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11.
The solution of the linear Molodensky problem by analytical continuation to point level is numerically the most convenient
of all the theoretically equivalent solutions. It is obtained by successively applying the same integral operator and it does
not depend explicitly on the terrain inclination. However, its dependence on the computation point restricts somehow the computational
efficiency. The use of the Fourier transform for the evaluation of the integral operator in planar approximation lessens significantly
the burden of computations. Using this spectral approach, the problem has been reformulated and solved in the frequency domain.
Moreover, it is shown that the solution can be easily split into two steps: (a) “downward” continuation to sea level, which
is independent of the computation point, and (b) “upward” continuation from sea to point level, using the values computed
at sea level. Such a treatment not only simplifies the formulas and increases the numerical efficiency but also clarifies
the physical interpretation and the theoretical equivalence of the continuation solution with respect to the other solution
types. Numerical tests have been performed to investigate which terms in the Molodensky series are of significance for geoid
and deflection computations. The practical difficulty of differences in the grid spacings of gravity and height data has been
overcome by frequency domain interpolation.
Presented at theXIX IUGG General Assembly, Vancouver, B.C., August 9–22, 1987. 相似文献
12.
K. P. Schwarz 《Journal of Geodesy》1985,59(1):33-54
The outpout of inertial survey systems is available to the user in two basic forms: as Kalman filtered information at updates or as integrated velocity and position information at regular time intervals. In case of the second data type, the post-mission processing starts with the approximation of the velocity error curve. This approximation is either based on a system error model as in Kalman filtering or uses curve fitting techniques. From there on, smoothing or adjustment procedures are used as further steps in the post-mission treatment of both data types. A unified treatment of the various post-mission approaches starts with the formulation of appropriate error models of the system outputs. It is then possible to present all existing methods as intermediate steps of a rigorous adjustment procedure. This unified approach gives insight into the limitations of individual methods and provides a means to detect inconsistencies in post-mission processing strategies. An analysis of existing approaches is made and a new method, spectral decomposition, is treated in detail. Compared to the existing procedures, it has advantages with respect to a rigorous covariance propagation and blunder detection. 相似文献
13.
14.
Charles R. Schwarz 《Journal of Geodesy》1982,56(2):165-176
There are many data base management systems now available as commercially marketed software packages. Although most of these
packages were initially aimed at bussiness or administrative data processing applications, they may frequently also be the
right tool for a scientific data processing task. This becomes more apparent as we notice that scientific computer programmers
are spending more and more time on data management requirements rather than the coding of mathematical algorithms.
In a scientific environment, a generalized data base management package is best viewed as a tool for programmers, rather than
as a tool for direct, independent use by end users or by agency management. To the end user, the most attractive feature of
a commerical DBMS is usually the interactive retrieval and update language. To the programmer, the most attractive feature
is more likely to be the strong support for various types of keyed access. All of the manipulations necessary to build and
maintain indices and other tables can be treated as procedural abstractions. Coupled with a procedural language, a DBMS offers
the programmer a higher level (in the sense of more abstract) language. The most important geodetic requirement on a commercial
DBMS is therefore that the package contain a strong Data Manipulation Language, with strong support for the algorithmic language
used for scientific processing.
Presented at International Symposium on Management of Geodetic Data, Copenhagen, August 24–26, 1981. 相似文献
15.
Although airborne gravimetry is now considered a fully operational technique, errors due to motion compensation using differential
GPS (DGPS) continue to influence both its accuracy and the range of applications in which it can be used. In typical medium-resolution
applications such as airborne geoid mapping, errors due to DGPS contribute considerably to the error budget of an airborne
gravity system. At the same time, efforts to increase the resolution of such systems for demanding applications such as resource
exploration remain impedded by errors in DGPS.
This article has three objectives. The first one is to compare eight industrially relevant DGPS software packages for the
determination of aircraft acceleration. The second objective is to analyze and quantify the effect that each relevant portion
of the DGPS error budget has on the determination of acceleration. Using data sets that represent a wide range of operational
conditions, this is done in the frequency domain over a range of frequencies corresponding to spatial resolution as high as
450 m. The third objective is to use that information to recommend and demonstrate approaches that optimize the estimation
of aircraft acceleration for determining the geoid and for resource exploration.
It is shown, for example, that the time of day in which the survey is carried out and the dynamic characteristics of the aircraft
being used are two of the most crucial parameters for very high-resolution gravity field estimation. It is demonstrated that
when following the above-mentioned recommendations, agreements with ground daa of better than 1.5 and 2.5 mGal can be achieved
for spatial resolutions (half-wavelengths) of 2.0 and 1.4 km, respectively. ? 2002 Wiley Periodicals, Inc. 相似文献
16.
The electronic structure of the three polymorphs of Al2SiO5, andalusite, sillimanite, and kyanite, is studied by linearized-augmented-plane-wave (LAPW) calculations using the WIEN code.
Total energy calculations verify, in agreement with recent pseudopotential calculations, that andalusite is the most stable
phase, followed by sillimanite and kyanite.We determine the electronic charge density distribution and find strong polarizations
on all oxygen ions. We identify different polarizations due to Al or Si neighbors which depend on their respective distances
to the oxygen atom. The chemical bonding is not purely ionic in nature but has important covalent contributions. Electric
field gradients (EFGs) at all sites are calculated and agree well (within 10%) with available experimental data on Al. We
identify the origin of the EFGs and demonstrate its relation to the nearest-neighbor coordination and the resulting anisotropy
of the electronic charge distribution.
Received: 22 March 2000 / Accepted: 3 August 2000 相似文献
17.
Geos I observations made at thirty optical and four Secor stations were analyzed in the geometric and short-arc modes for
the purpose of detecting systematic distortions in the North American Datum. The results indicate that the Nad at its origin
(Meades Ranch, Kansas) requires an easterly rotation in azimuth and a westerly rotation in the prime vertical plane, both
in the magnitude of one second of arc to fit the satellite data. There is also evidence of the need for a reduction in scale
of about 1:200.000. 相似文献
18.
Satellite gravity missions, such as CHAMP, GRACE and GOCE, and airborne gravity campaigns in areas without ground gravity will enhance the present knowledge of the Earths gravity field. Combining the new gravity information with the existing marine and ground gravity anomalies is a major task for which the mathematical tools have to be developed. In one way or another they will be based on the spectral information available for gravity data and noise. The integration of the additional gravity information from satellite and airborne campaigns with existing data has not been studied in sufficient detail and a number of open questions remain. A strategy for the combination of satellite, airborne and ground measurements is presented. It is based on ideas independently introduced by Sjöberg and Wenzel in the early 1980s and has been modified by using a quasi-deterministic approach for the determination of the weighting functions. In addition, the original approach of Sjöberg and Wenzel is extended to more than two measurement types, combining the Meissl scheme with the least-squares spectral combination. Satellite (or geopotential) harmonics, ground gravity anomalies and airborne gravity disturbances are used as measurement types, but other combinations are possible. Different error characteristics and measurement-type combinations and their impact on the final solution are studied. Using simulated data, the results show a geoid accuracy in the centimeter range for a local test area. 相似文献
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