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91.
A model of a multivariate covariance function with an ellipsoidal directional correlation scale has been developed. The axes of the ellipsoidal scale are related to the eigenvalues and eigenvectors of a matrix B which characterizes the ellipsoid of the range of influence. The matrix B is found to be related to a matrix T which can be estimated directly from sparse sampling data and can be used to determine estimates of the matrix B. The method has been applied to both two-dimensional and three-dimensional cases. The numerical results show that the satisfactory accuracy is obtained with sparse sampling data from an anisotropic random function. 相似文献
92.
We have theoretically considered the problem of interpretation of nutrient profiles in the upper ocean (100–2000m). We compare
the experimental depth profiles of nonconservative tracers, both stable and radioactive, with solutions of one-dimensional
steady state transport equations of increasing complexity including situations not encountered in the real oceans. Apart from
gaining insight into the nutrient transport processes, this analysis is useful in offering a way to obtain operational estimates
of depth dependent/independent eddy diffusivity and dissolution fluxes in the ocean. These parameters are essential for estimating
new production, total production and burial of carbon in the sediments. 相似文献
93.
根据严格的数学推演给出涡流地震检波器电压的频率响应特性、阻尼因数、位相等的正确公式;定义表征其某些基本特征的物理量;讨论了文献[1]中某些严重错误,简介了我们研制的新型涡流地震检波器的某些性能。 相似文献
94.
大地测量相关观测抗差估计理论 总被引:21,自引:4,他引:21
相关观测异常诊断、质量控制是测量数据处理领域亟待解决的难题之一。分别从方差膨胀模型和相关权元素压缩模型入手研究了相关观测的质量控制理论和方法;给出了误差影响函数;构造了方差膨胀函数和权因子收缩函数;利用观测量的等价协方差阵和等价权矩阵讨论了相关观测质量控制的计算方法。该等价协方差矩阵和等价权矩阵不仅保持了原有协方差矩阵和权矩阵的对称性,而且保持了原有协方差矩阵的相关性不变。计算结果表明异常观测的方差膨胀法和等价权法能有效地控制异常观测对参数估值的影响。 相似文献
95.
96.
97.
Katja Fennel 《Ocean Dynamics》2001,52(2):58-70
Elken et al. (1994) suggested that phytoplankton patchiness can be generated by mesoscale eddies in light-limited, nutrient-replete
environments. This hypothesis is explored using two ecological models of different physical complexity. The model results
support the idea that the coupling of mesoscale eddy circulation and phytoplankton growth leads to differential growth rates
and thus generates variability in phytoplankton distributions. The specific circulation of a cyclonic eddy isolates a phytoplankton
population in its core. Due to the reduced vertical mixing, a higher growth rate is supported in the core, and phytoplankton
concentrations increase compared to the surrounding environment. A one-dimensional model is used to explore the hypothesis
in general and to perform sensitivity studies. A more realistic simulation uses a coupled three- dimensional model for the
western Baltic Sea. Starting from vertically and horizontally homogeneous distributions for nutrients and plankton, the models
generate patchiness due to the proposed mechanism. The described mechanism may apply for other mesoscale variable environments
during light-limited growth periods as well, e.g., the frontal region of the Southern Ocean.
Received: 31 March 2001 / Accepted: 31 August 2001 相似文献
98.
Hans Güsten Günther Heinrich Ralf W. H. Schmidt Ulrich Schurath 《Journal of Atmospheric Chemistry》1992,14(1-4):73-84
A small, lightweight (1.5 kg) and fast-response ozone sensor for direct eddy flux measurements has been built. The basis for detection is the chemiluminescence of an organic dye adsorbed on dry silica gel in the reaction with ozone. The chemiluminescence is monitored with a cheap and small blue-sensitive photomultiplier. At a flow rate of 100 l min-1 the ozone sensor has a 90% response time of significantly better than 0.1 s with a detection limit lower than 50 ppt at S/N=3. There are no interferences from other atmospheric trace gases like NOx, H2O2 and PAN. Water vapour and SO2 enhance the chemiluminescence efficiency of the ozone sensor. Since their response times are 22 seconds and 30 minutes, respectively, no correlation between rapid ozone fluctuations and those of these two trace gases is noticed by the ozone sensor when operating at a frequency of 10 Hz.The ozone sensor was tested for several weeks in continuous measurements of ozone fluxes and deposition velocities over different croplands using the eddy correlation technique. Good agreement was found between ozone dry deposition velocities derived from profile measurements and by eddy correlation. 相似文献
99.
花岗岩的成岩作用和形成环境——存在的问题和解决的途径 总被引:3,自引:0,他引:3
本文针对当前花岗岩研究中存在的一些问题,结合笔者等近年来的工作,概述了进一步研究花岗岩成岩作用和形成环境的新思路。主要包括:(1)利用成分协变图,结合岩石包体成因类型的认识,探讨花岗岩化学演化进程;(2)在全面考察花岗岩的构造样式、岩石组合、岩浆演化和区域地壳不均一性基础上,分析花岗岩形成的构造背景。 相似文献
100.
In the estimation of momentum fluxes over land surfaces by the bulk aerodynamic method, no unique value of the drag coefficient
(C
D) is found in the literature. The drag coefficient is generally estimated from special observations at different parts of
the world. In this study an attempt is made to estimate drag coefficient over the western desert sector of India using data
sets of Monsoon Trough Boundary Layer Experiment (MONTBLEX) during the summer monsoon season of 1990. For this purpose, the
fast and slow response data sets obtained simultaneously from a 30 m high micro-meteorological tower at Jodhpur are used.
All the observations used in this study are confined to a wind speed regime of 2.5–9.0 ms−1.
A comparison of momentum fluxes computed by eddy correlation (direct estimation) with profile and bulk aerodynamic (C
D = 3.9 × 10−3, Garratt, 1977) methods revealed that though the nature of variation of the fluxes by all these methods is almost similar,
both the indirect methods give an under-estimated value of the fluxes. The drag coefficient is estimated as a function of
wind speed and surface stability by a multiple regression approach. An average value of the estimated drag coefficient is
found to be of the order of 5.43 × 10−3. The estimated value ofC
D is validated with a set of independent observations and found to be quite satisfactory. The recomputed momentum fluxes by
bulk aerodynamic method using the estimated drag coefficient are in close agreement with the directly estimated fluxes. 相似文献