全文获取类型
收费全文 | 217篇 |
免费 | 4篇 |
国内免费 | 7篇 |
专业分类
测绘学 | 8篇 |
大气科学 | 63篇 |
地球物理 | 19篇 |
地质学 | 33篇 |
海洋学 | 57篇 |
天文学 | 34篇 |
自然地理 | 14篇 |
出版年
2021年 | 2篇 |
2019年 | 3篇 |
2018年 | 4篇 |
2017年 | 2篇 |
2016年 | 6篇 |
2015年 | 6篇 |
2014年 | 16篇 |
2013年 | 9篇 |
2012年 | 16篇 |
2011年 | 10篇 |
2010年 | 12篇 |
2009年 | 16篇 |
2008年 | 8篇 |
2007年 | 6篇 |
2006年 | 7篇 |
2005年 | 3篇 |
2004年 | 5篇 |
2003年 | 9篇 |
2002年 | 8篇 |
2001年 | 6篇 |
2000年 | 4篇 |
1999年 | 8篇 |
1998年 | 5篇 |
1997年 | 4篇 |
1996年 | 3篇 |
1995年 | 1篇 |
1994年 | 7篇 |
1993年 | 1篇 |
1992年 | 5篇 |
1990年 | 2篇 |
1988年 | 2篇 |
1987年 | 1篇 |
1986年 | 4篇 |
1985年 | 2篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 1篇 |
1978年 | 3篇 |
1976年 | 6篇 |
1975年 | 2篇 |
1974年 | 1篇 |
1973年 | 2篇 |
1972年 | 1篇 |
1970年 | 1篇 |
1951年 | 1篇 |
排序方式: 共有228条查询结果,搜索用时 15 毫秒
191.
It is demonstrated that nonlinear Rossby modes, such as modons and IG eddies, can be excited in planetary fluids by a sufficiently strong forcing of potential vorticity. When a weak forcing is balanced with a weak dissipation, two (linear and nonlinear) equilibrium states can be produced, depending on the initial condition. When the fluid is inviscid, a sufficiently strong steady forcing may generate a sequence of propagating nonlinear eddies. A weak forcing, by contrast, only generates linear Rossby waves. The criterion which divides the high amplitude nonlinear state and the low amplitude linear state may be interpreted in terms of a ratio of a time necessary to force the eddy to a time for a fluid particle to circulate about the nonlinear eddy once. 相似文献
192.
Recursive computation of oblate spheroidal harmonics of the second kind and their first-, second-, and third-order derivatives 总被引:1,自引:0,他引:1
Toshio Fukushima 《Journal of Geodesy》2013,87(4):303-309
A recursive method is developed to compute the ratios of the oblate spheroidal harmonics of the second kind and their first-, second-, and third-order derivatives. The recurrence formulas consist of three kinds: (1) fixed-degree increasing-order, (2) mixed-degree increasing-order, and (3) fixed-order decreasing-degree. The three seed values are evaluated by rapidly convergent series. The derivatives of the ratios are recursively obtained from the values and lower-order derivatives of the same harmonic order and of the same or higher degrees. The new method precisely and quickly computes the ratios and their low-order derivatives. It provides 13 correct digits of the ratios of degree as high as 262,000 and runs 20–100 times faster than the existing methods. 相似文献
193.
Hiroshi A. Takahashi Eiichi Konohira Tetsuya Hiyama Masayo Minami Toshio Nakamura Naohiro Yoshida 《Tellus. Series B, Chemical and physical meteorology》2002,54(2):97-109
Diurnal variation in the atmospheric CO2 concentration and the carbon isotopic composition (Δ14 C and δ13 C) was measured in a forest in an urban area on 9 February 1999. The carbon isotope approach used in the present study differentiated between the quantitative contributions from anthropogenic and biogenic CO2 sources in the urban atmosphere. The anthropogenic (fossil fuel) and biogenic (soil respiration) contributions was estimated, and they ranged from 1 to 16% and from 2 to 8% of the total atmospheric CO2 . The diurnal variation of the anthropogenic CO2 was the major cause of the total atmospheric CO2 variation, while the biogenic CO2 remained relatively constant throughout the day. Estimating the contribution of soil respired CO2 provided the mean residence time of soil respired CO2 within the forest atmosphere. 相似文献
194.
195.
196.
A global data set describing the gridded mixed-layer depth (MLD) in 10-day intervals was produced using high-quality Argo
float data from 2001 to 2009. The characteristics and advantages provided by the new MLD data set are described here, including
a comparison based on two different thresholds and using data sets of different vertical and temporal resolution. The MLD
in the data set was estimated on the basis of a shallower depth of the iso-thermal layer (TLD) or iso-pycnal layer (PLD),
calculated using the finite difference method. The MLD data are incorporated into 2° × 2° grid in the global ocean, including
marginal seas. Also, two threshold values were used to examine differences in the MLD and its seasonal temporal variability.
