ANALYSIS OF THE ATMOSPHERIC AEROSOL OPTICAL DEPTH OVER CHINA IN 1980s^*     

LUO Yunfeng  LI Weiliang  ZHOU Xiuji  HE Qing  QING Jizu 《Acta Meteorologica Sinica》2000,14(4):490-502

This paper retrieves the yearly and monthly mean 0.75μm aerosol optical depth(AOD) of 41 A-class solar radiation stations over China from 1979 to 1990,and analyzes the spatial and temporal distribution of AOD over China mainland.The data employed are daily direct solar radiation and sunshine duration,as well as the TOMS version-7 ozone observation data in the same time.The results indicate that the Siehuan Basin is the largest center of yearly mean AOD over China.and the other two larger centers lie in Wuhan City and the South Xinjiang Basin,separately.AOD values are also relatively larger in the middle-and-lower reaches area of Changjiang River.Shandong Peninsula and coastal area of Guangdong Province:while in Yunnan Province,coastal area of Fujian Province.most parts of Northwest and Northeast China,AOD values are relatively smaller.The distribution of AOD varies with different months.In most parts of China.the maximum of AOD occurs in spring season;but the minimum varies in different regions,From 1979 to 1990.in the Qinghai-Xizang Plateau,West Siehuan Basin,North Guizhou Province.most areas of the middle-and-lower reaches of Changjiang River,Shandong Peninsula and west part of South Xinjiang Basin.AOD shows an increasing trend.But in Northeast China,most part of Northwest China,Yunnan-Guizhou Plateau,western Guangxi Region and the coastal areas of East China,AOD shows decreasing tendency.Generally,the seasonal variation characteristics of AOD in China can be classified into four typical models,i.e.,mono-modal types A and B,bimodal and Poly-modal.  相似文献   

A NUMERICAL SIMULATION OF THE EFFECT ON CHINESE REGIONAL CLIMATE DUE TO SEASONAL VARIATION OF LAND SURFACE PARAMETERS(PART I)     

SUN Jian  LI Weiliang  ZHOU Xiuji 《Acta Meteorologica Sinica》2001,15(2):129-143

Sensitivity experiment is an important method to study the effect on regional climate due toseasonal variation of land surface parameters.Using China Regional Climate Model(CRCM)nested in CCM1.we first simulate Chinese regional climate,then two numerical sensitivityexperiments on the effect of vegetation and roughness length are made.The results show that:(1)If the vegetation is replaced with the monthly data of 1997.precipitation and land-surfacetemperature are both changed clearly,precipitation decreases and land surface temperatureincreases,but there is no regional correspondence between these changes.And the results aremuch better than the results when climate average vegetation was used in the CRCM.(2)If theroughness length is replaced with the monthly data of 1997,there is significant change on landsurface temperature,and there is very good regional correspondence between these changes.Butthe effect on precipitation is very small.  相似文献   

热力强迫对湿斜压大气中南亚高压平衡态的影响   总被引：1，自引：0，他引：1  

李维亮  刘四臣 《气象学报》1991,49(4):448-457

本文基于Lorenz的湿模式,引入地形效应并进行适当简化,在低谱近似下得到了描述大气运动的非线性耗散系统。讨论了在热力强迫与大气环流的非线性相互作用下,湿、斜压大气在参数空间的平衡态与南亚高压的流型分布及其东西摆动。结果表明:南亚高压典型的平衡态流型是西部型、东部型和带状高压,而且东西部流型的转换并非高压中心的连续位移,而是表现为一个高压中心消失后经过流场上的调整重新建立新的高压中心的过程。  相似文献   

