PJ和MnE遥相关型对东亚夏季气温的协同影响（英文）          下载免费PDF全文

MING Jing  SUN Jianqi  YU Shui 《大气和海洋科学快报》2019,(3):208-217

本文研究发现太平洋–日本遥相关型(PJ)和地中海–欧亚北部遥相关型(MnE)对东亚夏季气温存在显著的协同影响。当PJ和MnE处于同位相时,两者相关的大气环流在东亚中部地区相互叠加抵消,从而对该地区气温的影响较弱,而此时显著的气温异常主要位于东亚北部。相反,当PJ和MnE处于反位相时,两者相关的大气环流在东亚地区相互叠加增强,从而对东亚中部和亚洲北部地区的气温产生显著影响。因此,在东亚夏季气温变化的理解与预测中需要考虑这两个遥相关的协同作用。  相似文献   

ANALYSIS OF LAND BRIDGE TRANSPORTATION     

祁勇  王雁 《中国地理科学(英文版)》1991,1(4):337-346

Land bridge transportation means transportation from one seaport to another by railway across continents instead of by ocean ship. At present, there are two common routes for using land bridge transportation in the world. One is Asia-America-Europe land bridge, the other is Europe-Asia land bridge.Eurasia land bridge has obvious advantages over Asia-America-Europe land bridge due to its shorter distance, shorter transportation time and special freight rate. China started Eurasia land bridge transportation business in 1980. It mainly used the mode of railway-railway combined transportation. The comparison between using Eurasia land bridge and using shipping transportation from China to Northern and Western Europe shows that Euraria land bridge transportation can save time and get foreign exchange in time, and commodity turnover will be speeded up. According to the port layout and railway network structure, China's land bridge transportation projects are proposed. They are Suifenhe project, Dalian project  相似文献   

世界地理结构与美国的全球战略及军力设计   总被引：3，自引：1，他引：2  

杜德斌  段德忠  夏启繁  曹宛鹏  马亚华  刘承良 《世界地理研究》2021,30(4):667-684

本文旨在阐明世界地理结构在大国战略制定及军力设计中的基础性作用,以助于认识中国全球发展道路上面临的地缘安全风险和机遇。由于世界陆地、人口和经济活动相对集中于东半球特别是欧亚大陆,欧亚大陆历来是世界大国逐鹿的中心舞台。美国作为人类历史上第一个非欧亚大陆上的霸权国家,一直把防范欧亚大陆上出现区域性霸权作为国家安全的最高目标。本文从世界地理结构及其动态变化的角度,分析东半球尤其是欧亚大陆孕育世界大国和人类文明的地理优势,解析美国的地理区位对其早期崛起的影响,以及在这一地理条件下其全球战略的形成,并重点探讨美国基于防范欧亚大陆出现区域性霸权的全球军力设计。文章最后指出,在中美战略博弈中,位于欧亚大陆东缘的中国具有天然的地缘优势。  相似文献   

1—3月欧亚大陆热力变化及其与中国降水的关系   总被引：1，自引：1，他引：0       下载免费PDF全文

晏红明  王灵  李蕊 《应用气象学报》2016,27(2):209-219

利用1979—2011年NCEP/NCAR再分析资料、我国160个站降水和气温资料,分析欧亚大陆热力变化特征,其在冬季和春季的气候变率最明显,且南北区域呈反相差异。在此基础上, 探讨1—3月欧亚大陆热力差异与中国降水异常的关系,欧亚大陆正 (负) 热力差异年,1—3月华南、西南至河套西部地区降水偏多 (少) 明显,后期夏季多雨带位于长江中下游地区 (华南地区)。大气环流异常特征显示:1—3月欧亚大陆南北热力差异与同期北极涛动 (AO)、东亚大槽、东亚高空急流等大尺度大气环流,以及后期东亚高空急流、南亚高压、低层季风风系异常的密切相关是欧亚大陆热力变化与中国降水联系的可能途径。  相似文献   

沿江与沿桥城市发展对比研究     

赵一如  姚建华 《地域研究与开发》2000,19(3):21-25

沿江产业带和沿桥经济带同是横跨我国东、中、西三大地带的经济建设的的级轴线,其城市经济发展状况存在很大差异。文章通过对二者的城市等级规模、空间结构、城市化程度及积能结构等方面进行具体的差异比较,对导致才者差异的主观及客观原因进行深入分析,提出了几点适合陆桥知身特点,结合陆桥现有机遇的具体建议。  相似文献   

欧亚和青藏高原冬春季积雪与我国夏季降水关系的分析和预测应用   总被引：56，自引：18，他引：38  

陈兴芳  宋文玲 《高原气象》2000,19(2):214-223

通过高原积雪和欧亚积雪与我国夏季降水的相关分析和统计检验,表明冬春季雪盖对我国夏季旱涝有重要的影响,虽然冬季和春季雪盖与我国夏季降水的相关分布存在差异,总趋势大致相仿。但是,冬春季高原积雪和欧 亚积雪与我国夏季降水的相关分布基本是相反的,其中高原积雪与长江中下游和西北东部地区夏季降水为正相关,欧亚积雪与东北和华北东部以及西南地区降水为正相关冬季节积雪异常偏多时,长江流域夏季易发生洪涝,这也是汛期降  相似文献   

