A framework for estimating cloudy sky surface downward longwave radiation from the derived active and passive cloud property parameters

被引:45
作者
Yang, Feng [1 ,2 ,3 ]
Cheng, Jie [1 ,2 ,3 ]
机构
[1] Beijing Normal Univ, State Key Lab Remote Sensing Sci, Beijing 100875, Peoples R China
[2] Chinese Acad Sci, State Key Lab Remote Sensing Sci, Inst Remote Sensing & Digital Earth, Beijing 100875, Peoples R China
[3] Beijing Normal Univ, Fac Geog Sci, Inst Remote Sensing Sci & Engn, Beijing 100875, Peoples R China
基金
中国国家自然科学基金;
关键词
Surface downward longwave radiation; Cloud-base temperature; Cloud-top temperature; Cloud thickness; Single-layer cloud model; Remote sensing; SATELLITE; FLUX; CLEAR; ALGORITHM; CERES; VALIDATION; MODEL; MODIS; SENSITIVITY; EMISSIVITY;
D O I
10.1016/j.rse.2020.111972
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The cloud-base temperature (CBT) is one of the parameters that dominates the cloudy sky surface downward longwave radiation (SDLR). However, CBT is rarely available at regional and global scales, and its application in estimating cloud sky SDLR is limited. In this study, a framework to globally estimate cloud sky SDLR during both daytime and nighttime is proposed. This framework is composed of three parts. First, a global cloudy property database was constructed by combing the extracted cloud vertical structure (CVS) parameters from the active CloudSat data and cloud properties from passive MODIS data. Second, the empirical methods for estimating cloud thickness (CT) under ISCCP cloud classification system and MODIS cloud classification system were developed. Additionally, the coefficients of CERES CT estimate models were refitted using the constructed cloud property database. With the estimated CT and reanalysis data, calculating the CBT is straightforward. The accuracy of the estimated CT for ISCCP cloud type is compared with the existing studies that were conducted at local scales. Our CT estimate accuracy is comparable to that of the existing studies. According to the validation results at ARM NSA and SGP stations, the CT estimated by the developed CT model for MODIS cloud type is better than that estimated by the original CERES CT model. Finally, the cloudy sky SDLR values were derived by feeding the estimated CBT and other parameters to the single-layer cloud model (SLCM). When validated by the ground measured SDLR collected from the SURFRAD network, the bias and RMSE are 5.42 W.m(-2) and 30.3 W.m(-2), respectively. This accuracy is comparable to the evaluation results of the mainstream SDLR products (Gui et al. 2010), the new evaluation results of SLCMs (Yu et al. 2018), and the accuracy of a new cloudy sky SDLR estimate method (Wang et al. 2018). All the derived CBTs improve the SDLR estimate accuracy more than the SLCM that directly uses cloud-top temperature (CTT). We will collect more ground measurements and continue to validate the developed framework in the future.
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页数:22
相关论文
共 108 条
[1]  
Ackerman S., 2010, DISCRIMINATING CLEAR
[2]  
Augustine JA, 2000, B AM METEOROL SOC, V81, P2341, DOI 10.1175/1520-0477(2000)081<2341:SANSRB>2.3.CO
[3]  
2
[4]   A 3D cloud-construction algorithm for the EarthCARE satellite mission [J].
Barker, H. W. ;
Jerg, M. P. ;
Wehr, T. ;
Kato, S. ;
Donovan, D. P. ;
Hogan, R. J. .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2011, 137 (657) :1042-1058
[5]  
BARKSTROM BR, 1984, B AM METEOROL SOC, V65, P1170, DOI 10.1175/1520-0477(1984)065<1170:TERBE>2.0.CO
[6]  
2
[7]  
Berk A., 1989, MODTRAN MODERATE RES, P7
[8]   Estimation of Net Radiation From the Moderate Resolution Imaging Spectroradiometer Over the Continental United States [J].
Bisht, Gautam ;
Bras, Rafael L. .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2011, 49 (06) :2448-2462
[9]   Estimation of net radiation from the MODIS data under all sky conditions: Southern Great Plains case study [J].
Bisht, Gautam ;
Bras, Rafael L. .
REMOTE SENSING OF ENVIRONMENT, 2010, 114 (07) :1522-1534
[10]  
BREON FM, 1991, J APPL METEOROL, V30, P17, DOI 10.1175/1520-0450(1991)030<0017:DLIATO>2.0.CO