青藏高原近25年来河流、湖泊的变迁及其影响因素

结合20世纪70年代中期的MSS图像和90年代末期的ETM 图像解译,对近25年来青藏高原河流、湖泊的分布现状及其变迁进行了分析。研究表明,青藏高原河流总体上变化不明显,部分地区外流水系个别河段略有摆动,内流水系少数河段发生改道、断流,入湖河流河口段发生延伸、退缩等变化。青藏高原多数天然湖泊变化较大,主要是部分湖泊面积缩小或扩大;少数湖泊解体或归并;有的已干涸的湖泊又重新汇水,有的湖泊则接近干涸。导致河流、湖泊演变的主要影响因素有气温变化、降水变化及冰川变化、气候雪线变化等。     

Benthic community response to habitat variation: A case of study from a natural protected area,the Celestun coastal lagoon

Little information currently exists on spatial and temporal benthic community variations in tropical coastal lagoons. Here, the benthic community response to habitat variation in the Celestun coastal lagoon, northwest Yucatan peninsula, was seasonally examined during the 1994–1995 climatic cycle into a grid of 12 sampling sites distributed along the salinity gradient of the lagoon. Habitat variation was assessed through physical factors associated both to the water column (e.g. salinity) and the bottom sediment (e.g. sand, silt and clay fractions). The benthic community response was assessed through species diversity measures and abundance. Under the influence of climatic seasonality, variations in habitat conditions followed by changes in the benthic community characteristics were expected. Results from two-way ANOVAs showed that for the period of study, Celestun lagoon was more heterogeneous along the spatial axis of variability than along the temporal one. Multiple regression analysis showed that salinity was spatially the main factor influencing the benthic community characteristics. Temporally, the sediment characteristics were observed to exert significant effects on the species diversity characteristics but not on abundance. Other variables assessed (dissolved oxygen, pH, temperature and water column transparency) exhibited no significant covariance with species diversity and abundance. Since generated from historical data, these results have the potential to be useful as a benchmark to the establishment of monitoring programs in the light of the increasing anthropogenic pressure on the natural resources of the lagoon and surrounding coastal area.     

基于数字高程模型制作山区坡度分级栅格数据

山区的坡度分析可为规划建设和土地利用提供所需的地理底图,对此较为准确、有效的方法是利用高精度的数字高程模型DEM进行坡度计算及分析,数字高程模型相比于其他数据更适用于数字地形分析.本文阐述了基于1∶50 000比例尺的数字高程模型并利用ArcGIS软件进行山区坡度的计算及坡度分级栅格数据的制作,将结果与高分辨率正射影像进行叠加以初步检查结果的正确性,最后将坡度在25°以上的区域提取出来并以矢量文件形式输出.     

Characterization of SNAP-25 gene from marine teleostean, Lateolabrax japonicus

The t-SNARE protein SNAP-25 (synaptosome-associated protein of 25 kDa) plays an essential role in regulating fusion between the vesicle and plasma membranes during exocytosis. To clone and characterize SNAP-25 gene, the first step in the functional study of SNARE proteins in marine teleostean, was to obtain the cDNA of sea perch SNAP-25 (SPsn25) by RT-PCR and RACE-PCR amplification of a Japanese sea perch. The full-length cDNA of 831bp contains a CDS of 615 bp, coding 204 amino acid residues, and a 5′UTR of 219bp. Bioinformatic analysis revealed that SPsn25 corresponds with SNAP-25a isoform and shares 91.1% identity with SNAP-25a of a goldfish and a zebrafish. The SPsn25 expression in both mRNA and protein levels in the Japanese sea perch had been identified through semi-quantitative RT-PCR and Western Blot assay. Together, these data again confirmed the nerve tissue specificity of the fish SNAP-25 gene expression.     

TCP/IP网络隧道技术研究

论述了TCP／IPTunnel技术的实现原理，研究了TCP／IPTunnel所依靠的IP协议与UDP协议，以及IP层（网际层）的部分协议，传输层的协议。并讨论了NetwareTCP／IPTunnel技术。     

基于SCO-UNIX的地市局办公业务网站(Intranet)建设

文中介绍了在SCO—UNIX操作系统上建设地市局办公业务网站的原理与方法，并结合本地实际，依托现有的X．25业务网络，初步建成白银市气象局办公业务内部网站，使之成为各科室、各县局传输资料、共享信息、交流技术的平台。     

甘肃省航危报编辑分发系统

文中全面介绍了航危报编辑分发系统的功能和运行流程 ,系统介绍了基于Unix平台先进的气象通信软件设计思想及实现方法。航危报编辑分发系统包括主控模块、航危报监控处理模块、编辑分发模块、业务监控和管理模块以及系统维护等 5大部分等组成。此系统的成功开发便于我们利用网络技术实现对航危报大用户的网络报文传输 ,达到节省大量电信传报费用的目的 ,带来了较可观的经济效益     

Construction of a high-resolution gridded rainfall dataset for Peru from 1981 to the present day

ABSTRACT

A new gridded rainfall dataset available for Peru is introduced, called PISCOp V2.1 (Peruvian Interpolated data of SENAMHI’s Climatological and Hydrological Observations). PISCOp has been developed for the period 1981 to the present, with an average latency of eight weeks at 0.1° spatial resolution. The merging algorithm is based on geostatistical and deterministic interpolation methods including three different rainfall sources: (i) the national quality-controlled and infilled raingauge dataset, (ii) radar-gauge merged precipitation climatologies and (iii) the Climate Hazards Group Infrared Precipitation (CHIRP) estimates. The validation results suggest that precipitation estimates are acceptable showing the highest performance for the Pacific coast and the western flank of the Andes. Furthermore, a meticulous quality-control and gap-infilling procedure allowed us to reduce the formation of inhomogeneities (non-climatic breaks). The dataset is publicly available at https://piscoprec.github.io/ and is intended to support hydrological studies and water management practices.     

Crystal structures of iron bearing tetrahedrite and tennantite at 25 and 250°C by means of Rietveld refinement of synchrotron data

Rietveld refinement of X-ray synchrotron data was performed for two synthetic tetrahedrite samples, with 0.61 and 1.83 Fe atoms, and two synthetic tennantite samples with 0.10 and 1.23 Fe atoms p.f.u. M₁₂(Sb,As)₄S₁₃. Measurements were performed at 25 and 250°C. For both the phases, increased Fe substitution is reflected in the increased tetrahedral ‘Cu1’–S distance (‘Cu1’ is a site of Fe substitution) and Cu2–S distances. Cu2 was refined as a split position; the Cu2–Cu2 split about the plane of the S1₂S2 triangle is about 0.56 and 0.65 Å for tetrahedrite and tennantite, respectively. Cu2–Cu2 distances in the structure cavity are 2.8–2.9 Å. Between 25 and 250°C, the lattice parameter a increased by 0.02–0.04 Å and the interatomic distances by 0.01 Å on an average. Thermal expansion coefficients of little-substituted samples are similar to those of unsubstituted samples, whereas thermal expansion appears to decrease with increasing substitution by Fe. The Cu2–Cu2 split increases at 250°C by about 0.1 Å for tetrahedrite and by more than 0.15 Å for tennantite but the cage expansion is minimal so that the Cu2–Cu2 distances in the cavity decrease with temperature. Difference Fourier maps indicate that there is little residual electron density left between the two Cu2 half-sites in tetrahedrite but this inter-site density is substantially higher in tennantite. It increases with temperature, especially in the little-substituted tennantite sample.