全文获取类型
收费全文 | 77篇 |
免费 | 1篇 |
专业分类
测绘学 | 1篇 |
大气科学 | 15篇 |
地球物理 | 25篇 |
地质学 | 16篇 |
海洋学 | 4篇 |
天文学 | 14篇 |
自然地理 | 3篇 |
出版年
2021年 | 3篇 |
2018年 | 1篇 |
2017年 | 1篇 |
2016年 | 1篇 |
2013年 | 3篇 |
2011年 | 1篇 |
2010年 | 2篇 |
2009年 | 4篇 |
2008年 | 6篇 |
2007年 | 4篇 |
2006年 | 2篇 |
2005年 | 1篇 |
2004年 | 2篇 |
2003年 | 4篇 |
2002年 | 1篇 |
2001年 | 5篇 |
2000年 | 2篇 |
1999年 | 1篇 |
1998年 | 1篇 |
1996年 | 5篇 |
1994年 | 1篇 |
1992年 | 1篇 |
1990年 | 1篇 |
1988年 | 1篇 |
1987年 | 3篇 |
1985年 | 1篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1982年 | 1篇 |
1980年 | 1篇 |
1979年 | 1篇 |
1978年 | 1篇 |
1977年 | 2篇 |
1976年 | 1篇 |
1975年 | 3篇 |
1972年 | 2篇 |
1969年 | 1篇 |
1967年 | 1篇 |
1965年 | 1篇 |
1963年 | 2篇 |
排序方式: 共有78条查询结果,搜索用时 0 毫秒
71.
Beginning in the mid-1990s, re-eutrophication has reemerged as severe problems in Lake Erie. Controlling non-point source (NPS) nutrient pollution from cropland, especially dissolved reactive phosphorus (DRP), is the key to restore water quality in Lake Erie. To address NPS pollution, previous studies have analyzed the effectiveness of alternative spatially optimal land use and management strategies (represented as agricultural conservation practices (CPs)). However, few studies considered both strategies and have analyzed and compared their sensitivity to expected changes in temperature and precipitation due to climate change and increased greenhouse gas concentrations. In this study, we evaluated impacts of climatic change on the economic efficiency of these strategies for DRP abatement, using an integrated modeling approach that includes a watershed model, an economic valuation component, and a spatial optimization model. A series of climate projections representing relatively high greenhouse gas emission scenarios was developed for the western Lake Erie basin to drive the watershed model. We found that performance of solutions optimized for current climate was degraded significantly under projected future climate conditions. In terms of robustness of individual strategies, CPs alone were more robust to climate change than land use change alone or together with CPs, but relying on CPs alone fails to achieve a high (>?71%) DRP reduction target. A combination of CPs and land use changes was required to achieve policy goals for DRP reductions (targeted at ~?78%). Our results point to the need for future spatial optimization studies and planning to consider adaptive capacity of conservation actions under a changing climate. 相似文献
72.
73.
Ulrich Foelsche Michael Borsche Andrea K. Steiner Andreas Gobiet Barbara Pirscher Gottfried Kirchengast Jens Wickert Torsten Schmidt 《Climate Dynamics》2008,31(1):49-65
High quality observations of the atmosphere are particularly required for monitoring global climate change. Radio occultation
(RO) data, using Global Navigation Satellite System (GNSS) signals, are well suited for this challenge. The special climate
utility of RO data arises from their long-term stability due to their self-calibrated nature. The German research satellite
CHAllenging Minisatellite Payload for geoscientific research (CHAMP) continuously records RO profiles since August 2001 providing
the first opportunity to create RO based climatologies for a multi-year period of more than 5 years. A period of missing CHAMP
data from July 3, 2006 to August 8, 2006 can be bridged with RO data from the GRACE satellite (Gravity Recovery and Climate
Experiment). We have built seasonal and zonal mean climatologies of atmospheric (dry) temperature, microwave refractivity,
geopotential height and pressure with 10° latitudinal resolution. We show representative results with focus on dry temperatures
and compare them with analysis data from the European Centre for Medium-Range Weather Forecasts (ECMWF). Although we have
available only about 150 CHAMP profiles per day (compared to millions of data entering the ECMWF analyses) the overall agreement
between 8 and 30 km altitude is in general very good with systematic differences <0.5 K in most parts of the domain. Pronounced
systematic differences (exceeding 2 K) in the tropical tropopause region and above Antarctica in southern winter can almost
entirely be attributed to errors in the ECMWF analyses. Errors resulting from uneven sampling in space and time are a potential
error source for single-satellite climatologies. The average CHAMP sampling error for seasonal zonal means is <0.2 K, higher
values occur in restricted regions and time intervals which can be clearly identified by the sampling error estimation approach
we introduced (which is based on ECMWF analysis fields). The total error of this new type of temperature climatologies is
estimated to be <0.5 K below 30 km. The recently launched Taiwan/U.S. FORMOSAT-3/COSMIC constellation of 6 RO satellites started
to provide thousands of RO profiles per day, but already now the single-satellite CHAMP RO climatologies improve upon modern
operational climatologies in the upper troposphere–lower stratosphere and can act as absolute reference climatologies for
validation of more bias-sensitive climate datasets and models. 相似文献
74.
