中国北方沙尘天气原因探讨   总被引：2，自引：1，他引：2  

吴绍洪  杨勤业  曹军 《干旱区资源与环境》2004,(Z1)

我国是沙尘暴易发的国家,进入20世纪90年代以来,强沙尘暴有频率增加、强度加大、范围扩展、危害程度加剧的趋势。沙尘暴的发生危害范围亦逐渐从西北干旱经济落后区扩展到经济发达的北京、天津及华北平原区,近年来的沙尘暴造成了社会经济和人民生命财产的重大损失。受大气环流场和季风气候类型影响,中国冬、春盛吹西北风,强劲而干燥。发生沙尘暴的天数与大风日数和地面热力稳定程度相关,3-5月中国西北内陆地表增温大,是风力场和热力场极不稳定的季节,地表气候容易发生蠕动,沙尘暴便由此启动并易发。除自然要素外,不合理的人类活动也将诱发沙尘暴天气的发生,有些情况下还起到比自然要素更重要的作用。从生态地理区域的角度看,沙尘暴的源地在干旱和半干旱地区,由于大气环流的作用,影响到下风向的半湿润甚至湿润地区。无论何地干旱、半干旱地区都将存在沙尘暴发生的自然条件,而其下风向必将受到不同程度的影响,只是因为中国的季风气候,决定西北干旱、半干旱地区发生的沙尘暴必然影响东南部地区。在现有的科学技术条件下,人类所能做的就是调节自身的行为。因此,在沙尘暴源地实施生态建设是减缓沙尘暴发生的最重要措施,也是消除东部城市沙尘天气的主要途径。根据生态地理区域的特征,沙尘暴源地的干旱区、半干?  相似文献   

导致一例强沙尘暴的若干天气因素的观测和模拟研究     

姜学恭  沈建国  刘景涛  陈受钧 《干旱区资源与环境》2004,(Z1)

利用常规观测资料和数值模拟方法对影响2001年4月6-8日强沙尘暴天气发生的若干天气因素进行了研究。结果表明在本次“锋面气旋型”沙尘暴过程中,气旋冷锋是引发强沙尘暴的主要系统,冷锋过境对沙尘暴的触发作用远强于气旋发展。冷锋的动力学特点决定其常与强沙尘暴伴随。影响沙尘暴的诸多天气因素中,影响地面大风形成的有效动量下传机制为高空急流下沉支使高空动量下传至对流层中层,其下方形成的深厚混合层使这一动量继续下传到地面。“混合层”从本质上反映了有利沙尘暴形成的大气层结特征,深厚混合层的是否形成很大程度决定着沙尘暴的强度。本次过程深厚混合层的形成是长时间地面加热的结果,这也是特强沙尘暴仅发生在内蒙古中部偏北地区而不是下垫面条件更为适宜的内蒙古西部的原因。混合层空气的平流对内蒙古中部偏北地区深厚混合层的形成具有相当的贡献,其影响程度与地形分布密切相关。地面热通量试验表明地面加热对冷锋过境时上升运动的强度、深厚混合层形成、高空动量下传等具有重要影响,并因此影响沙尘暴强度。  相似文献   

沙尘物质的来源与防治途径   总被引：4，自引：1，他引：4  

闫德仁  杨俊平 《干旱区资源与环境》2004,(Z1)

本文分析了沙尘暴形成的自然过程和危害特征,并探讨了内蒙古沙源区土壤颗粒物质的含量,指出沙尘暴的沙尘来源主要是退化草原、活化的沙地和裸露坡耕地等。同时根据风沙流运移规律及其和土壤颗粒的关系,提出了防治沙尘暴的关键技术原理,并探讨了有效控制沙尘暴的技术途径。  相似文献   

内蒙古沙尘暴的成因、趋势及其预报   总被引：2，自引：0，他引：2  

高涛  徐永福  于晓 《干旱区资源与环境》2004,(Z1)

本文利用内蒙古1961～2001年的天气气候资料,对内蒙古中西部地区沙尘暴作了统计分析,阐述了沙尘暴的危害并给出了沙尘暴的基本定义。分析了引起沙尘暴的天气和气候因子的变化趋势,研究了他们对沙尘暴的影响,结果表明近40年内蒙古的沙尘暴总体呈减少趋势,但从1998年开始有所增加;沙尘暴的空间分布以阿拉善盟偏北地区为最高发区;降水、气温、大风、寒潮、北半球极涡、西太平洋副热带高压、亚洲西风环流、东亚大槽和南方涛动等天气和气候因素均对该地区沙尘暴的发生有不同程度的影响。  相似文献   

