共查询到20条相似文献，搜索用时 0 毫秒
1.
YAO ZhengQuan XIAO GuoQiao & LIANG MeiYan State Key Laboratory of Loess Quaternary Geology Institute of Earth Environment Chinese Academy of Sciences Xi’an China Graduate University of the Chinese Academy of Sciences Beijing Institute of Geology Geophysics Beijing 《科学通报(英文版)》2010,55(9):787-790
Major element concentrations were analyzed on the sediments of a 203.6-m core from the North China Plain near Tianjin. The chemical index of alteration (CIA), Al2O3-(CaO+Na2O)-K2O diagram and elemental ratios, such as Al/K and Ti/Na, were used to reveal information of chemical weathering in the source regions since the late Pliocene. Results show that the fluvial materials in the North China Plain were derived from vast regions, which were in the early Na and Ca removal stage and underwent numerous upper-crustal recycling processes. Proxies of chemical weathering show a decreasing trend, in parallel with the global cooling since the late Pliocene, suggesting a strong role of the global cooing in controlling the continental chemical weathering intensity. 相似文献
2.
回顾北冰洋海平面观测和研究现状,总结了北冰洋海平面变化特征和变化机制。北冰洋海平面季节变化受海冰生消、蒸发降水和陆地径流季节变化的影响,由比容变化主导;年际到年代际海平面变化受北极涛动影响显著,可用风场异常导致的淡水分布来解释。盐比容变化是深水洋盆海平面变化的主导因素,由之引起的质量变化控制陆架海域和北冰洋平均的海平面变化。近期波弗特环流区域海平面上升极快,与波弗特高压持续增强及淡水积聚有关。气候变暖会导致北冰洋海平面持续上升。海冰快速减退和格陵兰岛冰川融化对北冰洋海平面变化的影响有待深入研究。数据的短缺和观测的不确定性目前仍然制约北冰洋海平面变化的研究工作,高分辨率数值模拟有望成为未来研究的重要工具。 相似文献
3.
^226Ra evidence for the ecosystem shift over the past 40 years in the North Pacific Subtropical Gyre 总被引：1，自引：0，他引：1
YANG JunHong CHEN Min QIU YuSheng LI YanPing MA Qiang LUE E ZHANG Run HUANG YiPu 《科学通报(英文版)》2007,52(6):832-838
Surface seawater was collected for ~(226)Ra measurement in the North Pacific Subtropical Gyre from July to October, 1999 and October to December, 2003. Combined with the historical data reported for this sea area, a declined trend of surface ~(226)Ra concentrations was observed since 1960s, indicating the ecosystem shift in response to global warming. On one side, the enhanced stratification of the upper water column resulting from global warming reduced the ~(226)Ra input from the depth, on the other, the temporal increase of biological production resulting from the climate-related ecosystem structure change strengthened the ~(226)Ra removal from the surface ocean. Both the physical and biological processes resulted in the decrease of surface ~(226)Ra concentrations in the North Pacific Subtropical Gyre. The temporal trend of surface ~(226)Ra concentrations was consistent with the trends of chlorophyll a, silicate, phosphate and primary production previously reported. This study provided ~(226)Ra evidence for the ecosystem shift under global change. 相似文献
4.
对我国的资产负债表日后事项准则同其他国家的进行比较，得出了一些差异，同时也分析了修订前后准则之间的差别，从而可以增强我们对中外有关财务会计信息的理解，进而借鉴他们的成功经验，促进我国会计的国际化的进程。 相似文献
5.
神农架大九湖12 500 a.B.P以来的孢粉植物群与气候变化 总被引：4，自引：0，他引：4
根据孢粉分析,将神农架大九湖12500a.B.P以来的孢粉植物群划分为15个演替阶段,从寒温带针叶林到北亚热带常绿阔叶混交林等多个植被型都有出现。植被带的垂直高度随气候变化上下移动,最冷时（12500－10700a.B.P）下移900－1100m,最暖时（5200－6450a.B.P）上移500－700m,孢粉植物群所反映的古气候变化具有明显的阶段性。12500－7400a.B.P气候相对冷干,但温度和降水回升很快,最冷时年平均温度和降水比今低6．1℃和195mm;7400－3300a.B.P气候最为暖湿,但仍有波动,最暖时年平均温度和降水比今高3．9℃和195mm;3300a.B.P以后气候小幅度波动,冷暖干湿多次交替。 相似文献
6.
