P-205L:Late-News Poster: Improvement of Viewing Angle Dependence and Out-Coupling Efficiency of OLEDs with Strong Microcavity Structure by Introduction of Nanoporous Polymer Films

2016 ◽  
Vol 47 (1) ◽  
pp. 1792-1795
Author(s):  
Beom Pyo ◽  
Hyung Suk Kim ◽  
Chul Woong Joo ◽  
Byoung-Hwa Kwon ◽  
Jeong-Ik Lee ◽  
...  
2020 ◽  
Vol 77 ◽  
pp. 105493
Author(s):  
Min Chul Suh ◽  
Dae Yeong Kim ◽  
Seon Hyeak Jung ◽  
Nam Su Kim

1996 ◽  
Vol 179 (1) ◽  
pp. 173-180 ◽  
Author(s):  
Kohki Takatoh ◽  
Hiroyuki Nagata ◽  
Tatsuo Saishu

2014 ◽  
Vol 14 (15) ◽  
pp. 8149-8163 ◽  
Author(s):  
M. J. M. Penning de Vries ◽  
S. Dörner ◽  
J. Puķīte ◽  
C. Hörmann ◽  
M. D. Fromm ◽  
...  

Abstract. The eruption of the Nabro volcano (Eritrea), which started on 12 June 2011, caused the introduction of large quantities of SO2 into the lower stratosphere. The subsequently formed sulfate aerosols could be detected for several months following the eruption. It is generally assumed that the formation of sulfate aerosols in the stratosphere is a relatively slow process, but in plumes from explosive eruptions significant amounts of aerosols have been seen to form within a few hours. We show that sulfate aerosols were present in the lower stratosphere within hours of the onset of the eruption of Nabro. Evidence comes from nadir UV Aerosol Index (UVAI) and SO2 measurements by SCIAMACHY, GOME-2 and OMI, and limb aerosol measurements by SCIAMACHY. The sulfate plume displays negative UVAI in the western part of OMI's swath and positive UVAI in the eastern part – an effect that is due to the strong viewing angle dependence of UVAI and can only be caused by a high-altitude (>11 km), non-absorbing (single-scattering albedo >0.97) aerosol plume. For the retrieval of the aerosol profile from limb measurements, the horizontal dimensions and the position of the aerosol plume need to be taken into account, otherwise both extinction and layer height may be underestimated appreciably. By combining nadir SO2 column density and UVAI with limb aerosol profiles, a stratospheric plume from Nabro could be tracked from 13 to 17 June, before the plumes from later, lower-altitude explosions started interfering with the signal. Our findings are in agreement with ground-based lidar and sun-photometer data from an MPLNET/AERONET station in Israel and with data from the satellite-borne CALIOP lidar.


Nanoscale ◽  
2018 ◽  
Vol 10 (30) ◽  
pp. 14755-14762 ◽  
Author(s):  
Zhipeng Meng ◽  
Suli Wu ◽  
Bingtao Tang ◽  
Wei Ma ◽  
Shufen Zhang

A freestanding structural colored film with a narrow bandgap, high angle dependence and good mechanical properties is demonstrated.


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