The Orbital Forcing of Climate Changes on Mars

Solar variability influences the climate of a planet by radiatively forcing changes over a certain timescale; orbital variations of a planet, which yield similar solar forcing modulations, can be studied within the same scientific context. It is known for Earth that obliquity changes have played a critical role in pacing glacial and interglacial eras. For Mars, such orbital changes have been far greater and have generated extreme variations in insolation. Signatures associated with the presence of water ice reservoirs at various positions across the surface of Mars during periods of different orbital configurations have been identified. For this reason, it has been proposed that Mars is currently evolving between ice ages. The advent of climate tools has given a theoretical frame to the study of orbitally-induced climate changes on Mars. These models have provided an explanation to many puzzling observations, which when put together have permitted reconstruction of almost the entire history of Mars in the last 10 million years. This paper proposes to give an overview of the scientific work dedicated to this topic.     

南航立式水洞实验技术及应用

本文介绍了南航270mm×270mm立式水洞,对水洞流态显示技术中较为关键的几个问题:如试验模型设计,彩色染色液体配方,灯光与摄影技术等进行了简述,并对其实际应用提供了几个示例,以供参考。     

跃变型介质中原油渗流有限元计算

本文建立跃变型介质中原油渗流的数学模型,可用来描述油层(尤其是低渗透层)超高压注水条件下的不稳定渗流过程及其特征。用Galerkin有限元法进行了数值计算,讨论了介质跃变的影响。     

Establishment of atmospheric weighted mean temperature model in the polar regions

Due to the special geographical location and extreme climate environment, the polar regions (Antarctic and Arctic) have an important impact on global climate change. Atmospheric weighted mean temperature (Tm) is a crucial parameter in the retrieval of precipitable water vapor (PWV) from the zenith wet delay (ZWD) of ground-based Global Navigation Satellite System (GNSS) signal propagation. In this paper, the correlation between weighted mean temperature and surface temperature (Ts) is studied firstly. It is shown that the correlation coefficients between Tm and Ts are 0.93 in the Antarctic and 0.94 in the Arctic. The linear regression Tm model and quadratic function Tm model of the Antarctic and the Arctic are established respectively using the radiosonde profiles of 12 stations in the Antarctic and 58 stations in the Arctic from 2008 to 2015. The accuracies of the linear regression Tm model, the quadratic function Tm model and GPT2w Tm model which is a state-of-the-art global Tm model are verified using the radiosonde profiles from 2016 to 2018 in the Antarctic and Arctic. Root Mean Square (RMS) errors of the linear regression Tm model, the quadratic function Tm model and GPT2w Tm model in the Antarctic are 3.07 K, 2.87 K and 4.32 K respectively, and those in the Arctic are 3.53 K, 3.38 K and 4.82 K, which indicates that the quadratic function Tm model has a higher accuracy compared to linear regression Tm model, and the accuracies of the two regional Tm models are better than that of GPT2w Tm model in the polar regions. In order to better evaluate the accuracy of Tm in the PWV retrieval, the PWV values of radiosondes are used for comparisons as the reference value. The RMS errors of PWV derived from the two Tm models are similar for 1.28 mm in the Antarctic and 1 mm in the Arctic respectively. In addition, the spatial and temporal variation characteristics of Tm are analyzed in the polar regions by spectral analysis of Tm data using fast Fourier transform. The results show that the Tm has obvious seasonality and annual periodicity in the polar regions, and the maximum difference between warm season and cold season is about 63 K. After comparing and analyzing the influences of latitude, longitude and elevation on the Tm in the polar regions, it is found that latitude and elevation have a greater influence on the Tm than the longitude. As the latitude and elevation increase, the Tm decreases, and vice versa in the polar regions.     

