KOSMA 12CO(2–1) and (3–2) observations toward Infrared Dark Clouds     

Dalei Li  Jarken Esimbek  Jianjun Zhou  Willem Baan  Gang Wu  Xindi Tang  Weiguang Ji  Ye Yuan  Yuxin He  Toktarkhan Komesh 《Astrophysics and Space Science》2016,361(7):220

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福安—南靖断裂带特征及其地质意义讨论   总被引：1，自引：0，他引：1  

马金清  徐维光 《福建地质》2010,29(1):67-72

通过对沉积建造、岩浆活动、构造变动以及地球物理和地球化学综合研究,在全国统一的一、二级构造单元划分框架下,以反映早古生代末构造格局为主,福建省大致以福安—南靖断裂构造带为省内一级构造单元为边界划分西部华夏地块、东部闽浙沿海火山侵入杂岩带2个三级构造单元,讨论了福安—南靖构造带特征及其地质意义。  相似文献   

叠前弹性波阻抗反演在四川FL地区礁滩型储层预测中的应用     

胡伟光  李发贵  杨鸿飞 《海相油气地质》2010,15(4)

叠前弹性波阻抗反演对礁滩型储层的预测和流体识别较叠后声阻抗反演的可信度更高,可对含油气性进行半定量—定量描述。以四川FL地区礁滩型储层为重点,以叠前弹性波阻抗反演为技术路线,对该地区反演出的数据体进行交汇解释,预测出了该区礁滩型储层的平面分布特点,预测结果与该区仅有的两口钻井资料相吻合。实践表明,用交会法并结合对储层响应敏感的两个参数泊松比和剪切模量进行储层解释,可靠度较高。  相似文献   

A study of the microphysical processes in a numerically simulated heavy snowfall event in North China: the sensitivity of different snow intercept parameters     

Wenshi Lin  Jinping Meng  C.-H. Sui  Weiguang Meng  Jiangnan Li 《Meteorology and Atmospheric Physics》2009,104(1-2):1-11

We performed a modeling study of the cloud processes in a heavy snowfall event occurring in North China on 20–22 December 2004. The nonhydrostatic Mesoscale Model (MM5) was used to carry out experiments with the Reisner-2 explicit microphysical parameterizations in four nested domains to test the sensitivity of simulated heavy snowfall to different snow intercept parameters. Results show that while the different intercept parameters do not significantly affect the accumulated snowfall amounts at the surface in either total amount or location, some microphysical characteristics of the modeled heavy snowfall event are impacted. The budget of cloud microphysics is analyzed to determine the dominant cloud processes. In the control experiment (CTL) with the snow intercept (N _os) specified as a function of temperature, the primary simulated hydrometeor is snow, and its mixing ratio is an order of magnitude larger than that of the other cloud species. Relative to CTL, the experiment with a fixed intercept (CON3E6) produced lower snow mixing ratios, more cloud water and graupel mixing ratios. Among the two experiments, while snowfall is slightly smaller in CON3E6, other processes like the rate of graupel fall, condensation and evaporation of cloud water, deposition and sublimation of graupel are all larger in CON3E6 than in CTL. Among CTL, CON3E6, and two more experiments (CON2E7: with a smaller fixed intercept; and NOSQS: N _os a function of snow mass mixing ratio), the budget shows that CON3E6 produces the smallest deposition and sublimation of snow, the largest deposition of cloud ice, and the largest conversion from cloud ice to snow.  相似文献   

