全文获取类型
收费全文 | 66296篇 |
免费 | 1122篇 |
国内免费 | 493篇 |
专业分类
测绘学 | 1634篇 |
大气科学 | 5286篇 |
地球物理 | 13749篇 |
地质学 | 21441篇 |
海洋学 | 5727篇 |
天文学 | 15225篇 |
综合类 | 134篇 |
自然地理 | 4715篇 |
出版年
2020年 | 473篇 |
2019年 | 495篇 |
2018年 | 935篇 |
2017年 | 920篇 |
2016年 | 1366篇 |
2015年 | 1012篇 |
2014年 | 1416篇 |
2013年 | 3244篇 |
2012年 | 1491篇 |
2011年 | 2276篇 |
2010年 | 1945篇 |
2009年 | 2920篇 |
2008年 | 2660篇 |
2007年 | 2394篇 |
2006年 | 2459篇 |
2005年 | 2133篇 |
2004年 | 2240篇 |
2003年 | 2063篇 |
2002年 | 1965篇 |
2001年 | 1775篇 |
2000年 | 1747篇 |
1999年 | 1511篇 |
1998年 | 1494篇 |
1997年 | 1481篇 |
1996年 | 1275篇 |
1995年 | 1210篇 |
1994年 | 1095篇 |
1993年 | 995篇 |
1992年 | 947篇 |
1991年 | 803篇 |
1990年 | 1011篇 |
1989年 | 850篇 |
1988年 | 755篇 |
1987年 | 928篇 |
1986年 | 817篇 |
1985年 | 1020篇 |
1984年 | 1184篇 |
1983年 | 1124篇 |
1982年 | 1016篇 |
1981年 | 980篇 |
1980年 | 835篇 |
1979年 | 815篇 |
1978年 | 867篇 |
1977年 | 788篇 |
1976年 | 751篇 |
1975年 | 697篇 |
1974年 | 704篇 |
1973年 | 709篇 |
1972年 | 442篇 |
1971年 | 386篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
681.
682.
Air temperature variations in Europe and northern Asia are strongly affected by atmospheric circulation. A large-scale study of temperature signals is presented, using a newly available global gridded daily temperature dataset. Major types of European Grosswetterlagen (large-scale weather patterns) and the Russian Vangengeim–Girs classification are compared in their spatial applicability to air temperatures within the past 110 years (1901–2010). The consistency of spatial patterns in the three most recent decades (1981–2010) is investigated, and temperature changes are interpreted against the backdrop of changes in character and frequency of circulation patterns. Both classifications largely explain the observed temperature variability. Spatial patterns are large-scale and strong in both regions, especially in winter. Both spatial extent and signal magnitude show a distinct seasonality with maximum values in winter and minimum ones in summer. Spatial patterns show little changes in Europe; yet the ability to explain temperature variability in northern Asia decreased within 1981–2010. European winter warming corresponds to increased maritime and to decreased continental air mass inflow, superimposed on the general warming trend. Northern Asian winter warming is partly explainable by circulation changes in January and February, but to a lesser extend in December. These results may be used to advance input variables of global climate models and to improve their performance in the European–Northern Asian area. 相似文献
683.
Villeta M. Valencia J. L. Saá A. Tarquis A. M. 《Theoretical and Applied Climatology》2018,131(3-4):1323-1335
Theoretical and Applied Climatology - Extreme climate events have recently attracted the attention of a growing number of researchers because these events impose a large cost on agriculture and... 相似文献
684.
V. Masson-Delmotte G. Raffalli-Delerce P. A. Danis P. Yiou M. Stievenard F. Guibal O. Mestre V. Bernard H. Goosse G. Hoffmann J. Jouzel 《Climate Dynamics》2005,24(1):57-69
A new paleoclimatic reconstruction for western France is obtained from tree-ring cellulose stable isotopes. Living trees from Rennes Forest and beams from two ancient buildings in Rennes city have been combined to cover the past four centuries with a gap from 1730 to 1750. The cellulose 13C reflects the progressive changes in atmospheric CO2 isotopic composition. The combined 13C and 18O measurements are used to propose a reconstruction of interannual fluctuations in local summer temperature and water stress. At the decadal time scale, the reconstructed water stress profile exhibits a significant similarity with the historical wine harvest dates, an indicator of warm and dry growth seasons, as well as with the summer central England and central Alps instrumental temperature records and climate model results. Combined with instrumental precipitation records from Paris, these reconstructions suggest a dramatic and widespread change in the seasonality of the precipitation at the beginning of the nineteenth century, with drier winters and wetter summers, which may have contributed to the Alpine glacier decline at the end of the Little Ice Age. The tree-ring isotope records also show a relationship with large-scale North Atlantic circulation changes and the interannual variability is modified between the nineteenth and twentieth centuries (7–8 year periodicities) and the seventeenth century (11–14 year periodicities). By classifying 20-year-long subsets of the reconstructed climatic parameters, we estimate that a decadal mean summer warming of 0.8±0.1°C induced extreme dry years to be 2.2±0.7 times more frequent. 相似文献
685.