XiangBin Cui Bo Sun Gang Tian XueYuan Tang XiangPei Zhang YunYun Jiang JingXue Guo Xin Li 《科学通报(英文版)》2010,55(4-5):425-431
Dome A, located in the central East Antarctic ice sheet (EAIS), is the highest summit of the Antarctic ice sheet. From ice-sheet evolution modeling results, Dome A is likely to preserve over one million years of the Earth’s paleo-climatic and -environmental records, and considered an ideal deep ice core drilling site. Ice thickness and subglacial topography are critical factors for ice-sheet models to determine the timescale and location of a deep ice core. During the 21st and 24th Chinese National Antarctic Research Expedition (CHINARE 21, 2004/05; CHINARE 24, 2007/08), ground-based ice radar systems were used to a three-dimensional investigation in the central 30 km×30 km region at Dome A. The successfully obtained high resolution and accuracy data of ice thickness and subglacial topography were then interpolated into the ice thickness distribution and subglacial topography digital elevation model (DEM) with a regular grid resolution of 140.5 m×140.5 m. The results of the ice radar investigation indicate that the average ice thickness in the Dome A central 30 km×30 km region is 2233 m, with a minimal ice thickness of 1618 m and a maximal ice thickness of 3139 m at Kunlun Station. The subglacial topography is relatively sharp, with an elevation range of 949–2445 m. The typical, clear mountain glaciation morphology is likely to reflect the early evolution of the Antarctic ice sheet. Based on the ice thickness distribution and subglacial topography characteristics, the location of Kunlun Station was suggested to carry out the first high-resolution, long time-scale deep ice core drilling. However, the internal structure and basal environments at Kunlun Station still need further research to determine. 相似文献
7.
8.
XiangBin Cui Bo Sun Gang Tian XueYuan Tang XiangPei Zhang YunYun Jiang JingXue Guo Xin Li 《科学通报(英文版)》2010,55(24):2715-2722
During the 24th Chinese National Antarctic Research Expedition (CHINARE 24, 2007/08), a ground-based ice radar was used to survey ice thickness and subglacial topography along the 1170 km traverse between Zhongshan and Dome A in East Antarctic ice sheet (EAIS). Ice-bedrock interface was detected along 82% of the traverse and data was collected at a horizontal resolution of <5.6 m. The data was processed to produce curves of ice thickness distribution and subglacial topography along the traverse. The results indicate that, along the traverse, the average ice thickness is 2037 m, smaller than the average ice thickness in EAIS; the thickest ice is at 730 km, and the thinnest ice (891 m) is at the edge of the ice sheet, but the slightly larger ice thickness (1078 m) in inland appears at 1020 km; the average subglacial topography elevation is 728 m, greatly larger than the average value in EAIS, and the largest elevation reaches up to 2650 m at 1034 km. The lowest terrain is located at 765 km. In further inland of 900–1170 km, the subglacial topography is relatively high due to the existence of the Gamburtsev Subglacial Mountains in the region. Generally, the influence of subglacial topography on ice surface is not significant, except at 900 km where great rise of subglacial topography causes evident uplift of ice surface. Where ice-bedrock interface was detected, the frequent and strong change of ice thickness and subglacial topography in small-scale means large bedrock roughness along the traverse, and is considered as the result of the integrated influence of ice flow, basal environments and geology. The segment where bedrock was not detected has very large ice thickness. The strong ice flow there also makes internal structure more complicated and induces serious attenuation of radar signals. 相似文献
9.
