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P. Alexander D. Luna A. de la Torre P. Llamedo T. Schmidt J. Wickert 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2010
The Global Positioning System (GPS) Radio Occultation (RO) technique has global coverage and is capable of generating high vertical resolution temperature profiles of the upper troposphere and lower stratosphere with sub-Kelvin accuracy and long-term stability, regardless of weather conditions. In this work, we take advantage of the anomalously high density of occultation events at the eastern side of the highest Andes Mountains during the initial mission months of COSMIC (Constellation Observing System for Meteorology, Ionosphere and Climate). This region is well-known for its high wave activity. We choose to study two pairs of GPS RO, both containing two occultations that occurred close in time and space. One pair shows significant differences between both temperature profiles. Numerical simulations with a mesoscale model were performed, in order to understand this discrepancy. It is attributed to the presence of a horizontal inhomogeneous structure caused by gravity waves. 相似文献
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P. Alexander R. Ruscica A.A. Sörensson C.G. Menéndez 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2011
Adequate representations of diverse dynamical processes in general circulation models (GCM) are necessary to obtain reliable simulations of the present and the future. The parameterization of orographic gravity wave drag (GWD) is one of the critical components of GCM. It is therefore convenient to evaluate whether standard orographic GWD parameterizations are appropriate. One alternative is to study the generation of gravity waves (GW) with horizontal resolutions that are higher than those used in current GCM simulations. Here we assess the seasonal pattern of topographic GW momentum flux (GWMF) generation for the late 20th and 21st centuries in a downscaling using the Rossby Centre regional atmospheric model under the Intergovernmental Panel on Climate Change A1B emission conditions. We focus on one of the world’s strongest extra-tropical GW zones, the Andes Mountains at mid-latitudes in the Southern Hemisphere. The presence of two GCM sub-grid scale structures locally contributing to GWMF (one positive and one negative) is found to the East of the mountains. For the late 21st century the strength of these structures during the GW high season increases around 23% with respect to the late 20th century, but the GWMF average over GCM grid cell scales remains negative and nearly constant around −0.015 Pa. This constitutes a steady significant contribution during GW high season, which is not related to the GWMF released by individual sporadic strong GW events. This characteristic agrees with the fact that no statistically significant variation in GWMF at source level has been observed in recent GCM simulations of atmospheric change induced by increases in greenhouse gases. 相似文献
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采用二维轴对称雷诺平均方程和标准κ-ε双方程湍流模型,数值研究了环型超声速引散器零二次流的流场结构及盲腔压强的变化,空间上采用二阶迎风格式进行耦合求解,时间上采用显示的Runge-Kutta方法进行迭代推进。结果表明,引射器几何参数不变的情况下,启动后的盲腔压强与引射气流总压之比为一常数;喷管马赫数不变情况下,喷管出口面积与混合室入口面积比越小,盲腔压强越低,扩压器性能越好,启动要求的总压越低,对超声速空气引射器的设计具有指导意义。 相似文献
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为研究侧向喷流对高超声速拦截弹喷流直接力控制性能的影响,发展了在有限体积离散方法框架下的三维非定常N—S方程,采用LU—SSOR隐式时间推进格式和残值项空间迎风型格式求解技术,对大气层内高超声速拦截弹多个姿态控制喷流发动机同时工作时的干扰流场进行了数值求解。计算给出了自由流与侧喷流、侧喷流与侧喷流之间复杂干扰流场结构图(等压云图、等马赫云图)以及喷流附近的压强分布,其结果与单一侧向喷流流场情况进行了比较和分析。结果显示,喷流前的压强场基本不受后喷流的影响,处于前喷流尾流区后的喷流的干扰效率将受到较大影响。 相似文献
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分析了高过载对固体火箭发动机流场和绝热层烧蚀的影响规律,提出一种新的研究思路:采用数值模拟方法来预示发动机三维两相流场,建立高过载流场模拟实验装置,开展绝热层烧蚀实验,建立高过载条件下的绝热层烧蚀模型,在此基础上发展高过载发动机绝热层设计和烧蚀预示方法。其中关键技术是高过载流场的模拟,对粒子加入法和弯管分离法两种方案进行了论证,认为弯管分离法原理上是可行的。为了验证这种方案的可行性,开展了弯管通道两相流的数值模拟研究,计算结果表明弯管装置具有使凝相粒子聚集形成高浓度粒子流的功能。 相似文献
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