川西高原红原机场建设气象条件可行性分析     

刘晓燕  牟银杰  曾晓东 《四川气象》2011,(3):35-38

在为川西高原红原机场气候论证观测取得连续一年多资料的基础上,结合相邻的红原县、阿坝县气象站30年整编气候资料,利用山地气候推算分析方法,对机场场址的气候资料进行推算分析,根据推算的气候资料结合实际观测资料,对机场建设可能产生影响的气象要素进行分析评估,形成了可行性综合论证报告。本研究为红原机场工程建设提供了气象科学依据,取得了良好的社会效益和经济效益。  相似文献   

A study of partitioning Q vector on background conditions of a torrential rainfall over Shanghai, China on 25 August 2008     

岳彩军  鲁小琴  李小凡  宗志平 《热带气象学报(英文版)》2011,17(3):231-247

A rainfall that occurred during 0200–1400 Beijing Standard Time(BST)25 August 2008 shows the rapid development of a convective system,a short life span,and a record rate of 117.5 mm h-1for Xujiahui station since 1872.To study this torrential rainfall process,the partitioning method of Q vector is developed,in which a moist Q vector is first separated into a dry ageostrophic Q vector(DQ)and a diabatic-heating component.The dry ageostrophic Q vector is further partitioned along isothermal lines in the natural...  相似文献   

四川东部和重庆西部一次ＭＣＣ致洪暴雨过程综合分析     

井喜  艾丽华  廖瑞德 《陕西气象》2011,(1):1-7

吕梁山区出现局地大暴雨为小概率事件,在县局的订正预报中有很大的难度。2010年8月11日位于吕梁市东北端的岚县出现了106．2mm的大暴雨,而吕梁的其它县、市只出现中雨以下量级降水。本文分析了造成本次强降雨的高低空环流形势、主要影响系统、水汽条件、云图与雷达回波资料以及本县特殊的地形特征等结果表明：本次局地大暴雨天气是由高空短波槽、中层切变线、副热带高压边缘西南暖湿气流共同作用产生的;对流层低层强盛的偏南气流为大暴雨提供了源源不断的水汽;地面弱低压加强了辐合上升运动,特殊地形的抬升与阻挡作用,使强回波雨团长时间在迎风坡下的平坦地段停留,从而造成局地性的强降水。  相似文献   

2011年龙眼挂果率高的气象成因分析     

陈国保  李永平  姚志东 《气象研究与应用》2011,32(4):45-48

通过对2010／2011年度玉林市龙眼秋梢抽生期一开花着果期的农业气象条件进行诊断分析,得出2011年挂果率高的主要原因是：2010年8-9月份的光温水条件配合较好对秋梢抽生相当有利,紧接着从10月份开始出现了秋、冬、春三季连旱,冬季和早春的气候也比较寒冷,在干旱和寒冷的双重作用下,非常有利于控制冬梢和促进花芽分化,也...  相似文献   

Zooplankton succession during extraordinary drought–flood cycles: A case study in a South American floodplain lake     

Griselda Chaparro  María Cristina Marinone  Ruben J. Lombardo  María Romina Schiaffino  Alice de Souza Guimarães  Inés O’Farrell 《Limnologica》2011,41(4):371-381

We examined the zooplankton abundance and composition of Laguna Grande, a floodplain wetland of the Lower Paraná Basin (Argentina), during an extraordinary drought–flood cycle that affected both the environment and the biological conditions of the lake. Low waters were characterised by remarkably high conductivities and pH values, and high phytoplankton and bacterioplankton abundances with cyanobacterial blooms, while high waters showed opposite features. In relation to zooplankton, the mean abundances of all the taxonomic groups (rotifers, cladocerans, copepods, ciliates, and heterotrophic nanoflagellates) were slightly higher at low waters. Major changes were observed in the specific composition of metazooplankton: the euryhaline species assemblage that dominated in the dry warm period was replaced by several oligohaline littoral and planktonic species characteristic of the Paraná River Basin, when the water level rose. Mean species richness values at high waters doubled those of low waters and were directly correlated to water depth. Most of the rotifers of the genus Brachionus and the cladoceran Moina micrura switched from parthenogenetic to sexual reproduction during low waters, as a response to a harsh environment and crowding. We suggest that the main changes in the environmental conditions in this eutrophic floodplain lake are driven by the hydrology, which regulates the zooplankton succession. The herein described shifts in the zooplankton structure and dynamics of Laguna Grande over an extraordinary drought–flood cycle contribute to the understanding of the processes that might occur under the scenarios predicted by climate change models.  相似文献   

Use of multi-temporal Landsat images for analyzing forest transition in relation to socioeconomic factors and the environment     

