Impact of air masses origin and trajectory on atmospheric phenomena
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1 Impact of air masses origin and trajectory on atmospheric phenomena Arianna Miniussi, Dario B. Giaiotti feat Fulvio Stel Politechnic of Turin (Italy) Regional Agency for Environmental Protection of Friuli Venezia Giulia (Italy)
2 Conclusions High (relatively) SO2 concentrations in Friuli Venezia Giulia are associated to air masses coming from eastern Europe High PM10 concentrations in Friuli Venezia Giulia are associated to air masses coming from west (Po Valley) and in the previous days air masses have to remain stick to the ground and be subject to subsidence High O3 concentrations do not have a privileged direction of air masses, but air masses have to remain relatively stick to the ground for a long time Heavy rain episodes are characterized by the Adriatic alley direction in the previous days
3 The study area (where Friuli Venezia Giulia is)
4 The study area Heavy rain events Pollution episodes (SO2, PM10, O3)
5 Materials and methods Significant episodes chosen on a daily basis Episodes spanning from 2005 up to 2014 Air masses trajectories determined through the HYSPLIT model ( Meteorological data used obtained from GDAS archive ( Tree 120 hours backward trajectories (SFC, 500 and 1000 m ASL) centered at 12:00 UTC in the day of the event
6 SO2 Backward trajectories that were at SURFACE level at the day of the event
7 SO2 Backward trajectories that were at 500 m above mean level at the day of the event
8 SO2 Backward trajectories that were at 1000 m above surface level at the day of the event
9 SO2 Largest dots indicate the position of air mass one day before the event Smallest dots indicate the position of air mass five days before the event
10 SO2 Left panel Air masses average vertical height (0 is the day of the event) Left panel - Surface air mass average vertical height and standard deviation
11 PM10 Backward trajectories that were at SURFACE level at the day of the event
12 PM10 Backward trajectories that were at 1000 m above surface level at the day of the event
13 PM10 Backward trajectories that were at 1000 m above surface level at the day of the event
14 PM10 Largest dots indicate the position of air mass one day before the event Smallest dots indicate the position of air mass five days before the event
15 PM10 Left panel Air masses average vertical height (0 is the day of the event) Left panel - Surface air mass average vertical height and standard deviation
16 O3 Backward trajectories that were at SURFACE level at the day of the event
17 O3 Backward trajectories that were at 500 m above mean level at the day of the event
18 O3 Backward trajectories that were at 1000 m above surface level at the day of the event
19 O3 Largest dots indicate the position of air mass one day before the event Smallest dots indicate the position of air mass five days before the event
20 O3 Left panel Air masses average vertical height (0 is the day of the event) Left panel - Surface air mass average vertical height and standard deviation
21 Heavy rain Backward trajectories that were at SURFACE level at the day of the event
22 Heavy rain Backward trajectories that were at 500 m above mean level at the day of the event
23 Heavy rain Backward trajectories that were at 1000 m above surface level at the day of the event
24 Heavy rain Largest dots indicate the position of air mass one day before the event Smallest dots indicate the position of air mass five days before the event
25 Heavy rain Left panel Air masses average vertical height (0 is the day of the event) Left panel - Surface air mass average vertical height and standard deviation
26 In general High (relatively) SO2 concentrations are associated to air masses coming from eastern Europe High PM10 concentrations are associated to air masses coming from west (Po Valley) and in the previous days air masses have to remain stick to the ground and be subject to subsidence High O3 concentrations do not have a privileged direction of air masses, but air masses have to remain relatively stick to the ground for a long time Heavy rain episodes are characterized by the Adriatic alley direction in the previous days
27 Thanks for your attention Благодаря
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