Impact of Megacity Shanghai on the Urban Heat-Island Effects over the Downstream City Kunshan     

Han-Qing Kang  Bin Zhu  Tong Zhu  Jia-Li Sun  Jian-Jun Ou 《Boundary-Layer Meteorology》2014,152(3):411-426

The impact of upstream urbanization on the enhanced urban heat-island (UHI) effects between Shanghai and Kunshan is investigated by analyzing seven years of surface observations and results from mesoscale model simulations. The observational analysis indicates that, under easterly and westerly winds, the temperature difference between Shanghai and Kunshan increases with wind speed when the wind speed \(<\) 5 m s \(^{-1}\) . The Weather Research and Forecasting (WRF) numerical model, coupled with a one-layer urban canopy model (UCM), is used to examine the UHI structure and upstream effects by replacing the urban surface of Shanghai and/or Kunshan with cropland. The WRF/UCM modelling system is capable of reproducing the surface temperature and wind field reasonably well. The simulated urban canopy wind speed is a better representation of the near-surface wind speed than is the 10-m wind speed at the centre of Shanghai. Without the urban landscape of Shanghai, the surface air temperature over downstream Kunshan would decrease by 0.2–0.4  \(^{\circ }\) C in the afternoon and 0.4–0.6  \(^{\circ }\) C in the evening. In the simulation with the urban landscape of Shanghai, a shallow cold layer is found above the UHI, with a minimum temperature of about \(-0.2\) to \(-\) 0.5  \(^{\circ }\) C during the afternoon hours. Strong horizontal divergence is found in this cold layer. The easterly breeze over Shanghai is strengthened at the surface by strong UHI effects, but weakened at upper levels. With the appearance of the urban landscape specific humidity decreases by 0.5–1 g kg \(^{-1}\) within the urban area because of the waterproof property of an urban surface. On the other hand, the upper-level specific humidity is increased because of water vapour transferred by the strong upward vertical motions.  相似文献   

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欧江霞  李明峰  王永明  徐燕 《大地测量与地球动力学》2014,34(3):160-163

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李明峰  欧江霞  王永明  解晨  王春 《大地测量与地球动力学》2014,34(3):68-71

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A Modified Certainty Coefficient Method（M-CF） for Debris Flow Susceptibility Assessment：A Case Study for the Wenchuan Earthquake Meizoseismal Areas   总被引：2，自引：1，他引：1  

WANG Jun  YU Yan  YANG Shun  LU Gui-hong  OU Guo-qiang 《山地科学学报》2014,11(5):1286-1297

In the meizoseismal areas hit by the China Wenchuan earthquake on May 12, 2008, the disasterprone environment has changed dramatically, making the susceptibility assessment of debris flow more complex and uncertain. After the earthquake, debris flow hazards occurred frequently and effective susceptibility assessment of debris flow has become extremely important. Shenxi gully in Du Jiangyan city, located in the meizoseismal areas, was selected as the study area. Based on the research of disaster-prone environment and the main factors controlling debris flow, the susceptibility zonations of debris flow were mapped using factor weight method（FW）, certainty coefficient method（CF） and geomorphic information entropy method（GI）. Through comparative analysis, the study showed that these three methods underestimated susceptible degree of debris flow when used in the meizoseismal areas of Wenchuan earthquake. In order to solve this problem, this paper developed a modified certainty coefficient method（M-CF） to reflect the impact of rich loose materials on the susceptible degree of debris flow. In the modified method, the distribution and area of loose materials were obtained by field investigations and postearthquake remote sensing image, and four data sets, namely, lithology, elevation, slop and aspect, wereused to calculate the CF values. The result of M-CF method is in agreement with field investigations and the accuracy of the method is satisfied. The method has a wide application to the susceptibility assessment of debris flow in the earthquake stricken areas.  相似文献   

