几种流量测量仪表的选择与节能

对国内能源系统常用的几种工业流量测量仪表实际应用选择及节能问题，简要地进行了原理分析和实际应用分析，供使用者优选流量仪表参考。     

Drought prediction using the Along Track Scanning Radiometer (ATSR2) on board ERS2 satellite

Frequent monitoring and estimation of the areas under drought danger is important for agriculture, hydrology, weather, natural hazards and crop yield prediction.     

飞行器热防护与利用一体化系统实验与模拟

通过设计一种基于主动冷却的点阵桁架结构,在降低飞行器质量的同时,实现有效的热防护效果,并在该结构中加入半导体温差发电装置,将产生的气动热转化为电能,可用于飞行器小型用电设备供电.对该热防护与利用一体化系统进行了实验研究.在不同工况下,温差发电功率远大于主动冷却系统的泵功消耗,可实现主动冷却系统的自驱动.通过添加管内表面...     

一种实现飞行品质参数实时辨识的实用方法

考虑到辨识算法收敛的可靠性及结果的精度，采用递推最小二乘估计、飞机运动模态连续－离散模型相互转换及递推极大似然估计，实现飞行品质参数的实时辨识。这种方法的优点在于算法的吸收域是全平面的。初值不影响算法的收敛性，能很好地满足实时性要求，同时还保证了结果精度。利用该方法对某型飞机铁鸟台实测数据进行了处理，取得了满意的结果。     

基于DSP与单片机双机系统的电能质量监测装置

电能质量监控装置在硬件上采用TI公司的C2000系列DSP作为主运算单元,WINBOND公司的W78E58单片机作为主要外设控制单元,在软件上使用了MATLAB算法模拟功能和uC/OS-Ⅱ嵌入式操作系统,设计出一款电能质量监测装置,对提高电能供电质量提供了保障.     

雷达视频地图的坐标变换

主要阐述了在雷达系统中所使用的雷达视频地图与地理点间的坐标变换问题。使用球极平面投影法,将地球上的点与线变换成平面上的点与线。     

标准转换过程中必须做好的几项工作

比较分析了2000版ISO9000族标准与94版标准的差别,提出了经94版标准认证注册的组织在实施转换时必须做好的几项工作和应注意的问题.     

锥形腔高能量激光能量计后向散射问题研究

高能量激光能量的准确计量对于相关研究至关重要。量热法是测量高能量激光能量的一种有效方法,其中涉及到的入射激光在能量计吸收腔内的后向散射总能量,是一个关键参量,它的准确测定与计量,将大大提高高能量激光能量计量的准确性。依据能量计内表面与入射激光相互作用的光学定律,详细推导了锥形吸收腔内入射激光光束能量的分布函数,并结合复化辛普森数值计算方法,分析和讨论了吸收腔结构一定时,环形和矩形两种不同光斑形状的高能量激光在锥形能量计吸收腔开口处的后向散射光功率密度分布和后向散射总功率以及它们对能量测量结果的影响。     

The energy release of substorm and magnetic storm: Its present state and future improvements by KuaFu mission

Considering the KuaFu mission, state of the energy release of substorm and storm is simply presented and it’s improvements by KuaFu mission are investigated. The KuaFu mission will provide us an opportunity to improve our understanding of the energy release during the storm and the substorms. The two KuaFu-B satellites flying in 180° phase-lagged formation in a polar orbit will allow synoptic observations of the auroral oval, central plasma sheet, ring current and other regions. It can monitor the polar region 24/7 continuously. The advantage of the KuaFu mission is to provide the data during all phases of storm and substorm time that can be used to study the global energy release during all phases continuously. The data from auroral imager and other in-situ instruments on board KuaFu-B can be used to study the auroral dynamics and Joule heating during a storm and substorm. The data from the neutral atom imager instrument can be used to study the dynamics and the energy release in the ring current region from sudden commencement to complete storm recovery. Furthermore the data from KuaFu-A, which is around L1 point, can be used to study the interplanetary conditions along with the data from the plasma sheet to study the triggering process and energy release during a substorm. So, KuaFu mission with its continuous time monitoring facilities would enable us to make much progress towards solving the underlying problems.     

Improvement in the GERB short wave flux estimations over snow covered surfaces

Because space-borne radiometers do not measure the Earth’s outgoing fluxes directly, angular distribution models (ADMs) are required to relate actual radiance measurement to flux at given solar angle, satellite-viewing geometries, surface, and atmospheric conditions. The conversion of one footprint broad-band radiance into the corresponding flux requires therefore one to first characterize each footprint in terms of surface type and cloud cover properties to properly select the adequate ADM.

A snow (and sea-ice) retrieval technique based on spectral measurements from the Spinning Enhanced Visible and Infrared Imager (SEVIRI) on board Meteosat 8 is presented. It has been developed to improve the scene identification and thus the ADM selection in the near-real time processing of the Geostationary Earth Radiation Budget (GERB) data at the Royal Meteorological Institute of Belgium. The improvement in the GERB short wave flux estimations over snow covered scene types resulting from angular conversion using dedicated snow ADMs (e.g., empirical snow ADMs and/or pre-computed theoretical snow ADM) instead of empirical snow-free ADMs is discussed.