白云鄂博褐钇铌矿族矿物的矿物化学与矿物演化   总被引：1，自引：0，他引：1  

贡伟亮 《矿物学报》1991,11(3):200-207

本文在大量矿物化学资料及高温XRD研究基础上提出了褐钇铌矿族矿物的分类命名方案,详细地研究了该族矿物的化学成分、稀土和特殊稀土组成及固溶关系。发现了M-钍褐铈铌矿、T-钛褐钕铌矿、M-钕褐铈铌矿以及T-钇褐钕铌矿等一批新变种矿物。确定了褐钇铌矿族矿物在时间和空间上的分异演化序列,并讨论了主稀土和特殊稀土在演化过程中的基本行为,首次提出了褐钇铌矿族矿物水解共沉淀形成机理新模式,并确认成矿流体多阶段演化过程中因介质物理化学条件不同,稀土元素配合物呈现的稳定性差异是本族矿物时空演化的根本原因。此外,本文还呼吁对白云鄂博西矿区铕等资源进行评介和开发。  相似文献   

Relativistic Information Entropy on Uncertainty Analysis   总被引：1，自引：0，他引：1  

Jin Weiliang Han Jie Professor  Dr. -Eng.  Dept. of Civil Engineering  Zhejiang University  Hangzhou  Lecturer. Dept. of Information Science  Electronic Engineering  Zhejiang University  Hangzhou 《中国海洋工程》1996,(4)

- in this paper, a new approach to relativistic information entropy is used to assess some relative uncertainties in structural reliability assessment. This approach is composed of the information theory and the relativistic theory, and can be used to measure the relativity of parameter uncertainty and system uncertainty in structural reliability theory based on the same generalized relativistic reference system. Therefore, the structural reliability assessment can be assessed reasonably by the approach.  相似文献   

Evalution of Application of p-y Curve Method in Offshore Engineering Foundation     

Jin Weiliang  Zhu Yuming  Li Linpu Associate Professor  Dr. -Eng.  Zhejiang University  Hangzhou Engineer  Metallurgical Building Design  Research Institute  Beijing Associate Professor  Dalian University of Technology  Dalian 《中国海洋工程》1993,(4)

- Based on the Mohr-Coulomb failure principle and Rankine's theory, the laterally loaded pile ultimate resistance formulas of sand and soft clay proposed by Reese and Matlock respectively are discussed in this paper. The authors put forward the modified ultimate resistance formulas on the basis of which the ultimate resistance formula is developed for horizontally loaded pile in multi-layer soil in consideration of the effect of the overburden soil pressure on the calculation of soil layer. It is significant to the correct application of the ultimate resistance formulas in API and ZCS Rules into offshore engineering.  相似文献   

浅海抗风浪网箱养鱼技术研究   总被引：1，自引：0，他引：1  

徐君义  金伟良 《海洋科学》2001,25(1):12-14

浅海网箱养殖是现代海水养殖业发展的重要途径。由于我国东南沿海多台风和热带风暴 ,加上现有海水网箱结构大多属于小型简陋型 ,结构非规范化 ,抵御海洋自然灾害能力弱。而国外开发的抗风浪网箱养鱼技术投资成本很高 ,技术复杂 ,在我国推广有一定的难度。因此 ,开发适合我国国情的浅海抗风浪网箱养鱼技术就成为必要。有关浅海抗风浪网箱养鱼技术至今未见报道。本文将作者近年在这方面开展的研究所获成果报道如下。１材料与方法１．１材料分别选择浙江乐清湾中心水域的抛西海区、大坦海区和湾口外侧的南排山海区为试验区。水深１０ｍ ,底质为…  相似文献   

MM5 Simulations of the China Regional Climate During the LGM.Ⅱ: Influence of Change of Land Area, Vegetation, and Large-scale Circulation Background          下载免费PDF全文

LIU Yu  HE Jinhai  LI Weiliang  CHEN Longxun 《Acta Meteorologica Sinica》2008,22(1)

