基于NS2的TCPW性能改进算法研究

TCP Westwood(TCPW)和Vegas都是基于测量的TCP New-Reno增强算法。TCPW针对ACK流直接估算可用带宽,在慢启动和线性递增部分依然采用传统Reno的盲目递增的机制,导致发送端较为频繁的重传。对这几种算法原理进行分析阐述,并提出1种改进方法,更精确的测量估计带宽,通过网络仿真工具NS2进行验证,明显去除TCP全局同步现象,增强网络性能。     

东海和黄海表层沉积物生物标志物的分布特征及古生态重建潜力

多参数生物标志物法已被广泛用于重建浮游植物生产力和种群结构.但目前还缺乏这一应用的现代证据,尤其是西太平洋边缘海地区.文中作者对东/黄海的表层沉积物中的浮游植物生物标志物的分布进行研究,发现东海表层沉积物中菜子甾醇、甲藻甾醇、长链烯酮的总含量变化范围为357～3 115 ng/g,黄海的总含量变化范围为2 898 ～6 714 ng/g,硅藻、甲藻和颗石藻生物标志物总量基本具有近岸高、离岸低的趋势,与现场调查资料所得到的趋势基本一致.生物标志物比例结果显示在东海的长江口方向离岸越远硅藻相对比例下降,而在长江口以南则是离岸越远硅藻比例升高.在东海和黄海颗石藻所占比例都很低,但是有离岸越远比例升高的趋势.用生物标志物所重建的种群结构的变化趋势与现场调查资料相符,但其绝对值却与现场资料存在差异.本研究为生物标志物重建种群结构提供了现代数据,但是此方法的定量应用还需做进一步的研究.     

基于GIS与三维激光扫描的占建筑保护研究

以三维激光扫描点云数据作为基础数据,以河南大学明伦校区近代建筑群为研究对象,结合地理数据库和三维建模技术.建立了古建筑数据库.利用ArcGIS Engine二次开发平台,设计了基于GIS的古建筑数字化保护系统,并同时探讨了系统建立过程中的若干技术问题.研究结果说明.基于三维激光扫描和GIS的新技术手段,为古建筑的数字化保护带来了新的契机.     

基于WebGIS长江流域防洪调度系统的研究与实现

从长江流域防洪调度实际工作出发,针对长江流域防洪指挥特点,利用ArcGIS Server,ArcSDE与.Net平台相结合,进行了B/S模式的长江流域防洪调度WebGIS系统设计与实现。系统利用高效、便捷的Internet/Intra-net网络资源和基于GIS技术的地图操作功能,实现了长江流域防汛指挥的全局化、实时化、可视化。     

2017-08-09新疆精河Ms6.6地震附近区域相对应变的变化分析

2017年精河M_S6.6地震震前,尼勒克、巴伦台和小泉沟台钻孔应变仪记录到显著的应变变化,经现场落实确认,异常是可靠的。根据这3个台的记录资料计算相对应变的变化,结果表明,地震前最大（小）主应变大小和方向分别出现明显加速和急剧偏转变化。此外还发现,相对应变场异常期间主方向与震源机制解P轴方位较为一致。     

Base cation concentrations in forest litter and topsoil have different responses to climate and tree species along elevational gradients

The forest litter is an essential reservoir of nutrients in forests, supplying a large part of absorbable base cations(BC) to topsoil, and facilitating plant growth within litter-soil system. To characterize elevational patterns of base cation concentrations in the forest litter and topsoil, and explore the effects of climate and tree species, we measured microclimate and collected the forest litter and topsoil(0-10 cm) samples across an elevational range of more than 2000 m(1243 ～ 3316 m a.s.l.),and analyzed the concentrations of BC in laboratory. Results showed that: 1) litter Ca concentration displayed a hump-shaped pattern along the elevational gradients, but litter K and Mg showed saddle-shaped patterns. Soil Ca concentration increased with elevation, while soil K and Mg had no significant changes. 2) Ca concentration in the forest litter under aspen(Populus davidiana) was significantly higher than that in all other species, but in topsoil, Ca concentration was higher under coniferous larch and fir(Larix chinensis and Abies fargesii). Litter K and Mg concentrations was higher under coniferous larch and fir, whereas there were nosignificant differences among tree species in the concentrations of K and Mg in topsoil. 3) Climatic factors including mean annual temperature(MAT), growing season precipitation(GSP) and non-growing season precipitation(NGSP) determined BC concentrations in the forest litter and topsoil. Soil C/N and C/P also influenced BC cycling between litter and soil. Observation along elevations within different tree species implies that above-ground tree species can redistribute below-ground cations, and this process is profoundly impacted by climate. Litter and soil Ca, K and Mg with different responses to environmental variables depend on their soluble capacity and mobile ability.     

基于散射计风场数据的台风强度诊断方法——以海洋二号卫星数据为例

本文提出了一种基于散射计风场数据的台风定强方法。该方法定义了台风所在海区的一个圆形区域上的风速平均值来对台风进行定强,并使用海洋二号卫星散射计历史数据对该方法进行了验证。验证结果表明,该台风定强方法可以克服散射计反演台风风速过低的问题。与台风强度监测的历史记录比较的结果显示,在台风强度低于"强台风"这一强度等级时,该方法能够有效估算台风强度。     

2015年台风“彩虹”过境后下山冷急流引起的南海北部海域异常海面降温

This study deals with a unusual cooling event after Typhoon Mujigea passed over the northern South China Sea(SCS) in October 2015. We analyze the satellite sea surface temperature(SST) time series from October 3 to 18,2015 and find that the cooling process in the coastal ocean had two different stages. The first stage occurred immediately after typhoon passage on October 3, and reached a maximum SST drop of –2℃ on October 7 as the usual cold wake after typhoon. The second stage or the unusual extended cooling event occurred after 7d of the typhoon passage, and lasted for 5d from October 10 to 15. The maximum SST cooling was –4℃ and occurred after 12d of typhoon passage. The mechanism analysis results indicate that after landing and moving northwestward to the Yunnan-Guizhou Plateau(YGP), Typhoon Mujigea(2015) met the westerly wind front on October 5. The lowpressure and positive-vorticity disturbances to the front triggered meridional air flow and low-pressure trough,thus induced a katabatic cold jet downward from the Qinghai-Tibet Plateau(QTP) passing through the YGP to the northwestern SCS. The second cooling reached the maximum SST drop 4d later after the maximum air temperature drop of –9℃ on October 11. The simultaneous air temperature and SST observations at three coastal stations reveal that it is this katabatic cold jet intrusion to lead the unusual SST cooling event.     

中国碱蓬属Suaeda植物研究中的分类学错误

以纠正碱蓬属Suaeda盐生植物研究中广泛存在的分类错误为目的,针对碱蓬属研究中因缺乏正确的种属鉴定与使用错误种名等导致无法确定研究对象是何植物,使研究结果丧失确定性和科学价值的问题,通过对相关错误文献的梳理,对包括《中国高等植物图鉴》在内的有关碱蓬属植物研究文献进行了初步分析,指出了有关碱蓬属植物研究中的同物异名、同名异物以及中文名与拉丁名错乱等问题并予以纠正。对提高碱蓬属植物研究的科学性与可靠性具有重要参考价值。