A series of Hokkaido events, recorded by the FBV Broadband Seismograph System at the KHC Seismic Station, is used to study the structure of the earthquake magnitude scale on the basis of maximum velocity amplitudesA
vmax of teleseismicPwaves in different period bands. Amplitude-periodband (APB) diagrams are constructed for each event. According to the shape of the APB diagrams the events investigated can be divided into three types: (a) events with largestA
vmax values in the intermediate period range (periods ofA
vmax from 2.2 to 23 sec), (b) events with largestA
vmax values in the short-period range (periods ofA
vmax from 1 to 2 sec), (c) events exhibiting anomalous APB diagrams. Type (a) events seem to represent the process of wave generation that prevails for shallow earthquakes. Type (b) events approach to explosive-like generation of seismic waves. The nature of the exceptionally occurring type (c) events must be clarified in further investigations. The influence of the type of earthquake on the magnitude values estimated on the basis of standard class A and B (short-period and intermediate-band) seismograms is demonstrated. It appears that for estimating correct values of earthquake magnitudes complementary information on the process of seismic wave generation in the focus is necessary. At teleseismic distances this information can be obtained from either APB diagrams or amplitude spectra ofP waves recorded, e.g., by broadband velocity sensing instruments. 相似文献
686.
687.
On the basis of the newest interpretations of all sufficiently long seismic profiles, a contour map of the Mohorovi?i? discontinuity for the conterminous United States is compiled. Differences from earlier interpretations are discussed. 相似文献
688.
Stable carbon isotope variations in northwest Europe during the last glacial–interglacial transition
Chris S. M. Turney David J. Beerling Douglas D. Harkness J. John Lowe E. Marian Scott 《第四纪科学杂志》1997,12(4):339-344
Stable carbon isotope data that span part of the last glacial–interglacial transition (ca. 14-9 ka 14C BP; ca. 15–11 ka cal. BP), and which derive from organ-specific plant macrofossils recovered from two lake sediment profiles in the UK and one in Norway, are compared. The recorded temporal variations show similar trends, which, over a millennial time-scale appear to parallel the main drift in δ18O as determined for the GRIP ice-core. It is postulated that some smaller scale variations in the δ13C profiles may reflect the shorter term oscillations in δ18O values evident in the GRIP record, although this is less certain. Overall, however, the results suggest that stable carbon isotope measurements based on organ-specific terrestrial plant macrofossils may provide (i) a means for establishing correlations between terrestrial successions and (ii) additional paleoenvironmental information, as the apparent ‘shadowing’ of the GRIP record indicates a common forcing mechanism for both Greenland δ18O and northwest European δ13C variations. From the evidence available we suggest that the recorded δ13C variations reflect fluctuations in air temperature and/or changes in water vapour pressure in the atmosphere. © 1997 John Wiley & Sons, Ltd. 相似文献
689.
L. Hernández J.W. Laundré K.M. GrajalesG.L. Portales J. López-PortilloA. González-Romero A. GarcíaJ.M. Martínez 《Journal of Arid Environments》2011,75(11):1043-1049
The abundance of black-tailed jackrabbits (Lepus californicus) can fluctuate dramatically. We used data from the Chihuahuan Desert to test the relative strength of top-down (predation) or bottom-up (food availability) limiting forces. Predictions for the top-down hypothesis were, 1) a positive relationship between coyote (Canis latrans) and jackrabbit abundance (numerical response) and 2) a positive relationship between percent occurrence of jackrabbits in coyote scats and jackrabbit abundance (functional response). Predictions for the bottom-up hypothesis were, 1) plant productivity is directly related to precipitation, 2) jackrabbit abundance is positively related to precipitation and plant productivity, and 3) changes in abundance of jackrabbits over the reproductive season will be directly related to precipitation and plant productivity. We found a limited numerical response but no functional response of coyotes to jackrabbit abundance. Forb productivity was significantly related to annual precipitation levels (r2 = 0.69, p = 0.002). Grass productivity was related to annual precipitation (r2 = 0.34, p = 0.028). Jackrabbit abundance (r2 = 0.38, p = 0.002) and changes in abundance (r2 = 0.73, p < 0.001) were significantly related to precipitation and forb and grass productivity. We conclude that precipitation levels and plant productivity affect jackrabbit abundance more than predation levels. 相似文献
690.
P. J. Fraser M. A. K. Khalil R. A. Rasmussen L. P. Steele 《Journal of Atmospheric Chemistry》1984,1(2):125-135
Results of more than 800 new measurements of methane (CH4) concentrations in the Southern Hemisphere troposphere (34–41° S, 130–150° E) are reported. These were obtained between September 1980 and March 1983 from the surface at Cape Grim, Tasmania, through the middle (3.5–5.5 km) to the upper troposphere (7–10 km). The concentration of CH4 increased throughout the entire troposphere over the measurement period, adding further support to the view that CH4 concentrations are currently increasing on a global scale. For data averaged vertically through the troposphere the rate of increase found was 20 ppbv/yr or 1.3%/yr at December 1981. In the surface CH4 data a seasonal cycle with a peak to peak amplitude of approximately 28 ppbv is seen, with the minimum concentration occurring in March and the maximum in September–October. A cycle with the same phase as that seen at the surface, but with a significantly decreased amplitude, is apparent in the mid troposphere but no cycle is detected in the upper tropospheric data. The phase and amplitude of the cycle are qualitatively in agreement with the concept that the major sink for methane is oxidation by hydroxyl radicals. Also presented is evidence of a positive vertical gradient in methane, with a suggestion that the magnitude of this gradient has changed over the period of measurements. 相似文献