Difference between revisions of "Dust"

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'''[[AeroCom]]''' wiki discussion  entry
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Go back to '''[[AeroCom]]''' wiki discussion  entry / '''[[AeroCom/Working group structure]]'''
  
Go back to '''[[AeroCom/Working group structure]]'''
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Enter the '''[[Talk:Dust|Discussion on dust]]''' or click on the flag 'discussion' above.
  
See also summary of '''[[AeroCom/Recommendations]]'''
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----
 
 
 
 
==AeroCom working group '''DUST''' ==
 
  
===Participants for analysis===
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'''AeroCom working group DUST'''
Ginoux, Balkanski, Mahowald, Schulz,
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Winker, Mann, Takemura, Miller?, Tegen?, Zender?,
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===Participants===
 +
Ginoux, Balkanski, Mahowald, Schulz, Miller, Tegen, Zender,  
 +
Winker, Mann, Takemura, (Textor)
  
NEXT Telephone conference:
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-
10th of January 17 UTC (= 18 Paris time, 12 ET, 10 Boulder Time?)
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NEXT Telephone conference: probably march 07, organised from NCAR
  
 
===Goals===
 
===Goals===
  
Investigate the possible impact of anthropogenic dust sources<br>
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Investigate the possible climate impact of anthropogenic dust sources<br>
 
Compare dust simulations to multiple observational datasets<br>
 
Compare dust simulations to multiple observational datasets<br>
 
Recommend properties for dust size and refractive index<br>
 
Recommend properties for dust size and refractive index<br>
  
===Processes and possible Diagnostics===
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===Short term actions===
  
Dust erosion - wind frequency and speed ; threshold velocities;
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- Provide specifications for a land use related dust source
effective source fluxes; source size distribution
+
to be implemented by participating modellers (Mahowald)<br>
 +
- Pull out of dust variables for one AeroCom model (Schulz)<br>
 +
- passed on to R. Miller for initial testing of Cakmur analysis<br>
 +
- establish an observational database beyond Cakmur et al and AeroCom<br>
 +
- revisit HTAP dust experiment design (see MS email to AeroCom in Dec)<br>
 +
- eventually come together at AGU Acapulco conference in May 2007<br>
 +
- suggest input for C. Zender for Perrugia conference
 +
===List of Observational data to be included in analysis===
  
Dust settling - dry removal velocities per size bin;
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Al in ocean water
  
Wet Dust removal - wet scavenging efficients; vertical distribution;
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Visibility
wet deposition of Calcium, dust;
 
  
Scattering and absorption - refractive index; AOD; size; absorption
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IDDI index
  
===Short-term actions/experiments===
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Satellite AOD in dust dominated regions
 +
(MISR, MODIS, TOMS, DEEPBLUE-MODIS, CALIPSO, Aeronet, Calipso)
  
Organise regular teleconferences<br>
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Coarse mode satellite derived AOD in dust regions?
  
Prepare a natural and an anthropogenic dust source for a joint
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Deposition
experiment<br>Follow up on ideas from earlier Mahowald publications.
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DIRTMAP, Fe, Ca in rain
  
Assemble observations<br>
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Surface concentrations
(Visibility, IDDI, MISR, MODIS, MODIS Deepblue, Deposition, Aeronet,
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Aeroce, Asian network
Aeroce, Calipso, Asian dust observations, Ca concentrations in rain)<br>
 
Retrieve from AeroCom database dust variables and wind speed fields<br>
 
  
Eventually participate in dust conference in Italy <br>
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Refractive index and size in literature
  
===Data to look at===
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===Processes and possible Diagnostics===
  
The AeroCom database has unanalysed data on dust deposition
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Dust erosion - wind frequency and speed ; threshold velocities;
and wind speed statistics in some models.
+
effective source fluxes; source size distribution
  
Aeronet dust dominated sites
+
Dust settling - dry removal velocities per size bin;
  
Refractive index and size in literature
+
Wet Dust removal - wet scavenging efficients; vertical distribution;
 +
wet deposition of Calcium, dust;
  
Dust, Fe and Ca concentrations in air and precipitation
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Scattering and absorption - refractive index; AOD; size; absorption
 
 
Satellite AOD in dust dominated regions
 
(MISR, MODIS, TOMS, DEEPBLUE-MODIS, CALIPSO)
 
  
Fine mode AOD in dust regions?
 
