行星大气1~3000GHz微波-亚毫米波辐射模拟

为模拟行星大气在微波elax-elax亚毫米波波段的辐射传输特性,利用逐线积分方法计算行星大气中各气体成分在1~3000GHz的吸收系数.基于HITRAN数据库中各气体分子的跃迁频率及线强等参数,有效模拟了各气体分子在此频段内的吸收特征,并与常用的微波elax-elax亚毫米波大气辐射传输模式进行对比.分析地球大气的组成及特性,利用辐射传输方程模拟临边探测方式下不同频段的大气辐射亮温.研究结果可为后续地球乃至行星大气成分探测模拟、频带选择以及大气成分廓线反演提供模型及理论依据.      

AGN activity triggered by circumnuclear starbursts

We present a radiative/hydrodynamical mechanism for triggering AGN activity; the intensive radiation from a circumnuclear starburst drives the nuclear fueling due to the Poynting-Robertson (radiation drag) effects. When the starburst is in an early and therefore super-Eddington phase, the radiative flux force is likely to obstruct severely the mass accretion onto the nucleus (radiative blizzard phase). But, in a later sub-Eddington phase, the radiation flux force builds up a wall of dusty gas. The wall absorbs the radiation from the starburst regions and re-emits infrared radiation, which causes the disk accretion due to the Poynting-Robertson effect, consequently leading to nuclear fueling (radiative avalanche phase). The radiative avalanche could link to an advection-dominated accretion flow (ADAF) onto a putative supermassive black hole. The radiatively triggered nuclear activity diminishes as the starburst dims. In this context, the AGN type could be discriminated not only by the viewing angles but also by the evolution of a circumnuclear starbursts. Based on such a picture, we reconsider the AGN activity in luminous IRAS galaxies.     

The dynamics of the solar radiative zone

The picture of the solar radiative zone is evolving quickly. This review is separated in two parts. We first recall how the two powerful probes of the solar interior, namely the neutrinos and helioseismology have scrutinized the microscopic properties of the solar radiative plasma. Recent observations stimulate today complementary activities beyond the standard stellar model through theoretical modeling of angular momentum transport by rotation, internal waves or (and) by magnetic fields to get access to the dynamical motions of this important region of the Sun. So in the second part, we summarize the first impact of such processes on the radiative zone.     

The correlation of the planetary atmosphere structural characteristics with their optical properties and radiative heat exchange peculiarities

The structure characteristics of the Earth-type planetary atmospheres are calculated solving the radiative heat exchange problem. Their correlations with the surface reflection characteristics and optical properties of their atmospheres are considered.     

含非均匀辐射气体空腔辐射特性计算研究

文章发展了求解积分辐射传输方程组的方法来计算充满非均匀辐射性气体封闭腔的辐射特性的方法,讨论了辐射空间分布及光谱分布的计算方法,并编制了相应的计算机程序.计算了某型发动机轴对称喷管的辐射分布,并与采用通常的辐射换热经验公式的计算结果进行了比较.     

地磁暴恢复相中间层低热层高纬温度响应

利用TIMEGCM模拟了2005年9月10日至20日由日冕物质抛射引起的地磁暴事件,研究了此地磁暴恢复相高纬度中间层低热层（MLT）区域温度的变化,揭示了磁暴恢复相时温度、垂直风、总加热项和NO辐射冷却的内在联系.结果表明:地磁暴恢复相刚开始时,温度对磁暴的响应在晨侧为负扰动（降温）,在其他地区都为正扰动（增温）;随着磁暴的恢复,整个北半球都变为正的温度扰动（增温）.这种高纬MLT区域的温度响应主要与垂直风密切相关.当垂直风为正时,总加热为负,增温减弱;当垂直风为负时,总加热为正,增温变强.辐射冷却特别是NO辐射冷却作用在热层被称为恒温器,降低了磁暴期间80%的热层增温.但是,在MLT区域NO辐射冷却作用不明显,一般比总加热项小一个量级,对温度响应造成的影响较小.      

