一种全天空气辉成像仪数据预处理方法和初步结果

大气重力波是大气中的基本波动形式之一,在中高层大气动力和热力学过程中起着十分重要的作用.全天空气辉成像仪是一种以大气气辉辐射为示踪物,能够有效对大气重力波成像的仪器.本文针对中国科学院国家空间科学中心空间天气学国家重点实验室中高层大气组自主研制的全天空气辉成像仪所观测的数据,提出了一种气辉图像预处理方法,进行平场校正、方位校正、星光去除和坐标映射等数据订正.利用该方法处理2015年5月17日21：00BLT至次日05：00BLT西宁台站（36.6°N,101.7°E）的OH气辉数据,发现一次重力波事件,分析并获得了该重力波的水平波长、观测水平相速度和传播方向（分别为17.72km,47m·s^-1,339°）.研究结果表明该方法是可行的.     

Evidence of change after 2001 in the seasonal behaviour of the mesopause region from airglow data at El Leoncito

Airglow intensities and rotational temperatures of the OH(6-2) and O₂b(0-1) bands acquired at El Leoncito (32°S, 69°W) provide good annual coverage in 1998–2002, 2006, and 2007, with between 192 and 311 nights of observation per year. These data can therefore be used to derive the seasonal variations during each of these seven years, in airglow brightness and temperatures at altitudes of 87 and 95 km. From 1998 to 2001, seasonal variations are similar enough so that they can be well represented by a mean climatology, for each parameter. On the other hand, these climatologies do not agree with what is usually observed at other sites, maybe due to the particular orographic conditions at El Leoncito. With respect to the last three fully documented years (2002, 2006, and 2007), the similarity from year to year deteriorates, and there are greater differences in the seasonal behaviour, more or less in all the parameters. The differences include, e.g., maxima occurring earlier or later than “normal”, by one or two months. All this may suggest the build-up of a new regime of intraseasonal variability, with a possible relationship to corresponding changes in wave activity.     

The Nonlinear Model of the Response of Airglow to Gravity Waves

In this paper, we develope a time-dependent, nonlinear, photochemical-dynamical 2-D model which is composed of 3 models: dynamical gravity wave model, middle atmospheric photochemical model, and airglow layer photochemical model. We use the model to study the effect of the gravity wave propagation on the airglow layer. The comparison between the effects of the different wavelength gravity wave on the airglow emission distributions is made. When the vertical wavelength of the gravity wave is close to or is shorter than the thickness of the airglow layer, the gravity wave can make complex structure of the airglow layer, such as the double and multi-peak structures of the airglow layers. However, the gravity wave that has long vertical wavelength can make large scale perturbation of the airglow emission distribution.     

中国山西地区法布里-珀罗干涉仪测风能力及数据质量检验

介绍了中国气象局山西岢岚大气观测站(39°N, 112°E) 法 布里-珀罗干涉仪(FPI) 的基本 构造、测风能力、程序处理流程、数据质量控制方法以及检验情况. 岢 岚观测站FPI可以观测892.0 (OH)nm, 557.7 (OI)nm和630.0 (OI)nm 波 长处气辉谱线的多普勒移动, 分别计算对应87km, 97km和250km高度处 的大气风速和大气温度, 可给出中间层顶区域及热层风的大气潮汐和扰动 情况. 采用水平风模型(HWM)输出结果进行交叉检验, 对FPI测风数据质量进行验证. 结果显示, 岢岚大气观测站FPI仪器的测风数据 在长期趋势上与HWM模式的输出数据一致, 风速变化幅度有季节性差异, 数据质 量控制方法有效, 测风误差在87km高度处为5.7m·s^-1, 97km处 为1.3m·s^-1, 250km处为4.1m·s^-1, 测风数据 通过了可靠性检验.     

Meteor radar temperatures over Collm (51.3°N, 13°E)

The method of obtaining absolute temperature estimates by measuring the ambipolar diffusion coefficient with meteor radars in the mesopause region is basically well known. However, there is still a need to refine and adjust the background temperature gradient model which is necessary to calculate the temperature values. Therefore, a detailed comparison with independent temperature measurements is necessary to evaluate the performance of the method and to obtain more information about the temperature gradient. Recent studies provide some evidence that the impact of the gradient model on temperature estimates affects the absolute temperatures, but that it is of minor importance for wave analysis. This paper focuses on a detailed evaluation of the meteor radar temperatures by comparing them with SABER satellite and OH-emission mesopause region temperatures. The seasonal variation of the observed temperatures is well reproduced by the COMMA general circulation model.     