西北地区沙尘暴的危害及对策   总被引：16，自引：3，他引：13  

黄维  牛耘 《干旱区资源与环境》1998,12(3):83-88

该文以大量的例证,详实的数据介绍了西北地区沙尘暴的危害,并综合分析了沙尘暴产生形成原因、危害方式,为保护生态环境提出了治沙防沙的基本对策。  相似文献   

京津风沙源治理工程省级管理系统的分析与设计     

温雪香  张会华 《林业资源管理》2003,(2):62-64

对京津风沙源治理工程省级管理系统的分析、设计、功能等进行简单论述。  相似文献   

柴达木盆地沙尘天气的气候特征及与气象要素的关系   总被引：1，自引：0，他引：1  

张焕平  张占峰  金惠瑛  马小萍 《安徽农业科学》2014,(5):1382-1384,1538

利用1961～2010年柴达木盆地10个气象站观测资料,采用气候统计学方法,对沙尘天气变化特征及与气象要素的关系进行分析。结果表明,近50年柴达木盆地扬沙、浮尘、沙尘暴日数均呈显著减少的趋势,4月为扬沙、浮尘、沙尘暴出现次数最多的月份;沙尘天气均表现为春季〉夏季〉冬季〉秋季的气候特征;沙尘天气与大风、降水呈正相关,与大风的相关性明显,与降水的相关性不明显;四季气温与沙尘天气呈不显著的负相关。可见大风日数的减少是沙尘天气减少的主要原因,降水增加和气温升高对沙尘天气的发生也起一定抑制作用。  相似文献   

Fire Environment Mechanism of Lightning Fire for Daxing''''an Mountains     

WANG Mingyu SHU Lifu TIAN Xiaorui LI JieInstitute of Forest Protection  Chinese Academy ofForestrv Forest fire management office. State Forestry Administration 《中国林业科技(英文版)》2003,(4)

Lightning fire is one of natural fires; its mechanism is very complex and difficult to control. Daxing'an Mountain is the main region that lightning fires occur in China. Research on lightning fires indicates that special fuel, dry-storm weather and high altitude form the lightning fire environment. Lightning fires have close relation with lights. When lightning occurs, especially dry-lightning which brings little precipitation with surface temperature growing and fuel dehydrating, these often lead to lightning fires. Lightning fires have characteristics of geography, time and topography. The higher altitude forest region in Daxing'an Mountain, the more lightning fires occur. Valley with altitude above 800 m in the north of 51.N and Larix gmelinii-Pinus pumila, Pinus sylvestris var. mongolica -Pinus pumila forests on the top of mountain are the most concentrating region where lightning fires occur. One serial dry-storming can ignites many lightning fires, the furthest between them is as long as 150 km.  相似文献   

Dust storm erosion and its impact on soil carbon and nitrogen losses in northern China   总被引：4，自引：0，他引：4  

Xiaobin Wang  O. Oenema  W.B. Hoogmoed  U.D. Perdok  Dianxiong Cai 《CATENA》2006,66(3):221-227

There is increased awareness of the environmental impacts of soil carbon (C) and nitrogen (N) losses through wind erosion, especially in areas heavily affected by dust storm erosion. This paper reviews the recent literature concerning dust storm-related soil erosion and its impact on soil C and N losses in northern China. The purpose of our study is to provide an overview of the area of erosion-affected soils and to estimate the magnitude of soil C and N losses from farmland affected by dust storm erosion.According to the second national soil erosion remote-sensing survey in 2000, the area affected by wind erosion was 1.91 million km², accounting for 20% of the total land area in China. This area is expanding quickly as the incidence of heavy dust storms has greatly increased over the last five decades, mainly as a result of the intensification of soil cultivation. The economic and ecological damage caused by wind erosion is considerable. Heavily affected areas show a loss of nutrients and organic carbon in soils and the heavily degraded soils are much less productive. Compared with the non-degraded soil, the C and N contents in degraded soils have declined by 66% and 73%, respectively. The estimated annual losses per cm toplayer of soil C and N by dust storm erosion in northern China range from 53 to 1044 kg ha^− 1 and 5 to 90 kg ha^− 1, respectively. Field studies suggest that soil losses by wind erosion can be reduced by up to 79% when farmers shift from conventional soil tillage methods to no-till. Thus shifting to no-till or reduced tillage systems is an effective practice for protecting soil and soil nutrients. Our study indicates that soil conservation measures along with improved soil fertility management measures should be promoted in dry-land farming areas of northern China. As erosion is a major mechanism of nutrient withdrawal in these areas, we plead for the development of accurate methods for its assessment and for the incorporation of erosion, as a nutrient output term, in nutrient budget studies.  相似文献   

神经网络与暴雨泥石流灾害预报   总被引：4，自引：0，他引：4  

文科军  吕巡贤  谢宝元  王礼先 《新疆农业大学学报》2001,24(3):54-58

建立了用于暴雨泥石流适时预报的人工神经网络模型，在荒溪分类和危险区划分基础上，结合北京山区暴雨泥石流例子，验证模型判别结果与实际情况相符，应用效果良好。  相似文献