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针对红外与可见光图像融合中特征损失严重、显著目标不突出的问题,提出了一种低秩表示分解与深度神经网络相结合的图像融合算法。首先,对源图像进行潜在低秩表示分解(DLatLRR),得到相应的低秩部分、显著部分及稀疏噪声。然后,分别采用16层的VGG Net模型和联合特征加权算法对低秩部分与显著部分进行融合,舍弃二者的稀疏噪声。最后,对融合得到的低秩部分和显著部分进行图像重建,得到最终的融合图像。实验结果表明:与其他算法进行比较,所提算法能够对图像的深层次细节特征进行融合,突出场景中的感兴趣区域,且融合图像的相关差异和、结构相似性、线性相关度等多种客观指标均有所提升,提升最大值分别为0.73、0.15、0.11,噪声产生率的最大缩减值为0.041 2。 相似文献
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Kugusheva A. D. Kalegaev V. V. Vlasova N. A. Petrov K. A. Bazilevskaya G. A. Makhmutov V. S. 《Cosmic Research》2021,59(6):446-455
Cosmic Research - The results of an analysis of the space–time characteristics and dynamics of precipitations of magnetospheric electrons with energies in the range from 0.1 to 0.7 MeV are... 相似文献
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Yongjie Ding Jia Boyang Hezhi Sun Liqiu Wei Wuji Peng Peng Li Daren Yu 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2018,61(3):837-843
Discharge characteristics of a non-wall-loss Hall thruster were studied under different channel lengths using a design based on pushing a magnetic field through a double permanent magnet ring. The effect of different magnetic field intensities and channel lengths on ionization, efficiency, and plume divergence angle were studied. The experimental results show that propellant utilization is improved for optimal matching between the magnetic field and channel length. While matching the magnetic field and channel length, the ionization position of the neutral gas changes. The ion flow is effectively controlled, allowing the thrust force, specific impulse, and efficiency to be improved. Our study shows that the channel length is an important design parameter to consider for improving the performance of non-wall-loss Hall thrusters. 相似文献
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The water content of magma oceans is widely accepted as a key factor that determines whether a terrestrial planet is habitable. Water ocean mass is determined as a result not only of water delivery and loss, but also of water partitioning among several reservoirs. Here we review our current understanding of water partitioning among the atmosphere, magma ocean, and solid mantle of accreting planetary embryos and protoplanets just after giant collisions. Magma oceans are readily formed in planetary embryos and protoplanets in their accretion phase. Significant amounts of water are partitioned into magma oceans, provided the planetary building blocks are water-rich enough. Particularly important but still quite uncertain issues are how much water the planetary building blocks contain initially and how water goes out of the solidifying mantle and is finally degassed to the atmosphere. Constraints from both solar-system explorations and exoplanet observations and also from laboratory experiments are needed to resolve these issues. 相似文献
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Muriel Bergé-Nguyen Jean-François Cretaux Stéphane Calmant Sarah Fleury Rysbek Satylkanov D. Chontoev Pascal Bonnefond 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2021,67(3):985-1001
Lake water height is a key variable in water cycle and climate change studies, which is achievable using satellite altimetry constellation. A method based on data processing of altimetry from several satellites has been developed to interpolate mean lake surface (MLS) over a set of 22 big lakes distributed on the Earth. It has been applied on nadir radar altimeters in Low Resolution Mode (LRM: Jason-3, Saral/AltiKa, CryoSat-2) in Synthetic Aperture Radar (SAR) mode (Sentinel-3A), and in SAR interferometric (SARin) mode (CryoSat-2), and on laser altimetry (ICESat). Validation of the method has been performed using a set of kinematic GPS height profiles from 18 field campaigns over the lake Issykkul, by comparison of altimetry’s height at crossover points for the other lakes and using the laser altimetry on ICESat-2 mission. The precision reached ranges from 3 to 7 cm RMS (Root Mean Square) depending on the lakes. Currently, lake water level inferred from satellite altimetry is provided with respect to an ellipsoid. Ellipsoidal heights are converted into orthométric heights using geoid models interpolated along the satellite tracks. These global geoid models were inferred from geodetic satellite missions coupled with absolute and regional anomaly gravity data sets spread over the Earth. However, the spatial resolution of the current geoid models does not allow capturing short wavelength undulations that may reach decimeters in mountaineering regions or for rift lakes (Baikal, Issykkul, Malawi, Tanganika). We interpolate in this work the geoid height anomalies with three recent geoid models, the EGM2008, XGM2016 and EIGEN-6C4d, and compare them with the Mean Surface of 22 lakes calculated using satellite altimetry. Assuming that MLS mimics the local undulations of the geoid, our study shows that over a large set of lakes (in East Africa, Andean mountain and Central Asia), short wavelength undulations of the geoid in poorly sampled areas can be derived using satellite altimetry. The models used in this study present very similar geographical patterns when compared to MLS. The precision of the models largely depends on the location of the lakes and is about 18 cm, in average over the Earth. MLS can serve as a validation dataset for any future geoid model. It will also be useful for validation of the future mission SWOT (Surface Water and Ocean Topography) which will measure and map water heights over the lakes with a high horizontal resolution of 250 by 250 m. 相似文献
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A. V. Bogatyi R. V. El’nikov I. P. Nazarenko G. A. Popov S. A. Semenikhin 《Russian Aeronautics (Iz VUZ)》2018,61(3):445-451
The paper presents the research results of the effect of a capacitor energy storage device configuration on the specific characteristics of advanced modern propulsion systems based on the ablative pulsed plasma thrusters (APPT). These thrusters are designed to perform specific tasks within the small spacecrafts with the onboard power capacity up to 200 W. 相似文献
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针对椭圆轨道卫星近/远地点的星下点对全球或特定纬度区域的访问问题,提出一种连续小推力下的对地覆盖控制策略。首先,推导了自然摄动对卫星拱线变化的影响,并探讨了进行小推力覆盖控制的必要性。然后,针对燃料消耗的优化问题,将控制方程展开成含傅里叶级数的形式,用以获得便于星上计算的解析形式的次优解,同时探讨了截取阶数与优化程度的关系。在进行拱线控制的同时,通过合理设置约束,对椭圆轨道的近地点高度进行保护,确保卫星安全运行。仿真结果表明,提出的方法能够以适当的燃料消耗代价实现椭圆轨道的近/远地点的全球覆盖控制或特定纬度区域的反复推扫,且控制力在可接受的范围内。 相似文献