基于VC++大地电磁数据处理软件开发

研究了GDP大地电磁系统AVG的数据格式,根据实际需要、结合先进的计算机技术和当今比较流行的Visual C++6.0开发工具开发了相应的软件—GDP大地电磁数据处理软件,其中主要功能有：(1)多类型参数数据的曲线显示、参数值的实时显示以及读取存储功能;(2)可视化数据编辑功能;(3)电阻率深度提取功能.笔者在软件系统的设计中,嵌入了模块化思想,为今后完善和移植GDP大地电磁系统数据处理软件奠定了基础.最后通过GDP大地电磁系统数据处理软件对青海某矿区的实测CSAMT资料进行校正处理,效果明显,说明GDP大地电磁系统数据处理软件有较强的实用性.     

利用量子力学势能数据预测温度、压力、盐度和沉积物孔径对甲烷水合物形成和分解的影响

介绍一个预测不同温度、压力、盐度和沉积物毛细管孔径条件下甲烷水合物 溶液 气体多相平衡模型。该模型以Van der Waals和 Platteeuw热力学模型、量子力学从头算粒子相互作用势能、DMW 92状态方程和Pitzer电解质理论为基础,能在很宽广温压范围内预测温度、压力、盐度和毛细管力对甲烷水合物形成和分解的影响。通过对比本模型的预测结果与实验数据,可知本模型能够准确地预测海水和多孔介质中甲烷水合物的相平衡条件。对于一定盐度下多孔介质中甲烷水合物的形成温压条件的在线计算可浏览: www.geochem model.org/models.htm。     

淮河中下游洪泽湖湖泊沉积物粒度特征及其沉积环境意义

以淮河中下游洪泽湖湖底沉积物为研究对象,将放射性核素计年与沉积物粒度分析、粒度平面分形研究以及历史文献资料相结合,初步探讨了洪泽湖湖底沉积物粒度特点及该区域近300年来的气候变化,为恢复百年尺度的气候干湿变化提供了一条新途径。研究发现,湖区气候的干湿变化大致可分为三个阶段。进一步说明沉积物粒度参数的变化不仅与自然环境改变有关,也与人类活动如黄河改道、湖泊周围建闸等关系密切。     

THE STUDY OF RETRIEVAL THEORY AND METHODS FROM SATELLITE REMOTE SENSING FOR METEOROLOGICAL PARAMETERS OVER EASTERN ASIA-PARTI:ISPRM AND SRRM

A review of ten-year's practice in developing the improved simultaneous physical retrievalmethod(ISPRM)is given in the hope that some creative ideas can be drawn from it.Theimprovement upon the SPRM is associated with the under-determinedness of this ill-posed inverseproblem.In our experiment,the precondition is observed that prior information must beindependent of the satellite measurements.The well-posed retrieval theory has told us that theforward process is fundamental for the retrieval,and it is the bridge between the input of satelliteradiance and the output of retrievals.In order to obtain a better result from the forward process.the full advantage of every prior information available must be taken.It is necessary to turn the ill-posed inverse problem into the well-posed one.Then by using the Ridge regression or Bayesalgorithm to find the optimal combination among the first guess,the theoretical analogueinformation and the satellite observations,the impact of the under-determinedness of this inverseproblem on the numerical solution is minimized.     

黄河河口二维泥沙有限元数学模型及应用(Ⅱ)--潮流和泥沙输运沉积过程模拟分析

利用多沙黄河河口潮波平面二维泥沙数学模型,通过典型时刻近海海区潮汐、河口口门河道、河海流场、含沙量、河床变形和海底等值线等图形对入海河口海域潮汐和潮流海洋动力特性、入海泥沙运动扩散输移规律、河口拦门沙形状、形成过程、泥沙冲淤和海底地形变化进行了分析,这些都与实测资料和遥感图像的分析基本一致。     

“野外地质掌中宝”系统的及其应用

“野外地质掌中宝”系统是以Ｗｉｎｄｏｗｓ ＣＥ为软件平台,以掌上电脑为硬件载体, 适用于野外地质勘探和国土资源调查的便携式工作平台。它包括前端工具软件包、后台伺服处理子外地质勘探和国土资源调查技术的一次重要实践,它的研制成功将为野外地质工作才提供面向２１的高效、实用、方便的现代化工作平台。     

四川省地面气象资料统计方法及产品简介

本文简明扼要地介绍了地面气象资料中常用要素的日、旬、月、年值的统计和缺测记录处理方法,对各要素原始观测数据和统计产品中常见的特定值做了较详细的说明.作者全面地介绍了四川省目前广泛用于服务的气候资料产品的文件类型、数据内容和数据格式.     

