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71.
The diurnal structure of the boundary layer during Indian summer monsoon period is studied using a one-dimensional meteorological
boundary layer model and the observations collected from the Monsoon Trough Boundary Layer Experiment conducted in 1990 at
Jodhpur, India. The model was initialized with the observed temperature profiles at 0530 LST on 17 July, 1990 at Jodhpur and
was run for 26 hours. The study is carried out with a geostrophic wind speed of 9.5 m s−1 corresponding to the strong wind simulation. The mean thermodynamic and wind structure simulated by the model are in good
agreement with those observed from 30 m tower. The computed surface layer characteristics such as the surface fluxes, TKE
and standard deviations of velocity components are found to be reasonably in good agreement with those based on turbulence
measurements. The shear and buoyancy budget computed from the model are also compared with the turbulence measurements. The
integrated cooling budget in the nocturnal boundary layer is examined. 相似文献
72.
J. Morales A. Goguitchaichvili J. Urrutia-Fucugauchi 《Studia Geophysica et Geodaetica》2007,51(2):315-326
Cooling rate (CR) effects on the intensity of thermoremanent magnetization has been documented for archaeomagnetic materials,
where cooling in laboratory conditions is generally much faster compared to natural cooling rates. Since the latter condition
also applies to many volcanic rocks, we have investigated in this study the influences of the CR on the determination of absolute
paleointensity using recent basaltic rocks. We used magnetically and thermally stable samples mainly containing Ti-poor pseudo-singledomain
titanomagnetites (the most widely used material for Thellier paleointensity experiments). These samples previously succeed
in retrieving the strength of laboratory field intensities with the Coe’s version of the Thellier method in a simulated paleointensity
experiment using similar cooling rates. Our experimental results indicate that the cooling rate effects produce systematic
and significant overestimates of the absolute intensity up to 70%. The effect can be much larger than predicted by Neél theory
for non-interacting single-domain grains. 相似文献
73.
山西省雾的分析和预报 总被引:7,自引:0,他引:7
公路为山西省经济发展做出巨大的贡献。为保证公路安全畅通,本文对影响公路安全行驶的重要天气--雾的地理和时间分布进行分析,并根据雾的发生条件,提出了雾的预报思路。 相似文献
74.
This paper analyses geographical trends in relative poverty in England and Wales over the last century by comparing key quantitative indicators from key dates. The comparison is made possible by interpolating all the datasets onto a single standardized geography. Results suggest rising inequality in spite of the decline in absolute poverty. 相似文献
75.
西部大开发中的农业结构调整思考 总被引:2,自引:2,他引:2
西部地区的农业发展直接影响到我国国民经济是否能够持续快速健康的发展,这是由于我国是农业大国,农业人口大约占全国人口比例的80%,而实现西部地区持续健康发展的关键在于对传统农业产业结构的调整,提高农业增长的结构变动效益,树立大农业观念,延长农业产业链,在联产承包责任制的基础上通过经营权的集中规模种植,达到实现农业结构调整生态化和产业一体化目标。西部地区在大开发战略实施中,如何将自身的发展环境劣势转变为优势,提出了农业结构调整模式的构想。 相似文献
76.
TU Xia ZHENG Fan Wang Jiliang CAI Huimei WANG Pinxian C.Bühring M.Sarnthein 《中国科学D辑(英文版)》2001,44(10):865-870
The high-resolution quantitative analysis of the planktonic foraminifera and the δ18O records of the section between 96.49– 137.6 mcd at ODP Site 1144 on the continental slope of northern South China Sea reveals
an abrupt cooling event of sea surface temperature (SST) during the last interglacial (MIS 5.5, i.e. 5e). The dropping range
of the winter SST may come to 7.5°C corresponding to 1.2‰ of the δ18O value of sea surface water. This event is comparable with those discovered in the west Europe and the northern Atlantic
Ocean, but expressed in a more intensive way. It is inferred that this event may have been induced by middle- to low-latitude
processes rather than by polar ice sheet change. Since the Kuroshio-index speciesPulleniatina obliquiloculata displayed the most distinct change at the event, it may also be related to the paleoceanographic change of the low-latitude
area in the western Pacific Ocean. This event can be considered as one of “Younger Dryas-style coolings” and is indicative
of climate variability of the last interglacial stage. 相似文献
77.
Variations in chemical compositions of the eolian dust in Chinese Loess Plateau over the past 2.5 Ma and chemical weathering in the Asian inland 总被引:5,自引:0,他引:5
Major and trace elements as well as strontium isotopic composition have been analyzed on the acid-insoluble (AI) phase of
the loess-paleosol sequence from Luochuan, Shaanxi Province, China. Results show that the chemical composition of AI phase
of loess and paleosols is distinctive to the average composition of upper continental crust (UCC), characterized by depletion
of mobile elements Na, Ca and Sr. The distribution pattern of elements in AI phase reveals that initial dust, derived from
a vast area of Asian inland, has suffered from Na- and Ca-removed chemical weathering compared to UCC. Some geochemical parameters
(such as CIA values, Na/K, Rb/Sr and87Sr/86Sr ratios) display a regular variation and evolution, reflecting that the chemical weathering in the source region of loess
deposits has decreased gradually since 2.5 Ma with the general increase of global ice volume. This coincidence reflects that
the aridity of Asian inland since the Quaternary is a possible regional response to the global climate change. 相似文献
78.
Zhao Wenyu Center of Material Research Analysis Wuhan University of Technology Wuhan Liu Rong Wang QinyanFaculty of Earth Sciences China University of Geosciences Wuhan Peng Changqi Zhang QingjieCenter of Material Research Anal 《中国地质大学学报(英文版)》2001,12(3)
INTRODUCTIONItisanacknowledgedfactthataragonite,ahigh pressurepolymorphofCaCO3 ,occurswidelyasanindexmineralofhigh pressureandlow temperaturemetamorphism (glaucophaneschistfacies)withinthegeodynamiccontextofsubduction obductionandcontinentalcollision (Liou… 相似文献
79.
The classic two-level or equivalent two-level model that includes only the statistical equilibriumof radiative and thermal processes of excitation and quenching between two vibrational energy levelsis extended by adding chemical production to the rate equations. The modifications to the non-localthermodynamic equilibrium source function and cooling rate are parameterized by φc, which characterizesthe ratio of chemical production to collisional quenching. For applications of broadband emission of O3 at9.6 μm, the non-LTE effect of chemical production on the cooling rate and limb emission is proportionalto the ratio of O to O3. For a typical [O]/[O3], the maximum enhancements of limb radiance and coolingrate are about 15%-30% and 0.03-0.05 K day-1, respectively, both occurring near the mesopause regions.This suggests that the broadband limb radiance above ~80 km is sensitive to O3 density but not sensitiveto the direct cooling rate along the line-of-sight, which makes O3 retrieval feasible but the direct coolingrate retrieval difficult by using the O3 9.6 μm band limb emission. 相似文献
80.
1. IntroductionInvestigations about atmospheric LFW have been a focus of research since Madden andJulian/s outstanding analysis works (1971, 1972). Many dynamical and thermal mechanisms(Chao et al., 1996; Fu et al., 1998; Hendon et al., 1998; Krishnamurti et al., 1988; Lau andChan, 1988) have been advised to explain LFW. Among them are oceanic effects, such as SSTeffect, thermal forcing and others. Usually atmosphere and ocean are taken as a coupled system, which is used to explain ENS… 相似文献