全文获取类型
收费全文 | 449篇 |
免费 | 89篇 |
国内免费 | 60篇 |
专业分类
测绘学 | 42篇 |
大气科学 | 96篇 |
地球物理 | 165篇 |
地质学 | 176篇 |
海洋学 | 63篇 |
天文学 | 10篇 |
综合类 | 5篇 |
自然地理 | 41篇 |
出版年
2023年 | 2篇 |
2022年 | 13篇 |
2021年 | 15篇 |
2020年 | 8篇 |
2019年 | 30篇 |
2018年 | 8篇 |
2017年 | 22篇 |
2016年 | 18篇 |
2015年 | 22篇 |
2014年 | 33篇 |
2013年 | 35篇 |
2012年 | 19篇 |
2011年 | 30篇 |
2010年 | 22篇 |
2009年 | 29篇 |
2008年 | 38篇 |
2007年 | 26篇 |
2006年 | 30篇 |
2005年 | 20篇 |
2004年 | 15篇 |
2003年 | 12篇 |
2002年 | 23篇 |
2001年 | 9篇 |
2000年 | 10篇 |
1999年 | 14篇 |
1998年 | 15篇 |
1997年 | 12篇 |
1996年 | 16篇 |
1995年 | 10篇 |
1994年 | 7篇 |
1993年 | 11篇 |
1992年 | 7篇 |
1991年 | 4篇 |
1990年 | 3篇 |
1989年 | 1篇 |
1988年 | 4篇 |
1986年 | 1篇 |
1985年 | 1篇 |
1980年 | 1篇 |
1979年 | 1篇 |
1954年 | 1篇 |
排序方式: 共有598条查询结果,搜索用时 515 毫秒
31.
地震时间序列的周期图分析方法和极大熵谱分析方法 总被引:1,自引:0,他引:1
利用华北地震区的地震资料(1000~1977),对地震时间序列进行了周期图分析和极大熵谱分析,提取了隐含在随机噪声中的隐含周期。结果表明,这两种方法所得结果很接近,地震应变能√Ei;释放的隐含周期利用周期图分析提取的主要周期是30年、245年和305年,极大熵谱分析方法提取的主要周期是30年、240年和300年。这三个主要周期存在“倍30”的关系,240年和300年周期是30年周期的整数倍。30年周期反映了各活跃幕中的幕式活动规律,300年周期同各活跃期高潮时段之间的时间差的平均值相符,华北自1000年以来的四个活跃期高潮时段之间的时间差平均值是300年。 相似文献
32.
江苏省近百年汛期旱涝变化的诊断分析 总被引:8,自引:2,他引:6
本文应用历史气候资料和现代降水记录,对近百年来汛期江苏省各区域各年代进行旱涝诊断分析,采用滑动平均方法探讨其变化趋势,并用最大搞谱方法提取显著周期。得出以下三个比较有意义的结论:(1)近百年来,汛期全省较易发生旱的灾害,20-30年代为旱灾濒发期;(2)淮北地区近年有向早年发展的趋势,江淮之间及苏南地区进入90年代以来向旱年发展的趋势则愈来愈明显;(3)全省具有2-3年、5-6年的旱涝周期。 相似文献
33.
中国最高、最低温度及日较差在海拔高度上变化的初步分析 总被引:1,自引:0,他引:1
本文利用中国740个气象台站1963~2012年均一化逐日最高温度和最低温度资料,分析了中国地区最高、最低气温和日较差变化趋势的区域特征及其与海拔高度的关系。结果表明:近50年气温的变化趋势无论是年或季节变化,最低温度的增温幅度都高于最高温度,且其增温显著区域都对应我国高海拔地区。除了春季,其他季节最高、最低温度及日较差的升温幅度随着海拔高度的升高而增大,其中最高温度的变化趋势与海拔高度的相关性最好。同一海拔高度上,最高、最低温度在不同年代的增幅具有不一致性:20世纪80年代,二者变化幅度最小;20世纪90年代,二者增幅最大,尤以低海拔地区最为明显。2000 m以上高海拔地区:最高温度和最低温度的变化趋势在20世纪90年代以前变化较小,而在近十年增幅十分明显;日较差季节变化大:夏季减小,冬季增加。20世纪90年代以前,最高、最低温度随海拔高度变化不大,而近20年随海拔高度升高,最高、最低温度的变化趋势几乎都是先减小后增加。高海拔地区比低海拔地区对全球变化反应更明显。 相似文献
34.
