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MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

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MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany
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Page 1: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

MRV approaches in the BMU Belarus peatland project

Hans Joosten

Greifswald University, Germany

Page 2: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Eastern Europe: famous for its vast and largely undisturbed peatlands...

Rospuda Valley, Poland

Page 3: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Belarus has high proportion of peatlands... fens (green), bogs (red), transitional peatlands

(purple): former extent ~15% of the area

Page 4: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Present area of natural peatlands: 1.5 mio ha

Page 5: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Present area of drained peatlands: 1.5 mio ha (agriculture 72%, forestry 25%, peat extraction 3%)

Page 6: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Drained peatlands are huge emittors of CO2 + N2O

Page 7: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

CO2 emission

Central Europe is peatland emission hot spot

Page 8: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Does rewetting reduce greenhouse gas emissions?

Page 9: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

How much less emissions after rewetting?

Page 10: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

BMU funded rewetting project (2008-2011)

builds on GEF funded rewetting project (42,000 ha)

strong support of Belarusian government:

carbon credits reduction of fires

(radioactivity!)…

Page 11: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

BMU funded rewetting project (2008-2011)

Deliverables: methodology for

GHG assessment standard for

voluntary trade 15,000 ha rewetted

and sustainably managed

local capacity

Page 12: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Measuring directly is complicated, time consuming,

expensive ( € 10,000 /ha/yr) proxy indicators

Page 13: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Mean water level is best predictor of emissions

(meta-analysis of 25 site parameters in W-Europe)

Page 14: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

-10

-5

0

5

10

15

20

25

30

-120 -100 -80 -60 -40 -20 0

mean water level [cm]

t C

O2-

eq∙h

a-1

∙a-1

bogs

fens

CO2 emissions clearly correlate with water levels: they become less with higher water levels

Page 15: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

-100

0

100

200

300

400

500

600

-100 -80 -60 -40 -20 0 20 40 60

mean water level [cm]

kg C

H4∙

ha

-1∙a

-1

-2

0

2

4

6

8

10

12

t C

O2-

eq∙h

a-1

∙a-1

bogs

fens

other

CH4 emissions clearly correlate with water levels: they increase when higher than 20 cm - surface

Page 16: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

-5

5

15

25

35

45

55

65

75

85

95

-100 -80 -60 -40 -20 0 20 40

mean water level [cm]

kg N

20∙h

a-1∙

a-1

-2

4

9

14

19

24

29

t C

O2-

eq∙h

a-1∙

a-1

bogs

fens - unfertilized

fens - fertilized

other

N2O emissions clearly correlate with water levels: they do not occur when higher than 15 cm - surface

Page 17: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

N2O erratic, but lower with higher water levels

Leave N2O emissions out conservative estimate

Page 18: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

-15

-10

-5

0

5

10

15

20

25

30

-100 -80 -60 -40 -20 0

mean water level [cm]

GW

P [

t C

O2-

eq ∙

ha

-1∙a

-1]

By rewetting, greenhouse gas emissions decrease, but less between – 20 cm and 0 cm

Page 19: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Emissions strongly related to water level Vegetation strongly related to water level

Use vegetation as indicator for emissions!

Page 20: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

In an environmental gradient some plant species occur together; others exclude each other.

Species groups (and their absence!) indicate site conditions much sharper than individual plant species: “vegetation forms”.

site factor gradient

species groups

site factor classes

subunits 1

1 2

2

3 4 5

1 2

Page 21: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Vegetation types calibrated for GHG emissions:

GESTs: Greenhouse gas Emission Site Types

Some examples: 2-, 2+, 2~ (3+/2+) 3+ 4+/3+ 4+ 5+ 6+MOD. MOIST FORBS & MEADOWS

MOIST FORBS & MEADOWS

VERY MOIST MEADOWS

VERY MOIST MEADOWS, FORBS & TALL REEDS

WET TALL SEDGE MARSHES

FLOODED TALL AND SHORT REEDS

0 1.5(1.3 – 2)

3.5(2.5 – 6)

