Title: Wolfgang Sch
1Wolfgang Schöpp
The RAINS model Ecosystems impacts
2Modelling ecosystems impactsApproach
- Computed deposition of SN compared with critical
loads estimates - For acidification and eutrophication
- For different ecosystem types
- For individual grids or on country-bases
- For ex-post evaluation or for setting targets for
optimization - Evaluation of dynamic acidification processes
- Ex-post evaluation
- Comparison of computed ozone concentrations with
critical levels - For forest trees
- Flux approach for crops not (yet) implemented in
RAINS, performed in context of benefit assessment
3Reducing deposition below the critical loadsAn
example for a French ecosystem
Slide prepared by Les White
4Reducing deposition below the critical loadsAn
example for a Spanish ecosystem
Slide prepared by Les White
Slide prepared by Les White
5Excess of critical loads at forests2000
Percentage of forest areawith acid deposition
above critical loads, using ecosystem-specific
deposition, Average of calculations for 1997,
1999, 2000 2003 meteorologies
6Percent of forest area with acid deposition
above critical loads
7Excess of critical loads at semi-natural
ecosystems including HABITAT areas, 2000
Percentage of area of semi-natural
ecosystemswith acid deposition above critical
loads, using ecosystem-specific deposition.
Average of calculations for 1997, 1999, 2000
2003 meteorologies
8Excess of critical loads of freshwater bodies2000
Percentage of catchments area with acid
deposition above critical loads, using
ecosystem-specific deposition. Average of
calculations for 1997, 1999, 2000 2003
meteorologies
9Excess of critical loads for eutrophication 2000
Percentage of ecosystems area with nitrogen
deposition above critical loads, using
grid-average deposition. Average of calculations
for 1997, 1999, 2000 2003 meteorologies
10Use of dynamic soil acidification models
- Critical loads reflect steady-state conditions
- Dynamic aspects important
- Recent progress in dynamic modelling for
acidification, but not for eutrophication - Are models and data good enough to be used?
11Use of dynamic modelling in RAINS
- No dynamic estimates available for many
ecosystems in Europe - For the ecosystems with data available, ex-post
evaluation for emission control scenarios
possible - Use as optimization targets problematic due to
missing estimates - Historic base cation deposition important, but
not modelled.
12Modelling of deposition
- Experiments with EMEP Eulerian model established
general linearity - However, co-deposition of S/NH3 identified
- Small effect on grid-average, thus ignored for
first approach - Importance for ecosystem-specific deposition
estimates will be further evaluated.
13Response of total S depositiondue to changes in
UK SO2 emissions
- Linear response of S deposition
- over full range of SO2 emissions
- Minor impacts of other emissions
14Response of total S depositiondue to changes in
UK NH3 emissions
- S deposition depends on NH3 levels
- Especially at high NH3 levels
- But limited magnitude!
15Response of total S depositiondue to changes in
all UK emissions
- S deposition responds linearly
- if all other emissions are reduced
simultaneously
16Conclusions
- Use of accumulated excess deposition for
different ecosystems in Europe as a summary
measure - Results from dynamic models can be used as an
ex-post analysis or for setting targets for the
RAINS optimization - Deposition of pollutants can be described with
linear source-receptor relationships