全文获取类型
收费全文 | 827篇 |
免费 | 181篇 |
国内免费 | 160篇 |
专业分类
测绘学 | 10篇 |
大气科学 | 405篇 |
地球物理 | 399篇 |
地质学 | 197篇 |
海洋学 | 28篇 |
天文学 | 3篇 |
综合类 | 19篇 |
自然地理 | 107篇 |
出版年
2024年 | 4篇 |
2023年 | 10篇 |
2022年 | 20篇 |
2021年 | 37篇 |
2020年 | 44篇 |
2019年 | 39篇 |
2018年 | 26篇 |
2017年 | 38篇 |
2016年 | 26篇 |
2015年 | 41篇 |
2014年 | 47篇 |
2013年 | 77篇 |
2012年 | 45篇 |
2011年 | 56篇 |
2010年 | 28篇 |
2009年 | 68篇 |
2008年 | 60篇 |
2007年 | 57篇 |
2006年 | 51篇 |
2005年 | 60篇 |
2004年 | 40篇 |
2003年 | 24篇 |
2002年 | 33篇 |
2001年 | 22篇 |
2000年 | 21篇 |
1999年 | 20篇 |
1998年 | 21篇 |
1997年 | 16篇 |
1996年 | 13篇 |
1995年 | 14篇 |
1994年 | 22篇 |
1993年 | 12篇 |
1992年 | 20篇 |
1991年 | 15篇 |
1990年 | 11篇 |
1989年 | 4篇 |
1988年 | 4篇 |
1987年 | 7篇 |
1986年 | 3篇 |
1985年 | 1篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1982年 | 3篇 |
1980年 | 2篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1976年 | 1篇 |
排序方式: 共有1168条查询结果,搜索用时 15 毫秒
91.
A comparison of TRMM to other basin-scale estimates of rainfall during the 1999 Hurricane Floyd flood 总被引:5,自引:2,他引:3
The volumetric rainfall attributed to Hurricane Floyd in 1999 was computed for the bulk of the Tar, Neuse, and Cape Fear River
Basins in eastern North Carolina, USA from the Tropical Rainfall Measuring Mission (TRMM) Multi-Satellite Precipitation Analysis
(TMPA) research product, and compared with volumes computed using kriged gauge data and one centrally located radar. TMPA
showed similar features in the band of heaviest rainfall with kriged and radar data, but was higher in the basin-scale integrations.
Furthermore, Floyd’s direct runoff volumes were computed and divided by the volumetric rainfall estimates to give runoff coefficients
for the three basins. The TMPA, having the larger storm totals, would suggest greater infiltration during Floyd than the gauge
and radar estimates would. Finally, we discuss a concept for adjusting the United States Department of Agriculture Natural
Resources Conservation Service rainfall-runoff model when predicting discharge values from real-time TMPA in ungauged river
basins.
相似文献
Scott CurtisEmail: |
92.
93.
94.
95.
Priya Narayanan Ashoke Basistha Sumana Sarkar Sachdeva Kamna 《Comptes Rendus Geoscience》2013,345(1):22-27
Spatial and temporal variability of rainfall over different seasons influence physical, social and economic parameters. Pre-monsoon (March, April and May – MAM) rainfall over the country is highly variable. Since heat lows and convective rainfall in MAM have an impact on the intensity of the ensuing monsoons, hence the pre-monsoon period was chosen for the study. The pre-whitened Mann Kendall test was used to explore presence of rainfall trend during MAM. The results indicate presence of significant (at 10% level) increasing trend in two stations (Ajmer, Bikaner). The practical significance of the change in rainfall was also explored as percentage changes over long term mean, using Theil and Sen's median slope estimator. Forecast using univariate ARIMA model for pre-monsoon months indicates that there is a significant rise in the pre-monsoon rainfall over the northwest part of the country. 相似文献
96.
