TMI被动微波遥感资料用于地表洪涝特征分析试验   总被引：4，自引：1，他引：4  

谷松岩  高慧琳  朱元竞  李万彪  赵柏林 《遥感学报》2004,8(3):261-268

星载被动微波遥感资料为云天条件下地表洪涝特征分析提供了可能。微波极化比 (PR)可以有效刻画地表洪涝特征 ,宏观反映地表湿度信息。正演模拟分析结果表明地表粗糙度、地表植被覆盖状况和地表湿度对上行微波亮温有影响 ;TRMM/TMI低频微波通道微波极化比能减弱大气因素的影响 ,清晰反映地表的洪涝特征。合理确定分类阈值 ,对 1 998年长江流域洪涝区进行地表洪涝特征分析 ,可以在TMI像元尺度 ,将洪涝区分类为不同等级。洪涝区分类结果与经过天 -地校验过的机载和星载SAR资料地表洪涝分类实况对比 ,TRMM/TMI低频微波通道微波极化比 1 0GHz的PR1 0和 1 9GHz的PR1 9的分类正确率不低于 75 %。  相似文献   

A self-sufficient approach for GERB cloudy radiance detection     

V. Cuomo  C. Filizzola  N. Pergola  C. Pietrapertosa  V. Tramutoli   《Atmospheric Research》2004,72(1-4):39

Geostationary Earth Radiation Budget (GERB) is the broadband radiometer onboard the Meteosat Second Generation (MSG) platform, launched at the end of August 2002 and still in commissioning phase. GERB data is planned to be used in many applications concerning Earth Radiation Budget (ERB) calculation. In order to evaluate the impact of clouds on ERB, a cloud detection is required and, at present, a cloud mask based on higher spatial and spectral resolution data acquired by Spinning Enhanced Visible and Infrared Imager (SEVIRI), the imager onboard the same MSG platform, is planned to be used in order to identify cloudy GERB soundings.As an alternative, a self-sufficient (only based on GERB data) method (OCA, the One-channel Cloudy-radiance-detection Approach) is proposed, as a time-saving and, probably, more suitable solution than the planned co-location approach.In this paper, preliminary results obtained by using several years of Meteosat data as well as GERB synthetic radiances (produced from Meteosat-7 observations) are presented. It is shown how results obtained by using GERB data alone can be comparable (and better in terms of number and spatial distribution of clear-sky GERB soundings identified) to the ones achieved if the co-location of a higher resolution cloud mask is used.  相似文献   

地物辐亮度方程及其讨论     

李绍新 《武汉大学学报(信息科学版)》1989,(4)

本文从物体的反射特性与热辐射特性出发,在考虑大气影响后,推导出遥感中轨道传感器接受到地物的辐亮度的表达式,并对发射光谱(热红外、微波波段)的情况进行了讨论。  相似文献   

风云一号遥感器可见光通道大气程辐射之间的关系     

张功伟  林寿仁  李勃东  毛天明 《海洋学研究》1993,(1)

本文利用光谱辐射计测量的大气程辐射资料,研究了相应于“风云一号”卫星上改进型甚高分辨率扫描辐射计(CAVHRR)4个可见光通道的大气程辐射量(N_a)之间的关系。结果表明它们满足((N_a(λ))/(N_a(λ_0)))=A(λ/λ_0)~B的关系。 经回归分析得:A为1.0887,B为3.6587。式中λ_0是CAVHRR第二通道的中心波长,即λ_0=0.875μm,λ是CAVHRR其他3个通道中心波长。  相似文献   

A Method for Retrieving Water-leaving Radiance from Landsat TM Image in Taihu Lake, East China   总被引：1，自引：0，他引：1  

WANG Deyu FENG Xuezhi MA Ronghua KANG Guoding 《中国地理科学(英文版)》2007,17(4):364-369

The visible and infrared bands of Landsat Thematic Mapper (TM) can be used for inland water studies. A method of retrieving water-leaving radiance from TM image over Taihu Lake in Jiangsu Province of China was investigated in this article. To estimate water-leaving radiance, atmospheric correction was performed in three visible bands of 485nm, 560nm and 660nm. Rayleigh scattering was computed precisely, and the aerosol contribution was estimated by adopting the clear-water-pixels approach. The clear waters were identified by using the Landsat TM middle-infrared band (2.1μm), and the water-leaving radiance of clear water pixels in the green band was estimated by using field data. Aerosol scattering at green band was derived for six points, and interpolated to match the TM image. Assuming the atmospheric correction coefficient was 1.0, the aerosol scattering image at blue and red bands were derived. Based on a simplified atmospheric radiation transfer model, the water-leaving radiance for three visible bands was retrieved. The water-leaving radiance was normalized to make it comparable with that estimated from other remotely sensed data acquired at different times, and under different atmospheric conditions. Additionally, remotely sensed reflectance of water was computed. To evaluate the atmospheric correction method presented in this article, the correlation was analyzed between the corrected remotely sensed data and the measured water parameters based on the retrieval model. The results show that the atmospheric correction method based on the image itself is more effective for the retrieval of water parameters from Landsat TM data than 6S (Second Simulation of the Satellite Signal in the Solar Spectrum) code based on standard atmospheric and aerosol models.  相似文献   

