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951.
Numerical investigation of Hurricane Gilbert (1988) effect on the Loop Current warm core eddy (WCE) in the Gulf of Mexico
is performed using the Modular Ocean Model version 2 (MOM2). Results show that the storm-induced maximum sea surface temperature
(SST) decrease in Gilbert’s wake is over 2.5°C, as compared with the 3.5°C cooling in the absence of the WCE. The near-inertial
oscillation in the wake reduces significantly in an along-track direction with the presence of the WCE. This effect is also
reflected between the mixed layer and the thermocline, where the current directions are reversed with the upper layer. After
two inertial periods (IP), the current reversal is much less obvious. In addition, it is demonstrated that Hurricane Gilbert
wind stress increases the current speed of the WCE by approximate 133%. With the forcing of Gilbert, the simulated translation
direction and speed of the WCE towards the Mexican coast are closer to the observed (42% more accurate in distance and 78%
more accurate in direction) compared with the simulation without the Gilbert forcing. The simulated ocean response to Gilbert
generally agrees with the recent observations in Hurricane Fabian. 相似文献
952.
Gravity data are the results of gravity force field interaction from all the underground sources. The objects of detection
are always submerged in the background field, and thus one of the crucial problems for gravity data interpretation is how
to improve the resolution of observed information. The wavelet transform operator has recently been introduced into the domain
fields both as a filter and as a powerful source analysis tool. This paper studied the effects of improving resolution of
gravity data with wavelet analysis and spectral method, and revealed the geometric characteristics of density heterogeneities
described by simple shaped sources. First, the basic theory of the multiscale wavelet analysis and its lifting scheme and
spectral method were introduced. With the experimental study on forward simulation of anomalies given by the superposition
of six objects and measured data in Songliao plain, Northeast China, the shape, size and depth of the buried objects were
estimated in the study. Also, the results were compared with those obtained by conventional techniques, which demonstrated
that this method greatly improves the resolution of gravity anomalies.
Translated from Progress in Geophysics, 2007, 22(1): 112–120 [译自: 地球物理学进展] 相似文献
953.
Chin‐Hsiung Loh Jerome P. Lynch Kung‐Chun Lu Yang Wang Chia‐Ming Chang Pei‐Yang Lin Ting‐Hei Yeh 《地震工程与结构动力学》2007,36(10):1303-1328
The performance aspects of a wireless ‘active’ sensor, including the reliability of the wireless communication channel for real‐time data delivery and its application to feedback structural control, are explored in this study. First, the control of magnetorheological (MR) dampers using wireless sensors is examined. Second, the application of the MR‐damper to actively control a half‐scale three‐storey steel building excited at its base by shaking table is studied using a wireless control system assembled from wireless active sensors. With an MR damper installed on each floor (three dampers total), structural responses during seismic excitation are measured by the system's wireless active sensors and wirelessly communicated to each other; upon receipt of response data, the wireless sensor interfaced to each MR damper calculates a desired control action using an LQG controller implemented in the wireless sensor's computational core. In this system, the wireless active sensor is responsible for the reception of response data, determination of optimal control forces, and the issuing of command signals to the MR damper. Various control solutions are formulated in this study and embedded in the wireless control system including centralized and decentralized control algorithms. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献
954.
A structural mode was used to characterize vegetation composition at the plant leaf level and a flourishing-withering ratio was developed. The spectral responses of vegetation with different flourishing-withering ratios were analyzed, the change rates of the chlorophyll and moisture content indices of vegetation with different flourishing-withering ratios were compared, and correlations between the chlorophyll and moisture content indices were analyzed. The results reveal that leaves with an intermediate flourishing-withering ratio can increase the absorption signatures of vegetation and that band ranges of 570–700 nm and 1300–1540 nm can play a role in indicating changes in the flourishing-withering ratios of vegetation; NPQI, NPCI, R695/R420, R695/R760, R750/R700, the peak-value area of red selvedge, the red selvedge amplitude, the ratio between the red selvedge amplitude and the minimum amplitude, and the NDVI of vegetation change regularly with the change in flourishing-withering ratios, and these nine vegetation indices are highly related to the chlorophyll content. Vegetation indexes of NDWI and PRI are very sensitive to the flourishing-withering change in vegetation and are closely related to the moisture content, and the correlation coefficient is higher than 0.9. The derivative of the spectra is more effective in describing changes in the structural mode of vegetation with different flourishing-withering ratios, especially at band ranges of 552–628 nm and 630–686 nm, and it is more sensitive to the mixed flourishing-withering ratios of leaves rather than to the vegetation indices. The red selvedge position in the spectrum is highly related to the chlorophyll content and is not sensitive to changes in the structural mode of mixed flourishing-withering leaves. The red selvedge parameters are sensitive to changes in the flourishing-withering ratio at the peak-value area of the red selvedge amplitude and the ratio between the red selvedge amplitude and the minimum amplitude. The effect of a sand background on the spectrum of withering leaves is higher than that of flourishing leaves; the effect of a sand background increases with increasing proportions of withering leaves, the superposition effect of the sand background on mixed flourishing-withering leaves is about 7% at visible light bands of 400–700 nm and 1300–1540 nm, and is over 10% at the near infrared band range of 700–1300 nm. 相似文献
955.
956.
This paper presents an optimal regulation programme, grey fuzzy stochastic dynamic programming (GFSDP), for reservoir operation. It is composed of a grey system, fuzzy theory and dynamic programming. The grey system represents data by covering the whole range without loss of generality, and the fuzzy arithmetic takes charge of the rules of reservoir operation. The GFSDP deals with the multipurpose decision‐making problem by fuzzy optimization theorem. The practicability and effectiveness of the proposed approach is tested on the operation of the Shiman reservoir in Taiwan. The current M5 operating rule curves of this reservoir also are evaluated. The simulation results demonstrate that this new approach, in comparison with the M5 rule curves, has superior performance with regard to the total water deficit and number of monthly deficits. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
957.
In this note the significance of heat of hydration and electronegativity in the study of oceanic residence times of elements is discussed. 相似文献
958.
An analysis is made to calculate input impedance of a loop antenna for radiation of the VLF whistler mode in the magnetosphere. The magnetosphere is assumed to be represented by a cold, uniform and collisionless magnetoplasma medium. Assuming a uniform current distribution of a circular loop, oriented at an arbitrary angle with respect to the Earth's magnetic field line, several closed-form expressions for the loop impedance have been derived. It is found that the loop input reactance is in substantial agreement with the self-inductance of a loop in free space and that the radiation resistance for a small loop can be as large as ~10 2 Ω. It is also found that a second order quasi-static theory is quite valid for determining the input impedance for small loops radiating VLF whistlers in the magnetosphere. 相似文献
959.
960.