城市化对北京地区日照时数和云量变化趋势的影响 总被引:4,自引:1,他引:3
利用1961~2008年北京城区和郊区12个台站的气候观测资料,采用趋势分析和累积距平的方法,研究了北京城区和郊区近48年的日照时数、总云量及低云量的年际和四季变化趋势,并探讨了城市化进程对日照和云量变化的影响。结果表明:近48年来,城区的总云量和日照时数呈减少趋势,但低云量呈增加趋势;郊区的总云量和低云量呈增加趋势,而日照时数呈减少趋势;具体到年代变化,1980年代初以后,城区总云量呈减少趋势,且1990年代减少的趋势最为明显,2000年后,城区总云量变化发生逆转,呈显著增加趋势。对于低云量,1960年代到1980年代,城区郊区低云量呈波动减少趋势,而1990年代到2000年代后呈波动增加趋势。对于日照时数,1960年代到1980年代城区郊区日照时数均呈增加趋势,1990年代至2000年代则呈明显减少的趋势。低云量与日照时数表现出明显负相关特征,这与北京城市化发展对区域气候的影响有密切的关系。 相似文献
97.
98.
利用热带降雨观测计划(TRMM)卫星雷达降雨数据驱动分布式陆面水文模型,研究流域尺度陆面水文过程,评估该数据在水文模拟与预报等研究领域的性能。通过与实测雨量资料比较,验证TRMM卫星雷达降雨数据的质量。分别将TRMM卫星雷达降雨与观测降雨作为耦合模型的气象输入,模拟和研究淮河流域1998~2003年的陆面水文过程时空变化。结果表明,TRMM卫星雷达降雨数据能够很好地描述降雨的时空分布,利用TRMM降雨模拟的结果与利用观测降雨模拟的结果精度相当;模拟流量与实测资料基本吻合。卫星雷达降雨数据在陆面水文过程研究中具有广泛的应用前景。 相似文献
99.
Rainfall, throughfall, stemflow and spring were studied in a secondary forest during a wet season from April to August in
2006. Some of the chemicals in throughfall, stemflow and spring were increased in contrast with incident rainfall. Specifically,
Cl−, HCO3
−, Na+ and Ca2+ were leached negatively in throughfall, but K+ and Mg2+ were leached positively. In stemflow, Cl− and Na+ were leached negatively, the others were leached positively and their concentrations were higher than those in throughfall.
Total carbon, organic carbon and inorganic carbon in throughfall and stemflow were increased as rainfall went through the
secondary forest. The concentration of free CO2 in rainfall was lower than both, throughfall and stemflow; the relationship between total acidity and free CO2 was linear. pH of throughfall and stemflow , such as maximum, minimum and mean, were lower than that of rainfall and the
extent of pH in spring was changed minimally. We came to a conclusion that rainfall via the secondary forest can lead to further
erosion, accelerate the biogeochemical cycle in epikarst zone, enhance the effective state of alkali elements in the soil,
supply vegetation with more nutrients and advance vegetation’s growth and succession, which are reasonably sufficient to form
a stable karst ecosystem. 相似文献
100.
Keming Tian Jingshi Liu Shichang Kang Iain B. Campbell Fei Zhang Qianggong Zhang Wei Lu 《Environmental Geology》2009,57(8):1775-1784
Hydrothermal processes and the regimes of frozen soil formed in alpine regions with glaciers and lake area are complex and
important for ecological environment but have not been studied in Tibet. Based on soil temperature and moisture data from
October 2005 to September 2006 collected in the Nam Co lake basin, Tibetan Plateau (TP), those questions were discussed. The
mean annual air temperature was −3.4°C with 8 months below 0°C. Air and soil temperature varied between −25.3~13.1°C and −10.3~8.8°C,
respectively. Soil moisture variations in the active layer were small with the minimum value of 1.4%, but were influenced
greatly by snowmelt, rainfall and evaporation, varying up to 53.8%. The active layer froze later, thawed earlier and was thinner,
however, the lower altitude limit of permafrost is higher than that in most areas of TP. The effects of soil moisture (unfrozen
water content) on soil temperature, which were estimated through proposed models, were more significant near ground surface
than the other layers. The surface soil temperature decreased with snowcover, the effect of cold snow meltwater infiltration
on soil thermal conditions was negligible, however, the effect of rainfall infiltration was evident causing thermal disruptions. 相似文献