中国主要沙尘暴源区稳定同位素背景值初步研究   总被引：1，自引：1，他引：0  

杜宏印  郭浩  崔向慧  芦霞  辛智鸣 《中国沙漠》2016,36(3):604-609

采用稳定同位素方法,对中国沙尘暴主要源区塔克拉玛干沙漠、柴达木盆地沙漠、库姆塔格沙漠、腾格里沙漠、乌兰布和沙漠、毛乌素沙地进行了采样分析。结果表明:22个样品¹⁸O和³⁰Si的δ值变化范围分别为9.6~14.8和-1.7~0.3,其中¹⁸O的δ值库姆塔格沙漠最大,柴达木盆地沙漠最小,³⁰Si的δ值毛乌素沙地最大,柴达木盆地沙漠最小。总体而言,样品中³⁰Si的δ值的变异系数要比¹⁸O的δ的变异系数大,因此³⁰Si更适合用于沙尘溯源。相邻的沙漠(沙地)呈现出³⁰Si的δ值相近的趋势,因此推断相邻的沙漠(沙地)沉积物可能来自同一地区。  相似文献   

Distribution of ice thickness and subglacial topography of the “Chinese Wall” around Kunlun Station,East Antarctica   总被引：1，自引：0，他引：1  

Xiang-Bin Cui  Bo Sun  Xiao-Gang Su  Jing-Xue Guo 《应用地球物理》2016,13(1):209-216

As fundamental parameters of the Antarctic Ice Sheet, ice thickness and subglacial topography are critical factors for studying the basal conditions and mass balance in Antarctica. During CHINARE 24 (the 24th Chinese National Antarctic Research Expedition, 2007/08), the research team used a deep ice-penetrating radar system to measure the ice thickness and subglacial topography of the “Chinese Wall” around Kunlun Station, East Antarctica. Preliminary results show that the ice thickness varies mostly from 1600 m to 2800 m along the “Chinese Wall”, with the thickest ice being 3444 m, and the thinnest ice 1255 m. The average bedrock elevation is 1722 m, while the minimum is just 604 m. Compared with the northern side of the ice divide, the ice thickness is a little greater and the subglacial topography lower on the southern side, which is also characterized by four deep valleys. We found no basal freeze-on ice in the Gamburtsev Subglacial Mountains area, subglacial lakes, or water bodies along the “Chinese Wall”. Ice thickness and subglacial topography data extracted from the Bedmap 2 database along the “Chinese Wall” are consistent with our results, but their resolution and accuracy are very limited in areas where the bedrock fluctuates intensely. The distribution of ice thickness and subglacial topography detected by ice-penetrating radar clarifies the features of the ice sheet in this “inaccessible” region. These results will help to advance the study of ice sheet dynamics and the determination of future locations of the GSM’s geological and deep ice core drilling sites in the Dome A region.  相似文献   

Altitude of the upper boundary of AAR based on observations of ion beams in inverted-V structures: A case study     

YanBo Cui  SuiYan Fu  QiuGang Zong  Lun Xie  WeiJie Sun  Duo Zhao  Tong Wu  George Parks 《中国科学:地球科学(英文版)》2016,59(7):1489-1497

Outflowing ion beams forming four successive inverted-V structures in the energy-time spectrograms of H+, He+, and O+ were observed at an altitude of 3.4 RE by Cluster satellites travelling above the auroral acceleration region (AAR) in the southern hemisphere on February 14, 2001. Energization by negative U-shaped potential structures in the AAR is believed to be responsible for the formation of these outflowing ion inverted-V structures. Thus, utilizing the different motion properties of the three ion species, the altitude of the upper boundary of the AAR is estimated to be ~11100 km. Moreover, based on multi-satellite observations, each of these U-shaped potential structures involved in this event crosses the latitudinal direction at ~0.4°–1° invariantlatitude (ILAT), moving poleward at an average speed of ~0.2° ILAT per minute, before disappearing at ~71.5° ILAT.  相似文献   

Has the upper portion of the Japan Sea Proper Water formation really been enhancing?     

Yanlin Cui  Tomoharu Senjyu 《Journal of Oceanography》2012,68(4):593-598

Weakening of the upper portion of the Japan Sea Proper Water formation was detected based on the dissolved oxygen concentration and potential temperature from 1970 to 2004, unlike the suggestion of previous studies that it has been enhanced since the 1970s. The revealed warming and decreasing trends in DO concentration throughout the water column indicate that the conveyor belt system in the Japan Sea is still slowing down even in the intermediate layers, though a relatively active dissolved oxygen supply into the intermediate layers is suggested. This fact leads us to modify the previous concept about the water mass formation; though a relatively active formation of the intermediate water mass occurs, the deep water formation is not counterbalanced by the intermediate water formation, and the overall Japan Sea Proper Water formation has been stagnating since the 1970s.  相似文献   

Evaluation and fusion of SST data from MTSAT and TMI in East China Sea, Yellow Sea and Bohai Sea in 2008   总被引：1，自引：0，他引：1  

