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81.
Øyvind Breivik Arthur A. Allen Christophe Maisondieu Jens-Christian Roth Bertrand Forest 《Ocean Dynamics》2012,62(5):741-752
The leeway of 20-ft containers in typical distress conditions is established through field experiments in a Norwegian fjord
and in open-ocean conditions off the coast of France with a wind speed ranging from calm to 14 m s−1. The experimental setup is described in detail, and certain recommendations were given for experiments on objects of this
size. The results are compared with the leeway of a scaled-down container before the full set of measured leeway characteristics
are compared with a semianalytical model of immersed containers. Our results are broadly consistent with the semianalytical
model, but the model is found to be sensitive to choice of drag coefficient and makes no estimate of the crosswind leeway
of containers. We extend the results from the semianalytical immersion model by extrapolating the observed leeway divergence
and estimates of the experimental uncertainty to various realistic immersion levels. The sensitivity of these leeway estimates
at different immersion levels are tested using a stochastic trajectory model. Search areas are found to be sensitive to the
exact immersion levels, the choice of drag coefficient, and somewhat less sensitive to the inclusion of leeway divergence.
We further compare the search areas, thus, found with a range of trajectories estimated using the semianalytical model with
only perturbations to the immersion level. We find that the search areas calculated without estimates of crosswind leeway
and its uncertainty will grossly underestimate the rate of expansion of the search areas. We recommend that stochastic trajectory
models of container drift should account for these uncertainties by generating search areas for different immersion levels
and with the uncertainties in crosswind and downwind leeway reported from our field experiments. 相似文献
82.
Inversion of inline and broadside marine controlled‐source electromagnetic data with constraints derived from seismic data
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Torgeir Wiik Janniche Irén Nordskag Eirik Øverland Dischler Anh Kiet Nguyen 《Geophysical Prospecting》2015,63(6):1371-1382
We present a structural smoothing regularization scheme in the context of inversion of marine controlled‐source electromagnetic data. The regularizing hypothesis is that the electrical parameters have a structure similar to that of the elastic parameters observed from seismic data. The regularization is split into three steps. First, we ensure that our inversion grid conforms with the geometry derived from seismic. Second, we use a seismic stratigraphic attribute to define a spatially varying regularization strength. Third, we use an indexing strategy on the inversion grid to define smoothing along the seismic geometry. Enforcing such regularization in the inversion will encourage an inversion result that is more intuitive for the interpreter to deal with. However, the interpreter should also be aware of the bias introduced by using seismic data for regularization. We illustrate the method using one synthetic example and one field data example. The results show how the regularization works and that it clearly enforces the structure derived from seismic data. From the field data example we find that the inversion result improves when the structural smoothing regularization is employed. Including the broadside data improves the inversion results even more, due to a better balancing between the sensitivities for the horizontal and vertical resistivities. 相似文献
83.
Sensitivity of simulated wintertime Arctic atmosphere to vertical resolution in the ARPEGE/IFS model
The current state-of-the-art general circulation models, including several of those used by the IPCC, show considerable biases
in the simulated present day high-latitude climate compared to observations and reanalysis data. These biases are most pronounced
during the winter season. We here employ ideal vertical profiles of temperature and wind from turbulence-resolving simulations
to perform a priori studies of the first-order eddy-viscosity closure scheme employed in the ARPEGE/IFS model. This reveals
that the coarse vertical resolution (31 layers) of the model cannot be expected to realistically resolve the Arctic stable
boundary layer. The curvature of the Arctic inversion and thus also the vertical turbulent-exchange processes cannot be reproduced
by the coarse vertical mesh employed. To investigate how turbulent vertical exchange processes in the Arctic boundary layer
are represented by the model parameterization, a simulation with high vertical resolution (90 layers in total) in the lower
troposphere is performed. Results from the model simulations are validated against data from the ERA-40 reanalysis. The dependence
of the surface air temperature on surface winds, surface energy fluxes, free atmosphere stability and boundary layer height
is investigated. The coarse-resolution run reveals considerable biases in these parameters, and in their physical relations
to surface air temperature. In the simulation with fine vertical resolution, these biases are clearly reduced. The physical
relation between governing parameters for the vertical turbulent-exchange processes improves in comparison with ERA-40 data. 相似文献
84.
M. D. Reed D. M. Terndrup R. Østensen S. Geier J. Gilker P. G. Beck P. Degroote J. Vanautgaerden C. Waelkens 《Astrophysics and Space Science》2010,328(1-2):83-86
During our campaign of acquiring follow-up photometric data to resolve short period pulsating sdB (EC14026 or V361 Hya) stars, we obtained data on the known pulsator KUV 04421+1416 and discovered that it is also in a reflection-effect binary. Here we present preliminary results of the pulsation analysis and provide some constraints on the companion, which is most likely an MV star. This makes KUV 04421+1416 only the second known system with an EC14026-type pulsator in a reflection-effect binary. 相似文献
85.
