全文获取类型
收费全文 | 53624篇 |
免费 | 697篇 |
国内免费 | 562篇 |
专业分类
测绘学 | 1448篇 |
大气科学 | 3799篇 |
地球物理 | 9896篇 |
地质学 | 19207篇 |
海洋学 | 4906篇 |
天文学 | 12906篇 |
综合类 | 188篇 |
自然地理 | 2533篇 |
出版年
2022年 | 365篇 |
2021年 | 629篇 |
2020年 | 658篇 |
2019年 | 707篇 |
2018年 | 1583篇 |
2017年 | 1505篇 |
2016年 | 1871篇 |
2015年 | 988篇 |
2014年 | 1748篇 |
2013年 | 2866篇 |
2012年 | 1854篇 |
2011年 | 2373篇 |
2010年 | 2068篇 |
2009年 | 2677篇 |
2008年 | 2295篇 |
2007年 | 2347篇 |
2006年 | 2193篇 |
2005年 | 1621篇 |
2004年 | 1638篇 |
2003年 | 1548篇 |
2002年 | 1472篇 |
2001年 | 1298篇 |
2000年 | 1218篇 |
1999年 | 993篇 |
1998年 | 1039篇 |
1997年 | 947篇 |
1996年 | 816篇 |
1995年 | 782篇 |
1994年 | 685篇 |
1993年 | 604篇 |
1992年 | 592篇 |
1991年 | 593篇 |
1990年 | 622篇 |
1989年 | 493篇 |
1988年 | 504篇 |
1987年 | 528篇 |
1986年 | 487篇 |
1985年 | 610篇 |
1984年 | 673篇 |
1983年 | 590篇 |
1982年 | 561篇 |
1981年 | 499篇 |
1980年 | 469篇 |
1979年 | 477篇 |
1978年 | 458篇 |
1977年 | 368篇 |
1976年 | 345篇 |
1975年 | 357篇 |
1974年 | 308篇 |
1973年 | 342篇 |
排序方式: 共有10000条查询结果,搜索用时 0 毫秒
951.
S. N. Kulichkov I. P. Chunchuzov O. I. Popov 《Izvestiya Atmospheric and Oceanic Physics》2010,46(1):60-68
The results of simulating the influence of an atmospheric fine structure on the characteristics of acoustic signals propagating
throughout the atmosphere for long distances from their sources are presented. A numerical model of an atmospheric fine inhomogeneous
structure within the height range z = 20…120 km is proposed to perform calculations. This model and its numerical parameters are based on the current notions
of the formation of an atmospheric fine structure due to internal gravity waves. The numerical calculations were performed
using the parabolic-equation method. A spatial structure of the acoustic field and the structure of an acoustic signal at
long distances from a pulsed source were calculated. It is shown that the presence of an atmospheric fine structure results
in a scattering of acoustic signals and their recording in the geometric shadow region. The results of calculations of signal
forms are in a satisfactory agreement with data on signals recorded in the geometric shadow region which is formed at a distance
of about 300 km from an experimental explosion. 相似文献
952.
A plane problem of free stationary gravitational waves in a horizontal current with vertical shear of the velocity is studied
in the linear statement. The determination of the parameters of waves is reduced to the solution of the Sturm–Liouville boundary-value
problem. For some vertical distributions of current velocity, we obtain analytic solutions. We propose a numerical algorithm
for finding the parameters of waves. On the basis of the performed analysis, we establish the possibility of existence of
stationary surface waves in currents for certain ranges of the Froude number. As the Froude number decreases, the waves become
shorter, which leads to a faster attenuation of waves disturbances with depth. Under the actual conditions, the waves are
short and suffer the influence of shear currents only in the subsurface layer of the ocean. 相似文献
953.
A conceptual variant for constructing a computer database for the theory of wave processes in the World's Ocean is suggested.
Five basic model components have been singled out, namely, acoustic waves, surface waves, internal waves, gyroscopic waves,
and Rossby waves. The structure of each block is described. The main principle of organizing the databank consists in dividing
the entire variety of wave processes into categories and in generating a hierarchical system of models for each, category,
using the principle of transition from general to partial.
Translated by Vladimir A. Puchkin. 相似文献
954.
