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91.
塔里木盆地周边地区冰雹云特征分析 总被引:3,自引:0,他引:3
对1998~2001年6~9月在塔里木盆地普查得到105个降雹云团进行分类,按尺度大小分为雷暴云、对流云、中尺度对流系统、冷云核和系统云系云区5类。塔里木盆地2000年降雹云团出现最多,半数以上出现在5月和6月。塔里木盆地降雹云团尺度小、形状不规则、云顶温度较高。 相似文献
92.
该文利用GMS 5原始数据、GMS 5展宽数据、FY-2A展宽数据和FY-2B展宽数据, 采用伪彩色增强和灰度直方图分析方法, 分别对这4种数据的红外、水汽、可见光通道图像进行了针对杂散光的对比分析以及对杂散信号来源分析。分析表明这三颗静止气象卫星的图像中都存在一定的杂散信号。该文提出了解决杂散光问题主要依靠优化辐射计光路设计; 地面系统在实时处理、展宽图像时采取简单剔除处理, 可以减小或消除图像冷空间区域的杂散信号, 但是去掉地球圆盘图像内部的杂散信号将非常困难。 相似文献
93.
哈密南部暴雨成因分析 总被引:6,自引:1,他引:6
通过对 2 0 0 2年 6月 1 8~ 1 9日哈密南部暴雨的环流背景、物理机制、T2 1 3产品的物理量及卫星云图分析 ,揭示形成暴雨的成因 相似文献
94.
导航卫星自主定轨的算法研究及模拟结果 总被引:5,自引:2,他引:5
讨论了利用卫星-卫星间的距离观测值建立导航卫星系统自主定轨的数学方法,并用GPS星座模拟星间观测值,采用滤波算法计算卫星的状态参数。模拟结果表明,在空间测距精度一定的情况下,自主定轨精度能高于GPS广播星历,因而能较精确地维持卫星系统的坐标框架。 相似文献
95.
This article presents an econometric analysis of land‐cover change in western Honduras. Ground‐truthed satellite image analysis indicates that between 1987 and 1996 net reforestation occurred in the 1,015‐km2 study region. While some reforestation can be attributed to a 1987 ban on logging, the area of reforestation greatly exceeds that of previously clear‐cut areas. Further, new area was also deforested between 1987 and 1996. Thus, the observed land‐cover changes represent a complex mosaic of changing land‐use patterns across time and space. The analysis contributes to the literature on land‐cover change modeling in that: (1) it compares two econometric approaches to capture complex and often bidirectional changes in land cover from 1987 to 1996 as a function of agricultural suitability and transportation costs, and (2) it addresses techniques to identify and correct for spatial autocorrelation in a categorical regression framework. 相似文献
96.
97.
New satellite technology to measure changes in the Earth’s gravity field gives new possibilities to detect layers of low viscosity inside the Earth. We used density models for the Earth mantle based on slab history as well as on tomography and fitted the viscosity by comparison of predicted gravity to the new CHAMP gravity model. We first confirm that the fit to the observed geoid is insensitive to the presence of a low viscosity anomaly in the upper mantle as long as the layer is thin ( 200 km) and the viscosity reduction is less than two orders of magnitude. Then we investigated the temporal change in geoid by comparing two stages of slablet sinking based on subduction history or by advection of tomography derived densities and compared the spectra of the geoid change for cases with and without a low viscosity layer, but about equal fit to the observed geoid. The presence of a low viscosity layer causes relaxation at smaller wavelength and thus leads to a spectrum with relatively stronger power in higher modes and a peak around degrees 5 and 6. Comparing the spectra to the expected degree resolution for GRACE data for a 5 years mission duration shows a weak possibility to detect changes in the Earth’s gravity field due to large scale mantle circulation, provided that other causes of geoid changes can be taken into account with sufficient accuracy. A discrimination between the two viscosity cases, however, demands a new generation of gravity field observing satellites. 相似文献
98.
David Crossley Jacques Hinderer Jean-Paul Boy 《Geophysical Journal International》2005,161(2):257-264
99.
Pascal Willis Claude Boucher Hervé Fagard Zuheir Altamimi 《Comptes Rendus Geoscience》2005,337(7):653-662
IGN is in charge of the installation and maintenance of the DORIS orbit determination network. More recently, in collaboration with JPL, precise geodetic computations were performed. The goal of this paper is to recall the various historic contributions of IGN to the DORIS system in their international context and then to describe a new estimation technique developed for a multi-satellite mode, making full profit of a better modeling for satellites and ground clocks as well as tropospheric correction parameters. Derived geodetic results demonstrate a precision in the order of 1 cm for station positions. To cite this article: P. Willis et al., C. R. Geoscience 337 (2005). 相似文献
100.
Effects of temporal scales and space mismatches on the TRMM 3B42 v7 precipitation product in a remote mountainous area 下载免费PDF全文
Shiva Ebrahimi Cheng Chen Qiuwen Chen Yinsheng Zhang Ning Ma Qammerul Zaman 《水文研究》2017,31(24):4315-4327
The accurate measurement of precipitation is essential to understanding regional hydrological processes and hydrological cycling. Quantification of precipitation over remote regions such as the Tibetan Plateau is highly unreliable because of the scarcity of rain gauges. The objective of this study is to evaluate the performance of the satellite precipitation product of tropical rainfall measuring mission (TRMM) 3B42 v7 at daily, weekly, monthly, and seasonal scales. Comparison between TRMM grid precipitation and point‐based rain gauge precipitation was conducted using nearest neighbour and bilinear weighted interpolation methods. The results showed that the TRMM product could not capture daily precipitation well due to some rainfall events being missed at short time scales but provided reasonably good precipitation data at weekly, monthly, and seasonal scales. TRMM tended to underestimate the precipitation of small rainfall events (less than 1 mm/day), while it overestimated the precipitation of large rainfall events (greater than 20 mm/day). Consequently, TRMM showed better performance in the summer monsoon season than in the winter season. Through comparison, it was also found that the bilinear weighted interpolation method performs better than the nearest neighbour method in TRMM precipitation extraction. 相似文献