Rehabilitation and Sustainable Use Pattern of Rocky-desertified Land in Southwest China''s Poverty-stricken Karst Mountainous Areas——A Case Study in Benggu Township, Xichou County, Yunnan, China     

YANG Zisheng  LIU Yansui  BAO Guangjing  LI Zhiguo  HE Yimei 《山地科学学报》2006,(3)

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Regional Features of Vapor Transfer and Precipitation Distributed in Northwest China          下载免费PDF全文

TAO Jianhong  WANG Baojian  HUANG Yuxi  WANG Jinsong 《Acta Meteorologica Sinica》2006,20(5):31-39

This article investigates regional distribution features of rainfall and vapor transport in Northwest China during 1961-2002, achieving that: (1) Three climate zones in this vast region differ in trends of annual precipitation, with rainfall in the westerly belt (denoted as zoneWB) exhibiting an increasing trend from the 1970s, rainfall in the East Asian monsoon belt (denoted as zoneMB) displaying a decreasing trend in the study period and the Qinghai Plateau zone (denoted as zoneQP) precipitation fluctuating roughly around the mean; (2) The net vapor fluxes (NVF) in zoneWB and zoneQP show an increasing trend as opposited to zoneMB, for which the reason may lie behind that the NVF increase in zoneWB and zoneQP is attributed to pronounced decrease in deficit of westerly NVF, whereas the decrease in zoneMB NVF is ascribed to the significant drop in meridional vapor transfer; (3) ZoneWB rainfall and atmospheric vapor transport change abrupt in 1990 and 1985, respectively, without such happening in zoneMB and zoneQP; (4) ZoneWB rainfall increase occurs when atmospheric vapor budget/NVF increases, so that the latter has to occur ahead of the former; zoneMB rainfall decrease relates to the decrease in atmospheric vapor budget after the 1990s,leading to (more and even) successive droughts in the east of Northwest China on a synchronous basis except zoneQP of which the precipitation factors include river evaporation, glaciers, and snow cover in addition to atmospheric vapor.  相似文献   

Southern high latitude climate anomalies associated with the Indian Ocean dipole mode     

刘娜贾贞  陈红霞华锋 《中国海洋湖沼学报》2006,24(2):125-128

1 INTRODUCTION In southern high latitudes, recent observations have shown a standing mode of ACW (Antarctic Circumpolar Wave) with eastward propagation across the Southern Ocean of the Antarctic in co- varying SST (sea surface temperature) and SLP (sea le…  相似文献   

Late Glacial fluvial response of the Niers‐Rhine (western Germany) to climate and vegetation change     

C. Kasse  W. Z. Hoek  S. J. P. Bohncke  M. Konert  J. W. H. Weijers  M. L. Cassee  R. M. Van Der Zee 《第四纪科学杂志》2005,20(4):377-394

The Niers valley was part of the Rhine system that came into existence during the maximum Saalian glaciation and was abandoned at the end of the Weichselian. The aim of the study was to explain the Late Pleniglacial and Late Glacial fluvial dynamics and to explore the external forcing factors: climate change, tectonics and sea level. The sedimentary units have been investigated by large‐scale coring transects and detailed cross‐sections over abandoned channels. The temporal fluvial development has been reconstructed by means of geomorphological relationships, pollen analysis and ¹⁴C dating. The Niers‐Rhine experienced a channel pattern change from braided, via a transformational phase, to meandering in the early Late Glacial. This change in fluvial style is explained by climate amelioration at the Late Pleniglacial to Late Glacial transition (at ca. 12.5 k ¹⁴C yr BP) and climate‐related hydrological, lithological and vegetation changes. A delayed fluvial response of ca. 400 ¹⁴C yr (transitional phase) was established. The channel transformations are not related to tectonic effects and sea‐level changes. Successive river systems have similar gradients of ca. 35–40 cm km^?1. A meandering river system dominated the Allerød and Younger Dryas periods. The threshold towards braiding was not crossed during the Younger Dryas, but increased aeolian activity has been observed on the Younger Dryas point bars. The final abandonment of the Niers‐Rhine was dated shortly after the Younger Dryas to Holocene transition. Traces of Laacher See pumice have been found in the Niers valley, indicating that the Niers‐Rhine was still in use during the Younger Dryas. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   