Polarity reversal sequences have been observed in the Brushy Basin Member of the Morrison Formation (Upper Jurassic, Kimmeridgian-Tithonian age) at two sites in western Colorado separated by 80 km. The two polarity reversal sequences display a good correlation of relative lengths and number of polarity intervals and thus may provide a significant correlation tool in this laterally variable formation.The whole polarity sequence observed in the Morrison Formation correlates very well with the oldest portion of lineated anomalies of the sea floor. The sedimentary record on land and the anomaly pattern of the oceanic crust both show the same relative lengths and approximate number of polarity intervals, as well as ratio of reversed to normal polarity. 相似文献
75.
76.
The impact of rainfall pattern on the interrill erosion process is not fully understood despite its importance. Systematic rainfall simulation experiments involving various rainfall intensities, stages, intensity sequences, and surface cover conditions were conducted in this study to investigate their effects on the interrill erosion process. Five rainfall patterns designed with the same total kinetic energy/precipitation (increasing, decreasing, rising–falling, falling–rising and constant patterns) were randomly delivered to a pre‐wet clay loam soil surface at a 10° slope gradient. Significant differences in soil losses were observed among the different rainfall patterns and stages, but there was no obvious difference in runoff. Kinetic energy flux (KEr) was a governing factor for interrill erosion, and constant rainfall pattern (CST) produced nine times greater soil loss than runs with no KEr. Varied‐intensity patterns had a profound effect on raindrop‐induced sediment transport processes; path analysis results indicated that said effect was complex, interactive and intensity‐dependent. Low hydraulic parameter thresholds further indicated that KEr was the dominant factor in detaching soil particles, while overland flow mainly contributed to transporting the pre‐detached particles. This study not only sheds light on the mechanism of interrill sediment transport capacity and detachability, but also may provide a useful database for developing event‐based interrill erosion prediction models. Copyright © 2017 John Wiley & Sons, Ltd. 相似文献
77.
Abstract. The intestinal loops of two species of the genus Bathoxiphus (Entalinidae) and of Cadulus aberrans (Gadilidae) have been reconstructed from serial sections. The results are compared to the 'textbook scaphopod' Antalis dentalis having the hindgut coiled in three loops. Bathoxiphus ensiculus has four or five intestinal loops, B. sp. S 153 four, and C. aberrans two. The buccal pouch contents included Foraminifera in all species, with agglomerates of sediment being found only in Bathoxiphus and Antalis. The mean ratio of intestinal length to body length ranges from 1.05 in B. ensiculus , over 0.98 in the four-looped B. sp. S 153, to 0.7 in A. dentalis and 0.6 in the twice-looped C. aberrans. The correlation of intestinal length with diet—additional deposit-feeding in Bathoxiphus and highly specialized 'carnivory' in C. aberrans —is probable. Despite the differences in feeding ecology, the elongated hindgut of both deep-sea species of Bathoxiphus resembles the adaptations of some bivalves to poorly nutritious deep-sea sediments. 相似文献
78.
The chromitite occurrences in the Central Palawan ophiolite can be classified into four groups based on their chemistry and geological relationships. Group-I chromites from a deep tectonite level of the ophiolite complex show Cr/(Cr+Al) values of between 0.78 and 0.90, whereas group II from a shallower level gives values of 0.64–0.78, and group III from the immediate gabbro lower contact (dunite: cumulates and diapirs) show values of 0.5–0.64. Group-IV chromites from the gabbro zone have ratios around 0.38–0.5. Larger orebodies (type A), representing a first stage of partial melting of a primordial mantle, show Cr/Fe ratios between 2.5 and 4.5, whilst those of small chromitite bodies with a thin dunite envelope (type B) lie below 2.5. These small bodies belong to a second stage of magma generation. For both types the Cr/Fe ratio increases with the chromite/silicate ratio within individual occurrences. An additional method which may help to subdivide these chromitites involves their silicate and ore inclusions. The platinum-group minerals, for example, occur mainly in chromites of group II, type A. The intensive Tertiary tectonic activity to which the ophiolite was subjected during and after emplacement disturbs the regular pattern of the ophiolite stratigraphy and its chromitite occurrences. 相似文献