Numerical Study on Tidally Induced Cross-Frontal Mean Circulation     

Changming Dong  Dake Chen  Hsien-Wang Ou 《大气与海洋》2015,53(3):363-375

An analytical solution for a circulation across a tidal front obtained by Dong, C., Ou, H-W., Chen, D., &; Visbeck, M. (2004 Dong, C., Ou, H-W., Chen, D., &; Visbeck, M. (2004). Tidally induced cross-frontal mean circulation: Analytical study. Journal of Physical Oceanography, 34, 293–305. doi: 10.1175/1520-0485(2004)034<0293:TICMCA>2.0.CO;2[Crossref], [Web of Science ®] , [Google Scholar]). Tidally induced cross-frontal mean circulation: Analytical study. Journal of Physical Oceanograph, 34, 293–305) suggests that the cross-frontal circulation can be decomposed into four parts: frontal cell, Ekman cell, Bernoulli cell, and Stokes drift. This study examines the analytical solution thoroughly using a two-dimensional numerical model solving primitive Navier-Stokes equations. The direct comparison between the numerical and the analytical models of three cases (winter tidal front, summer tidal front, and no front) with the same configurations demonstrates that the analytical solution captures the major features of the cross-frontal circulation. A series of numerical experiments are applied to study the sensitivity of the cross-frontal circulation to physical variables: tidal intensity, horizontal topography scale, frontal strength, and vertical eddy viscosity. The ratio of the tidal excursion distance to the topographical scale is crucial to the Ekman cell in the homogenous ocean. With a greater density gradient, both the Bernoulli and Ekman cells are enhanced. Assumptions made in the analytical model are also examined. The uniform eddy viscosity and linearization in the analytical model could overestimate the bottom flow in the Ekman cell and underestimate the Bernoulli cell in the shallower region, respectively. The influence of the internal tide on the cross-frontal circulation is discussed.  相似文献   

辽河东部凹陷火山岩相测井响应特征及储集意义     

刘宗利  王祝文  刘菁华  赵淑琴  欧伟明 《吉林大学学报(地球科学版)》2018,48(1):285-297

在郯庐断裂多期构造活动作用下,辽河坳陷东部凹陷发生了多期火山活动,致使中基性火山岩广泛发育,以玄武岩和粗面岩为主,可分为5相14亚相。以常规测井曲线特征为基础,结合电成像的分析,识别出了爆发相（火山碎屑流和热基浪亚相）、溢流相（玻质碎屑岩、板状熔岩流和复合熔岩流亚相）、侵出相（内带、中带和外带亚相）和火山沉积相（含外碎屑和再搬运火山碎屑沉积亚相）10种岩相/亚相：火山碎屑流亚相具"焊接"特征,热基浪亚相具层理特征;玻质碎屑岩亚相具高CNL的特征,板状熔岩流亚相DEN、CNL和AC测井曲线显示微齿平滑的特征,而复合熔岩流亚相测井曲线呈指状叠加的特征;侵出相内带→中带→外带电阻率逐渐减小;含外碎屑和再搬运火山碎屑沉积亚相GR值范围不同,并且再搬运火山碎屑沉积亚相具水平层理特征。火山岩相控制原生储集空间的类型,并作用于后期的次生改造,从而影响储层的物性、储集性和有效性。复合熔岩流亚相储层孔隙发育,物性好,但由于内部纵向上结构不一致,非均质性强,因而储层含油性差。火山碎屑流亚相内部在纵向上岩性及结构相对一致,因而储层物性相对均一、分布集中,为有利的火山岩储层,可以作为东部凹陷进一步勘探开发的有利相带。  相似文献   

对部分简单形体产生的自然电位进行定量分析     

欧塬圩 《地质与勘探》2017,53(2):310-317

本文提出了一种新的特征点法,并在前人的基础上改进了一种数值计算方法(最小二乘法),以此来确定部分具有自然电位异常简单地质体的形态(形态系数)、埋藏深度、极化角和电偶极矩。特征点法通过剖面上三个特殊点(两个极值点和零电位点)的值以及它们相互间的距离便可快速求取地质体各参数。改进的最小二乘法则是在前人的基础上加入了零电位点的计算及其它处理方法,以此来获得准确性更高的地质体各参数。两种方法都被用来计算加入±5%随机误差的理论模型数据,并在土耳其的一个实际野外数据中得到测试。结果表明所求的参数与实际参数具有较好的一致性。  相似文献   