Holocene paleoenvironmental changes inferred from diatom assemblages in sediments of Kusawa Lake, Yukon Territory, Canada 总被引:1,自引:0,他引:1
The southwest Yukon Territory, Canada, is an important region for recovering sensitive records of Holocene paleoclimatic change. More information is needed, however, to constrain the timing of the major Holocene climatic transitions, and to understand associated impacts on different ecosystems. For example, paleolimnological studies have focused on small lakes and ponds, but the history of large lakes has received little study. We analyzed diatom assemblages, species richness, valve concentrations, and biogenic silica, in the sediments of Kusawa Lake (60°16.5'N; 136°10.9'W; 671 m a.s.l.) to reconstruct the responses of this large (surface area = 142 km2), deep (Zmax = 135 m) freshwater ecosystem to Holocene climatic transitions. Diatoms colonized the lake soon after ice retreat, around 11,000 cal yr BP; assemblages throughout the record were dominated by planktonic types. Diatom concentrations and biogenic silica were high during the Holocene Thermal Maximum between 10,700 and 7300 cal yr BP, then began to decrease in response to cooling associated with orbitally driven reductions in insolation. Diatom assemblages shifted towards taxa with lower surface water temperature optima after 8300 cal yr BP, perhaps in response to abrupt and progressive cooling. Our study confirms that diatom assemblages in large lakes are sensitive to regional-scale paleoclimatic changes. 相似文献
35.
Shengyi Mao Guodong Jia Xiaowei Zhu Nengyou Wu Daidai Wu Hongxiang Guan Lihua Liu 《海洋学报(英文版)》2022,41(8):22-30
Long-chain n-alkanols and n-alkanes in core sediments from the northern South China Sea (SCS) were measured to make a comparison during terrestrial vegetation reconstruction from ~42 ka to ~7 ka. The results showed that terrestrial vegetation record from long-chain n-alkanes matched well with previous studies in nearby cores, showing that more C4 plants developed during the Last Glacial Maximum (LGM) and C3 plants dominated in the interglacial period. However, these scenarios were not revealed by terrestrial vegetation reconstruction using long-chain n-alkanols, which showed C3 plant expansion during the LGM. The discrepancy during the interglacial period could be attributed to the aerobic degradation of functionalized long-chain n-alkanols in the oxygen-rich bottom water, resulting in poor preservation of terrestrial vegetation signals. On the other hand, the different advantages of functionalized n-alkanols and non-functional n-alkanes to record local and distal vegetation signals, respectively, may offer a potential explanation for the contradiction during the LGM when the SCS was characterized by low-oxygen deep water. Nevertheless, large variations on n-alkyl lipid compositions in C3/C4 plants could play a part in modulating sedimentary long-chain n-alkanols and n-alkanes toward different vegetation signals, thereby suggesting that caution must be taken in respect to the terrestrial vegetation reconstruction using long-chain n-alkanes and long-chain n-alkanols. 相似文献
36.
中国东部气温异常型与海表温度异常模关系的诊断 总被引:2,自引:1,他引:1
基于国家气候中心整编的160站常规观测气温资料和HADLEY中心的海表温度资料,应用最大协方差分析方法,诊断了中国东部各季节气温异常型和前期海表温度异常(SSTA)模的关系,并重点分析冬季气温与SSTA模的最佳耦合模态及海温异常对大气环流的影响。结果表明:中国东部四季气温异常型与前期海盆SSTA模的显著耦合关系表现出不同的特征。超前6个月的热带太平洋第二模和南印度洋第二模与东部地区冬季气温一致变化型耦合关系最佳。西南冷东北暖的气温异常型与超前4个月热带大西洋一致增暖模有最佳耦合关系。大气环流对与全区气温一致偏冷型对应的SSTA模的回归表现为:西伯利亚高压和阿留申低压增强,东亚大槽加深,中纬度西风加强。对与气温西南冷东北暖型对应的SSTA模的回归表现为:西伯利亚高压和阿留申低压略有增强,东亚大槽槽区附近位势升高,大槽变浅,槽线偏向西南,东部40°N以北风速加强,以南风速减弱。 相似文献
37.
