Title: Recent developments in CHIMERE
1Recent developments in CHIMERE
2Accuracy and Realismfor research and operational
applications
Accuracy
3Code Structure
4Building a new application from scratch
- Download all source codes and files
- Make model domain files. This can be complicated
if domain outside Europe (atmosphere-biosphere
interface). - Build emission files
- Build meteorological files (MM5 or other)
- Optimize by testing options
5Model domain files
- Europe ? not russia, not Scandinavia
- Use the prepdomains interface as a first attempt.
Then possibly replace the biogenic emissions,
landuse
- Outside Europe
- Construct landuse independently from GLCF or
anything else - Construct biogenic emission potentials or provide
a file with hourly biogenic emissions in the
required format. - Change Bcalbio.f for growing season if necessary,
change DEPO_PARS if necessary
6Dealing with meteorology
- Using MM5
- Now MM5 interface quite general, MM5 domain must
include CHIMERE domain - Changes in MM5 V3.6 recommended (V3.7 not
tested) see website. - Define MM5 domain, compute TERRAIN, run MM5 and
provide a COORD_MM5ltdomgt file in meteo dir
(utility program).
- Using another model
- Provide an interface giving mandatory and
possibly optional variables interpolated
horizontaly to the CHIMERE grid, a METINFOS file
for options. - Add lines in the top script to call this interface
7Dealing with anthropic emissions
- Use the existing interface and build ASCII
monthly emission data files with exactly the same
format as specified for 3 day types, for the
MELCHIOR primary species (file ANTHROPIC).
Example EMEP interface soon available on website. - Provide an interface that gives hourly MELCHIOR
species emissions (VOC aggregation necessary, no
standard procedure). Change the calling
sequence in the top script.
8Optimization
- CHIMERE, like any other CTM, is NOT a plug and
play tool. - Test various options recalculation of PBL
height, u, cloud attenuation using RH or CLW. - Care must be taken for dust emission, due to high
sensitivity to soil water. Testing needed, first
without dust emission, then with and tuning of
constants in Bcalbio.f may be necessary for some
regions. - Use (or not) the emission layer option for
comparing with more traffic stations .
9Bio
- 1997 5 box model for Paris
- 1998 3 layers, 6km grid for Paris
- 1999 3 layers, continental scale
- 2000 First forecasts over Europe
- 2002 Aerosols
- 2003 More physics, 8 layers, interface AVNMM5
- 2004 Erosion, saharan dust boundary conditions
with GOCART/NASA - 2005 Aerosol/GP merged, Sea salt, improved dry
deposition
10Recent developments
- Merging of aerosol and gas phase versions
- Dry deposition from Emberson et al. (2000)
- Aerosol changes, species change, dust emission,
sea salt in test. - Meteorological interface, minor changes/options
11Dry deposition
- Use of the Emberson et al (2000) surface
resistance model, the multiplicative moldel for
O3 surface conductance in src/Bdepvel.f
max
Takes into account temperature, radiation,
phenology, growth, relative humidity, soil water
potentially.
12Aerosols
- V200501G New species list ASOA and BSOA
grouped, DUST added, SALT for inert/active salt
versions in test, not fully recommended yet
- V200410A 1.Boundary conditions. 2.Dust biogenic
emissions from local erosion, resuspension.
13Aerosol Boundary Conditions
From GOCART NASA model
PM10 at the spanishZarra EMEP Station
14Dust local emission
Adapted from White (1979), Marticorena and
Bergametti (1995)
- Depends on the saltation friction velocity us,
the threshold velocity (depends on soil water).
Does not depend on land use. - Highly sensitive to soil water, needs testing
PM10 Increase for Summer 2003
15Resuspension
Adapted from Loosmore (2003)
Bulk formula. Depends on soil water, friction
velosity. Also highly sensitive to SW.
SUMMER Rural S Rural N All
Base Model 0.53 0.51 0.56
With bound. Dust 0.66 0.53 0.61
With erosion 0.67 0.56 0.62
With resuspension 0.66 0.64 0.68
16Meteorology
- V200501G MM5 interface problems fixed (now
general interface). - Problems with recalculation of u, PBL height now
fixed. - Urban corrections, in compensation of the lack of
anthropogenic heat fluxes. Minimal PBL over urban
area (150m for Paris), additional flux (50W/m2).
Work to be done in MM5 itself. - Bad UHI in MM5 Changes to V3.6 proposed by Liu
in MM5.