介绍了电离层和中性大气反演问题和采用的程序流程。
The inversion theory of ionosphere and neutral atmosphere, as well as the adoptive program flow are presented.
因此，MODIS大气可降水量资料经过修正后，可以为卫星反演模式提供同化性较好的输入资料。
So we can conclude that after revised the MODIS atmospheric precipitable water data can be used to satellite derived model and can improve the retrieval accuracy of some satellite remoting model.
利用GPS探测结果、探空资料和气象站常规地面观测资料反演了青藏高原及其周边地区的大气总水汽量。
And atmospheric water vapor distribution and change are studied synthetically based on GPS, radiosonde and other ground weather observations data over Tibet Plateau and around area.
软件还具有NO_2浓度自动反演功能，根据对参考光谱和样品光谱的差分比较，可较为简便地获得样品光谱采集地区大气中NO_2浓度。
What's more, the function of spectrum analyzing is also included in the software, with which, the concentration of NO2 in the atmosphere can be got quite easily.
针对神舟四号飞船微波辐射计（RAD）特殊入射角、频率的特点，开发了海面和大气参数的反演算法。
We developed a sea surface emissivity model and atmospheric model for special frequencies and incidence angles of RAD.
如何精确而成功地反演地表或大气组分参量信息是定量遥感研究的热点与难点。
How to successfully and accurately extract information on atmospheric and soil constituents through inversion analysis is the hotspot and frontier.
第四章根据反演得到的气溶胶光学厚度和大气水汽含量，利用辐射传输模型计算大气校正参数的方法来对遥感图像进行大气校正。
The forth one gives a method to correct the atmospheric effects by taking the AOD and water vapor content inversion results into the atmospheric radiation transferring model.
运用地基GPS气象学的理论，进行了反演大气水汽含量的计算研究。
The calculation research of retrieving atmospheric water vapor with GPS was made, using theories of Ground Based GPS Meteorology.
建立了一种数值算法，从光波在湍流大气中传播的闪烁时间频谱的高频特征反演大气光学湍流谱。
A numerical algorithm is set up for the retrieval of optical turbulence spectrum from high-frequency temporal spectra of a light wave propagating through a turbulent atmosphere.
介绍了利用GPS掩星反演地球中性大气参数的原理。
The theory and the procedure of inversion of Earth′s neutral atmospheric parameters with GPS occultation are briefly introduced.
在用遥感影像反演地面参数时，即使天气晴朗，也要受大气、气溶胶、云的影响。
When using the remote sensing images to reverse the land parameters, the results may he influenced by the atmosphere, aerosol and clouds etc. even if in the sunshine.
本文对双多普勒天气雷达反演大气三维风场进行了初步探讨。
In this paper it is primarily discussed that the retrieval of the atmospheric three-dimensional wind field by Dual-Doppler radar.
此项工作为反演大气参数、建立大气散射辐射偏振特性模型提供素材。
This work can provide material in retrieving the parameter of atmospheric aerosol and modeling polarized properties of the atmospheric aerosol scattering radiation.
提出了辐射光谱、测量区域内大气透过率谱的算法模型，以及应用非线性最小二乘拟合算法实现气体浓度反演的方法。
The algorithm of radiance spectra and transmittance spectra in measured region was proposed, and the method of retrieving gas concentrations with NLLS fitting algorithm was also proposed.
本文在几何光学和薄相位屏的假设下，分别介绍GPS/LEO无线电掩星反演地球大气技术中振幅反演的计算方法。
Under the assumptions of geometric optics and thin phase screen the retrieval algorithms of amplitude in GPS/LEO occultation technique were listed in this paper, respectively.
这对于进一步分析大气透过率和反演大气中红外活性气体浓度具有实际意义。
This calibration method is of significance to the further analysis of atmospheric transmission and the retrieval of the concentration of infrared active gas in atmosphere.
影响HY-1卫星海温反演精度的主要因素为大气中的水汽吸收和云覆盖。
The main factors affecting the accuracy of the HY-1 satellite SST are the atmospheric water vapor absorption and cloud cover.
介绍了地基微波辐射计遥感反演大气柱中的水汽总量和云液态水总量的辐射传输原理和反演方法。
The fundamental and method of the ground-based microwave radiometer remote sensing retrieval of integrated water vapor(V) and cloud liquid water(L) in the atmosphere are introduced herein.
介绍了利用双光路差分吸收光谱(DOAS)技术监测大气气溶胶并反演其粒谱分布的新方法。
With the method of differential optical absorption spectroscopy (DOAS), aerosol along the light path is monitored and its size distribution is measured with double optical path method.
太阳辐射计通过测量不同波段的直接太阳辐射反演地球大气中水汽、臭氧及氮氧化物等气体的含量。
Sunphotometer is designed to measure the direct solar irradiance for retrieving the amount of the vapor of water, ozone and nitrogen oxide etc. in the atmosphere.
因此，数据采集后需对回波信号进行适当的反演，从而获得大气消光系数。
So, it is important to processing the return signal for getting extinction coefficient.
以湿绝热过程的变态方程为积分方程，由卫星TBB资料反演出大气中各等压面层湿度场。
Taking the wet-adiabatic equation as integral equation, the humidity field on each standard isobaric surface derived from satellite TBB-data is used to improve the model initial conditions.
陆面微波比辐射率较高且易变，造成陆面上反演降水以及其它大气参数较为困难。
The larger and highly variable microwave emissivity over land results in more difficulties to retrieve the precipitation and other atmospheric parameters over land.
通过探测高层大气中气辉（极光）辐射线的多普勒频移，可以反演出高层大气中的速度、温度和压强等物理量。
Through detecting the Doppler shifts of airglow (aurora) in upper atmosphere, the physical quantity such as velocity, temperature and pressure of upper atmosphere is derived.
通过探测高层大气中气辉（极光）辐射线的多普勒频移，可以反演出高层大气中的速度、温度和压强等物理量。
Through detecting the Doppler shifts of airglow (aurora) in upper atmosphere, the physical quantity such as velocity, temperature and pressure of upper atmosphere is derived.
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