颗粒态有机物在长江口及其邻近海域的夏季分布和影响因素初析 总被引:1,自引:1,他引:0
利用气相色谱法对长江口及其邻近海域的表层颗粒态木质素(p-lignin)进行测定和分析,结合粒度、有机碳(OC%)、叶绿素a(Chl a)、碳稳定同位素(δ13C)等参数研究颗粒态有机物的夏季分布,并对其分布影响因素进行了初步分析。结果表明,悬浮颗粒物粒度组成以粘土和粉砂为主,平均粒径为7.9μm;OC%的值为0.57—7.41%,Chl a的值为0.35—3.71μg/L,δ13C的值为-25.7‰—–16.6‰,在口门外水华站位出现OC%、Chl a和δ13C的最大值,表明浮游生物的现场生产是主要贡献;紫丁香基酚类(S)、香草基酚类(V)和肉桂基酚类(C)8种木质素酚单体的含量Λ8(相对于总有机碳的含量)为0.0406—1.47mg/100mg OC;紫丁香基系列与香草基系列的质量比值(S/V)的分布范围较宽,为0.5—1.6之间,均值为0.8;肉桂基含量与香草基含量比值(C/V)的分布范围为0.02—0.2之间,均值为0.09;香草基酚类的酸醛比值[(Ad/Al)v]在0.24—2.30之间。盐度、总悬浮颗粒物(TSM)浓度是控制长江口内区与邻近海域颗粒态有机物来源与分布差异的重要控制因素,颗粒态木质素在向海输送过程中还会受到矿物组分、生物降解、浮游生物现场生产等各种因素的作用,使其组成成分和性质发生改变。木质素等参数表明最大浑浊带尽管对颗粒态有机物向海输送有改造作用,但是影响区域有限。 相似文献
38.
The increasing trend of the Southern Annular Mode (SAM) in recent decades has influenced climate change in the Southem Hemisphere (SH).How the SAM will respond increased greenhouse gas concentrations in the future remains uncertain.Understanding the variability of the SAM in the past under a colder climate such as during the Last Glacial Maximum (LGM) might provide some understanding of the response of the SAM under a future warmer climate.We analyzed the changes in the SAM during the LGM in comparison to pre-industrial (PI) simulations using five coupled ocean-atmosphere models (CCSM,FGOALS,IPSL,MIROC,HadCM) from the second phase of the Paleoclimate Modelling Intercomparison Project (PMIP2).In CCSM,MIROC,IPSL,and FGOALS,the variability of the simulated SAM appears to be reduced in the LGM compared to the PI simulations,with a decrease in the standard deviation of the SAM index.Overall,four out of the five models suggest a weaker SAM amplitude in the LGM consistent with a weaker SH polar vortex and westerly winds found in some proxy records and model analyses.The weakening of the SAM in the LGM was associated with an increase in the vertical propagation of Rossby waves in southern high latitudes. 相似文献
39.
Richard C. Chiverrell Ian M. Thrasher Geoffrey S. P. Thomas Andreas Lang James D. Scourse Katrien J. J. van Landeghem Danny Mccarroll Chris D. Clark Colm Ó Cofaigh David J. A. Evans Colin K. Ballantyne 《第四纪科学杂志》2013,28(2):200-209
We present an 8000‐year history spanning 650 km of ice margin retreat for the largest marine‐terminating ice stream draining the former British–Irish Ice Sheet. Bayesian modelling of the geochronological data shows the ISIS expanded 34.0–25.3 ka, accelerating into the Celtic Sea to reach maximum limits 25.3–24.5 ka before a collapse with rapid marginal retreat to the northern Irish Sea Basin (ISB). This retreat was rapid and driven by climatic warming, sea‐level rise, mega‐tidal amplitudes and reactivation of meridional circulation in the North Atlantic. The retreat, though rapid, is uneven, with the stepped retreat pattern possibly a function of the passage of the ice stream between normal and adverse ice bed gradients and changing ice stream geometry. Initially, wide calving margins and adverse slopes encouraged rapid retreat (~550 m a?1) that slowed (~100 m a?1) at the topographic constriction and bathymetric high between southern Ireland and Wales before rates increased (~200 m a?1) across adverse bed slopes and wider and deeper basin configuration in the northern ISB. These data point to the importance of the ice bed slope and lateral extent in predicting the longer‐term (>1000 a) patterns and rates of ice‐marginal retreat during phases of rapid collapse, which has implications for the modelling of projected rapid retreat of present‐day ice streams. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
40.
Analysis of soil samples from above and below trimlines representing the upper limit of glacial erosion at the Last Glacial Maximum demonstrates that soils with prolonged weathering histories above such trimlines yield significantly different mineral magnetic signatures from soils below trimlines. The nature of the contrast is conditioned by lithology. Basalt soils above the trimline yield significantly higher values of concentration‐dependent magnetic parameters (χ, χarm, IRM3T, soft IRM and hard IRM) than those below the trimline, due probably to transformation of non‐magnetic iron‐bearing minerals into magnetic forms. Conversely, for sandstone soils most magnetic parameters yield significantly lower values for above‐trimline samples, probably reflecting loss of ferrimagnetic minerals by dissolution and oxidation to aniferrimagnetic forms. These significant contrasts represent a new approach to validating high‐level weathering limits as periglacial trimlines cut at the Last Glacial Maximum. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献