Linear stokes imaging spectropolarimeter based on the static polarization interference imaging spectrometer

2017 ◽  
Vol 391 ◽  
pp. 30-36 ◽  
Author(s):  
Naicheng Quan ◽  
Chunmin Zhang ◽  
Tingyu Yan ◽  
Qiwei Li ◽  
Ruiru Gao ◽  
...  
2012 ◽  
Vol 37 (17) ◽  
pp. 3507 ◽  
Author(s):  
Tingkui Mu ◽  
Chunmin Zhang ◽  
Wenyi Ren ◽  
Chenling Jia

2002 ◽  
Vol 203 (1-2) ◽  
pp. 21-26 ◽  
Author(s):  
Chunmin Zhang ◽  
Bin Xiangli ◽  
Baochang Zhao ◽  
Xingjing Yuan

2000 ◽  
Author(s):  
Chunmin Zhang ◽  
Xiangli Bin ◽  
Baochang Zhao

2020 ◽  
Vol 13 (6) ◽  
pp. 1-8
Author(s):  
AN Ling-ping ◽  
◽  
WANG Shuang ◽  
ZHANG Geng ◽  
LI Juan ◽  
...  

2020 ◽  
Vol 28 (10) ◽  
pp. 2103-2111
Author(s):  
Mei-hong ZHAO ◽  
◽  
Xin-yu WANG ◽  
Yan-xiu JIANG ◽  
Shuo YANG ◽  
...  

2011 ◽  
Vol 37 (6) ◽  
pp. 1039-1048 ◽  
Author(s):  
Fang-Yong WANG ◽  
Ke-Ru WANG ◽  
Shao-Kun LI ◽  
Shi-Ju GAO ◽  
Chun-Hua XIAO ◽  
...  

2017 ◽  
Vol 2 (6) ◽  
Author(s):  
Yaseen Kadhim Abbas Al-Timimi ◽  
Ali Challob Khraibet

Aerosol Optical Depth (AOD) is the measure of aerosol distributed with a Column of air from earth’s surface to the top of atmosphere, in this study, temperature variation of aerosol optical depth (AOD) in Baghdad was analyzed Moderate Resolution Imaging Spectrometer (MODIS) from Terra and its relationship with temperature for the period 2003 – 2015 were examined. The highest values for mean seasonal AOD were observed in spring and summer and the maximum AOD values ranged from 0.50 to 0.58 by contrast minimum AOD values ranging from 0.30 to 0.41 were found in winter and autumn. Results of study also showed that the temperature (max., min., mean air temperature and DTR) have a strong correlation with AOD (0.82, 0.83, 0.82 and 0.65) respectively.


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