设计模式及其在J2ME中的应用   总被引：2，自引：0，他引：2  

韩鹏  李成忠 《成都信息工程学院学报》2004,19(3):332-335

设计模式被描述为在一定的环境中解决某一类问题的方案.已成为现代软件系统设计的重要研究对象.介绍了J2ME体系结构,并深入探讨了3种典型设计模式在J2ME开发中的应用.  相似文献   

辽宁水泉金矿成矿规律及矿山远景评价     

陈永良  裴效渤  许亚光 《国土资源》1996,(1)

用综合信息矿产资源定量预测的理论和方法，系统研究了辽宁水泉金矿成矿规律及控矿因素，特别是对控矿构造特征作了深入的研究，并建立了研究区的综合信息找矿模型。对水泉金矿的区域成矿远景和深部成矿远景进行了综合预测。  相似文献   

中下扬子地区的壳幔结构及其与地震相关性的研究     

周国藩 《大地测量与地球动力学》1994,(4)

针对中下扬子地区人口稠密、经济建设蓬勃发展、而其地壳构造十分复杂、天然地震比较活跃的现实情况，以实测的地球物理资料与卫星重力异常等相结合，分析了该地区地壳构造和上地幔深部构造的基本特征，指出该地区中强震的形成和发生既有可能与地壳层中存在的低速带和高导层有关，还可能与更深部上地幔内部构造的背景因素有关。文中还提出了一些值得进一步探讨的问题。  相似文献   

用区域重力资料确定的华北地台南缘地缝合线及其地质意义     

张晓春  冯凤雪  王正晓 《河南国土资源》1997,(4)

利用１∶２０万区域重力资料，结合航磁，电磁测深、遥感、天然地震等丰富的地质、地球物理资料，根据断裂的地质、地球物理标志，在华北地台南缘发现并确定了控制火山喷发的裂隙—中心式古火山通道，即隐伏的北西西向的上戈—铁炉坪—付店超壳断裂带。该断裂属华北地台南缘不同时代、不同性质的近东西向的地缝合线。研究认为：该断裂及其次级断裂不仅是重要的长期多次活动的控岩、导矿和容矿构造，而且也为矿床的多次改造、叠加和再富集提供了热源。它的发现，对重新认识豫西地区大地构造的演化特征，建立新的成矿模式，拓宽该区的找矿前景具有重要意义。  相似文献   

STUDY ON THE MIGRANT LABOUR FORCE OF CHINA IN RECENT YEARS──A Case Study of Nanhai City of Guangdong Province     

阎小培 《中国地理科学(英文版)》1997,(1)

I.INT~IOWFOralOngthe,thesyStemofPermanentresidencempistrationhasdividedChineseampleintOthO8ewith"tirbanresidence"andthOSehaving"rUralresidence".TherationingsyStem,underwhichedibleoilandgrainwasdistributedonlytOthOSewith"urbanresidence"Calds,hasbeendondnant.Bothsystems,beingcentraltorestrictingthegrowthofurbanpopulation,havestagnatedrUral-tirbaningration.Duringthe30yearsbefore1978,thestatedidsPOnsorpopulationmovementsfromrUraltourbanareasbymeansofenrollingnewworkers,butingeneral,thiss…  相似文献   

数据挖掘在高校学生管理决策中的应用模式分析   总被引：1，自引：0，他引：1  

刘雨露 《成都信息工程学院学报》2006,21(3):373-377

随着因特网的广泛应用,各高校在开展现代远程教育过程中记录了大量复杂的学生信息,基于这些历程信息,在高校学生管理决策中利用数据挖掘技术,提出了现代高校学生管理工作的新模式,并就几个管理决策的应用模式进行了实例分析.  相似文献