广州地区雷暴过程云-地闪特征及其环境条件   总被引：5，自引：2，他引：3       下载免费PDF全文

蒙伟光  易燕明  杨兆礼  万齐林 《应用气象学报》2008,19(5):611-619

应用雷电定位系统和高空观测资料并结合雷达回波资料, 对广州地区雷暴过程云-地闪特征进行分析, 并就有、无云-地闪出现的两组不同对流天气过程的环境条件进行了比较研究。结果表明:广州地区的雷暴过程以负的云-地闪为主, 负云-地闪所占比例在90%以上。云-地闪发生频率与雷暴系统强度演变有直接联系, 对于同一系统来说, 随着系统回波强度的增强, 云-地闪发生的频率也增高。但不同系统中, 云-地闪发生频率有很大不同, 回波强(弱)的对流系统并不意味着云-地闪发生的频率就高(低)。有云-地闪记录的对流天气过程具有更大的垂直切变、更高的相对风暴螺旋度以及更多的对流抑制能量, 云-地闪现象更易于出现在更加有组织和更强的对流系统中。研究还发现广州及周边城市区域对雷暴系统回波强度及云-地闪现象可能有影响, 两个典型个例分析表明, 雷暴系统移经城市区域时回波强度减弱, 云-地闪发生频率减小, 雷暴移过城市区域后, 强度可重新加强, 云-地闪发生频率增大。  相似文献   

塔里木盆地库车坳陷白垩纪层序地层格架及古地理演化   总被引：12，自引：1，他引：11       下载免费PDF全文

梅冥相  于炳松  靳卫广 《古地理学报》2004,6(3):261-278

白垩纪的库车坳陷是一个干旱气候条件下的内陆坳陷,其中只发育下白垩统,为一套干旱红层地层,进一步划分为亚格列木组、舒善河组、巴西盖组和巴什基奇克组。该套干旱红层,包括洪积扇砾岩、间歇性河流砂砾岩、风成砂岩和沙漠湖紫红色泥岩等沉积。这些沉积在地层记录中常以一种特别的旋回性形式产出,在不整合面及其相关面之上首先沉积的是洪积扇砾岩和间歇性河流砂砾岩所构成的冲积沉积物,向上逐渐演变为沙漠湖红色泥岩,在成湖初期或湖退期发育了滨湖相风成砂岩,它们构成了一个较为典型的沙漠沉积体系。从冲积沉积到湖泊沉积构成总体向上变细的沉积相序组合。按照地层记录的旋回性进行三级沉积层序划分,将库车坳陷下白垩统划分为5个三级沉积层序即SQ1至SQ5。下白垩统的顶和底界面均为间断时间很长的区域不整合面,由它们所限定的下白垩统本身则构成一个二级构造层序,在二级构造层序内三级沉积层序常常形成有规律的叠加形式,下部的SQ1和上部的SQ5发育较多的冲积粗碎屑物,中部SQ2至SQ4则以湖泊相沉积为主。与海相地层不同,库车坳陷白垩系中由三级层序和二级层序所代表的地层记录中的中周期和长周期旋回的主要控制因素是幕式构造沉降,沉降初期由于地形高差大而以发育冲积粗碎屑物为主,均衡沉降期则与成湖期相对应从而发育较多的细粒沙漠湖沉积。以沉积物的时间演化序列和沉积相的空间展布形式所代表的规律性入手,建立库车坳陷下白垩统的层序地层格架,在层序地层框架内,系列层序地层格架栅状图和相应的古地理图较为清晰地反映出早白垩世库车坳陷的古地理面貌,以及相应的沉积岩相古地理演变过程。  相似文献   

Assimilation of Hourly Surface Observations with the Canadian High-Resolution Ensemble Kalman Filter     

Weiguang Chang  Dominik Jacques  Luc Fillion  Seung-Jong Baek 《大气与海洋》2017,55(4-5):247-263

An hourly-cycling ensemble Kalman filter (EnKF) working at 2.5?km horizontal grid spacing is implemented over southern Ontario (Canada) to assimilate Meteorological Terminal Aviation Routine Weather Reports (METARs) in addition to the observations assimilated operationally at the Canadian Meteorological Centre. This high-resolution EnKF (HREnKF) system employs ensemble land analyses and perturbed roughness length to prevent an ensemble spread that is too small near the surface. The HREnKF then performs continuously for a four-day period, from which twelve-hour ensemble forecasts are launched every six hours. The impact on analyses and short-term forecasts of assimilating METAR data is given special attention.

