in the sediments appeared to influence the vertical patterns of bacterial abundance and biomass. Cell size decreased significantly with water depth. Bacterial abundance and biomass were characterised by clear seasonal changes in response to seasonal OM pulses. The strong coupling between protein flux and bacterial biomass together with the strong bacterial dominance over the total biomass suggest that the major part of the carbon flow was channelled through the bacteria and the benthic microbial loop. 相似文献