Multi-year behaviour of the midnight OH1 temperature according to observations at Zvenigorod over 2000–2016

Using spectral measurements of the hydroxyl airglow at the Zvenigorod station (56° N, 37° E), Moscow region, over 2000–2016, we obtained the long-term set of data comprising 1822 midnight values of the OH¹ temperature in the mesopause region. These data revealed a 17-year series of its mean annual values, as well as amplitudes and phases of the first two harmonics of its annual variation. The obtained parameters were analyzed to determine statistically relevant characteristics of their long-term variations. As a result, we found that the long-term behaviour of the mean annual OH¹ temperature features a small negative linear trend (?0.07 ± 0.03 K/year) over the addressed period. Besides, its dependence on solar activity is shown to be 4.1 ± 0.5 K/100 SFU. Regarding the long-term behaviour of the mean annual OH¹ temperature, we revealed the existence of two oscillations with 3-year (the amplitude being 1.3 ± 0.2 K) and 4.1-year (the amplitude being 0.6 ± 0.2 K) periods. We obtained empirical relations describing year-to-year variations in the amplitudes and phases of the annual and semi-annual harmonics.     

2009年1月5日廊坊OH气辉观测图像的谱分析

2009年1月5日在中国河北省廊坊市韩村镇(39.4°N,116.6°E)进行了中国首次中间层顶大气重力波成像观测实验,记录了近4 h的OH气辉辐射数据,给出了依据该数据计算所得的该时间段内廊坊韩村附近水平方向约185 km范围内的中间层顶OH气辉扰动的谱分析结果.所得到的传播方向确定的二维功率谱和角度谱揭示了该时间段内重力波活动的波长和传播方向分布特点,表明波长下限较短,西向传播分量明显大于东向分量.     

基于钠激光雷达观测数据的中间层顶大气温度分布特性研究

作为中间层和热层的边界层,中间层顶存在多种能量交换方式,是大气能量耦合的重要区域。本文利用部署于中国科学院廊坊临近空间大气探测站的钠荧光多普勒激光雷达2013年的观测数据,研究了廊坊上空中间层顶区域大气温度的年度和季节分布特性,并分析了影响温度分布的多种因素。年平均温度廓线图显示,中间层顶位于约97.5 km高度处,温度约191.2 K。受放热化学反应的影响,年平均温度廓线91 km高度处出现了一个198 K的相对温度高点。中间层顶区域大气温度的季节分布受太阳辐射和大气动力学因素综合影响,夏季在大气动力学影响下,中间层顶高度较低,位于88 km高度处,温度也较低,约177 K;冬季太阳辐射起主导作用,中间层顶位于99 km高度处,温度为181 K。通过拟合月平均温度分析了中间层顶区域大气温度年变化和半年变化的振幅和相位特征。结果显示,中间层顶区域上部温度分布主要受太阳辐射的影响;在中间层顶区域下部,大气波动主导了温度分布。     

TIMED卫星探测的全球大气温度分布及其与经验模式的比较

利用TIMED卫星遥感探测的全球温度分布与NRLMSISE-00大气经验模式进行了对比研究.研究表明,在中间层下部以下的高度范围内,经验模式与卫星探测的大气温度分布有很好的一致性.但是比较发现,在中层顶区域,经验模式的计算结果与实测结果有较大的差异.卫星探测表明,在春分季节的低纬地区中层顶区存在稳定的逆温层,但是经验模式不能给出低纬地区春分季节中间层逆温层的分布特征.卫星观测表明在全球范围内中层顶有两个非常不同的高度,一个处于100km附近,另一个处于85km附近,但是经验模式不能给出这一中层顶高度的分布特征.同时在低热层,经验模式计算的温度分布与卫星遥感的探测结果有很大的差异.     