高温目标辐射亮度比的方向性研究     

张雪峰  潘军  蒋立军  王凯  仲伟敬  张文哲 《世界地质》2019,(2):522-531

为研究高温目标在短波红外发射辐射的方向性,建立多角度观测物理模型;以燃烧竹炭作为小面元高温目标,在暗室条件下使用ASD FieldSpec3光谱仪对高温目标的辐射亮度进行多角度观测和分析。仅使用一台光谱仪无法同时获取多个角度的观测数据,且以不同角度观测时,高温目标温度发生明显改变,本文采用一种自定义的降温模型计算多角度观测的参比辐射亮度,并提出一个概念-辐射亮度比(多角度辐射亮度/参比辐射亮度),用以消除高温目标降温的影响。结果表明,降温模型精度很高,辐射亮度比这一概念很好地刻画了高温目标在短波红外辐射的方向性,余弦函数、傅里叶级数均可实现对辐射亮度比随角度变化的高精度拟合。  相似文献   

Application of direct assimilation of ATOVS microwave radiances to typhoon track prediction   总被引：27，自引：1，他引：26  

ZHANG Hu  XUE Jishan  ZHU Guofu  ZHUANG Shiyu  WU Xuebao  ZHANG Fengying 《大气科学进展》2004,21(2):283-290

In order to solve the difficult problem of typhoon track prediction due to the sparsity of conventionaldata over the tropical ocean, in this paper, the No. 0205 typhoon Rammasun of 4-6 July 2002 is studiedand an experiment of the typhoon track prediction is made with the direct use of the Advanced TIROS-NOperational Vertical Sounder (ATOVS) microwave radiance data in three-dimensional variational dataassimilation. The prediction result shows that the experiment with the ATOVS microwave radiance datacan not only successfully predict the observed fact that typhoon Rammasun moves northward and turnsright, but can also simulate the action of the fast movement of the typhoon, which cannot be simulated withonly conventional radiosonde data. The skill of the typhoon track prediction with the ATOVS microwaveradiance data is much better than that without the ATOVS data. The typhoon track prediction of theformer scheme is consistent in time and in location with the observation. The direct assimilation of ATOVSmicrowave radiance data is an available way to solve the problem of the sparse observation data over thetropical ocean, and has great potential in being applied to typhoon track prediction.  相似文献   

HJ-1A星辐射定标及近海水体大气校正的精度验证   总被引：1，自引：0，他引：1  

肖艳芳  朱琳  赵文吉 《海洋科学进展》2012,30(1):54-62

以应用HJ-1A星数据进行近海水体定量反演为目的,对HJ-1A星CCD的星上定标系数的精度进行验证,并基于Landsat-5TM数据对其进行交叉定标。在此基础上反演近海水体的反射率,将反演结果与实测水体反射率进行比较发现:对HJ-1A星CCD数据进行交叉定标能在一定程度上能提高近海水体反射率反演的精度。结果表明,HJ-1A星CCD影像的星上定标系数不够精确,在利用该数据进行近海水体的定量反演研究时,需要利用交叉定标对星上定标参数进行修正。  相似文献   

Laboratory measurements on radon exposure effects on local environmental temperature: Implications for satellite TIR measurements     

《Physics and Chemistry of the Earth》2015

Surface latent heat flux (SLHF) is proportional to the heat released by phase changes during solidification, evaporation or melting. Effects of SLHF on the earth’s surface could be measured by satellite techniques capable of measuring thermal infrared radiation (TIR). Recent studies have found a possible correlation between SLHF and earthquakes, hence satellite techniques are widely used in research into the possible link between SLHF and earthquakes. Possible fluctuations in SLHF values during seismic periods have been attributed to different causes, such as the expulsion from the ground of greenhouse gases or because of radon. In particular, ionization processes due to radon decay could lead to changes in air temperature. Laboratory experiments have been carried out to highlight the possible role of radon in the thermal environmental conditions of a laboratory-controlled atmospheric volume.  相似文献   

地表温度反演的数值方法     

宋金红  陈圣波  包书新  汪自军  韩念龙  吕航 《吉林大学学报(地球科学版)》2007,(Z1)

陆地表面温度(LST)是区域和全球尺度上陆地表面物理过程的一个关键参数,它综合了地表和大气相互作用以及能量交换的结果。研究地表温度对全球能量平衡的研究有着重要的意义。地表温度反演以地表热辐射传输方程为基础,直接求解辐射传输方程是不可能的,也就是说它是不适定的。因此要采用一系列的数值计算方法来求解。主要介绍了几种方程解算的非线性数值方法,并阐述了其大致过程及优缺点。  相似文献