Using a regional climate model MM5 nested to an atmospheric global climate model CCM3, a series of simulations and sensitivity experiments have been performed to investigate the relative LGM climate response to changes of land-sea distribution, vegetation, and large-scale circulation background over China.Model results show that compared with the present climate, the fluctuations of sea-land distribution in eastern Asia during the LGM result in the temperature decrease in winter and increase in summer. It has significant impact on the temperature and precipitation in the east coastal region of China. The impact on precipitation in the east coastal region of China is the most significant one, with 25%-50% decrease in the total precipitation change during the LGM. On the other hand, the changes in sea-land distribution have less influence on the climate of inland and western part of China. During the LGM, significant changes in vegetation result in temperature alternating with winter increase and summer decrease, but differences in the annual mean temperature are minor. During the LGM, the global climate, i.e., the large-scale circulation background has changed significantly. These changes have significant influences on temperature and precipitation over China. They result in considerable temperature decreases in this area, and direct the primary patterns and characteristics of temperature changes. Results display that, northeastern China has the greatest temperature decrease, and the temperature decrease in the Tibetan Plateau is larger than in the eastern part of China located at the same latitude. Moreover, the change of large-scale circulation background also controls the pattern of precipitation change. Results also show that, most of the changes in precipitation over western and northeastern parts of China are the consequences of changing large-scale circulation background, of which 50%-75% of precipitation changes over northern and eastern China are the results of changes in large-scale circulation background. Over China, the LGM climate responses to different mechanisms in order of strength from strong to weak are, the large-scale circulation pattern, sea-land distribution, vegetation, CO2 concentration, and earth orbital parameters.  相似文献   

中全新世时期中国地区水循环因子变化的模拟研究     

刘煜  李维亮  何金海  陈隆勋 《气象学报》2009,67(2):201-209

利用全球气候模式CAEM3嵌套区域模式MM5模拟了现代和中全新世时的气候,从模拟结果可以发现中全新世有效降水变化中心随季节变化,最大的有效降水增加出现在夏季东北地区和内蒙古东部,最大值超过3 mm/d;同时,黄河与长江之间区域降水减少,最大变化超过2 mm/d.中国北方地区云量增加,同时,中国东部的长江流域云量减少.高云量变化较小,低云量变化最大,最大变化超过2成.夏季,对应着黄河与长江之间区域的云量减少,这个区域的温度升高最大.从水汽的变化可以看到长江流域地区水汽减少,相对湿度也减少,这与云量的变化一致;华南地区水汽的变化与季节有关;东北地区水汽增加,相对湿度增大,对应云量的增加和降水增多.从结果可以发现相对湿度最大的变化超过15%,不是一个常数.有些地区温度升高,但是水汽却减少.但是,在LGM的温度降低的区域,水汽一致减少.这说明温度降低水汽对应减少,但温度升高不一定对应水汽增加.这与全球尺度水汽相对湿度基本保持常数的结果不同.中全新世时,长江流域除春季外变得干燥、少雨和高温,东北和内蒙古东部变得多雨和潮湿.  相似文献   

非均相化学过程在青藏高原臭氧低谷形成中的作用   总被引：1，自引：0，他引：1  

刘煜  李维亮  周秀骥 《气象学报》2010,68(6):836-846

分析SAGE II资料发现:青藏高原对流层顶最高不超过17.6 km,夏季平均在17 km以下:来自对流层中低层的物质很少能被输送到17.5 km以上,来自对流层中低层的输送不会长时间持续地影响17.5 km以上的区域。青藏高原以及同纬度地区在15 20 km高度温度低于210 K,非均相化学反应可能在此起着重要作用。夏季青藏高原臭氧低谷的形成高度主要是15—20km,而且是长时间持续性的。分析结果显示:15—20km非均相化学过程在夏季青藏高原臭氧低谷的形成中可能起重要作用,特别在17.5—20km高度其所起的作用可能是主要的;而在17.5 km以下,从以往的研究可以知道青藏高原的动力和热力作用对夏季青藏高原臭氧低谷的形成起着主要作用。在春季和秋季,青藏高原上15—20km的臭氧"亏损"也可能是由于非均相化学过程造成的,使得青藏高原臭氧低谷每年从4月持续到10月。并且,影响非均相化学过程的主导因素可能是温度。  相似文献