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111.
Susanne C. Schneider A.E. LawniczakJ. Picińska-Faltynowicz K. Szoszkiewicz 《Limnologica》2012,42(3):204-211
We analyzed species composition and abundance of macrophytes, diatoms and non-diatom benthic algae, water chemistry and habitat structure of 24 river sites in Poland, in order to better understand which parameters structure macrophyte and benthic algae communities. Community patterns for macrophytes and diatoms are most closely related, while macrophytes and non-diatom benthic algae have the weakest relationship. Environmental parameters best explaining community patterns are channel substrate parameters for non-diatom benthic algae, and a combination of channel substrate and river bank characteristics for submerged macrophytes, emergent macrophytes and diatoms. Among the organism groups investigated, the diatom community pattern is best correlated to the environmental data similarity matrix. We hypothesize that the results can be explained by the shorter generation time of diatoms compared to macrophytes, and by a higher dispersal rate of diatoms compared to macrophytes and non-diatom benthic algae. This has several practical consequences for bioindication: (1) Diatoms are usually the organism group most closely following environmental parameters, for both increasing and decreasing impact. (2) Since the biotic indices developed for the Water Framework Directive are meant to primarily indicate ecological changes, not water chemistry, the nature of diatoms to closely reflect water chemistry is not necessarily advantageous. (3) The applicability of macrophyte and probably also non-diatom benthic algae indices is more locally restricted, while diatom indices are applicable to greater areas. (4) In ecosystems which are subject to changing environmental conditions, differences in biotic indices between macrophytes, diatoms and non-diatom benthic algae are to be expected. These differences could provide information relating to ecosystem stability. (5) In stable ecosystems, analyzing one of the three organism groups “diatoms”, “non-diatom benthic algae” and “macrophytes” will be sufficient to characterize the quality element “macrophytes and phytobenthos”, as required by the Water Framework Directive. However, in ecosystems subject to increasing pressure, macrophytes likely will have a tendency to indicate “too good”, while in ecosystems subject to decreasing pressure, diatoms will have a tendency to indicate “too good”. 相似文献
112.
In 2011, northern fulmars (Fulmarus glacialis) from Iceland were used to test the hypothesis that plastic debris decreases at northern latitudes in the Atlantic when moving away from major human centres of coastal and marine activities. Stomach analyses of Icelandic fulmars confirm that plastic pollution levels in the North Atlantic tend to decrease towards higher latitudes. Levels of pollution thus appear to link to regions of intense human coastal and marine activities, suggesting substantial current inputs in those areas. 相似文献
113.
Sources and fate of nutrients in a subtropical reservoir 总被引:1,自引:0,他引:1
Michele?A.?BurfordEmail author Susanne?A.?Green Andrew?J.?Cook Suzanne?A.?Johnson Jason?G.?Kerr Katherine?R.?O’Brien 《Aquatic Sciences - Research Across Boundaries》2012,74(1):179-190
This study examined the sources and fate of nutrient inputs from two principal tributaries to the eutrophic subtropical Wivenhoe
reservoir: an unregulated river and a dammed river with regular releases, during a period of declining reservoir water levels.
Nutrient budgets were constructed over a period of 6 years, and combined with short-term data on nutrient concentrations and
forms, and δ15N stable isotope data. Our study found that over a 6 year period, there was net retention of phosphorus (P) in the reservoir,
with 60% of inputs retained. Most of the P input load came from the unregulated river, with an agricultural catchment, during
periods of high flow. During one event half of the total TP load from the unregulated river in the study period was delivered
in only 12 days. Much of the P was dissolved inorganic P (DIP) and was derived from high P concentrations in soils and sediments.
This highlights the importance of appropriate catchment management practices to reduce P losses from terrestrial systems because
retention of P in reservoir sediments reduces the availability of this nutrient for agricultural production. In contrast,
there was negligible retention of nitrogen (N). The unregulated river was an important source of N derived from N fixation
in the river and adjacent soils, while the source from the dammed river was mostly reprocessed N. The high retention of P
relative to N is consistent with relatively higher accumulation of P in sediments. 相似文献
114.
Claus Gebhardt Jean-Raymond Bidlot Johannes Gemmrich Susanne Lehner Andrey Pleskachevsky Wolfgang Rosenthal 《Ocean Dynamics》2016,66(6-7):839-852
This article investigates the penetration of ocean waves into the marginal ice zone (MIZ), observed by satellite, and likewise provides a basis for the future cross-validation of respective models. To this end, synthetic aperture radar images from the TerraSAR-X satellite (TS-X) and numerical simulations of the European Centre for Medium-Range Weather Forecasts (ECMWF) are used. The focus is an event of swell waves, developed during a storm passage in the Atlantic, penetrating deeply into the MIZ off the coast of Eastern Greenland in February 2013. The TS-X scene which is the basis for this investigation extends from the ice-free open ocean to solid ice. The variation of the peak wavelength is analysed and potential sources of variability are discussed. We find an increase in wavelength which is consistent with the spatial dispersion of deep water waves, even within the ice-covered region. 相似文献
115.