Changes in the radiative balance of the atmosphere due to increases in CO2 and trace gases

Increases in CO₂ and trace gases in the earth's atmosphere can lead to changes in the radiative balance of the earth's atmosphere in two ways. Changes in the amount of these constituents leads directly to changes in outgoing longwave radiation. This change in outgoing longwave radiation causes the thermal structure of the atmosphere to change. These changes in thermal structure can then alter the distribution of outgoing longwave radiation. Changes in the distribution and amount of outgoing radiation due to various increases in CO₂ and trace gases are presented from a model with a spectral resolution of 5 cm⁻¹. The effects of stratospheric aerosols, and the use of general circulation models for detecting changes in the radiative balance are discussed.     

免疫遗传算法在百叶窗最优化热设计中的应用

考虑优化过程中辐射能量交换的特殊性,为了加速优化过程的进行,通过引入漫反射系统单元表面间辐射传递系数与角系数之间的关系来处理百叶窗的辐射能量交换;同时为了克服传统优化算法存在的缺陷,提出了一种免疫遗传算法,并且应用于百叶窗最优化热设计中。优化设计表明,与标准遗传算法相比,该优化算法具有较强收敛度与全局寻优能力,可以较好地用于最优化热设计中。     

The motion of an artificial satellite under the terrestrial radiation pressure

The terrestrial infrared radiation pressure effects on the motion of an artificial satellite are investigated. The radiative field is described by a series of spherical harmonics. The equations for the changes of the elements are found and numerical examples for the case of the satellite D-5-B (1975 39 B) are given.     

基准星辐射定标的辐射传递链路研究

为进一步提高遥感信息定量化应用水平,提高在轨辐射定标精度和定标频次,提出一种基于基准星的全谱段、全口径在轨绝对辐射定标方法,方法适用于可见近红外谱段;定标传递中辐射基准可溯源至SI(国际单位)。通过比较现有定标方法和基准星辐射定标的优缺点,分析基准星辐射基准溯源特性,建立太阳 基准星 遥感器的辐射传递模型,以高分一号和高分二号卫星为例,其作为待定标遥感器,对基准星定标的约束条件进行仿真分析,得出基准星辐射传递不确定度为13%。仿真结果验证了基准星定标方法的可行性,对遥感器辐射定标精度、频次的进一步提高提供了依据。     

Comparison of ground reflectance measurement with satellite derived atmospherically corrected reflectance: A case study over semi-arid landscape

Atmospheric corrections to satellite data are important for comparing multitemporal data sets over tropical regions with variable aerosol loading. In this study, we evaluated the potential of 6S radiative transfer model for atmospheric corrections of IRS-P6 AWiFS satellite data sets, in a semi-arid landscape. Ground measurements of surface reflectance representing different land use/land cover categories were conducted to relate IRS-P6 AWiFS top of atmospheric reflectance. The 6S radiative transfer model was calibrated for local conditions using ground measurements for aerosol optical depth, water vapor and ozone with a sun photometer. Surface reflectance retrieved from 6S code was compared with top of atmosphere (TOA) reflectance and ground based spectroradiometer measurements. Accurate parameterization of the 6S model using measurements of aerosol optical depth, water vapor and ozone plays an important role while comparing ground and satellite derived reflectance measurements.     

Optical/X-ray correlations as a signature of jet-disc coupling in the accreting black hole XTE J1118+480

We interpret the rapid correlated UV/optical/X-ray variability of XTE J1118+480 as a signature of the coupling between the X-ray corona and a jet emitting synchrotron radiation in the optical band. We propose a scenario in which the jet and the X-ray corona are fed by the same energy reservoir where large amounts of accretion power are stored before being channelled into either the jet or the high energy radiation. This time-dependent model reproduces the main features of the rapid multi-wavelength variability of XTE J1118+480. A strong requirement of the model is that the total jet power should be at least a few times larger than the observed X-ray luminosity, implying a radiative efficiency for the jet _j  3 × 10⁻³. This would be consistent with the overall low radiative efficiency of the source. We present independent arguments showing that the jet probably dominates the energetic output of all accreting black holes in the low-hard state.     

Monitoring of biologically effective UV irradiance at El Arenosillo (INTA), Andalucia, in Spain.