It is shown that using ensemble land surface analyses increases near-surface ensemble spreads for temperature and specific humidity. Perturbing roughness length enlarges the spread for surface wind. Given sufficient ensemble spread, the four-day case study shows that the near-surface model state is brought closer to surface observations during the cycling process. The impact of assimilating surface data can also be seen at higher levels by using aircraft reports for verification. The ensemble forecast verification suggests that METAR data assimilation improves ensemble forecasts of air temperature and dewpoint near the surface up to a lead time of six hours or even longer. However, only minor improvement is found in surface wind forecasts.  相似文献   

国有企业创新发展与东北三省经济增长：基于VEC模型的分析     

王伟光  侯军利  白雪飞 《地理科学》2016,36(9):1293-1300

在构建国有企业创新发展对地区经济增长影响的理论模型基础上,设计国有企业创新发展与经济增长评价指标体系,基于协整和VEC模型,对东北三省国有企业对经济数量增长和经济质量增长的作用进行了实证分析。实证结果表明：东北三省国有企业创新发展与地区经济增长数量和质量之间的关系存在着非同步性,而且这种关系特点也与全国地区的实证结果存在显著的差异性。  相似文献   

Crust and upper mantle structures beneath Northeast China from receiver function studies          下载免费PDF全文

Zhen Guo  Yuliang Cao  Xianguang Wang  Y. John Chen  Jieyuan Ning  Weiguang He  Youcai Tang  Yongge Feng 《地震科学（英文版）》2014,27(3):265-275

P-wave and S-wave receiver function analyses have been performed along a profile consisted of 27 broadband seismic stations to image the crustal and upper mantle discontinuities across Northeast China. The results show that the average Moho depth varies from about 37 km beneath the Daxing’anling orogenic belt in the west to about 33 km beneath the Songliao Basin, and to about 35 km beneath the Changbai mountain region in the east. Our results reveal that the Moho is generally flat beneath the Daxing’anling region and a remarkable Moho offset (about 4 km) exists beneath the basin-mountain boundary, the Daxing’anling-Taihang Gravity Line. Beneath the Tanlu faults zone, which seperates the Songliao Basin and Changbai region, the Moho is uplift and the crustal thickness changes rapidly. We interpret this feature as that the Tanlu faults might deeply penetrate into the upper mantle, and facilitate the mantle upwelling along the faults during the Cenozoic era. The average depth of the lithosphere-asthenosphere boundary (LAB) is ~80 km along the profile which is thinner than an average thickness of a continental lithosphere. The LAB shows an arc-like shape in the basin, with the shallowest part approximately beneath the center of the basin. The uplift LAB beneath the basin might be related to the extensive lithospheric stretching in the Mesozoic. In the mantle transition zone, a structurally complicated 660 km discontinuity with a maximum 35 km depression beneath the Changbai region is observed. The 35 km depression is roughly coincident with the location of the stagnant western pacific slab on top of the 660 km discontinuity revealed by the recent P wave tomography.  相似文献   

基于MODIS谱纹信息融合的海洋溢油检测方法     

苏伟光  苏奋振  杜云艳 《地球信息科学学报》2014,16(2):299-306

鉴于仅依赖光谱特征或纹理特征的传统溢油检测算法的信息检测精度较低的问题,本文提出了一种新的光学遥感数据的谱纹海面溢油检测方法。谱是光学遥感数据的油膜敏感波段图像,纹是利用灰度共生矩阵计算获得的图像纹理特征,将这些特征相结合,引入支持向量机方法（Support Vector Machine,SVM）,建立谱纹海面溢油检测模型。本文以2006年渤海溢油事故为例,利用中等分辨率成像光谱仪MODIS的光学遥感数据对溢油进行检测,MODIS的第2波段为油膜敏感波段,所以,第2波段图像即为选取的谱特征,经过对各个纹理特征的分析得到,均值、对比和相关3个特征量可作为溢油提取的纹理特征。检测结果的总体精度达91.23%。试验结果表明,将MODIS图像的光谱特征和纹理特征相结合,可有效地对渤海海洋油膜信息进行检测,并具有很强的抑制噪声能力。  相似文献