116.
Nicolas Reul Severine Fournier Jaqueline Boutin Olga Hernandez Christophe Maes Bertrand Chapron Gaël Alory Yves Quilfen Joseph Tenerelli Simmon Morisset Yann Kerr Susanne Mecklenburg Steven Delwart 《Surveys in Geophysics》2014,35(3):681-722
While it is well known that the ocean is one of the most important component of the climate system, with a heat capacity 1,100 times greater than the atmosphere, the ocean is also the primary reservoir for freshwater transport to the atmosphere and largest component of the global water cycle. Two new satellite sensors, the ESA Soil Moisture and Ocean Salinity (SMOS) and the NASA Aquarius SAC-D missions, are now providing the first space-borne measurements of the sea surface salinity (SSS). In this paper, we present examples demonstrating how SMOS-derived SSS data are being used to better characterize key land–ocean and atmosphere–ocean interaction processes that occur within the marine hydrological cycle. In particular, SMOS with its ocean mapping capability provides observations across the world’s largest tropical ocean fresh pool regions, and we discuss from intraseasonal to interannual precipitation impacts as well as large-scale river runoff from the Amazon–Orinoco and Congo rivers and its offshore advection. Synergistic multi-satellite analyses of these new surface salinity data sets combined with sea surface temperature, dynamical height and currents from altimetry, surface wind, ocean color, rainfall estimates, and in situ observations are shown to yield new freshwater budget insight. Finally, SSS observations from the SMOS and Aquarius/SAC-D sensors are combined to examine the response of the upper ocean to tropical cyclone passage including the potential role that a freshwater-induced upper ocean barrier layer may play in modulating surface cooling and enthalpy flux in tropical cyclone track regions. 相似文献
117.
Jun A. Zhang Kristina B. Katsaros Peter G. Black Susanne Lehner Jeffrey R. French William M. Drennan 《Boundary-Layer Meteorology》2008,128(2):173-189
Boundary-layer secondary circulations or ‘roll vortices’ can have a significant influence on the turbulent exchange of momentum,
sensible heat and moisture throughout the hurricane boundary layer. In this study, analyses of data from a WP-3D aircraft
of the National Oceanic and Atmospheric Administration (NOAA) are presented. As part of the Coupled Boundary Layer Air-Sea
Transfer (CBLAST)-hurricane experiment sponsored through the Office of Naval Research and NOAA’s annual hurricane research
program, flights were conducted to investigate energy exchange across the air–sea interface. We present the first in-situ
aircraft-based observations of rolls in the hurricane boundary layer and investigate their influence on energy and momentum
exchange. The rolls detected in Hurricane Isidore (year 2002) have a characteristic wavelength of about 900 m, in good agreement
with analyses of data from a synthetic aperture radar image captured by the Canadian Space Agency’s RADARSAT satellite in
the same storm. Our analyses of the airborne data suggest that roll vortices may be a significant factor modulating the air–sea
momentum exchange. 相似文献
118.
119.
Susanne Seitz Lukas P. Baumgartner Anne‐Sophie Bouvier Benita Putlitz Torsten Vennemann 《Geostandards and Geoanalytical Research》2017,41(1):69-75
Two quartz samples of igneous origin, UNIL‐Q1 (Torres del Paine Intrusion, Chile) and BGI‐Q1 (Shandong province, China), were calibrated for their oxygen isotope composition for SIMS measurements. UNIL‐Q1 and BGI‐Q1 were evaluated for homogeneity using SIMS. Their reference δ18O values were determined by CO2 laser fluorination. The average δ18O value found for UNIL‐Q1 is 9.8 ± 0.06‰ and that for BGI‐Q1 is 7.7 ± 0.11‰ (1s). The intermediate measurement precision of SIMS oxygen isotope measurements was 0.32–0.41‰ (2s; UNIL‐Q1) and 0.40–0.48‰ (2s; BGI‐Q1), respectively. While less homogeneous in its oxygen isotope composition, BGI‐Q1 is also suitable for SIMS trace element measurements. 相似文献
120.
A partial instructional module on global and regional land use/cover change: assessing the data and searching for general relationships 总被引:4,自引:0,他引:4
Susanne C. Moser 《GeoJournal》1996,39(3):241-283
Land use/cover change has occurred at all times in all parts of the world. Most affected and involved in these processes are the environmental spheres of water, soil, and vegetative cover, which are closely linked to geomorphology, climate, fauna, and especially human societies. These linkages between spheres are highly complex and, as of yet, incompletely understood. The most profound questions with respect to land use/cover and global change are: “What forces drive land use/land cover change?”, “What impacts — direct and indirect, now and in the future — do these changes have on the environment and on human society?” and “Can and should we, and if so, how, respond to these changes?” This partial teaching module, developed under the auspices of the Second Commission on College Geography of the Association of American Geographers, introduces students to the complexities inherent in these questions, but mainly focusses on the first of these. It illustrates the central role of the study of land land use/cover change within the large field of global environmental and climatic change, and is thus a good unit to introduce this area of interest. 相似文献