  
 
[[Image:Sink DUST an2000 mALLYEAR WORLD Fraction.ps.png|Sink repartitioning among AeroCom models]]
 
[[Image:Sink DUST an2000 mALLYEAR WORLD Fraction.ps.png|Sink repartitioning among AeroCom models]]
 
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Figure taken from [http://www.copernicus.org/EGU/acp/acp/6/1777/acp-6-1777.pdf Textor et al., ACP 2006]
== Enter the DISCUSSION '''HERE''' ==
 
 
 
----
 
=== Thursday December 14th 2006  Michael Schulz  ===
 
 
 
Dear dust colleagues,
 
 
 
Having met Nathalie and Paul in Paris during the GEIA conference I am motivated again for suggesting joint dust work.
 
I think there is a good chance to get a better 'dust analysis'
 
going on the basis of the AeroCom data. But we probably need to do/propose some additional experiments.
 
 
 
During the AeroCom workshop we have said that a working group should be installed and Paul kindly agreed to lead it (for now). As suggested by the meeting we intend to maintain wiki pages for joint discussion and I have set up one with basic initial thoughts:
 
 
 
http://wiki.esipfed.org/index.php/Dust
 
 
 
However - Nathalie and me thought that some few telephone conferences would be really  helpful to get things going. I have no real experience but can only propose skype. Any better suggestion would be perfect!! I just tested: we could also download images on the wiki page prior/during a telecon.
 
Not so complicated. I suggest you use the wiki page to enter propositions for a first teleconference.
 
 
 
Right now I am not sure we will manage to start before Christmas. But some reaction to this proposal would be nice,
 
 
 
have nice winter days!
 
Michael
 
 
 
 
 
=== Friday December 15th 2006, Ina Tegen ===
 
 
 
 
 
Dear colleagues,
 
a dedicated AEROCOM-DUST analysis is a good idea and is quite timely considering the ever-increasing interest in dust aerosol, and I would be happy to contribute. I agree with Michael that some new experiments would be needed, which obviously have to be carefully designed. To have Paul lead a working group on this is great. I suggest to also include Stephanie Woodward from the Hadley Center in this exercise. (stephanie.woodward@metoffice.gov.uk).
 
 
 
After having looked at the WIKI page, here are some additional comments:
 
 
 
- What is the best choice for an anthropogenic dust source? While the estimates for total anthropogenic dust contribution to total dust are now considerably lower compared to the IPCC 2001 number, this emission and the geographical distribution is still very uncertain. In addition to ‘direct’ anthropogenic dust sources as from agricultural soil disturbance it would be nice to have a ‘second order’ anthropogenic dust source that is caused by anthropogenic climate change, ie present-preindustrial sources taking into  account any changes in surface wind and precipitation as well as vegetation, such as estimated recently by Natalie. In addition to her results it would be useful to have additional estimates from other models to minimize a possible model dependence of these results. Maybe putting together  a map of vegetation  changes from different vegetation model results for the preindustrial to present can be helpful.
 
 
 
- A while ago I looked at the AEROCOM results for dust– it seemed that the differences between the results for Experiment B (fixed sources) were larger than to be expected from differences in deposition schemes alone (although these may be considerable too)- and indeed it seems that while everyone used the same emission fluxes they were distributed quite differently on the different particle sizes, due to the different treatments of size distribution in the models (mode vs bin schemes) and of course if the same mass it put into larger size bins, the atmospheric load depletes more quickly due to higher gravitational settling velocities, and the importance of the different deposition processes (as seen in the Figure included in the Wiki page)) partly differs  simply due to this. It is  crucial to pay attention to this  for any new runs comparing results with  identical dust source fluxes– if the effect of the different transport and deposition schemes are to be compared it has to be ensured that the sources are in fact identical, including identical initial size distribution.
 