近50a河池市日照时数空间变化特征分析

基于河池市10个气象站1961-2010年的日照时数数据,采用线性趋势分析、逐步回归分析等方法,依托GIS技术对河池市近50a日照时数的气候倾向率、年代际变化趋势进行分析。结果表明:河池南部及东南部的都安、宜州、巴马、大化县的年日照时数较多(大于1200h),北部及西北部的天峨、南丹、环江县的北部年日照时数较少(小于1000h);全市各地区的年日照时数变化速率值在-82.66 h/10a～19.8 h/10a之间;河池各县的日照时数年代际变化特征各不相同,其中东兰、凤山和都安大部地区的年日照时数的四个年代都是呈现下降的变化趋势。     

EVALUATION OF CORRECTIONS ON TURBULENT FLUXES OBTAINED BY EDDY COVARIANCE METHOD IN HIGH WINDS

This paper investigates processing of fast-response data and corrections of turbulent fluxes obtained by using eddy covariance method based on data collected at an offshore observation tower during three Cold-intrusion(CI)events in the South China Sea in 2010. This study presents the data processing procedure in detail and compares frictional velocities(u*), sensible heat fluxes(H) and latent heat fluxes(LE) yielded by using different averaging periods and different coordinate rotation methods; evaluates the sonic temperature correction for sensible heat flux and the Webb correction for latent heat flux as a function of 10 m wind speed(u10) during the CIs. The results show(1) that the different averaging periods of 30 min and 10 min cause biases of u*(H, LE) within 5%(15%, 62%). The values of u*(H,LE) averaged from 30 mins are mostly larger than those averaged from 10 mins. We suggest that the averaging period of 10 min is not sufficiently long to capture all scale eddies and recommend 30 min averaging period in calculating turbulent fluxes using eddy covariance method during CIs;(2) that the values of u*(H, LE) obtained from double rotation(DR2) and those obtained from planar fit rotation(PF) have good agreements and correlation coefficients between them are larger than 0.99. Because PF method requires unchanged environment and it is easier to apply DR2 method, we suggest DR2 coordinate rotation method in processing fast-response data; and(3) that the median values of frictional velocity(sensible heat flux and latent heat flux) binned according to 2 m s~(-1) intervals of u_(10) increase(decrease,increase) by less than 9%(4%, 10%) by Coriolis corrections(sonic temperature corrections, Webb corrections), which decreases(decreases, increases) with increasing u10 when u10 are 5-17 m s~(-1).     

通过数据挖掘调查气候变化的长期趋势及其因区域和地方环境而产生的空间差异（英文）

Climate change is a global phenomenon but is modified by regional and local environmental conditions.Moreover,climate change exhibits remarkable cyclical oscillations and disturbances,which often mask and distort the long-term trends of climate change we would like to identify.Inspired by recent advancements in data mining,we experimented with empirical mode decomposition(EMD) technique to extract long-term change trends from climate data.We applied GIS elevation model to construct 3 D EMD trend surface to visualize spatial variations of climate change over regions and biomes.We then computed various time-series similarity measures and plot them to examine spatial patterns across meteorological stations.We conducted a case study in Inner Mongolia based on daily records of precipitation and temperature at 45 meteorological stations from 1959 to 2010.The EMD curves effectively illustrated the long-term trends of climate change.The EMD 3 D surfaces revealed regional variations of climate change,while the EMD similarity plots disclosed cross-station deviations.In brief,the change trends of temperature were significantly different from those of precipitation.Noticeable regional patterns and local disturbances of the changes in both temperature and precipitation were identified.The trends of change were modified by regional and local topographies and land covers.