3 7(5.0 – 9.5)

1(0.3 – 1.7)

24 15 13(8.5 – 16.5)

8 0 0

24 16.5 16.5 11 7 1

Water level

Vegetation

CH4

CO2

GWP

Page 22: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Vegetation type Typical/differentiating species WL class

CH4 CO2 GWP

Sphagnum-Carex limosa-marsh

Sphagnum recurvum agg., Carex limosa, Scheuchzeria

5+ 12.5<0

(±0)12.5

Sphagnum-Carex-Eriophorum-marsh

Sph. recurvum agg., Carex nigra, C. curta, Eriophorum angustifolium

Drepanocladus-Carex-marsh Drepanocladus div. spec., Carex diandra, Carex rostr., Carex limosa - Carex dominated

Scorpidium-Eleocharis-marsh Scorpidium, Eleocharis quinqueflora - Carex (shunt) dominated

Sphagnum-Juncus effusus-marsh

Juncus effusus, Sphagnum recurvum agg.

Equisetum-reeds Equisetum fluviatile

Scorpidium-Cladium-reeds Cladium, Scorpidium

Sphagnum-Phragmites-reeds Phragmites, Solanum dulcamara

5+ 10<0 / ±0

10

Solano-Phragmitetum Scorpidium, Eleocharis quinqueflora - Phragmites + Solanum without Urtica-gr.

Rorippa-Typha-Phragmites-reeds

Typha latifolia, Phragmites, Rorippa aquatica, Lemna minor

Bidens-Glyceria-reeds Glyceria maxima, Berula erecta, Bidens tripartita, B. cernua

Red or green Sphagnum lawn (optimal)

Sph. magellanicum, Sph. rubellum, Sph. fuscum, Sph. recurvum agg.

5+ 5 -2 3

Green Sphagnum hollow Sph. cuspidatum, Scheuchzeria 5+ 10 -2 8

Polytrichum-lawn Polytrichum commune 5+ 2 <0 2

GESTs with indicator species groups

Each GEST with typical species

Each GEST with typical GHG emissions

Page 23: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Benefits of vegetation as a GHG proxy:

• reflects long-term water levels

provides indication on GHG fluxes per yr

• is controlled by factors that control GHG emissions (water, nutrients, acidity, land use…)

• is responsible for GHG emissions via its own organic matter (root exudates!)

• may provide bypasses for increased CH4 via aerenchyma (“shunt species”)

• allows rapid and fine-scaled mapping Vegetation is a more comprehensive proxy

than water level!

Page 24: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Disadvantages of vegetation as a proxy:

• slow reaction on environmental changes:

~3 years before change in water level is reflected in vegetation (negative effect faster)

• needs to be calibrated for different climatic and phytogeographical conditions

Page 25: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Vegetation forms: developed for NE Germany test of correlations in Belarusian peatlands

Page 26: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

BMU Belarus project:

• Calibration of NE German model for Belarus:– relation vegetation ↔ water level (CIM position)– relation water level ↔ GHG emissions (CIM position)

• Completion of model (“gap filling”)• Consistency test with international literature• Development of conservative approaches

• Selection of rewetting sites• Mapping of vegetation before rewetting

(assessment of emission baseline )• Monitor water level and vegetation development

(ex-post emission monitoring)

Page 27: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Major gap: abandoned peat extraction sites

Page 28: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Perspectives of GEST-approach:

• Ex-ante baseline assessment with ex-post evaluation

• Fine-scaled mapping

• Remote sensing monitoring

• Continuous refinement with progressing GHG research

• Addition of new modules (forest, transient dynamics)

• Simple, cheap, reliable…

Page 29: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

Developed with

• Jürgen Augustin (ZALF)• John Couwenberg (DUENE)• Dierk Michaelis (Uni Greifswald)• Merten Minke (APB / CIM)• Annett Thiele (APB/ CIM)• And many more…

Page 30: MRV approaches in the BMU Belarus peatland project Hans Joosten Greifswald University, Germany.

info: [email protected]

GESTs!


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