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排序方式: 共有72条查询结果,搜索用时 156 毫秒
51.
P.V. Radhadevi S.S. Solanki R. Ramchandran R. Krishnan 《International Journal of Applied Earth Observation and Geoinformation》2008,10(2):133-1
Wide image swath with a high geometric resolution is required for photogrammetric applications. Both demands can be satisfied using staggered line arrays. Different bands of IRS-P6 LISS-4 sensor use staggered arrays for imaging. This paper describes a method for computing the offset for geometric alignment of odd and even lines of the staggered array of IRS-P6 LISS-4 imagery. The odd and even pixel rows are separated by 35 μm (equal to 5 pixels) in the focal plane in the along-track direction. Slightly different viewing angles of both lines of a staggered array can result in a variable sampling pattern on the ground because of the attitude fluctuations, satellite movement, terrain topography, PSM steering and small variations in the angular placement of the CCD lines (from the pre-launch values) in the focal plane. Non-accounting of this variable sampling value during the video data alignment will introduce deterioration of image quality and geometric discontinuity of features. The stagger parameters can be computed by the reconstruction of the viewing geometry with a calibrated camera geometry model and a public domain DEM. The impact of the line separation in the focal plane during imaging for different viewing configurations and terrain heights are studied and reported in this paper. Computed values from the model are in good agreement with what is observed in the raw image for different view angles. The results verify the model and are representative of the stability of the platform. 相似文献
52.
高拴柱 《热带气象学报(英文版)》2001,7(2):209-217
Using the T63L16 analysis data with the resolution of 1.875╳1.875 degree of latitude and longitude
obtained from National Meteorological Center (NMC) and the real central position information of tropical
cyclone (referred to as TC hereafter) numbered by NMC, the basic environmental geostrophic flow at 126
time levels of 25 TCs in 1996 are calculated. The vertical distribution features of the flows are analyzed. Besides, the deviation of real TC tracks from the flows (referred as steering deviation hereafter, namely, the deviation between the real central position of TC and the position calculated according to the steering flow) is also investigated. The result shows that the steering deviation would be different if the domain used to calculate the steering flow is different. The present paper obtains the optimum domain size to calculate the steering flow. It is found that the steering deviation is related to the velocity of steering flow and the initial latitude and intensity of TC itself, and that TC motion has relationship with the vertical shear structure of environmental geostrophic flow. The result also shows that the optimum steering flow is the deep-layer averaged basic flow from 1000 hPa to 200 hPa. Having the knowledge of these principle and features would help make accurate forecast of TC
motion. 相似文献
53.
本文利用WRF模式及其伴随模式研究了2005年发生在西北太平洋的一对双台风玛娃和古超的移动路径与强度的伴随敏感性特征,一方面探讨了环境场对双台风的影响,另一方面也讨论了双台风之间的相互影响过程的差异.首先,利用双台风初始化技术准确地模拟了双台风的演变过程,并以此模拟结果为背景场计算了台风的中心扰动气压和引导气流的伴随敏感性.研究结果表明:伴随敏感性不但能反映环境场对双台风的影响,还能指示双台风之间相互影响过程的差异.从台风强度的敏感性来看,影响台风强度变化的高影响区均位于台风中心附近,弱台风古超的强度敏感性的量级要大于强台风玛娃的强度敏感性,表明双台风中较弱的那个更容易受到外部环境变化的影响.台风引导气流的敏感性分布也存在较大差异,强台风玛娃的移动主要受到其西北侧的高空槽,其自身环流以及台风古超的影响,而弱台风古超的引导气流的敏感性主要位于其自身环流附近以及双台风之间的区域.最后,通过在理想试验中增加初始时刻高空槽的强度以及弱台风古超的强度,证实了台风玛娃的移动路径的变化与伴随敏感性的分析一致. 相似文献
54.
