https://www.selleckchem.com/products/brd0539.html
The growth in PM2.5 concentration and the increasing wind speed at high altitudes lead to the upward trend in PM2.5 flux. As the altitude increases, the high-value area of PM2.5 concentration tilts towards the warm air mass. The transit of the cold front at night led to more unstable convection within the boundary layer; the height of the boundary layer increased from north to south, reaching over 1 km, breaking the rules characteristic of the diurnal evolution of the boundary layer. The results indicate that the combination of vertical
Like
Comment
Share
