合作原则对大学英语四六级听力测试对话的指导   总被引：1，自引：0，他引：1  

黄舒 《成都信息工程学院学报》2008,23(3):349-353

听力理解在英语四六级考试中占有重要的比例,提高听力水平既是教学的要求也是通过大学英语四六级考试的关键。因此在分析近年来大学英语四六级听力理解对话部分的难点的基础上,提出合作原则及相关理论对解答听力理解对话部分具有指导作用。  相似文献   

南海北部C4站柱状沉积中的孢粉组合及其古环境意义     

张玉兰  龙江平 《海洋学研究》2009,27(2):1-6

对南海北部C4站柱状沉积剖面进行了高分辨率孢粉、藻类成分的分析和研究,同时测定了部分样品的AMS14C年代,划分了该站柱状沉积物地层时代,相应恢复了南海北部9 800 a B P以来植被、气候、环境的3个演替阶段.南海北部C4站从下至上可划分成3个孢粉组合带,依次为:1带(258～194 cm):以Pinus-Quercus(常绿)-Polypodiaceae-Pterdium-Pteris-Dicranopteris-Adiantum为主孢粉带;2带(194～94 cm):以Pinus-Quercus(常绿)-Pteridium-Polypodiaceae-Microlepia-Dicranopteris为主孢粉带;3带(94～4 cm):以Pinus-Pteridium-Polypodiaceae-Quercus(常绿)-Microlepia-Dicranopteris为主孢粉带.与3个孢粉带相对应的古植被阶段依次为:伴有针叶树的常绿阔叶、落叶阔叶混交林,热带半常绿季雨林,热带常绿阔叶、落叶阔叶混交林,与周边地区的植被演替相一致.由此可见,研究区经历了全新世早期气候转暖,中期气候炎热、干湿季明显、海平面上升以及晚期气候暖热、湿润3个古环境演变阶段.  相似文献   

浅谈基于全数字摄影工作站的等高线立体采集方法     

石海燕 《测绘与空间地理信息》2009,32(4):94-95

地形图等高线是4D产品的基本要素,等高线的采集精度直接决定着4D产品的质量.根据作业实践,提出等高线立体采集的方法与采集时常见问题及其对策.本文对类似的4D产品的等高线采集与编辑有一定的借鉴和参考价值.  相似文献   

DLG质量检查探究   总被引：1，自引：1，他引：0  

黄海英  钟生伟  胡景海 《地理空间信息》2009,7(6):135-137

介绍使用4DChecker进行质量检查时所需检查的内容,分析质量问题产生的原因,阐述质量检查的方法（手段）,总结4DChecker软件的应用方法。  相似文献   

2DVAR方法在台湾海峡海表流场融合中的应用          下载免费PDF全文

邹婷  朱大勇  张俊鹏  王晓春 《应用海洋学学报》2020,39(4):469-479

高频地波雷达可以提供沿岸大面积海表流的观测,但单个地波雷达只能提供径向流观测。本研究发展了一套二维变分(Two-Dimensional VARiational Method， 2DVAR)数据融合方法，将台湾海峡海域的地波雷达径向流数据与ROMS (Regional Ocean Model System)模式输出结果进行融合，得到一套较好的融合产品。结果显示，融合产品与雷达径向流的平均相对误差相较于模式输出与雷达径向流的平均相对误差由9.70%降低至1.54%。为进一步检验融合方法，设计了两种独立样本试验。试验一将雷达径向流按空间均匀划分为融合样本与独立样本，使用雷达融合样本与模式输出进行融合，此时融合结果的平均均方根误差(Root Mean Square Error, RMSE)相较于模式输出由0.41 m/s降低至0.19 m/s。试验二将雷达径向流和模式输出在空间上都均匀划分为融合样本与独立样本，对两种数据的融合样本进行融合，使用TC (Triple Collocation)方法估计模式输出、雷达观测与融合结果的误差方差，此时融合结果的平均误差方差最小，且其误差方差相对于独立的雷达径向流与模式输出在远岸处有明显减小。以上结果都表明融合数据更加接近实际海流，证明了2DVAR方法融合海表流的有效性。  相似文献   

GAIM电离层同化方法进展   总被引：2，自引：0，他引：2  

黄珹  郭鹏  洪振杰  严豪健  胡小工  丁金才  张训械 《天文学进展》2007,25(3):236-248

电离层是复杂的空间层结,其变化受太阳活动强度、地球磁场等因素影响。随着空间技术发展的需求,电离层天气变化成为目前空间天气预报最重要的内容之一。最近10年,人们利用卫星在电离层观测方面取得了重大进展,尤其引人注意的是:无线电掩星观测技术正走向应用的新阶段,加上已经建立的全球大量的地基GPS观测网,它们不仅为电离层动力学模式研究提供了丰富的电离层资料,而且为电离层预报提供了很好基础。因此,电离层天气预报成为当前重要的、前瞻性的研究方向,电离层资料同化是电离层预报最重要的研究内容之一。该文系统介绍这方面国际动态,重点是美国的USC/JPL和犹他州大学开展全球电离层同化模型研究、全球电离层同化研究的进展,以及在电离层天气预报中应用的初步成果。  相似文献   

Intermittent jet activity in the radio galaxy 4C 29.30?     