Topographic steering of dense overflows: Laboratory experiments with V-shaped ridges and canyons 总被引:1,自引:0,他引:1
Topographic corrugations such as canyons and ridges cross-cutting the path of a dense plume may effectively steer all or part of the plume downslope. Here, topographically steered flows are investigated experimentally, as laminar, dense gravity currents are observed to impinge on and flow along sloping, V-shaped canyons and ridges. Ridges, as well as canyons, were observed to steer the dense water downslope. A dynamical regime, in which the along-slope transport is balanced by a return flow in the Ekman layer to maintain a geostrophically balanced downslope flow along the corrugation, has been proposed. Results from a previously published analytical model describing such flows are compared with the laboratory experiments. The response of the flow to variations in four governing parameters (slope, rotation, volume flux and reduced gravity) is generally described well by the model and results agree qualitatively, although theory slightly underestimates the dense layer thickness. Vertical velocity profiles resolving the Ekman spiral were obtained using a laser Doppler velocimeter and they showed the secondary, transverse circulation superimposed on the primary, downslope flow. A particle flowing down the canyon/along the ridge can be expected to follow a helix-like path, and dye released within the dense layer showed this. The experiments support the analytical model and the dynamical regime proposed for topographically steered flows. The gravity current split in two when the transport capacity of the corrugation was exceeded; one part continued along the slope and the other flowed downslope along the corrugation. 相似文献
55.
贺海晏 《热带气象学报(英文版)》1995,1(1):12-22
A basic equation governing the movement of a typhoon has been derived based on the system of primitive equations of motion in the atmosphere. The role of several forcing factors which cause the deviation of the typhoon from the steering current have been discussed based on the governing equation. What is presented in Part Ⅰ is a theoretical analysis on the effects of diabatic heating and the horizontal temperature distribution. It is shown that the accelerations of a typhoon caused by diabatic heating and temperature advection coincide with the direction of the volume-averaged "diabatic steering velocity" QV and the "steering velocity of temperature advection" ATV (V is the air velocity,Q the diabatic heating rate and AT the temperature advection ), respectively. The precipitation (or condensation heating) on the right (left) side of a typhoon will accelerate (decelerate) the typhoon. The precipitation in the front (rear ) of the typhoon will turn it to the left (right) of its ordainal path. A typhoon will speed up (slow down) when it moves towards a region of cold (warm) air. 相似文献
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57.
北斗广域高精度时间服务原型系统 总被引:1,自引:0,他引:1
基于精密单点定位(precise point positioning,PPP)的时间传递技术以其精度高、覆盖范围广的优点成为性能最优的GNSS时间传递方法之一。随着广域差分产品时效性的提高,实时PPP时间传递开始应用于精密授时的研究。本文在PPP时间传递技术的基础上,结合实时卫星钟差估计、接收机时钟调控及硬件延迟标校技术,建立了基于北斗卫星导航系统(BeiDou navigation satellite system,BDS)的广域高精度时间服务(wide-area precise timing,WPT)系统,可为用户实时提供准确、稳定、可溯源的时间。WPT系统分为时间服务平台和用户终端两个部分。时间服务平台引入高精度的时间作为系统的参考时间基准,并提供广域实时差分改正数;用户终端基于实时PPP时间传递算法获取本地钟与系统时间基准的差异,并采用精密调钟技术实现终端与系统的同步。为了验证系统的实时授时性能,本文进行了零基线、短基线及广域环境下的性能测试和评估。试验结果表明,该系统零基线、短基线时间同步精度优于0.5 ns,广域条件下单天的授时精度均优于1 ns,为基于北斗系统的精密授时技术发展提供了参考。 相似文献
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60.
光控相控阵雷达在子阵级别上引入光纤实时延迟线OTTD(Optical True Time Delay)进行子阵级的延时补偿,减轻了传统相控阵雷达因渡越时问和孔径效应对信号瞬时带宽的限制,实现了宽带宽角扫描。光控相控阵雷达通过其波控系统控制OTTD和移相器的状态,实现波束快速、灵活扫描。在简要探讨光控相控阵雷达原理的基础上,讨论了其分布式波拉系统的设计方法,同时由于在OTTD的设计中采用了新型光学器件,给出了波控系统与OTTD的接口驱动电路的设计方法。 相似文献