Xueyuan Tang Zhanhai Zhang Bo Sun Yuansheng Li Na Li Wang Bangbing Xiangpei Zhang 《自然科学进展》2008,18(2):173-180
The three-dimensional finite difference thermodynamic coupled model on Antarctic ice sheet, GLIMMER model, is described. An idealized ice sheet numerical test was conducted under the EISMINT-1 benchmark, and the characteristic curves of ice sheets under steady-state was obtained. Based on this, this model was simplified from a 3-dimensional one to 2-dimensional one. Improvement of the difference method and coordinate system was proposed. Evolution of the 2-dimensional ice flow was simulated under coupled temperature field conditions. The results showed that the characteristic curves deriving from the conservation of the mass, momentum and energy agree with the results of ice sheet profile simulated with GLIMMER model and with the theoretical results. The application prospect of the simplified 2-dimensional ice flow model to simulate the relation of age-depth-accumulation rate in Dome A region was discussed. 相似文献
10.
Zhenxia Liu Tiegang Li Peiying Li Qiyu Huang S. Berne Y. Saito Zhenbo Cheng Gangjian Wei Lejung Liu Zhen Li 《科学通报(英文版)》2001,46(2):153-157
Planktonic foraminiferal δ 18O record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The δ 18O curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling factor. 相似文献
11.
Xueyuan Tang Zhanhai Zhang Bo Sun Yuansheng Li Na Li Wang Bangbing Xiangpei Zhang 《自然科学进展(英文版)》2008,18(2):173-180
The 3-dimensional finite difference thermodynamic coupled model on Antarctic ice sheet, GLIMMER model, is described. An idealized ice sheet numerical test was conducted under the EISMINT-1 benchmark, and the characteristic curves of ice sheets under steady state were obtained. Based on this, this model was simplified from a 3-dimensional one to 2-dimensional one. Improvement of the difference method and coordinate system was proposed. Evolution of the 2-dimensional ice flow was simulated under coupled temperature field conditions. The results showed that the characteristic curves deriving from the conservation of the mass, momentum and energy agree with the results of ice sheet profile simulated with GLIMMER model and with the theoretical results. The application prospect of the simplified 2-dimensional ice flow model to simulate the relation of age-depth-accumulation in Dome A region was discussed. 相似文献
12.
渤海连续冰层关键力学参数预报模式 总被引：4，自引：0，他引：4
为反映海冰的物理和力学特性,利用实验室获取水平方向加载冰样的单轴压缩强度、三点弯曲强度和侧限剪切强度与孔隙率间的统计关系,把海冰温度、盐度和密度对强度的效应统一起来,建立了预报模式。之后,依据渤海海冰多年调查资料和近期研究成果,将冰层内的温度、盐度和密度表示成气温、水温和冰厚的函数,获得冰层的孔隙率剖面,进而得到冰层力学参数剖面。在选取冰层平均强度时还考虑了渤海冰层底部骨架部分有厚度无强度的特点,实现了利用已知冰厚、气温和水温预报冰层水平方向强度分布的目标。 相似文献
13.
通过对上海地区鹤鸣孔和东海1井两个钻孔进行孢粉分析鉴定和对比,结合AMS14C测年等资料,划分出了6个孢粉组合带,恢复了本区的植被演化和气候波动的6个阶段.对鹤鸣孔的大西洋期、亚北方期和亚大西洋期各划分出了两个孢粉组合亚带,反应了大气候环境下气候的次一级波动.在晚更新世晚期的硬绿色粘土中还发现了以环纹藻为主的孢粉组合,从孢粉学角度上证实了这一硬绿色粘土层“水成沉积”的观点. 相似文献
14.
孙宗富 《北京交通大学学报(自然科学版)》1987,(2)
浮冰对桥墩的作用力在某些情况下是一项重要的荷载。冰的挠曲强度远小于其挤压强度。在桥墩上设置破冰锥体,可大大减轻浮冰的水平压力,同时还可把大块浮冰破碎成小块浮冰,有可能减少产生冰坝、冰塞。在北方地区河道中修建大跨度桥梁时,采用此方案,可能产生有利的效果。这一设想也可应用到有类似冰害的结构中。 相似文献
15.
