TY  -  
T1  - The effect of aerosols on long wave radiation and global warming 
SN  -  /  
UR  - URN:NBN:fi:hulib-201711155702; http://hdl.handle.net/10138/228853 
T3  -  
A1  - Zhou, You 
A2  -  
PB  - Helsingfors universitet 
Y1  - 2015 
LA  - eng 
AB  - Long wave (LW) radiation in the Earth's atmosphere is defined as the radiation at wavelengths longer than 4 µm (infrared). The short wave (SW) radiation wavelengths are less than 4 µm (visible light, ultraviolet). SW radiation is usually from solar origin. The absorbed solar SW radiation is closely balanced by the outgoing LW radiation in the atmosphere. This radiation balance keeps the global average temperature stable. The main cause of the current global warming trend is human expansion of th... 
VO  -  
IS  -  
SP  -  
OP  -  
KW  - aerosols; long wave radiation; radiative forcing; long wave heating rate; long wave radiation scheme; Lan Zhou city; climate change 
N1  -   
PP  -  
ER  -