GPM卫星DPR和GMI探测的2018年5月重庆超级单体云团降水结构特征分析

目前人们对超级单体云团降水回波结构的认知仍有限。本文采用GPM (Global Precipitation Measurement)卫星搭载的测雨雷达DPR (Dual-frequency Precipitation Radar)和微波成像仪GMI (GPM Microwave Imager)的探测结果,结合FY-4A静止卫星多通道扫描成像辐射计(AGRI)的热红外10.8μm通道观测结果、探空站的温湿风观测结果及欧洲天气预报中心再分析数据,利用雷达回波剖面和回波反射率因子概率密度随高度分布的方法,分析了2018年5月重庆地区超级单体云团的降水结构特征。结果表明:该超级单体云团由西北向东南运动的冷空气与暖湿空气交汇而引发;超级单体云团内存在对流降水和层状降水等次尺度系统;强降水区位于云贵高原与四川盆地交界处至盆地的西南部;超级单体暴雨云中冰相粒子多;对流降水的回波顶高度超过12 km,且最大回波强度多数位于地面上空4—5 km;对流降水比层状降水拥有更高的降水粒子浓度,而粒子大小却小于后者;对流降水的粒子尺度随着高度下降而明显增大,反映了其明显碰并增长过程。     

汉江上游沉积记录的东汉时期古洪水事件考证研究

总结近年来在汉江上游古洪水研究成果的基础之上,采用文献资料分析和洪水模拟计算方法,对汉江上游6个沉积剖面纪录的东汉时期古洪水事件进行了年代考证和洪水模拟计算。结果表明,通过分析文献记载的汉江上游东汉时期洪水影响范围、强度和程度,以及结合洪痕沉积规律,在时间上考证认为这6个沉积剖面记录的东汉时期古洪水事件可能是东汉建安二年（197年）九月的一次特大洪水事件。选取合适的河槽横断面和糙率系数,采用HEC-RAS模型对距离较近的4个沉积面记录的东汉时期古洪水事件进行洪水模拟计算,模拟洪水位与各剖面依据古洪水SWD恢复的洪水位误差在-0.18%~0.25%,而且模拟的1983年洪水位与剖面及其附近发现的1983年洪痕水位误差小于0.25%,说明洪水模拟计算选取的河槽横断面和水文参数准确、可靠,从洪水模拟计算的角度也说明了汉江上游沉积记录的东汉时期古洪水事件可能为一次特大洪水事件。该研究结果不仅延长了汉江上游洪水序列,而且也为汉江上游水利工程建设、水资源管理和防洪减灾等提供重要的水文资料。     

An Effective Model to Retrieve Soil Moisture from L- and C-Band SAR Data

This study investigated an appropriate method for soil moisture retrieval from radar images and coincident ground measurements acquired over bare soil and sparsely vegetated regions. The adopted approach based on a single scattering integral equation method (IEM) was developed to establish the relationship between backscatter coefficient and surface soil parameters including volumetric soil moisture content and surface roughness. The performance of IEM in 0–7.6 cm is better than that in 0–20 cm. Moreover, IEM can simulate correctly the backscatter coefficients only for the root mean square (RMS) height s < 1.5 cm at C-band and s < 2.5 cm at L-band by using an exponential correlation function and for s > 1.5 cm at C-band and s > 2.5 cm at L-band by using Gaussian function. However, due to the difficulties involved in the parameterization of soil surface roughness, the estimated accuracy is not satisfactory for the inversion of IEM. This paper used a combined roughness parameter and Fresnel reflection coefficient to develop an empirical model. Simulations were performed to support experimental results and to highlight soil moisture content and surface roughness effects in different polarizations. Results showed that a good agreement was found between the IEM simulations and the SAR measurements over a wide range of soil moisture and surface roughness characteristics. The model had a significant operational advantage in soil moisture retrieval. The correlation coefficients were 77.03 % at L-band and 81.45 % at C-band with the RMSEs of 0.515 and 0.4996 dB, respectively. Additionally, this work offered insight into the required application accuracy of soil moisture retrieval at a large area of arid regions.     

