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Robert Balk 《International Journal of Earth Sciences》1953,41(1):90-103
English summary Near the eastern base of the Taconic Range, in extreme southwestern Vermont, a complex of chlorite slate is exposed in the position of the floor of a thrust along which a mass of dolomite-limestone has been pushed from the east against, and over, the slate. In addition to the common structure, exhibiting westward-overturned open folds, with slip cleavage dipping eastward, about parallel with the axial pianos, the slate displays a number of subsidiary shears or thrust zones having the same orientation as the principal thrust. In these zones, a strong lineation as well as axes of small folds plunge E—SE, parallel with the direction of propagation of the thrust blocks. The origin of the lineation and lamination is believed to be identical with that of corresponding structures in rolled steel and glass.However, the formation of folds with axes parallel to the direction of thrust requires an additional shear stress acting perpendicularly to the direction of thrusting. The inhomogeneous composition, strength, and mobility of the flooring rocks are pointed out, and it is suggested that unequal rates of yielding of local rock masses below the thrust block generated these supplementary stresses, producing slight movements of small masses sideways. That this is a reasonable explantation is shown by experiments on salt dome structure byEscher andKuenen, in which also axes of folds and lineation parallel with the direction of maximum forward propagation were produced. 相似文献
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Ohne Zusammenfassung 相似文献
997.
H. R. B. Hack 《Theoretical and Applied Climatology》1961,11(1):60-69
Summary Solar radiation intensity has been recorded on a single trace strip chart potentiometer and integrated automatically. The integral can be printed at frequencies from minutes to hours as required. The performance of the integration equipment has been assessed by (1) comparing chart area expected from a calibration of the printed digital output with the area as measured by planimeter and (2) estimating the scatter in the relation of chart area to printed output per hour on a number of days over periods up to a month. The errors (95% limits) are about ±1 cal cm–2 for hourly values and ±4 cal cm–2 for daily values.
With 4 Figures 相似文献
Zusammenfassung Die Intensität der Sonnenstrahlung wurde mit einem selbstabgleichenden Millivoltschreiber registriert und automatisch integriert. Das Integral kann nach Bedarf über Zeiten von der Größenordnung von Minuten bis Stunden gebildet werden. Die Leistungsfähigkeit des Integrators wurde abgeschätzt 1. durch Vergleich der auf Grund der Eichung des Integrators aus seinen Angaben errechneten Fläche unter der Registrierkurve mit der planimetrierten Fläche und 2. durch Abschätzung der Streuung der Werte des Zusammenhanges zwischen den pro Stunde angegebenen Integratorwerten und der Fläche auf dem Registrierstreifen an einer Anzahl von Tagen aus Perioden von einer Dauer bis zu einem Monat. Der Fehler (bei einer Genauigkeitsgrenze von 95%) liegt bet ±1 cal cm–2 für Stundensummen und bei ±4 cal cm–2 für Tagessummen.
Résumé L'intensité du rayonnement solaire fut enregistrée par un millivoltmètre compensateur et intégrée automatiquement. L'intégration peut s'étendre à des temps allant de la minute à plusieurs heures. L'exactitude de l'intégrateur fut estimée 1) en comparant la surface résultant de ses indications à celle que l'on planimètre, et 2) en calculant la dispersion des écarts entre les valeurs données par heure par l'intégrateur et celles qui résultent de la planimétrie, cela pour un certain nombre de jours choisis dans des périodes pouvant atteindre le mois. L'erreur (pour un domaine de validité de 95%) est de ±1 cal cm–2 pour des sommations horaires, de ±4 cal cm–2 pour des sommations diurnes.
With 4 Figures 相似文献
998.
Zhenglong LI Jun LI Pei WANG Agnes LIM Jinlong LI Timothy J.SCHMIT Robert ATLAS Sid-Ahmed BOUKABARA Ross N.HOFFMAN 《大气科学进展》2018,35(10):1217-1230
Accurate atmospheric temperature and moisture information with high temporal/spatial resolutions are two of the key parameters needed in regional numerical weather prediction(NWP) models to reliably predict high-impact weather events such as local severe storms(LSSs). High spectral resolution or hyperspectral infrared(HIR) sounders from geostationary orbit(GEO) provide an unprecedented source of near time-continuous, three-dimensional information on the dynamic and thermodynamic atmospheric fields—an important benefit for nowcasting and NWP-based forecasting. In order to demonstrate the value of GEO HIR sounder radiances on LSS forecasts, a quick regional OSSE(Observing System Simulation Experiment)framework has been developed, including high-resolution nature run generation, synthetic observation simulation and validation, and impact study on LSS forecasts. Results show that, on top of the existing LEO(low earth orbit) sounders, a GEO HIR sounder may provide value-added impact [a reduction of 3.56% in normalized root-mean-square difference(RMSD)] on LSS forecasts due to large spatial coverage and high temporal resolution, even though the data are assimilated every 6 h with a thinning of 60 km. Additionally, more frequent assimilations and smaller thinning distances allow more observations to be assimilated, and may further increase the positive impact from a GEO HIR sounder. On the other hand, with denser and more frequent observations assimilated, it becomes more difficult to handle the spatial error correlation in observations and gravity waves due to the limitations of current assimilation and forecast systems(such as a static background error covariance). The peak reduction of 4.6% in normalized RMSD is found when observations are assimilated every 3 h with a thinning distance of 30 km. 相似文献
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Sami Eria Robert B. McMaster 《International journal of geographical information science》2017,31(5):884-906
Despite myriad studies having been carried out on the diffusion of geographical information systems (GIS) technology, only a limited number have been done within the context of developing countries. This paper addresses the research question, how did the diffusion of GIS technology occur in Uganda? Mixed methods were used for data collection, and analysis was performed using a theoretical framework called the diffusion of innovations (DOI). The results of the study showed that the adoption of GIS by institutions in Uganda occurred in a classic diffusion pattern consistent with diffusion theory. Adoption of GIS was promoted by its relative advantage over, and compatibility with, existing technologies. It was characterized by both heterophilous and homophilous communication channels, and influenced by change agents and champions. Its rate of adoption followed an S-shaped diffusion curve, and was hampered by bureaucracy, and patronage-based societal norms. This study makes a contribution to literature on GIS diffusion in developing countries. 相似文献