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1.
北京晴天紫外波段气溶胶光学厚度反演与分析   总被引:4,自引:1,他引:4  
利用太阳一大气紫外光谱辐射计(SAUVS),测量到达北京地表的太阳直接和散射紫外光谱辐射,给出反演大气气溶胶光学厚度的一种方法。结果表明:在紫外波段,大气气溶胶的光学厚度随波长的增加而单调减小,用指数函数可以很好地拟合反演结果。统计得到了3个水平能见度状况下拟合函数的系数值,与全球气溶胶监测网络(AERONET)北京站的资料对比,表明反演结果基本合理。  相似文献   

2.
北京地面紫外辐射(光谱)的观测与分析   总被引:13,自引:0,他引:13       下载免费PDF全文
通过对北京大气物理研究所与长春光机所合作研制的地基太阳紫外辐射光谱仪观测资料的分析,和用辐射传输模式UVSS计算的结果,对影响到达地面的UVB辐照度的主要因子太阳高度角(SZA)、臭氧总量和地表反照率进行了分析研究。最后对紫外光谱仪的观测资料做了总量和谱分析。  相似文献   

3.
到达地面的太阳紫外辐射强度的观测   总被引:7,自引:0,他引:7  
吴兑 《气象》2001,27(3):26-29
紫外辐射强度的公众服务一般用紫外线指数来表示,是衡量某地正午前后到达地面的太阳紫外辐射对人体皮肤(或眼睛)可能损害的程度指标,沱主要依赖于纬度,季节,平流层臭氧,云况,海拔,地面反照率和大气污染状态等条件,紫外线辐射强度的观测主要使用紫外光谱辐射计与滤光片式的紫外辐射表。  相似文献   

4.
南京地区紫外辐射初步研究   总被引:11,自引:1,他引:10  
采用简化型辐射传播模型计算了南京地区到达地表的太阳紫外辐射(UV辐射),同时根据地面紫外辐射的观测资料分析了南京地区紫外辐射的年变化、晴天与阴天的变化规律及与太阳总辐射的关系。  相似文献   

5.
影响地面紫外辐射的因素分析   总被引:31,自引:2,他引:29       下载免费PDF全文
通过作者改进的离散坐标法(DISORT)辐射传输模式和部分观测资料考察了臭氧总量及其垂直分布、二氧化硫、气溶胶及火山气溶胶、地表反照率、太阳天顶角对到达地面紫外辐射的影响,以及云与紫外辐射的相互作用,给出了一些最主要的结果。此外,还简要地介绍了国内外紫外辐射观测研究的一些进展,特别是欧盟委员会资助开展的“确定UV-B辐射观测网标准”的科学计划。  相似文献   

6.
上海地区地面太阳紫外辐射的观测和分析   总被引:21,自引:0,他引:21  
通过对上海地区2001~2003年地面太阳总辐射和紫外辐射观测资料的分析表明:(1)上海地区太阳辐射和紫外辐射年总量分别为4487.1MJ/m^2和149.6MJ/m^2。(2)紫外辐射的季节变化特征十分明显,夏半年(4-9月)各月极大紫外辐射强度远大于冬半年(10月~次年3月),7月份最强,12月份最弱。(3)不同天气条件下,紫外辐射日变化显示出明显的差异,晴天强且稳定,多云天气波动较大,阴天则次之。(4)紫外辐射占总辐射的比例(η)也显示冬半年低,夏半年高的分布特征。(5)影响上海地区到达地面紫外辐射的主要因子有:太阳高度角的大小大致决定了到达地面紫外辐射的强弱,两者具有相近的年变化趋势;云、雨等天气类型是影响紫外辐射的重要因子;大气能见度对紫外辐射也有比较明显的影响。  相似文献   

7.
北京地区太阳紫外辐射的观测与分析研究   总被引:10,自引:2,他引:10  
白建辉  王庚辰 《大气科学》1994,18(3):341-347
利用北京地区太阳辐射和其它常规气象观测资料,得到了到达地面的太阳紫外辐射的计算公式,并将计算值与观测值进行了比较,两者吻合得比较好。最后给出了北京地区地面太阳紫外总辐射的变化趋势,计算结果表明,地面太阳紫外总辐射对大气浑浊度的变化比对大气臭氧总量的变化敏感得多。  相似文献   

8.
西藏羊八井辐射观测初步分析   总被引:1,自引:0,他引:1  
利用西藏羊八井2009年5月至2010年4月的辐射观测数据,统计了总辐射、紫外辐射、长波辐射、净辐射的日变化、月变化和季节变化,并分析了地表辐射超过太阳常数的发生频率及原因。结果表明,羊八井地区总辐射、紫外辐射、长波辐射、净辐射均表现出明显的日变化、月变化和季节变化特征;总辐射与地表短波反射辐射、总辐射与紫外辐射均表现出明显的正相关关系;大气逆辐射和地表长波辐射之间呈现出一定的的正相关关系。  相似文献   

