全文获取类型
收费全文 | 5047篇 |
免费 | 173篇 |
国内免费 | 54篇 |
专业分类
测绘学 | 125篇 |
大气科学 | 436篇 |
地球物理 | 1078篇 |
地质学 | 1678篇 |
海洋学 | 478篇 |
天文学 | 918篇 |
综合类 | 12篇 |
自然地理 | 549篇 |
出版年
2021年 | 51篇 |
2020年 | 61篇 |
2019年 | 83篇 |
2018年 | 83篇 |
2017年 | 86篇 |
2016年 | 115篇 |
2015年 | 119篇 |
2014年 | 118篇 |
2013年 | 279篇 |
2012年 | 162篇 |
2011年 | 241篇 |
2010年 | 214篇 |
2009年 | 291篇 |
2008年 | 215篇 |
2007年 | 196篇 |
2006年 | 180篇 |
2005年 | 172篇 |
2004年 | 176篇 |
2003年 | 178篇 |
2002年 | 168篇 |
2001年 | 104篇 |
2000年 | 111篇 |
1999年 | 103篇 |
1998年 | 97篇 |
1997年 | 61篇 |
1996年 | 79篇 |
1995年 | 68篇 |
1994年 | 64篇 |
1993年 | 61篇 |
1992年 | 58篇 |
1991年 | 71篇 |
1990年 | 55篇 |
1989年 | 54篇 |
1988年 | 48篇 |
1987年 | 69篇 |
1986年 | 50篇 |
1985年 | 64篇 |
1984年 | 84篇 |
1983年 | 67篇 |
1982年 | 56篇 |
1981年 | 71篇 |
1980年 | 62篇 |
1979年 | 52篇 |
1978年 | 69篇 |
1977年 | 52篇 |
1976年 | 56篇 |
1975年 | 36篇 |
1974年 | 45篇 |
1973年 | 36篇 |
1971年 | 36篇 |
排序方式: 共有5274条查询结果,搜索用时 46 毫秒
71.
72.
Richard B. Olsen 《Ocean Engineering》1987,14(6)
Empirical orthogonal function (EOF) analysis is used in conjunction with Markov chains to generate simultaneous current time series at several depths with a random walk model. Duration statistics and probability distributions for EOF modes obtained from real data are used to generate transition probability matrices for the random walk model. New time series of EOF modes are generated, and then combined to produce current time series. The technique has been tested on data from Haltenbanken. Statistical properties of real and simulated time series were compared. Results indicate that the model is acceptable as a tool in simulating current time series to be used in offshore operation models. 相似文献
73.
To improve resolution of seismic-reflection profiles in continental slope water depths of 900 to 1500 m, a single hydrophone
was towed about 150 m off the bottom to receive reflected signals from a surface-towed sparker sound source. That deep-towed
hydrophone data show that valleys which appear V-shaped in records from a surface-towed hydrophone are flat-bottomed, and
that subbottom reflections from an erosional unconformity can be much better resolved. The data produced by this technique
are very hepful when used in conjunction with records from conventional surface-towed seismic-profiling equipment. 相似文献
74.
Image processing techniques are discussed that correct distortions in GLORIA II side scan sonar imagery including water column
offset, slant-range distortion, multiple returns, aspect ratio, speckle noise, striping, and cross-track power drop-off. The
software operates within NASA's ELAS image processing system and is applied to the original 12-bit GLORIA II data. Procedures
are discussed for generating large scale mosaics and three-dimensional overlays with sea floor bathymetry. The results are
shown in four sonographs acquired off the southern coast of California. 相似文献
75.
Coals are oil source rocks in many of the Tertiary basins of Southeast Asia. The precursors of these hydrogen rich and oxygen poor coals are coastal plain peats which have mainly developed in an everwet and tropical climate. In these environments water flow and reworking can concentrate liptinitic kerogen in preference to vitrinitic kerogen. The distribution, petrography and chemistry of the coaly Miocene source rocks present in the Kutai Basin are described. The recognition of environmental controls on the accumulation of potentially oil-prone coals and coaly shales in deltaic environments is an aid to predictive source bed recognition in petroleum exploration. Comments on the environment of deposition of coaly sediments in the basins of the Norwegian Sea are discussed with reference to their possible oil and/or gas sourcing potential. The Triassic - Jurassic coals of the Haltenbanken area may become more oil-prone towards the delta margins, and facies mapping could aid oil exploration in this area. 相似文献
76.