 
 
- The choice of the  dust refractive index is of course important for computing radiative  flux changes, but to my knowledge no model uses yet refractive indices which vary with the source region to account eg for hematite/goethite content (my apologies if I have overlooked something here). Also, I see that you intend to compare Ca contents of the dust – this should also vary for the different source regions. So I am not sure if we can make any real progress by model intercomparison, apart from compiling
 
appropriate literature data.  BTW, the German SAMUM dust experiment that took place in
 
Morocco past  summer should have some  very good data on dust optical properties by next year (the measurement results are  currently still being analysed).
 
 
 
- Which should be the focus year(s) for those models which are driven by reanalysis fields or nudged meteorology? For the AEROCOM years  I suggest to concentrate on 2001, which had Ace Asia, and some nice Saharan dust events.
 
If additional years will be simulated, I suggest 2006 of course, if we want to make use of Calipso data. Also, for this year eventually some results from the  SAMUM and AMMA field campaigns results will become available.
 
 
 
- If this is possible it would be useful to perform an emissions only experiment in addition to the full atmospheric dust run to systematically compare the performance of the different schemes, e.g. computing dust emissions for the different schemes with identical surface wind speeds in addition to compute the fluxes with their own wind fields. Of course it will difficult to decide on the ‘best’ emission scheme by this as there are no global scale dust emission flux data, but  a test of the performance  could possibly be done be  in terms of modelled ’emission events’ compared to meteorological dust storm data, IDDI, and TOMS AI > 0.7 (?)events (any other ideas?).
 
 
 
Regarding a telephone conference, sometime January would be fine. Having never set up one myself,  I cannot offer any other suggestions on the best way to do this, sorry.
 
 
 
A happy holiday season to all of you,
 
Best wishes, Ina
 
 
 
 
 
-----------------------
 
Dr. Ina Tegen
 
Leibniz Institute for Tropospheric Research Permoserstr. 15
 
04318 Leipzig
 
Germany
 
 
 
Tel.: +49 (0)341 235 2146
 
Fax:  +49 (0)341 235 2139
 
Email: itegen@tropos.de
 

Latest revision as of 05:35, August 12, 2012

Go back to AeroCom wiki discussion entry / AeroCom/Working group structure

Enter the Discussion on dust or click on the flag 'discussion' above.


AeroCom working group DUST

Participants

Ginoux, Balkanski, Mahowald, Schulz, Miller, Tegen, Zender, Winker, Mann, Takemura, (Textor)

- NEXT Telephone conference: probably march 07, organised from NCAR

Goals

Investigate the possible climate impact of anthropogenic dust sources
Compare dust simulations to multiple observational datasets
Recommend properties for dust size and refractive index

Short term actions

- Provide specifications for a land use related dust source to be implemented by participating modellers (Mahowald)
- Pull out of dust variables for one AeroCom model (Schulz)
- passed on to R. Miller for initial testing of Cakmur analysis
- establish an observational database beyond Cakmur et al and AeroCom
- revisit HTAP dust experiment design (see MS email to AeroCom in Dec)
- eventually come together at AGU Acapulco conference in May 2007
- suggest input for C. Zender for Perrugia conference

List of Observational data to be included in analysis

Al in ocean water

Visibility

IDDI index

Satellite AOD in dust dominated regions (MISR, MODIS, TOMS, DEEPBLUE-MODIS, CALIPSO, Aeronet, Calipso)

Coarse mode satellite derived AOD in dust regions?

Deposition DIRTMAP, Fe, Ca in rain

Surface concentrations Aeroce, Asian network

Refractive index and size in literature

Processes and possible Diagnostics

Dust erosion - wind frequency and speed ; threshold velocities; effective source fluxes; source size distribution

Dust settling - dry removal velocities per size bin;

Wet Dust removal - wet scavenging efficients; vertical distribution; wet deposition of Calcium, dust;

Scattering and absorption - refractive index; AOD; size; absorption


Sink repartitioning among AeroCom models Figure taken from Textor et al., ACP 2006