9.
吴兑 《气象》2001,27(3):26-29
紫外辐射强度的公众服务一般用紫外线指数来表示,是衡量某地正午前后到达地面的太阳紫外辐射对人体皮肤(或眼睛)可能损害的程度指标,它主要依赖于纬度、季节、平流层臭氧、云况、海拔高度、地面反照率和大气污染状态等条件。紫外线辐射强度的观测主要使用紫外光谱辐射计与滤光片式的紫外辐射表。  相似文献   

10.
太阳紫外辐射在大气中衰减的探讨   总被引:7,自引:2,他引:5  
在对北京紫外辐射观测资料分析的基础上,提出了参与光化学反应的物质对太阳紫外辐射能量的吸收作用.计算表明北京地区1990年云天比晴天紫外辐射减少约为21W m-2,此值与CeSS等人的观测结果比较接近.这表明了大气中参与光化学反应的物质对光化辐射能量的吸收基本上等于云对太阳短波辐射的"异常吸收"之值.所以,在辐射传输模式、大气化学模式、气候模式中,应该考虑参与光化学反应的物质对光化辐射能量的吸收作用.  相似文献   

11.
Numerous factors can influence the radiative transfer simulation of hyper-spectral ultraviolet satellite observation,including the radiative transfer scheme, gaseous absorption coefficients, Rayleigh scattering scheme, surface reflectance, aerosol scattering, band center wavelength shifts of sensor, and accuracy of input profiles. In this study, a Unified Linearized Vector Radiative Transfer Model(UNL-VRTM) is used to understand the influences of various factors on the top of atmosphere(TOA) normalized radiance in the ultraviolet(UV) region. A benchmark test for Rayleigh scattering is first performed to verify the UNL-VRTM accuracy, showing that the model performances agree well with earlier peer-reviewed results. Sensitivity experiments show that a scalar radiative transfer approximation considering only ozone and a constant surface reflectance within the UV region may cause significant errors to the TOA normalized radiance. A comparison of the Ozone Mapping and Profiler Suite(OMPS) radiances between simulations and observations shows that the surface reflectance strongly influences the accuracy for the wavelengths larger than 340 nm. Thus, using the surface reflectivity at 331 nm as a proxy for simulating the whole OMPS hyperspectral ultraviolet radiances is problematic. The impact of rotational Raman scattering on TOA radiance can be simulated through using SCIATRAN, which can also reduce the difference between measurements and simulations to some extent. Overall, the differences between OMPS simulations and observations can be less than 3% for the entire wavelengths. The bias is nearly constant across the cross-track direction.  相似文献   

12.
The Multivariate and Minimum Residual(MMR) cloud detection and retrieval algorithm, previously developed and tested on simulated observations and Advanced Infrared Sounder radiance, was explored and validated using various radiances from multiple sensors. For validation, the cloud retrievals were compared to independent cloud products from Cloud Sat, MODIS(Moderate Resolution Imaging Spectroradiometer), and GOES(Geostationary Operational Environmental Satellites). We found good spatial agreement within a single instrument, although the cloud fraction on each pixel was estimated independently. The retrieved cloud properties showed good agreement using radiances from multiple satellites, especially for the vertically integrated cloud mask. The accuracy of the MMR scheme in detecting mid-level clouds was found to be higher than for higher and lower clouds. The accuracy in retrieving cloud top pressures and cloud profiles increased with more channels from observations. For observations with fewer channels, the MMR solution was an "overly smoothed" estimation of the true vertical profile, starting from a uniform clear guess. Additionally, the retrieval algorithm showed some meaningful skill in simulating the cloudy radiance as a linear observation operator, discriminating between numerical weather prediction(NWP) error and cloud effects. The retrieval scheme was also found to be robust when different radiative transfer models were used. The potential application of the MMR algorithm in NWP with multiple radiances is also discussed.  相似文献   

13.
区域极轨卫星ATOVS辐射偏差订正方法研究   总被引:19,自引:0,他引:19  
近年来,卫星辐射资料在数值天气预报(NWP)系统中的直接同化研究取得了长足进展。为了利用TIROS业务垂直探测器(ATOVS)的辐射资料,必须对卫星观测辐射值的系统性偏差进行订正。在ECMWF原全球TOVS辐射偏差订正方案基础上,结合ATOVS资料特征和中国的实际情况,建立了适用于区域NOAA-15/16/17极轨气象卫星ATOVS辐射资料的偏差订正方案。该方案偏差订正分两步进行:首先进行扫描偏差订正,然后进行气团偏差订正。扫描偏差是临边测量相对于星下点测量的系统偏差,统计显示该种偏差具有一定的纬度依赖性,所以订正时按每10度的纬度带分别进行订正。气团偏差订正主要就是根据当时的天气条件进行订正,而天气条件一般用预报因子来定量表示。文中从中国国家气象中心T213背景场导出预报因子:(1)1000—300 hPa的厚度,(2)200—50 hPa的厚度,(3)模式地表温度,(4)总可降水量。模式预报因子的使用从观念上将对观测值的订正变为对计算前向辐射值的订正问题。试验结果表明,订正结果显著。  相似文献   

