晚更新世以来贵州清水江阶地发育及地貌意义

对贵州清水江上游马寨、翁东、三江、施洞沿江4个剖面的阶地特征、年代学结果进行了综合分析。发现以凯里断层为界,上游地区的马寨和翁东2个剖面的T2阶地形成时代约为51~57 ka B.P.,T1阶地的形成时代约为25 ka B.P.,下游地区的三江和施洞2个剖面的T2阶地形成时代约为122~102 ka B.P.,T1阶地的形成时代约为78 ka B.P.。选取各剖面的T2阶地的基座高度来计算了河流下切速率,发现上游地区2个剖面（马寨、翁东）的河流下切速率较接近,约为0.41~0.34 m/ka,明显高于下游地区的2个剖面（三江、施洞）的0.16~0.20 m/ka,表现为上游下切速率高,越往下游方向下切速率逐渐降低。这表明自晚更新世以来,清水江上游区域受到构造作用的影响而发生差异抬升,具体表现为西部构造抬升幅度大,阶地下切速率快;东部构造抬升幅度小,阶地下切速率慢。     

基于球面投影的单站地面激光点云直线段提取方法

由于激光点云离散分布于三维空间,导致特征计算困难,目前针对地面激光扫描点云的直线提取方法普遍存在计算量大、提取错误、或适应性不足等问题。本文提出了一种基于球面投影的单站地面激光点云直线段提取方法:首先将三维点云投影到球面上,球面投影后的三维点云保持了正确的邻接关系,同时也解决了三维数据计算量大的问题;然后,利用球面霍夫变换,正确提取球面投影后点云中的直线段特征;最后,利用稳健的直线拟合算法计算点云中的三维直线段参数。通过对室内室外场景数据的直线段提取试验及与商业软件Geomagic Studio等方法的对比试验,验证了本方法的正确性、适用性和准确性。     

一次南方冷季降水过程揭示的热带水汽羽与降水的关系

利用逐日降水量资料、FY-2E卫星资料以及NCEP/NCAR再分析资料,对2012年1月13~16日的一次南方冷季降水过程进行分析,剖析了热带水汽羽形成的水汽输送源和动力机制,及其与降水的关系。分析表明,热带水汽羽不但表征了中高层孟加拉湾水汽的输送,它实际上反映了对流层整层水汽的输送、辐合,低层南海水汽输送带为水汽羽的维持和降水的产生做出了贡献;高空槽前急流与低空切变线的耦合促使了上升运动的形成,导致降水的产生。后期高空槽的移动填塞致使急流轴发生移动及转向,从而引导了热带水汽羽的移动,最终导致热带水汽羽的断裂消亡;热带水汽羽上不存在强对流云团,未形成强对流过程,但由于水汽输送条件较好,配合弱的上升运动产生了这次强降水过程。     

Impacts of meteorology and emission variations on the heavy air pollution episode in North China around the 2020 Spring Festival

Based on the Weather Research and Forecasting model and the Models-3 community multi-scale air quality model(WRF-CMAQ),this study analyzes the impacts of meteorological conditions and changes in air pollutant emissions on the heavy air pollution episode occurred over North China around the 2020 Spring Festival(January to Februray 2020).Regional reductions in air pollutant emissions required to eliminate the PM2.5 heavy pollution episode are also quantified.Our results found that meteorological conditions for the Beijing-Tianjin-Hebei and surrounding"2+26"cities are the worst during the heavy pollution episode around the 2020 Spring Festival as compared with two other typical heavy pollution episodes that occurred after 2015.However,because of the substantial reductions in air pollutant emissions in the"2+26"cities in recent years,and the32%extra reduction in emissions during January to February 2020 compared with the baseline emission levels of the autumn and winter of 2019 to 2020,the maximum PM2.5 level during this heavy pollution episode around the 2020 Spring Festival was much lower than that in the other two typical episodes.Yet,these emission reductions are still not enough to eliminate regional heavy pollution episodes.Compared with the actual emission levels during January to February 2020,a 20%extra reduction in air pollutant emissions in the"2+26"cities(or a 45%extra reduction compared with baseline emission levels of the autumn and winter of 2019 to 2020)could help to generally eliminate regionwide severe pollution episodes,and avoid heavy pollution episodes that last three or more consecutive days in Beijing;a 40%extra reduction in emissions(or a 60%extra reduction compared with baseline emission levels of the autumn and winter of 2019 to 2020)could help to generally eliminate regionwide and continuous heavy pollution episodes.Our analysis finds that during the clean period after the heavy pollution episode around the 2020 Spring Festival,the regionwide heavy pollution episode would only occur with at least a 10-fold increase in air pollutant emissions.     

Analyses of active faults, seismic activities and sea floor unstable factors of the Zhujiang River Mouth Basin and its adjacent areas

-On the basis of the data of geophysics and seismic activities, the analyses of the active faults, seismic activities and the sea floor unstable factors of the Zhujiang River Mouth Basin have been made so as to study the characteristics of the compressional subactive continental margin of Cathaysian system, arc littoral strongly active fracture zone, the division of seismic subzone and seismic zone of the continental margin of northern South China Sea, the potential focal area, and to analyze the regional stability. We consider that the Zhujiang River Mouth Basin belongs to a stable or a moderately stable region.     

腾格里沙漠东南缘生物土壤结皮对土壤理化性质的影响

生物土壤结皮是荒漠生态系统地表景观的重要组成部分,在沙化土地恢复和流沙固定中起着重要作用。研究了腾格里沙漠东南缘固沙植被区不同类型生物土壤结皮理化性质及结皮发育对下层土壤性质的影响。结果表明：结皮层厚度、孔隙度、黏粉粒和田间持水量以及有机碳、无机碳、全氮、碱解氮、速效磷、速效钾含量和电导率均表现为藓类结皮 > 混生结皮 > 地衣结皮 > 藻类结皮;砂粒含量和容重表现为藻类结皮 > 地衣结皮> 混生结皮 > 藓类结皮。结皮下0~2 cm和2~5 cm土层理化性质表现出与结皮层相同的变化规律。总体上,生物土壤结皮对下层土壤理化性质的影响表现为藓类结皮和混生结皮大于地衣结皮和藻类结皮;而结皮对下层土壤理化性质的影响随土壤深度的增加而减小。生物土壤结皮的拓殖和发育是荒漠生态系统成土过程和土壤质量的关键影响因素。     

2018年贵州省常规站温度要素数据评估

随着气象观测的自动化,地面气象观测在观测时次和空间密度上得到极大提高。常规站资料是地面观测资料的重要组成部分,其站点分布合理、监测连续,对于气候变化监测、预测和影响评估有着极为重要的作用。质量控制确保资料的可靠性和代表性,提高资料的应用价值。目前,经过已有的自动化质量控制之后,常规站观测资料中质量控制仍有错判、漏判等问题存在。该文以2018年贵州省常规站气温相关要素数据评估为例,实现本地常规气象资料质量控制方法的优化。