CHENG xiao LI XiaoWen SHAO Yun LI Zhen 《科学通报(英文版)》2007,52(3):358-366
Grove Mountain is an important nunatak region on East Antarctic Glacier that blocks the ice flow to- ward Lambert Glacier. The existence of nunataks and subglacial mountains leads to complex ice flow patterns, which are difficult to be measured by conventional ground-based methods. In this study, several JERS-1 and ERS-1/2 SAR images covering this area are used for 3-pass and 4-pass differential interferometric processing. The ice flow field of Grove Mountain and the eastern zone are derived and validated with related knowledge. The research shows that DINSAR is an effective method for meas- uring complex ice flow in Antarctic inland glacier. L-band DINSAR is more suitable for mid or fast ice flow than C-band over this region. 相似文献
16.
Quantitative estimates of the precipitation on different lake sites at the three time phases, i.e. 30, 18, and 6 kaBP by using the combined hydrological and energy budget model, make it possible to reconstruct the large changes in spatial precipitation patterns since the late Quaternary. The results have shown that, very strong precipitation occurred in western China at 30 kaBP, suggesting extremely enhanced summer Indian monsoon. Precipitation was high in southwestern China at 18 kaBP, especially the southern part of southwestern China, due to the southward shift of the westerlies and a low pressure cell occurred over northern India. The precipitation at 6 kaBP shows the complicated patterns for different regions of China, suggesting different climate dynamics. The comparison of the independent lake level/ area-based reconstruction of precipitation and the palaeo-climate simulations is an effective way for the validation ofeach method to reconstruct the palaeo-precipitation quantitatively, and for understanding the dynamic mechanisms of climatic change. 相似文献
17.
The late Quaternary paleosols in the Yangtze Delta area developed in the period of 25 000-12 000 aBP. Phytolith ratios (value A) of contents of fan, square and rectangle types indicating the warm and humid climate to those of bar, hat and point types indicating cold and dry climates decrease upwards overall on profiles of the paleosols, suggesting that the climates turned from warm and humid to cold and dry. So, the paleosols developed mainly during the regression before the last glacial maximum. Changes of value A indicate no trend of warming, suggesting that the transgression was rapid after the last glacial maximum. The development of the paleosols exhibited obvious stages, which were controlled remarkably by transgression and regression : Ⅰ . Period of alternation of deposition and pedogenesis, which was from the occurrence of regresson before the last glacial maximum to the time when sea levels fell close to the lowest; Ⅱ . Exposure period with continual pedogenesis, which was terminated when the paleosols were drown in the post-glacial transgression; Ⅲ . Period of being drown and buried, the paleosols were buried by marine sediments, and reworked by early diagenesis. 相似文献
18.
杜君健 《太原师范学院学报(自然科学版)》2012,(3):122-127,131
文章试图通过对太阳周期性变化影响下的各类气候事件、小冰期、冰期——间冰期周期性气候脉动规律的均衡趋势及全球气温均衡规律的研究,揭示全球变暖对于全球繁荣的积极意义,以及全球变冷对于造成全球萧条及更加严重的人类文明终结的事实.而文章试图阐述全球变冷的消极意义对于全球的危害更加严重. 相似文献
19.
ZHANG Mingjun LI Zhongqin XIAO Cunde YANG Huian KANG Jiancheng LI Jun 《自然科学进展(英文版)》2001,11(7):525-528
A 50 m firn core drilled in Princess Elizabeth Land, Antarctica, during the 1996/1997 Chinese First Antarctic Inland Expedition, has been measured for б18O and major ions. Based on these data, the features of the climate change in the investigated region in the past 250 years have first been studied. In the past 250 years, the change trend of climate in this region can be divided into two periods by the year 1860. Both the temperature and accumulation rate display increasing trend before 1860, while after 1860, the decreasing trend of the temperature is obvious but the change of the accumulation rate is not clear. Although both the temperature and the accumulation rate are increasing in the past 50 years, they are not the highest values in the past 250 years. So it is clear that the climate change in this region during this period does not reflect recent global wanning. 相似文献
20.