西安某粘接材料厂室内供暖、热水系统的设计

基于厂方对供热系统的要求,根据供热建筑物、机房和可利用设施的实际情况,采用一台换热器,通过阀门的切换,实现了供暖和供热水的分段运行。将蒸汽发生器的进水与系统补水有机地整合为一个系统,有效地解决了机房面积过小的实际困难。利用自来水的压力和热水箱与浴室的高差解决了热水供应的实际问题。     

微藻反应器用于水气净化与产氧的功能验证

将微藻和电去离子技术引入密闭生态系统,设计单元反应器旨在验证其在空气再生、水净化和潜在食物的生产。在反应器中对尿液进行消解和NH4＋硝化转化得到超过90%NH4＋-N硝化为NO-3-N-的培养液适宜于螺旋藻养殖并获得高质量的微藻生物量;此时,CO2的平均吸收速率VCO2=458.6 mL/m3·min、O2产生速率VO2=616.5 mL/m3·min,即螺旋藻的同化系数VCO2/VO2≈0.74,接近人的呼吸系数VCO2/VO2=0.86;EDI法水净化率97%可直接回用。结果表明：该体系能实现CO2吸收、O2释放和螺旋藻生物量的生产,同时将水净化。     

海洋大气环境下微动开关触点回跳时间增大故障的试验复现与分析

结合某型微动开关触点回跳时间增大导致某系统故障问题,设计了由干湿交替酸性盐雾试验和湿热试验组成的海洋大气环境效应加速模拟试验剖面,选取与外场故障件型号一致的微动开关为研究对象,通过实验室加速模拟试验,成功复现了外场故障现象,并结合试验结果对腐蚀性环境、电烧蚀等因素对触点回跳时间增大的影响机制进行了分析。     

提升民用飞机水废水系统运营经济性技术研究

基于现代民机绿色环保设计理念和对经济性的追求,减重是飞机设计中重点考虑因素,关于降低民用飞机水废水系统运营载重、提高运营经济性研究,国内外尚未发布公开文献。本文基于对航线用水统计数据研究,形成航线运营所需水量计算技术;基于我国航线飞行时长分布特点,提出基于航线实际运营时间和载客人数为需求、为系统设定分档加水设计技术。结果表明：与同类机型数据对比,本文的水量计算技术是有效的;分档加水设计技术能够有效地降低系统在航线运营过程中的运营重量,可以提升民用飞机水废水系统的运营经济性。     

受平行壁限制的燃油喷雾二相流特征

通过试验诊断了燃油喷雾在模拟环形燃烧室火焰筒内、外壁面间的二相流型。其结果显示 ,与不受壁面限制的结果相比 ,其基本流型在下游有明显改变     

Validation on MERSI/FY-3A precipitable water vapor product

The precipitable water vapor is one of the most active gases in the atmosphere which strongly affects the climate. China's second-generation polar orbit meteorological satellite FY-3A equipped with a Medium Resolution Spectral Imager (MERSI) is able to detect atmospheric water vapor. In this paper, water vapor data from AERONET, radiosonde and MODIS were used to validate the accuracy of the MERSI water vapor product in the different seasons and climatic regions of East Asia. The results show that the values of MERSI water vapor product are relatively lower than that of the other instruments and its accuracy is generally lower. The mean bias (MB) was ?0.8 to ?12.7?mm, the root mean square error (RMSE) was 2.2–17.0?mm, and the mean absolute percentage error (MAPE) varied from 31.8% to 44.1%. On the spatial variation, the accuracy of MERSI water vapor product in a descending order was from North China, West China, Japan -Korea, East China, to South China, while the seasonal variation of accuracy was the best for winter, followed by spring, then in autumn and the lowest in summer. It was found that the errors of MERSI water vapor product was mainly due to the low accuracy of radiation calibration of the MERSI absorption channel, along with the inaccurate look-up table of apparent reflectance and water vapor within the water vapor retrieved algorithm. In addition, the surface reflectance, the mixed pixels of image cloud, the humidity and temperature of atmospheric vertical profile and the haze were also found to have affected the accuracy of MERSI water vapor product.