首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   43752篇
  免费   644篇
  国内免费   298篇
测绘学   1051篇
大气科学   2870篇
地球物理   8774篇
地质学   15175篇
海洋学   3772篇
天文学   10796篇
综合类   97篇
自然地理   2159篇
  2021年   404篇
  2020年   456篇
  2019年   458篇
  2018年   1049篇
  2017年   955篇
  2016年   1163篇
  2015年   644篇
  2014年   1134篇
  2013年   2173篇
  2012年   1284篇
  2011年   1727篇
  2010年   1535篇
  2009年   2173篇
  2008年   1796篇
  2007年   1810篇
  2006年   1682篇
  2005年   1259篇
  2004年   1260篇
  2003年   1182篇
  2002年   1127篇
  2001年   1015篇
  2000年   957篇
  1999年   828篇
  1998年   850篇
  1997年   821篇
  1996年   690篇
  1995年   702篇
  1994年   624篇
  1993年   537篇
  1992年   501篇
  1991年   508篇
  1990年   581篇
  1989年   498篇
  1988年   461篇
  1987年   585篇
  1986年   486篇
  1985年   611篇
  1984年   688篇
  1983年   656篇
  1982年   573篇
  1981年   607篇
  1980年   502篇
  1979年   472篇
  1978年   476篇
  1977年   424篇
  1976年   405篇
  1975年   406篇
  1974年   385篇
  1973年   424篇
  1971年   259篇
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
991.
992.
993.
994.
A new inversion technique for obtaining temperature, pressure, and number density profiles of a planetary atmosphere from an occultation light curve is described. This technique employs an improved boundary condition to begin the numerical inversion and permits the computation of errors in the profiles caused by photon noise in the light curve. We present our assumptions about the atmosphere, optics, and noise and develop the equations for temperature, pressure, and number density and their associated errors. By inverting in equal increments of altitude, Δh, rather than in equal increments of time, Δt, the inversion need not be halted at the first negative point on the light curve as required by previous methods. The importance of the boundary condition is stressed, and a new initial condition is given. Numerical results are presented for the special case of inversion of a noisy isothermal light curve. From these results, simple relations are developed which can be used to predict the noise quality of an occultation. It is found that fractional errors in temperature profiles are comparable to those of pressure and number density profiles. An example of the inversion method is shown. Finally, we discuss the validity of our assumptions. In an appendix we demonstrate that minimum fractional errors in scale height determined from the inversion are comparable to those from an isothermal fit to a noisy isothermal light curve.  相似文献   
995.
996.
The effective temperatures radii and bolometric magnitudes of Ap, Am and normal A stars have been estimated from their energy distribution curves between 478 nm and 680 nm. All the Am stars and one Ap star (i.e. CrB) were found to be affected by line blanketing, a rough estimation of which in the respective (B-V) colours has been found out in each case.The range in effective temperature is 0.45–0.60 in terms of (=5040/T e), while it is 1.8–4.8R in the case of radius, that in bolometric magnitude being from-0m.67 to+1m.61. An approximate estimate of the masses shows that they are between 1.5 and 3.0M . All these estimates are in agreement with those of the normal A stars. The Ap and Am stars are found to be slightly evolved and, therefore, are probably in the hydrogen shell-burning phase.  相似文献   
997.
G.S. Orton  R.J. Terrile 《Icarus》1978,35(3):297-307
Prior analysis of 20- and 45-μm flux measurements made from Pioneer 10 of broad regions near the Jovian equator revealed a cold longitudinal inhomogeneity (interpreted as a cloud obscuration) on the rising limb in the South Equatorial Belt. This feature appeared quite prominently at 45 μm and also at 5 μm in ground-based maps made simultaneously with the spacecraft measurements, but it does not appear at visible wavelengths. We describe a method by which the 5-μm observations are used to determine the fraction of 45-μm flux originating from only the region of the SEB obscured by this “anomalous” cloud. This allows the 45-μm data to constrain the cloud properties. On one extreme, the top of the SEB cloud was about 160°K, some 10°K warmer than a cloud in the neighboring South Tropical Zone, if the cloud was optically thick (nontransmissive). On the other hand, if the SEB cloud was as cool as the STrZ cloud, it must have been 60 to 80% transmissive, i.e., somewhat diffuse. With less uncertainty in the fraction of cloud obscuration, the ambiguity between tansmissivity and temperature is significantly diminished. The method described offers a potentially valuable tool for monitoring properties of clouds which do not necessarily appear at visible wavelengths.  相似文献   
998.
Observations of the April 8, 1976 occultation of ? Gem by Mars made at the Agassiz Station of the Harvard College Observatory have been analyzed to yield temperature profiles of the Martian atmosphere for number densities between 1013 and 1015 cm?3. Pronounced wavelike structure is evident in both immersion and emersion profiles, with a peak-tto-peak variation of up to 50°K and a vertical scale of 20 km.  相似文献   
999.
Petr Chýlek  G.W. Grams 《Icarus》1978,36(2):198-203
Ultraviolet spectral reflectance data obtained from the Mariner 9 during the 1971 Mars dust storm were analyzed at two wavelengths to deduce the complex index of refraction of Martian dust. Martian dust particles were considered to be irregularly shaped and randomly oriented nonspherical particles. The analysis shows that the Mariner 9 data are consistent with the scattering by irregular particles with an index of refraction m = 1.59 ? 0.0015i at λ = 0.305 μm and m = 1.55 ? 0.004i at λ = 0.268 μm. Both the real and the imaginary parts of refractive index found are considerably smaller than previously reported results using a spherical shape model for Martian dust particles.  相似文献   
1000.
A generation mechanism for 1–30 Hz waves of the second category, observed near the plasmapause by Taylor and Lyons (1976), is suggested in terms of a resonant electron instability. The instability arises because of the resonant interaction between the ring current electrons outside the plasmapause and the ordinary mode drift waves. The instability can generate waves in the frequency range from 0.45 to 35.0 Hz in the region between L = 4.5 and 5.5. The instability can also explain satisfactorily the other properties such as no changes in the proton distributions, the direction of the wave magnetic field and the localization of the region of wave activity, associated with these waves.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号