Permian palaeomagnetism of East Kazakhstan and the amalgamation of Eurasia     

Natalia M. Levashova  Kirill E. Degtyarev  Mikhail L. Bazhenov  Adam Q. Collins  Rob Van der Voo 《Geophysical Journal International》2003,152(3):677-687

  相似文献   

Eurasia spreading basin to Laptev Shelf transition: structural pattern and heat flow   总被引：3，自引：0，他引：3  

S. S. Drachev  N. Kaul  V. N. Beliaev 《Geophysical Journal International》2003,152(3):688-698

  相似文献   

Intraplate mountain building in response to continent–continent collision—the Ancestral Rocky Mountains (North America) and inferences drawn from the Tien Shan (Central Asia)     

Patricia Wood Dickerson   《Tectonophysics》2003,365(1-4):129

The intraplate Ancestral Rocky Mountains of western North America extend from British Columbia, Canada, to Chihuahua, Mexico, and formed during Early Carboniferous through Early Permian time in response to continent–continent collision of Laurentia with Gondwana—the conjoined masses of Africa and South America, including Yucatán and Florida. Uplifts and flanking basins also formed within the Laurentian Midcontinent. On the Gondwanan continent, well inboard from the marginal fold belts, a counterpart structural array developed during the same period. Intraplate deformation began when full collisional plate coupling had been achieved along the continental margin; the intervening ocean had been closed and subduction had ceased—that is, the distinction between upper versus lower plates became moot. Ancestral Rockies deformation was not accompanied by volcanism. Basement shear zones that formed during Mesoproterozoic rifting of Laurentia were reactivated and exerted significant control on the locations, orientations, and modes of displacement on late Paleozoic faults.Ancestral Rocky Mountain uplifts extend as far south as Chihuahua and west Texas (28° to 33°N, 102° to 109°W) and include the Florida-Moyotes, Placer de Guadalupe–Carrizalillo, Ojinaga–Tascotal and Hueco Mountain blocks, as well as the Diablo and Central Basin Platforms. All are cored with Laurentian Proterozoic crystalline basement rocks and host correlative Paleozoic stratigraphic successions. Pre-late Paleozoic deformational, thermal, and metamorphic histories are similar as well. Southern Ancestral Rocky Mountain structures terminate along a line that trends approximately N 40°E (present coordinates), a common orientation for Mesoproterozoic extensional structures throughout southern to central North America.Continuing Tien Shan intraplate deformation (Central Asia) has created an analogous array of uplifts and basins in response to the collision of India with Eurasia, beginning in late Miocene time when full coupling of the colliding plates had occurred. As in the Laurentia–Gondwana case, structures of similar magnitude and spacing to those in Eurasia have developed in the Indian plate. Within the present orogen two ancient suture zones have been reactivated—the early Paleozoic Terskey zone and the late Paleozoic Turkestan suture between the Siberian and East Gondwanan cratons. Inverted Proterozoic to early Paleozoic rift structures and passive-margin deposits are exposed north of the Terskey zone. In the Alay and Tarim complexes, Vendian to mid-Carboniferous passive-margin strata and the subjacent Proterozoic crystalline basement have been uplifted. Data on Tien Shan uplifts, basins, structural arrays, and deformation rates guide paleotectonic interpretations of ancient intraplate mountain belts. Similarly, exhumed deep crustal shear zones in the Ancestral Rockies offer insight into partitioning and reorientation of strain during contemporary intraplate deformation.  相似文献   

Quaternary folding of the eastern Tian Shan, northwest China   总被引：3，自引：0，他引：3  

Bihong Fu  Aiming Lin  Ken-ichi Kano  Tadashi Maruyama  Jianming Guo 《Tectonophysics》2003,369(1-2):79-101

The Tian Shan, east–west trending more than 2000 km, is one of most active intracontinental mountain building belts that resulted from India–Eurasia collision during Cenozoic. In this study, Quaternary folding related to intracontinental mountain building of the Tian Shan orogenic belt is documented based on geologic interpretation and analyses of the satellite remote sensing images [Landsat Thematic Mapper (TM)/Enhanced Thematic Mapper (ETM) and India Remote Sensing (IRS) Pan] combined with field geologic and geomorphic observations and seismic reflection profiles. Analyses of spatial–temporal features of Quaternary folded structure indicate that the early Quaternary folds are widely distributed in both piedmont and intermontane basins, whereas the late Quaternary active folds are mainly concentrated on the northern range-fronts. Field observations indicate that Quaternary folds are mainly characterized by fault-related folding. The formation and migration of Quaternary folding are likely related to decollement surfaces beneath the fold-and-fault zone as revealed by seismic reflection profiles. Moreover, analysis of growth strata indicates that the Quaternary folding began in late stage of early Pleistocene (2.1–1.2 Ma). Finally, tectonic evolution model of the Quaternary deformation in the Tian Shan is presented. This model shows that the Quaternary folding and faulting gradually migrate toward the range-fronts due to the continuous compression related to India–Eurasia collision during Quaternary time. As a result, the high topographic relief of the Tian Shan was formed.  相似文献