Jeffrey M. Napp Christine T. Baier Richard D. Brodeur Kenneth O. Coyle Naonobu Shiga Kathy Mier 《Deep Sea Research Part II: Topical Studies in Oceanography》2002,49(26)
The southeastern Bering Sea shelf ecosystem is an important fishing ground for fin- and shellfish, and is the summer foraging grounds for many planktivorous seabirds and marine mammals. In 1997 and 1998, Northern Hemisphere climate anomalies affected the physical and biological environment of the southeastern Bering Sea shelf. The resulting anomalous conditions provided a valuable opportunity to examine how longer-term climate change might affect this productive ecosystem. We compared historical and recent zooplankton biomass and species composition data for the southeastern Bering Sea shelf to examine whether or not there was a response to the atmosphere–ocean–ice anomalies of 1997 and 1998. Summer zooplankton biomass (1954–1994) over the southeastern shelf did not exhibit a decline as previously reported for oceanic stations. In addition, zooplankton biomass in 1997 and 1998 was not appreciably different from other years in the time series. Spring concentrations of numerically abundant copepods (Acartia spp., Calanus marshallae, and Pseudocalanus spp.), however, were significantly higher during 1994–1998 than 1980–1981; spring concentrations of Metridia pacifica and Neocalanus spp. were not consistently different between the two time periods. Neocalanus spp. was the only taxon to have consistent differences in stage composition between the two time periods—CV copepodites were much more prevalent in May of the 1990s than early 1980s. Since relatively high zooplankton concentrations were observed prior to 1997, we do not attribute the high concentrations observed in the summers of 1997 and 1998 directly to the acute climate anomalies. With the present data it is not possible to distinguish between increased production (control from below) and decreased predation (control from above) to explain the recent increase in concentrations of the species examined. 相似文献
77.
78.
Miriam J. Doyle Kathryn L. Mier Morgan S. Busby Richard D. Brodeur 《Progress in Oceanography》2002,53(2-4)
The coastal regions of the northeast Pacific support large, economically valuable fishery resources and provide nursery areas for many fish species. Over the last few decades, there have been dramatic shifts in species abundance and composition in this area. In this paper, we examine the springtime spatial patterns in the ichthyoplankton of three oceanographically different regions, the Southeast Bering Sea, the Gulf of Alaska and the U.S. West Coast. The data examined are a subset of a larger database (comprising data from cruises conducted from 1972 to 1997) that is being used to investigate spatial, seasonal and interannual patterns in ichthyoplankton of the northeast Pacific in relation to environmental conditions. Ichthyoplankton were collected during seven cruises using 60-cm bongo nets. Spatial patterns of ichthyoplankton were examined using both classification and ordination techniques. Relative Bray-Curtis dissimilarity coefficients calculated from the log10 (n+1) of abundance data were used as input to the numerical classification of species and stations. Nonmetric multidimensional scaling was also applied to the abundance data to examine geometric patterns in the data. The numerical analyses of the species abundance data sets for each cruise revealed spatial patterns in the ichthyoplankton that suggest the occurrence of geographically distinct assemblages of fish larvae in each region. For all three sampling regions, the assemblage structure is primarily related to bathymetry, and Shelf, Slope, and Deep-Water assemblages are described. This shallow to deep-water gradient in species occurrence and abundance reflects the habitat preference and spawning location of the adult fish. Another degree of complexity is superimposed on this primary assemblage structure in each region and seems to be related to local topography and the prevailing current patterns. The patterns in ichthyoplankton assemblages of the three regions in the northeast Pacific Ocean described here form the basis for future investigations of spatial and temporal patterns in the ichthyoplankton of the subarctic Pacific.Regional Index Terms: Northeast Pacific Ocean, Southeast Bering Sea, Gulf of Alaska, U.S. West Coast. 相似文献
79.
Hector A. Hernndez-Arana Ashley A. Rowden Martin J. Attrill Richard M. Warwick Gerardo Gold-Bouchot 《Estuarine, Coastal and Shelf Science》2003,58(4):825-841
The influence of large-scale natural disturbance from winter storms (‘northers’) and river runoff on the macrobenthic community structure of the southern Gulf of Mexico was investigated in both carbonate and transitional carbonate–terrigenous sedimentary environments. Samples of the infauna were obtained in three seasons from 13 stations from two 250 km transects along 80–170 and 20–50 m water depth. Samples after the northers season had the lowest total number of families and individuals, 114 and 2940, respectively, compared to the dry and rainy seasons with 129 and 132 families and 11580 and 15266 individuals, respectively. Spatial patterns of macroinfauna composition varied across and along the shelf as a response to sedimentary environments and depth. Coarser sediments from the carbonate area harboured the highest mean densities per station with 500–24,000 individuals m−2 and 108–122 families in total, compared to the transitional sediment with 500–8200 individuals m−2 and 56–74 families across the three seasons. Univariate and multivariate statistical techniques demonstrated that low densities and number of taxa were associated with winter storms, but storm influence was dependent on depth and sediment type. Multiple linear regression analysis and BIOENV analysis indicated that sediment mean grain size, percentage of clay and organic matter best explained the macroinfauna spatial patterns, although BIOENV indicated that depth has an overriding role. An increase in densities of opportunistic taxa (numerous polychaetes of small sizes) was observed four months after the ‘northers’ and this was more evident in the area of carbonate sediment. Additionally a combined disturbance from northers and river runoff is suspected to be responsible for a naturally impoverished macroinfauna community in the transitional sedimentary environment. 相似文献
80.