Imaging spectroscopy of the Venus 1.27-μm O2 airglow with ground-based telescopes

Several ground-based observations of the Venus 1.27-μm O₂ airglow were carried out from 2002 to 2005. Spectral image cubes were taken with the Okayama Astrophysical Observatory/infrared imaging spectrometer (superOASIS), the Gunma Astronomical Observatory/Cassegrain Near-Infrared Camera and NASA’s Infrared Telescope Facility/cryogenic echelle spectrograph (CSHELL). The brightest airglow features were found at around the anti-solar point, which is in agreement with previous studies. We derived the rotational temperature distributions on the nightside hemisphere from observed airglow spectra. The temperature shows a weak positive correlation with the airglow intensity. The result indicates the bright region is heated chemically and/or dynamically, and supports the existing scenario for the Venus O₂ airglow. That is, the airglow is excited by the descending oxygen transported from the dayside.     

拉普拉斯-高斯滤波图象的过零边界及其分形维数

本文考察了用拉普拉斯—高斯滤波器对遥感图象过零边界的计算方法.给出了直接从遥感图象边界转换成过零边界的稳函数.分析可看到,从遥感图象边界化算出过零边界是局地性决定的方式,得到的过零边界相对于原遥感图象边界的偏差主要取决于图象尺度、边界的局地曲率半径和所用高斯函数的尺度常数.证明拉普拉斯—高斯滤波过零边界法在图象尺度和曲率半径都大于高斯尺度常数10倍以上时,是获得遥感图象边界的精确方法.     

基于DEM的星载SAR图像模拟以及用于图像精校正

根据星载SAR的距离-多普勒成像原理对DEM的三维位置点进行成像几何位置的计算,然后根据经验公式给出了雷达后向散射系数的模拟方法。针对DEM格网间隔和SAR图像分辨率的不同,以及由于侧视成像雷达的特点而导致山区的迎坡和背坡模拟图像点密度不均匀等问题,采用了基于DEM格网点内插的算法。最后应用模拟的SAR图像和真实图像匹配来实现星载SAR图像的几何精校正处理。通过采用RADARSAT的实际图像进行了图像的模拟和几何校正,证明了方法的可行性。     

图象的GD表示法的子图象抽取方法

在图象数据库的存贮结构及图象的数据压缩等应用中,GD等这类线性四元树表示方法得到了大量的研究。在对图象的各种处理中,子图象的抽取是个很基本的操作,但用线性四元树方法存贮图象并在其上实现这一操作并不象数组表示那样简单、直观。文内给出了一个基于GD表示方法的子图象抽取方法。     

分体对开式高低温发生装置研究

介绍了一种分体对开式高低温发生装置,并详细叙述了其结构组成,测试结果表明高低温发生装置温度范围为-80℃~400℃,温度偏差为±2℃,温度均匀度为2℃,该装置可作为专用实验设备用于力传感器高低温环境下的校准。     

基于多层次特征的跨域图像生成评估方法

针对弗雷歇初始距离（Fréchet Inception Distance;FID）指标在跨域图像生成评估时约束力低的问题;提出了一种基于多层次特征对齐距离（Multi-Level Feature Alignment Distance,MLFAD）的域差计算方法。通过引入多层次特征提取与特征对齐机制;实现生成图像与真实图像在不同层次特征尺度分布差异的全面度量;更加精确地反映图像的细节和全局信息;大幅度增强了对生成图像的约束力。试验结果表明;MLFAD的表现显著优于FID;在图像翻译、风格迁移、图像修复和图像增强等跨域图像生成任务中;域差计算值分别降低了31.7%、26.8%、41.1%和34.6%。因此;MLFAD在跨域图像生成任务的评估中具有良好的准确性和稳定性;显著提升了生成图像的清晰度、细节还原度及色彩精准度。     

高温材料光谱发射率测量技术研究

针对发射率测量技术现状及面临的问题,明确了建立高温材料光谱发射率测量装置的意义,对所研究的测量装置的技术路线和设计方案进行了介绍。     

一种基于SPIHT的ROI图像编码

感兴趣区域的ROI（Region of Interest）编码是正在制订的静止图像压缩国际新标准JPEG2000支持的一种创新方法,在渐进重构的初始阶段,ROI的保真度高于图像其余部分（背景）,该方法可观地节省了传输时间和存储空间。由于SPIHT是嵌入式编码,所以在按一定比例放大ROI系数（或者按一定比例缩小背景系数）后,ROI便可以比背景更快更清晰的重构出来。