S. F. Dotsenko 《Physical Oceanography》1998,9(4):249-258
The paper analyses the transformation of tsunami-type solitary waves, propagating from the abyssal part of the Black Sea towards
its shelf zone. The study is performed by solving numerically unidimensional non-linear equations for non-dispersive long
waves, using the finite-difference slope and shelf, with the full wave reflection prescribed at a 10 m depth contour. The
non-linearity of the process is shown to throughly impact the reflection of waves by the shore and the shape of the reflected
wave. Tsunami wave heights have been seen to increase by several times in the Black sea shelf area.
Translated by Vladimir A. Puchkin. 相似文献
955.
On the southwestern Barents Sea shelf, sediments containing gas hydrates that overlie free gas have been inferred from multichannel
seismic data. The volume of suspected gas hydrate is tentatively estimated to about 1.9×108 m3. The gas hydrate zone probably formed from thermogenic gas leaking from a deeper source. The hydrate zone may have thickened
during the Neogene by including gas originally trapped as free gas below the hydrate following a significant downward migration
of the isotherms caused by erosion and/or subsidence. Within the present oceanographic conditions, gas hydrate is suspected
to be stable or slowly decomposing.
Received: 20 December 1996 / Revision received: 20 August 1997 相似文献
956.
This study experimentally investigates the nonlinear response stability and transition behaviour of a submerged, moored ocean structural system which consists of a spherical buoy and attached multi-point mooring lines. The system is excited by a periodic wave field in a closed channel. System nonlinearities include complex geometric restoring (stiffness) force and coupled fluid-system interaction exciting forces. Experimental set-up, operating procedures and analysis of the measured results are presented. Characteristic motions observed include harmonic, subharmonic and ultraharmonic responses, which demonstrate a signature of the intricate pattern of the nonlinear global behaviour. Good agreements between the measured and most predicted responses are demonstrated in both time and frequency domains. These results confirm the validity of the analytical model presented and calibrate the accuracy of the existing numerical predictions. Primary and secondary resonances in the response are identified via frequency response curves. Response bifurcation cascades are observed in the experimental results and the possible existence of higher-order nonlinear responses is inferred. 相似文献
957.
In this paper the probability of green water occurrence is investigated by taking into account the threshold of the vertical relative motion exceeding the freeboard. The number of wetting of the unit/vessel is predicted using probabilistic method. This paper compares the significant load, due to shipping of green water with the works of other researchers, and the loads are found to be close with the results presented in this paper. There is no direct relation between the velocities in the waves and the water velocity over the deck. The water velocities around the bow are heavily distributed by the presence of the bow. This scenario makes the flow very complex for schematic modelling. 相似文献
958.
The basic relations of the classical dyamic method have been complemented with the condition allowing for the non-monotonicity
of the vertical kinematic structure. The elements of the multi-layered system of geostrophic currents have been found to correlate
over depth with seawater density and hydrostatic pressure distribution. An example of the analysis of the vertical structure
of currents, involving specific hydrological data, is given.
Translated by Vladimir A. Puchkin. 相似文献
959.
Acoustic behavior of gas-bearing sediments is significantly different from that of gas-free sediments. In situ velocity profiles and acoustic signal characteristics in gas-bearing sediments of the upper several meters of the sea floor in Kiel Bay are presented in this study. Observed velocities in gas-bearing sediments are both higher and lower than those of the gas-free sediments. Small amounts of gas appear to cause signal reverberation without much attenuation. whereas large amounts of gas cause substantial attenuation. 相似文献
960.
Daniel S. Scheirer Ken C. Macdonald Donald W. Forsyth Stephen P. Miller Dawn J. Wright Marie-Hélène Cormier Charles M. Weiland 《Marine Geophysical Researches》1996,18(1):1-12
Four large-scale bathymetric maps of the Southern East Pacific Rise and its flanks between 15° S and 19° S display many of the unique features of this superfast spreading environment including abundant seamounts (the Rano Rahi Field), axial discontinuities, discontinuity migration, and abyssal hill variation. Along with a summary of the regional geology, these maps will provide a valuable reference for other sea-going programs on-and off-axis in this area, including the Mantle ELectromagnetic and Tomography (MELT) experiment. 相似文献