Zhi-Hua Shi  Lu Li  Wei Yin  Lei Ai  Nu-Fang Fang  Yan-Tun Song 《International Journal of Applied Earth Observation and Geoinformation》2011

Recently there have been reports of forest regrowth occurring in different regions across the world. There is also a growing recognition of the potential beneficial impact that secondary forests may have on the global environment: providing crucial ecosystem services such as soil conservation, stabilization of hydrological cycles, carbon sequestration, and support for forest dependent communities. Consequently, there is a growing awareness of the need to recognize that landscapes are complex shifting mosaics wherein forest clearing and reforestation take place. In this study, the rates of reforestation, deforestation, forest regrowth and degradation were measured using multi-temporal Landsat images of Danjiangkou, China. Landsat data from 1990, 1999 and 2007 were (1) classified as dense forest, open forest and non-forest areas and (2) compared between years to identify forest cutting, regeneration and degradation. The results showed that there was a net gain of 29,315 ha of forest area (including dense and open forest) from 1990 to 2007, showing a clear trend of reforestation in the study area. Forest modification (degradation and regrowth) and change categories (deforestation and reforestation) occurred simultaneously during the observation time period. Socioeconomic data from public statistics and environmental attributes allowed the assessment of the socioeconomic factors and the environmental conditions that caused these changes using non-metric multidimensional scaling (NMDS). The research showed that the socioeconomic factors due to different policies were major driving forces of forest transition, whereas environmental attributes of the underlying landscape constrained forest cover changes. These findings have led to a better understanding of forest transition at a local scale in our study region. Comprehensive knowledge of these relationships may be useful to reconstruct past forest transitions and predict future changes, and may help to enhance sustainable management practices aimed at preserving essential ecological functions.  相似文献   

鸡西盆地梨树镇坳陷晚白垩世构造演化与油气成藏条件     

李占东  马金龙  刘文超  邹越  肖佃师  陈海峰  胡慧婷  李阳 《大地构造与成矿学》2011,35(1):47-55

运用地层学、构造地质学以及成藏系统等理论和方法,系统阐述了梨树镇坳陷油藏的成藏条件.梨树镇坳陷断裂经历了城子河组时期的伸展变形、穆棱组时期的走滑变形和猴石沟组时期的强烈反转构造变形三个阶段.依据断裂发育特征和各级不整合面,将坳陷自下而上划分为下部城子河组断陷构造层、中部穆棱组断坳转化构造层和上部猴石沟组坳陷构造层,各个...  相似文献   

柴西地区上干柴沟组上段咸水湖相烃源岩生烃条件研究     

何金先  段毅  张晓丽  吴保祥  徐丽 《矿产与地质》2011,25(3):242-247

柴西地区上干柴沟组上段(N12)烃源岩的沉积水体环境为咸水湖相。其烃源岩的有机质总体丰度不高;有机质类型主要有腐殖腐泥型和腐殖型,具体分布受烃源岩所处位置及沉积环境控制;有机质成熟度多为未成熟-低成熟;有机质的烃转化率较高,反映其大部分有机质已经进入生烃门限,少量已经进入生烃高峰期。其烃源岩具有咸化湖泊相未熟-低熟有机质生烃的特点,而其生烃机理很可能是藻类生物类脂物和细菌的早期成烃。柴西地区上干柴沟组上段(N12)烃源岩作为该区未熟-低熟石油主要源岩之一,具有非常大的勘探潜力。  相似文献   

冻土水文研究进展   总被引：3，自引：0，他引：3  

阳勇  陈仁升 《地球科学进展》2011,26(7):711-723

冻土改变了区域水热条件、产汇流过程、产流量多寡及年内/际变化,冻土水文成为寒区生态-水文过程的核心环节.系统总结了国内外冻土水文研究进展,包括冻土水热传输特征,特殊的产汇流过程,流域尺度水平衡,以及各种水热传输物理模型和流域尺度水文模型.未来冻土水文的发展应在数据和方法积累的基础上,进一步探索产汇流过程机理,并建立完善...  相似文献   

甘肃省金边寺矿床铀矿化特征及成矿条件分析   总被引：1，自引：0，他引：1  

陈云杰  赵如意  李涛 《甘肃地质》2011,(3):46-50

金边寺矿床位于龙首山东部的青山堡岩体西南部边缘,其周边还发育有较多铀矿（化）点、异常点,具有较好的铀成矿背景。文章从矿床的岩浆岩条件、构造条件、热液蚀变条件、淋积成矿条件、以及区域上广泛与铀成矿密切相关的碱交代热液蚀变条件进行了全面分析,系统的阐述了该矿床的铀成矿条件。在此基础上,初步探讨了下一步找矿方向,即在该区下一步找矿工作重点是寻找深部未被淋积的碱交代型铀矿体和继续扩大淋积型铀矿化,寻找新的赋矿空间。  相似文献