M. Jamrozy  C. Konar  D. J. Saikia  &#;. Stawarz  K.-H. Mack  A. Siemiginowska 《Monthly notices of the Royal Astronomical Society》2007,378(2):581-593

We present radio observations at frequencies ranging from 240 to 8460 MHz of the radio galaxy 4C 29.30 (J0840+2949) using the Giant Metrewave Radio Telescope (GMRT), the Very Large Array (VLA) and the Effelsberg telescope. We report the existence of weak extended emission with an angular size of ∼520 arcsec (639 kpc) within which a compact edge-brightened double-lobed source with a size of 29 arcsec (36 kpc) is embedded. We determine the spectrum of the inner double from 240 to 8460 MHz and show that it has a single power-law spectrum with a spectral index of ∼0.8. Its spectral age is estimated to be ≲33 Myr. The extended diffuse emission has a steep spectrum with a spectral index of ∼1.3 and a break frequency ≲240 MHz. The spectral age is ≳200 Myr, suggesting that the extended diffuse emission is due to an earlier cycle of activity. We re-analyse archival X-ray data from Chandra and suggest that the X-ray emission from the hotspots consists of a mixture of non-thermal and thermal components, the latter being possibly due to gas which is shock heated by the jets from the host galaxy.  相似文献   

Wide-field mid-infrared and millimetre imaging of the high-redshift radio galaxy, 4C 41.17     

T. R. Greve  D. Stern  R. J. Ivison  C. De Breuck  A. Kovács  F. Bertoldi 《Monthly notices of the Royal Astronomical Society》2007,382(1):48-66

  相似文献   

On the ultracompact nature of 4U 1822−000     

T. Shahbaz  C. A. Watson  H. Hernandez-Peralta 《Monthly notices of the Royal Astronomical Society》2007,376(4):1886-1888

We report the discovery of a periodic modulation in the optical lightcurve of the candidate ultracompact X-ray binary 4U 1822−000. Using time-resolved optical photometry taken with the William Herschel Telescope we find evidence for a sinusoidal modulation with a semi-amplitude of 8 per cent and a period of 191 min, which is most likely close to the true orbital period of the binary. Using the van Paradijs & McClintock relation for the absolute magnitude and the distance modulus allowing for interstellar reddening, we estimate the distance to 4U 1822−000 to be 6.3 kpc. The long orbital period casts severe doubts on the ultracompact nature of 4U 1822−000.  相似文献   

Towards a 4D topographic view of the Norwegian sea margin   总被引：1，自引：1，他引：0  

Morten Smelror  John Dehls  Jrg Ebbing  Eiliv Larsen  Erik R. Lundin   ystein Nordgulen  Per Terje Osmundsen  Odleiv Olesen  Dag Ottesen  Christophe Pascal  Thomas F. Redfield  Leif Rise 《Global and Planetary Change》2007,58(1-4):382

The present-day topography/bathymetry of the Norwegian mainland and passive margin is a product of complex interactions between large-scale tectonomagmatic and climatic processes that can be traced back in time to the Late Silurian Caledonian Orogeny. The isostatic balance of the crust and lithosphere was clearly influenced by orogenic thickening during the Caledonian Orogeny, but was soon affected by post-orogenic collapse including overprinting of the mountain root, and was subsequently affected by a number of discrete extensional events eventually leading to continental break-up in Early Eocene time. In the mid-Jurassic the land areas experienced deep erosion in the warm and humid climate, forming a regional paleic surface. Rift episodes in the Late Jurassic and Early Cretaceous, with differential uplift along major fault zones, led to more pronounced topographic contrasts during the Cretaceous, and thick sequences of clastic sediments accumulated in the subsiding basins on the shelf. Following renewed extension in the Late Cretaceous, a new paleic surface developed in the Paleocene. Following break-up the margin has largely subsided thermally, but several Cenozoic shortening events have generated positive contraction structures. On the western side of the on-shore drainage divide, deeper erosion took place along pre-existing weakness zones, creating the template of the present day valleys and fjords. In the Neogene the mainland and large portions of the Barents Sea were uplifted. It appears that this uplift permitted ice caps to nucleate and accumulate during the Late Pliocene northern hemisphere climatic deterioration. The Late Pliocene to Pleistocene glacial erosion caused huge sediment aprons to be shed on to the Norwegian Sea and Barents Sea margins. Upon removal of the ice load the landmass adjusted isostatically, and this still continues today.  相似文献