Sonja Schuh Roberto Silvotti Ronny Lutz Björn Loeptien Elizabeth M. Green Roy H. Østensen Silvio Leccia Seung-Lee Kim Gilles Fontaine Stéphane Charpinet Myriam Francœur Suzanna Randall Cristina Rodríguez-López Valerie van Grootel Andrew P. Odell Margit Paparó Zsófia Bognár Péter Pápics Thorsten Nagel Benjamin Beeck Markus Hundertmark Thorsten Stahn Stefan Dreizler Frederic V. Hessman Massimo Dall’Ora Dario Mancini Fausto Cortecchia Serena Benatti Riccardo Claudi Rimvydas Janulis 《Astrophysics and Space Science》2010,329(1-2):231-242
In 2007, a companion with planetary mass was found around the pulsating subdwarf B star V391 Pegasi with the timing method, indicating that a previously undiscovered population of substellar companions to apparently single subdwarf B stars might exist. Following this serendipitous discovery, the EXOTIME (http://www.na.astro.it/~silvotti/exotime/) monitoring program has been set up to follow the pulsations of a number of selected rapidly pulsating subdwarf B stars on time scales of several years with two immediate observational goals:
- determine $\dot{P}$ of the pulsational periods P
- search for signatures of substellar companions in O–C residuals due to periodic light travel time variations, which would be tracking the central star’s companion-induced wobble around the centre of mass
86.
87.
In connection with the construction of a tunnel collecting water beneath a glacier (Bondhusbreen/Folgefonni) in SW Norway the amount of sediments transported by meltwater has been investigated. According to the values obtained the volume of the sedimentation chamber which has to take a one-years-amount of sediment was fixed at 5000 m3. In 1978 there has been a sedimentation of 3000 m3 of coarse material. The results obtained are not only of practical value, but also of scientific interest. 相似文献
88.
Christian Christiansen Henning Christoffersen JØrgen Dalsgaard Per NØrnberg 《Sedimentary Geology》1981,28(3):163-173
The die-back of eel-grass (Zostera marina, L.) is found to have played an important role with regard to near-shore sedimentation and coastal changes.In a natural harbour at Kyholm, Denmark a hiatus is found between silty sediments that date from about 4000 BC and overlying modern sandy sediments. It is suggested that this is a consequence of the die-back of eel-grass in the nineteen-thirties, resulting in mobilisation and disturbance of nearshore sediments and the shoreward movement of mobilised sandy material into the harbour. The coastal morphology of Kyholm was relatively stable from 1802 to 1933, but between 1933 and 1978 there have been two periods of drastic progradation correlated with die-back of eel-grass. 相似文献
89.
øystein Hov Asgeir Sorteberg Norbert Schmidbauer Sverre Solberg Frode Stordal David Simpson Anne Lindskog Hans Areskoug Pedro Oyola Heikki Lättilä Niels Z. Heidam 《Journal of Atmospheric Chemistry》1997,28(1-3):173-193
Observations and model calculations of the concentration of hydrocarbonsat five Scandinavian rural sites during March–June 1993are reported.Decreasing concentrations from March to June are observedat all sites. The highest concentrations of hydrocarbons were found in air massescoming in from the southwest to southeast, indicating that long rangetransport fromcontinental Europe and the U.K. is important in pollution episodes. An episode of elevated concentrations of hydrocarbons observed at three of the sites in the middle of Marchis described and discussed in relation to the synoptic situation and thepresenceof other chemical compounds (NO2, PAN, total nitrate andozone).A Lagrangian numerical model is used to calculate the concentrations of theindividual hydrocarbons at the fivesites and comparison with observations is made.The calculated concentrations for nonmethane hydrocarbons with quite longchemicallifetimes agree well with the observations.For the sum of observed and calculated hydrocarbons the correlationcoefficientsare in the range of 0.65–0.88 for the five sitesand the ratio between calculated and measured concentrations was0.72–0.97, indicating thatthe European VOC emission inventory is quite well estimated. 相似文献
90.
Several years of continuous measurements of surfaceozone at Norwegian monitoring sites are studied in aclimatological way. The monitoring sites are at rurallocations extending from 58°N, a few hundredkilometers from the European continent and into theArctic at 79°N. The ozone observations are sorted intoclasses of integrated NOx emissions along 96 h backtrajectories. The average seasonal cycles of ozone areestimated for each class separately. The differencesindicate the change from the background air due toanthropogenic emissions. The average seasonal cycle ofozone in the cleanest air masses showed a maximum inspring and a minimum during summer and autumn at allsites, but the spring maximum was more pronounced atthe southernmost locations. Polluted air masses showedan ozone deficit during winter and a surplus duringsummer. The deviation from the background was clearlylinked to the integrated NOx emission along thetrajectories. In summer the calculations indicate thatthe number of ozone molecules formed per NOx moleculedrops with increasing emissions. The average seasonalcycle of ozone at Birkenes for different transportsectors indicate that the most pronounced ozoneformation takes place in air masses from E-Europe/Russia. 相似文献