The characteristics and advantages of using the Argo 10-day intervals to determine the MLD were then confirmed by comparing
those data with the station buoy daily means and the Argo monthly means. With respect to vertical and temporal resolutions,
the Argo 10-day data has two distinct advantages: (1) improved representation of the MLD vertical change due to high vertical
resolution, especially during periods of large MLD variability and (2) more detailed representation of the temporal change
in MLD than achieved with the Argo monthly mean data, especially from winter to spring in mid and high latitudes. These advantages
were maintained in the case of a larger threshold despite the fact that the MLD is rather deep and the detailed variation
in its distribution differs depending on the season and location. This study also investigated the relative influence of TLD
and PLD to the MLD calculation for each grid. Generally, the MLD is primarily determined based on the PLD at low and mid latitudes
(TLD > PLD), whereas the TLD is more important at high latitudes, especially in winter (TLD < PLD). In the case of a larger
threshold, the area of the larger PLD influence spreads polewards because of the greater effect of salinity in winter. Although
there are some differences in the effect of temperature and salinity in estimations of the MLD, both are indispensable factors
for the MLD estimations even at different thresholds. 相似文献
197.
Toshio Furuta 《Marine Geology》1976,20(3):229-237
All the tephra layers sampled from a core in the northwest Pacific have both ortho-and clinopyroxenes as essential minerals, most of them containing hornblende and some of them biotite, zircon, apatite and olivine. Refractive indices of volcanic glass shards range between 1.49 and 1.53. Comparison of the refractive indices with those of artificial glass beads as well as the mineralogical composition of the tephra suggest that its sources are possibly acidic volcanoes in the Japanese island arc. Magnetic and crystallographic features of the ferromagnetic constituents in tephra have also shown that the tephra originated not from oceanic basalt but from acidic volcanoes. 相似文献
198.
Eitarou Oka Masao Ishii Toshiya Nakano Toshio Suga Shinya Kouketsu Masatoshi Miyamoto Hideyuki Nakano Bo Qiu Shusaku Sugimoto Yusuke Takatani 《Journal of Oceanography》2018,74(2):115-145
The 137°E repeat hydrographic section of the Japan Meteorological Agency across the western North Pacific was initiated in 1967 as part of the Cooperative Study of the Kuroshio and Adjacent Regions and has been continued biannually in winter and summer. The publicly available data from the section have been widely used to reveal seasonal to decadal variations and long-term changes of currents and water masses, biogeochemical and biological properties, and marine pollutants in relation to climate variability such as the El Niño-Southern Oscillation and the Pacific Decadal Oscillation. In commemoration of the 50th anniversary in 2016, this review summarizes the history and scientific achievements of the 137°E section during 1967–2016. Through the publication of more than 100 papers over this 50-year span, with the frequency and significance of the publication increasing in time, the 137°E section has demonstrated its importance for future investigations of physical–biogeochemical–biological interactions on various spatiotemporal scales, and thereby its utility in enhancing process understanding to aid projections of the impact of future climate change on ocean resources and ecosystems over the twenty-first century. 相似文献
199.
Global surface layer salinity change detected by Argo and its implication for hydrological cycle intensification 总被引:1,自引:0,他引:1
Shigeki Hosoda Toshio Suga Nobuyuki Shikama Keisuke Mizuno 《Journal of Oceanography》2009,65(4):579-586
We investigated changes in the global distribution of surface-layer salinity by comparing 2003–2007 Argo-float data with annual
mean climatological surface-layer salinity data for 1960–1989 from the World Ocean Database 2005. The two datasets showed
similar patterns, with low values in subpolar and tropical regions and higher values in the subtropics. The recent Argo data
indicate that the contrast between low and high salinity has intensified in all areas except the subpolar North Atlantic.
The intensified contrast of the surface layer salinity was maintaining for 2003–2007. Using a simple method, we attempted
to estimate evaporation and precipitation changes on the basis of surface-layer salinity changes. The results show a high
probability that the global hydrological cycle has increased in the past 30 years. 相似文献
200.
Toshio Yamagata Shin-Ichiro Umatani Noriaki Masunaga Tomonori Matsuura 《Continental Shelf Research》1984,3(4):475-488
Detailed hydrographic observations were made in Wakasa Bay, Japan, in August 1979 as the first of a series on the topic of bay intrusions. An anomalous water tongue, evident at a depth of 50 m, was observed to move eastward into the bay at a speed of about 10 km day−1. The width of the tongue was about 20 to 30 km in agreement with the Rossby internal radius of deformation. The results of current meter measurements and the observed temporal and spatial evolution of the temperature field near the front of the anomalous water tongue have suggested that ageostrophic cross-frontal motion, in balance with the along-front acceleration, may be important in our understanding of intrusion processes. 相似文献