14.
卫星探测辐射率在数值天气预报中的直接应用   总被引:6,自引:2,他引:6       下载免费PDF全文
该文叙述在数值天气预报中直接应用辐射率而不经过反演的原因,变分法在辐射率直接应用中的作用,以及介绍变分问题计算中的伴随方法。还指出ATOVS辐射率同样可以在NWP中直接应用。最后,介绍业务NWP直接应用辐射率的情况。  相似文献   

15.
Intensity forecasting is one of the most challenging aspects of tropical cyclone (TC) forecasting. This work examines the impact of assimilating high-resolution all-sky infrared radiance observations from geostationary satellite GOES-13 on the convection-permitting initialization and prediction of Hurricane Joaquin (2015) with an ensemble Kalman filter (EnKF) based on the Weather Research and Forecasting (WRF) model. Given that almost all operational global and regional models struggled to capture Hurricane Joaquin (2015)’s intensity, this study examines the potential in improving Joaquin’s prediction when assimilating all-sky infrared radiances from GOES-13’s water vapor channel. It is demonstrated that, after a few 3-hour cycles assimilating all-sky radiance, the WRF model was able to forecast reasonably well Joaquin’s intensity, including its rapid intensification (RI). The improvement was largely due to a more realistic initial hurricane structure with a stronger, warmer, and more compact inner-core. Ensemble forecasts were used to further explore the important physical mechanisms driving the hurricane’s RI. Results showed that the RI forecasts were greatly impacted by the initial inner-core vortex structure.  相似文献   

16.
In this paper, firstly, the bias between observed radiances from the Advanced TIROS-N Operational Vertical Sounder (ATOVS) and those simulated from a model first-guess are corrected. After bias correction, the observed minus calculated (O-B) radiances of most channels were reduced closer to zero, with peak values in each channel shifted towards zero, and the distribution of O-B closer to a Gaussian distribution than without bias correction. Secondly, ATOVS radiance data with and without bias correction are assimilated directly with an Ensemble Kalman Filter (EnKF) data assimilation system, which are then adopted as the initial fields in the forecast model T106L19 to simulate Typhoon Prapiroon (2006) during the period 2-4 August 2006. The prediction results show that the assimilation of ATOVS radiance data with bias correction has a significant and positive impact upon the prediction of the typhoon’s track and intensity, although the results are not perfect.  相似文献   

17.
The impacts of AMSU-A and IASI (Infrared Atmospheric Sounding Interferometer) radiances assimila-tion on the prediction of typhoons Vicente and Saola (2012) are studied by using the ensemble transform ...  相似文献   

18.
在NCEPGDAS中同化MSG和GOES资料   总被引:1,自引:0,他引:1  
首次将MSG-2(Meteosat Second Generation-2)卫星上的旋转增强可见光及红外成像仪(Spin—ning Enhanced Visibleand Infrared Imager,SEVIRI)的观测资料同化到美国国家环境预报中心(Na—tional Centers for Environmental Prediction,NCEP)全球资料同化系统(globaldataassimilationsys—tern,GDAS)中。对当前的地球静止业务环境卫星(Geostationary Operational Environmental Satel—lite,GOES)成像仪资料的同化问题也进行了进一步探讨。利用CRTM(The Community Radiative Transfer Model)模式,对SEVIRI辐射率观测资料进行了模拟。为了对红外辐射率资料进行模拟,CRTM模式中的几个关键部分得到改进,例如:动态更新地面发射率资料以及采用了快速精确的气体吸收模块。为了改进对SEVIRI和GOES成像仪辐射率资料的模拟效果,采用了GSICS(The Global Space—Based Inter—Calibration System)标定订正。初步研究结果表明,包含对SEVIRI辐射率资料的水汽通道(6.25和7.35μm)和二氧化碳通道(13.40μm)的同化对GFS(Global Forecast System)6d预报具有显著的正影响;而对其他5个SEVIRI红外窗口通道资料的同化则减小了这种正影响。通过应用GSICS标定算法,订正了SEVIRI和GOES-12成像仪观测资料的偏差,提高了对GFS预报的影响。此外,还需作进一步研究来提高对SEVIRI红外窗口通道辐射率资料同化的有效性。  相似文献   

19.
Satellite measurements are an important source of global observations in support of numerical weather prediction (NWP). The assimilation of satellite radiances under clear skies has greatly improved NWP forecast scores. However, the application of radiances in cloudy skies remains a significant challenge. In order to better assimilate radiances in cloudy skies, it is very important to detect any clear field-of-view (FOV) accurately and assimilate cloudy radiances appropriately. Research progress on both clear FOV detection methodologies and cloudy radiance assimilation techniques are reviewed in this paper. Overview on approaches being implemented in the operational centers and studied by the satellite data assimilation research community is presented. Challenges and future directions for satellite sounder radiance assimilation in cloudy skies in NWP models are also discussed.  相似文献   

20.
Precipitation detection is an essential step in radiance assimilation because the uncertainties in precipitation would affect the radiative transfer calculation and observation errors. The traditional precipitation detection method for microwave only detects clouds and precipitation horizontally, without considering the three-dimensional distribution of clouds.Extending precipitation detection from 2D to 3D is expected to bring more useful information to the data assimilation without using the a...  相似文献   

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