伍玉梅  申辉  崔雪森  杨胜龙  樊伟 《中国海洋湖沼学报》2012,30(4):697-702

Two typical satellite sea surface temperature (SST) datasets, from the Multi-functional Transport Satellite (MTSAT) and Tropical Rainfall Measuring Mission Microwave Imager (TMI), were evaluated for the East China Sea, Yellow Sea, and Bohai Sea throughout 2008. Most monthly-mean availabilities of MTSAT are higher than those of TMI, whereas the seasonal variation of the latter is less than that of the former. The analysis on the one-year data shows that the annual mean availability of MTSAT (61%) is greater than that of TMI (56%). This is mainly because MTSAT is a geostationary satellite, which achieves longer observation than the sun-synchronous TMI. The daily availability of TMI (28%-75%) is more constant than that of MTSAT (9%-93%). The signal of infrared sensors on MTSAT is easily disturbed on cloudy days. In contrast, the TMI microwave sensor can obtain information through clouds. Based on in-situ SSTs, the SST accuracy of TMI is superior to that of MTSAT. In 2008, the root mean square (RMS) error of TMI and MTSAT were 0.77 K and 0.84 K, respectively. The annual mean biases were 0.14 K (TMI) and -0.31 K (MTSAT). To attain a high availability of SSTs, we propose a fusion method to merge both SSTs. The annual mean availability of fusion SSTs increases 17% compared to MTSAT. In addition, the availabilities of the fusion SSTs become more constant. The annual mean RMS and bias of fusion SSTs (0.78 K and -0.06 K, respectively) are better than those of MTSAT (0.84 K and -0.31 K).  相似文献   

交通路况基态修正模型及其效率分析     

李婷  徐柱  卢彩霞  于冰  李木梓  黄萌萌 《地球信息科学学报》2012,14(6):712-718

 交通路况在时间上和空间上具有连续变化的特征,在时空维度上对交通路况进行高分辨率采样得到的数据,对研究交通路况的时空动态十分有利。但长时间大范围的高分辨率交通路况信息数据量巨大,给数据的组织和管理带来了困难。目前,尚没有一种成熟的时空数据模型对高时空分辨率交通路况数据进行高效(顾及数据存储与访问效率)的组织管理。本文提出一种基于线性参照系统的交通路况基态修正模型。此模型应用基态修正模型的基本思想,在时间维度上对交通路况数据进行无损压缩,又引入动态分段技术和线性参照系统,以路划作为交通路况载体,在空间维度上对交通路况数据进行压缩存储。利用成都市区真实交通路况数据,本文验证了此模型的有效性,比较了6种不同参数下交通路况基态修正模型的存储和访问效率,给出了最佳模型建议。  相似文献   

基于物联网的心音监测系统的设计与实现     

杨波  张翠  李庆  赵旭  唐慧 《成都信息工程学院学报》2012,27(5):453-457

针对行动不便或有长期监测需求的心血管疾病患者,研发了一套远程心音信号监测系统,在家中患者可以实现心脏状况的检测。系统由心音信号采集器、智能手机和远端监护计算机构成。心音信号经过心音信号采集器处理后,通过电信网络传送到医护中心的监护计算机上。借助于Visual C++6.0开发平台,系统实现了患者数据管理,对心音信号进行希尔伯特黄变换方法的去噪处理,对不正常心音情况进行疾病报警。系统成本低、安全无创,监护软件能够采集、处理、显示、存储、分析心音信号,文中通过对13例心音数据进行处理,验证了系统的有效性和可行性。  相似文献   

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高宁  崔希民  高彩云  王果  赵万东 《大地测量与地球动力学》2012,32(1):114-117

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山东省GNSS基准站的建设     

冯志军  王强  崔居全  王伟  陈安方  刘作华  申健  潘双进 《大地测量与地球动力学》2012,32(Z1):76-80

介绍山东省GNSS基准站土建、供电避雷、通讯以及仪器设备安装调试的技术工艺.  相似文献   

巴丹吉林沙漠高大沙山沉积物粒度特征及其与植被、地貌关系   总被引：1，自引：1，他引：0  

崔徐甲  董治宝  罗万银  逯军峰  李继彦  王蒙  焦原磊  刘铮瑶  张玉  李超 《中国沙漠》2015,35(4):857-864

沙丘形成演变是风-沉积物-其他地理因子相互反馈作用的一个动态系统过程,粒度可以揭示其中包含的部分环境信息并被广泛应用于风沙地貌研究。本文分析了巴丹吉林沙漠伊和吉格德湖高大沙山区沉积物粒度特征及其与植被、地貌形态的关系。结果表明:迎风坡中上部及中部剖面各层沉积物主粒径均一,分别为中沙、细沙;迎风坡中下部及底部剖面细沙、中沙及粗沙等不同主粒径层交替,粒配复杂,其成因与粗沙粒保护作用、风向季节变化及地质时期气候变迁等因素有关;背风坡表层沉积物以细沙为主,趋向底部粗沙、中沙及极细砂增多,说明不同粒径对风及重力作用的响应存在差异;粒度参数散点图可以区分不同部位样品,趋向迎风坡底部剖面,沙粒分选性变差,正偏、负偏及近对称沙层交替,说明风力分选作用在不同部位差异明显及存在其他外力作用;沙层粒配影响植被多样性,迎风坡中上部中沙含量高,背风坡表层中部偏上极细沙及大于2.65 Φ细沙含量突然增加,是植被影响粒配的反映;迎风坡沉积环境的差异,说明随地质时期气候变迁,沙山形成可能经历了两个重要阶段,一是早期风力和水动力交替影响、具有风成与非风成环境交替特征的基底形成时期,二是以风力作用为主的现代沙山形成时期。  相似文献