Differences
This shows you the differences between two versions of the page.
Both sides previous revision Previous revision Next revision | Previous revision | ||
emep:page1:pm_underestimation [2011-08-24 13:09:38] hildef |
emep:page1:pm_underestimation [2022-05-31 09:29:32] (current) |
||
---|---|---|---|
Line 2: | Line 2: | ||
Participants: | Participants: | ||
- | DS,ST,DS, | + | DS, |
Possible reasons: | Possible reasons: | ||
+ | |||
* pH dependency of SO2 ox rate \\ | * pH dependency of SO2 ox rate \\ | ||
* wet scavenging (in ice, scavenging rates ...)\\ | * wet scavenging (in ice, scavenging rates ...)\\ | ||
- | * emission heights (probably not important)\\ | + | * emission heights:\\ |
- | * Size of vertical layers\\ | + | DS:I have started this, testing different plume-rise |
- | * BIC for aerosols\\ | + | formula together with the IIASA . Peter contributed with a subroutine to |
- | * Wood burning emissions\\ | + | spread the emissions into flexible vertical layers also. Should all be |
+ | ready soon-ish, but probably won't change things very much as you say. (probably not important)\\ | ||
+ | |||
+ | * Size of vertical layers, boundary layer mixing \\ | ||
+ | * Secondary Organic Aerosol contribution\\ | ||
+ | * Agricultural and Industrial dust in windy, dry conditions | ||
+ | * BIC for aerosols, dust in southern Europe\\ | ||
+ | * Wood burning emissions | ||
+ | when we know they are wrong. | ||
+ | We could change the time-series though, using a " | ||
+ | Betrand used. That would be good, but requires some testing. I think | ||
+ | that SNAP-2 in general should have this, and wood-burning especially, | ||
+ | but I also suspect that wood-burning starts at a lower temperature than | ||
+ | Betrand' | ||
+ | * Station representativity for some specific sites (Susceptibility to inversion situations in winter? | ||
+ | * Kz, Hmix - currently our minimum mixing height is in the 2nd layer | ||
+ | (k=19). I have some test versions which allow very shallow mixing | ||
+ | heights. These cause a slight increase in surface PM, and are | ||
+ | scientifically ok I think. I can commit next week if all looks well. \\ | ||
+ | (What I am less sure about is what we should do for Kz above Hmix. Now | ||
+ | we have zero, earlier we used critical Richardson numbers, etc. Seems | ||
+ | better to use the latter.) \\ | ||
+ | |||
+ | * I suggested some ideas for David H. here to work with, but that seems | ||
+ | to be progressing slowly. I'll check again on this next week. \\ | ||
+ | |||
+ | * Ammonium nitrate formation \\ | ||
+ | * Emission seasonality for SO2 missing\\ | ||
+ | |||
+ | Which Analysis : | ||
+ | |||
+ | * Separate discussion by aerosol component\\ | ||
+ | * AMS measurements EUSAAR ?\\ | ||
+ | * Caliop extinction profiles for European subregions become available shortly, extinction profile in model needed, \\ | ||
+ | * EUCAARI aircraft measurements? | ||
+ | * Seasonal and spatial bias analysis \\ | ||
+ | ** When do we underestimate?? | ||
+ | if we can see patterns in the days when we underestimate compared to | ||
+ | when we don't. Is it on very cold days, or generally for example? | ||
+ | compounds cause most of the problem? Might give a clue on whether it is | ||
+ | meteorology of chemistry. \\ | ||
+ | |||
+ | ===== Minutes ===== | ||
+ | |||
+ | * [[emep: |