Biological UV (ultraviolet) dosimetry was applied using the biofilm-technique (DLR patent) to determine the UV levels weighted of biologically weighted UV radiation at the INTA Sounding Station of El Arenosillo at Huelva, Spain (37 degrees 06'N, 6 degrees 44'W, 50 m a s 1=above sea level) on 2 days in 1997 [correction of 1977] (April 1, and May 5). Exposure periods were calculated for clear sky days using a radiative transfer model for erythemal doses to reach 1.3 to 1.5 MED (minimal erythemal dose). Reliability of the radiative transfer model was demonstrated by the doses registered by a Yankee-UV biometer for the same exposure periods as used for the biosensor. This work presents the methodology employed (biofilm-technique utilized [correction of utiliced], calculation of exposing periods with radiative transfer model, etc) and the results obtained with the Yankee biometer and the biofilm. At noon, the ratio of biofilm measurements (Ieff, W/m2=biological effective irradiance, in W/m2) to the UV Biometer data (in MED/h) was 3-4.     

Effect of surface roughness on microwave brightness temperature from lunar surface: Numerical analysis with a hybrid method

A hybrid method, combining the radiative transfer theory and the method of moments (MoM), is proposed to study the potential effect of the lunar surface roughness on the microwave brightness temperature. The total upward emission reaching the lunar surface from below media is calculated by the radiative transfer theory, and then the brightness temperature is obtained by weighting the bidirectional transmission coefficients which is computed using the MoM. The method is validated by both flat and rough surface models with analytic solutions. With the hybrid method, brightness temperatures from simulated lunar model are calculated and compared to those from a flat layered model. The comparisons show that the effect of rough surface on brightness temperature cannot be ignored and also depends on many other factors, such as observation angle and polarizations. For vertical polarization, an optimal observation angle may exist to reduce the effect of surface roughness. These results indicate that the knowledge of lunar surface roughness is important in microwave remote sensing to the Moon and may probably provide a guide to lunar projects in future.     

利用6S进行月光条件下遥感器信号模拟研究

以太阳为光源的卫星遥感器,可以采用6S或MODTRAN等辐射传输计算软件对其入瞳处的辐亮度进行计算。而在微光或月光条件下,遥感器是对观测目标反射的月亮辐射进行遥感观测,因此在进行辐射传输计算时需要代入月球的辐照度数据。可以利用已公布的月球表面反射率和已知的大气层外太阳辐照度来计算月球辐照度,并对6S辐射传输计算进行适当的修改进行计算。通过对月球辐照度计算原理进行了详细的描述并计算得到了波长在0.250μm~1.500μm范围内的月球表面辐照度,并给出了一个宽波段遥感器的微光动态范围。     

Boundary layer aerosol retrieval from thermal infrared nadir sounding – Preliminary results

A non-empirical algorithm is presented to retrieve the optical depth in the 750–1250 cm⁻¹ spectral range, of aerosol located in the boundary layer over the ocean, from nadir high-resolution radiance spectra in the thermal infrared. The algorithm is based on a line-by-line radiative transfer forward model and used the Optimal Estimation Method for the retrieval. Its performance strongly depends on the quality of the a priori temperature and H₂O atmospheric profiles. To demonstrate the relevance of the algorithm, distributions of maritime aerosol parameters have been retrieved from IMG/ADEOS data for December 1996, using the algorithm with the LBLRTM radiative transfer code, and ERA40 (ECMWF) a priori atmospheric profiles and surface conditions.     

用半经验模型研究耀斑大气的能量耗散

本文利用南京大学太阳塔多波段光谱资料推求出的两个耀斑(一个SB级,一个2B级)的半经验模型;计算了耀斑不同时刻的辐射损失速率,并与电子束轰击和X线作用下的产能率作了比较.结果表明,耀斑不同时刻的色球辐射损失变化可达一个量级以上;耀斑脉冲相前后电子束轰击加热相当有效;耀斑强度极大时,电子束轰击和X线加热都有作用;耀斑主相时,X线加热更能有效地平衡辐射损失.但是,尤其是对大耀斑来说,色球低层和光球上层的加热既不能用电子束轰击,也不能用X线的作用来解释;可能存在某种把能量从色球上层向低层转移的机制.研究也表明,耀斑随时间变化的半经验模型为研究耀斑的能量耗散过程提供了很好的工具.