A1B情景下东亚地区未来春季沙尘变化趋势预估     

宿兴涛  张志标  欧磊 《中国沙漠》2017,37(2):315-320

采用区域气候与沙尘耦合模式RegCM4-Dust,模拟研究了A1B情景下东亚地区未来（2015-2100年）春季沙尘变化趋势。结果表明：（1）总体上,东亚沙尘源区起尘通量与沉降通量存在明显的振荡特征,而沙尘光学厚度呈现显著的波动减小趋势;源区下游沙尘光学厚度和沉降通量均呈现显著的波动增大趋势。（2）沙尘子源区中,仅塔克拉玛干沙漠及周边地区起尘通量有显著波动减少趋势,速度达-2.1%/10a;萨雷耶西克阿特劳沙漠和呼伦贝尔沙地沙尘光学厚度减小速度最快,分别达到-2.8%/10a、-2.3%/10a。（3）未来,中国华北南部、黄淮以及长江中下游地区以及中国东、南部近海春季沙尘光学厚度增速均为1.5%/10a;中国近海沙尘沉降通量显著上升,速度达1.9%/10a。（4）地面风速尤其是最大风速变化是导致起尘通量变化的主要因素,而影响光学厚度的主要因素是地面最大风速。  相似文献   

Robust estimation for correlated observations: two local sensitivity-based downweighting strategies   总被引：1，自引：1，他引：0  

Jianfeng Guo  Jikun Ou  Haitao Wang 《Journal of Geodesy》2010,84(4):243-250

An iterative robust estimation procedure for correlated observations is proposed, in which the a-prior correlation coefficient matrix is not updated to alleviate the computational burden. Selection of the downweighting strategy plays a key role in the proposed method. Two local sensitivity-based strategies, one is based on the uniformly most powerful test statistics, the other is based on the standardized least squares residuals, are developed and analyzed. Monte Carlo simulations in the GPS network adjustment scenario demonstrate that, the two strategies can provide a certain resistance against the deteriorating effect of outlying observations on the parameter estimates; the former downweighting strategy is superior to the latter one, both in terms of robustness and computational efficiency.  相似文献   

贵州喀斯特石漠化防治的国家重点生态功能区生态系统健康度评价     

邓欧  李亦秋  杨广斌  李若霜 《中国岩溶》2020,39(5):689-696

文章以桂黔滇喀斯特石漠化防治的国家重点生态功能区贵州区为研究对象,以2010、2015年遥感影像、基础地理信息、降水、土壤等数据资料为基础,集成3S技术和生态评估模型,对水源涵养、土壤侵蚀和石漠化进行定量和定位研究。结果表明:研究区4个亚区的水源涵养功能等级处于“中”、“高”等水平,2015年比2010年的水源涵养指数有所提高;威宁—赫章区、关岭—镇宁区和册亨—望谟区3个亚区的土壤侵蚀模数较大,水土保持功能等级处于“低”等,罗甸—平塘区的土壤侵蚀模数最低,其水土保持功能等级为“中”等;威宁—赫章区2010年中度以上石漠化比重达16.36%,2015年降为8.74%,生态系统健康度从“低”转为“中”;关岭—镇宁2010年和2015年中度以上石漠化比重分别为8.64%和4.49%,生态系统健康度从“中”转化“高”;册亨—望谟和罗甸—平塘的健康度均为“高”,2015年相比2010年均有所提升;4个亚区的石漠化恶化面积所占比重均不到1.00%,石漠化好转区域分别占27.00%、14.10%、10.24%和5.13%,石漠化得到了有效遏制。今后应继续因地制宜,恢复植被和生态系统,巩固和扩大石漠化防治成果。   相似文献