1976年以来香港入境旅游关系圈变化及指示性

入境旅游是衡量一个旅游目的地发展和国际化程度的重要标志。本文引入社会学人际关系理论与地理学距离衰减理论相结合,提出入境旅游关系圈（ITRC）的三层结构概念模型：周边圈、洲内圈和洲际圈。随后,以香港为案例提出了香港入境旅游关系圈（HKITRC）概念模型假设与实际HKITRC变化的指示性假设。在1976-2013年香港各入境客源地的旅游统计数据的基础上,利用空间分层与时间分段的方法对40年来实际HKITRC的变化及指示性进行了深入的实证分析。研究结果验证了假设,总结得出了40年来实际HKITRC三层结构和其内部各地区的变化规律,也证明了实际HKITRC变化对签证政策、人口规模、政治归属、文化传统和经济兴衰这5种因素的指示性。研究对学界及业界认识旅游目的地入境旅游关系圈的变化规律及其指示作用有一定启发和现实意义。     

“天绘一号”卫星在轨几何定标方法

构建了"天绘一号"卫星三线阵影像的严格几何模型,并在此基础上提出了适用于"天绘一号"卫星三线阵相机的在轨几何定标模型,该模型将定标参数分为内外定标参数,并采用分部迭代策略解算。通过对登封地区两景影像的实验表明:本文的定标方法能较好地解决定标参数间的相关性问题;定标后平面精度达到了6.93m,高程精度达到了3.96m;将内外定标参数用于外推定位时,三视立体像对对地目标定位的平面和高程精度分别优于8m和9m。     

Prismatine含义的变化及其在南极中山站区的产出

本文对prismatine(Prs)名称的来历作了简要介绍,指出kornerupine(Krn)系列中一个四面体位置上的B含量可变化于0和1之间(在22(O,OH,F)的分子式中),并伴随成分、晶体结构及矿物组合的变化。以 B=0.5为界划分可出两种不同的矿物:若B<0.5,为Krnss,包括两种情形:B=0,为无B之Krnss,0相似文献   

A coupled ice-ocean model for the Bohai Sea I. Study on model and parameter

1 IntroductionAs an important compartment of global cli-mate system, the development and variation ofsea ice directly affect the global atmosphere andocean environment, especially the deep watersformation and circulation. Therefore, it be-comes one of the keys of the global climatestudy to explore the coupling physical processof sea ice to atmosphere and ocean in the cli-mate system and to set up the global coupledairiceocean system. The studies on the in-teraction of iceocean and its coupled…     

A coupled ice-ocean model for the Bohai Sea Ⅱ. Case study

The coupled ice-ocean model for the Bohai Sea is used for simulating the freezing, melting, and variation of ice cover and the heat balance at the sea-ice, air-ice, and air-sea interfaces of the Bohai Sea during the entire winter in 1998～1999 and 2000～2001. The coupled model is forced by real time numerical weather prediction fields. The results show that the thermodynamic effects of atmosphere and ocean are very important for the evolvement of ice in the Bohai Sea, especially in the period of ice freezing and melting. Ocean heat flux plays a key role in the thermodynamic coupling. The simulation also presents the different thermodynamic features in the ice covered region and the marginal ice zone. Ice thickness, heat budget at the interface, and surface sea temperature, etc. between the two representative points are discussed.     

中华绒螯蟹与日本绒螯蟹线粒体COI基因片段的序列比较研究

以相应引物 PCR扩增了黄河口中华绒螯蟹线粒体细胞色素氧化酶 I亚基基因 (COI)片段 ,PCR产物经 T载体连接之后进行克隆、测序 ,得到 70 9bp的碱基序列 ,其 A,T,G,C含量分别为 34.4 1% ,2 7.93% ,2 0 .0 3%和 17.6 3%。并比较它与珠江流域中华绒螯蟹 COI序列和日本绒螯蟹 COI序列的差异 ,发现黄河口中华绒螯蟹与珠江流域中华绒螯蟹 COI序列完全相同 ,而与日本绒螯蟹差异非常明显 ,70 9或 6 5 8(不计引物 )位点中核苷酸差异数为 32 ,核苷酸差异率为 4 .5 1%或 4 .86 % (不计引物 ) ,其中 2 5个位点为转换 ,7个位点为颠换。作者倾向于支持存在中华绒螯蟹和日本绒螯蟹 ,或它们为同一种的两个地理亚种的观点     

四种鳕鱼的形态学研究

本文对蓝鳕 (Micromesistius poutassou)、远东宽突鳕 (Eleginusgracilis)、大西洋鳕(Gadusmorhua)和太平洋鳕 (G. macrocephalus)等 4种经济鳕鱼类进行了细致的观察 ,对其分节及量度特征进行了测定分析 ,发现所测数据与国内外资料存在一些差异 ;并补充描述了各种的鼻孔、牙齿等形态特征。统计检验表明 :蓝鳕的第 1臀鳍鳍条数、鳃耙数与其他鳕鱼存在显著差异 ;远东宽突鳕的脊椎骨数与其他鳕鱼存在显著差异 ;大西洋鳕和太平洋鳕在上述性状上的差异不明显 ,但 2者的体色有明显差异。从形态特征聚类分析图得知宽突鳕属与鳕属亲缘关系近 ,而蓝鳕属与鳕属亲缘关系远。