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TEAM Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore Torsten Sachs 1,2 , Pia Gottschalk 1 , Christian Wille 1 , Franziska Koebsch 3 1 GFZ - German Research Centre for Geosciences, Potsdam, Germany 2 Technische Universität Braunschweig, Germany 3 Landscape Ecology, University of Rostock, Germany

Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

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Page 1: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

TEAM

Treibhausgasdynamik & Klimawirksamkeit

wiedervernässter Moore

Torsten Sachs1,2, Pia Gottschalk1, Christian Wille1, Franziska Koebsch31GFZ - German Research Centre for Geosciences, Potsdam, Germany2Technische Universität Braunschweig, Germany3Landscape Ecology, University of Rostock, Germany

Page 2: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 225. September 2018

Wetlands as carbon sink…

• Wetlands can be found in 175 countries• Cover only 3% of the land surface but store >500 Gt C in peat• Twice as much C as in entire forest biomass

Slide: Modified from Joosten

Page 3: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 325. September 2018

… or source

• Drained peatlands on 0.4% of the land surface emit 5 % of the anthropogenic CO2 worldwide: Nr. 1. Indonesia, Nr. 2. EU, ….

• In Germany: ~ 5 % of national emissions• In Mecklenburg-Vorpommern: ~ 30 % of state-wide emissions

Slide: Modified from Joosten

Page 4: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 425. September 2018

Agriculture on peatlands

• Peatlands used for agriculture in Germany emit almost twice as much CO2 as the 7th dirtiest power plant in the world

Slide: Modified from Joosten

Page 5: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 525. September 2018

Foto: Sabine Wichmann

• German peatland agriculture causes 3,6 Billion € in climate damage per year…

… with the help of 300 Million € inEU-subsidies

Agriculture on peatlands

Slide: Modified from Joosten

Page 6: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 625. September 2018

The emerging role…

Page 7: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 725. September 2018

Solution: re-wetting?

• Objectives: Protecting… … biodiversity … climate … soils … water

Page 8: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 825. September 2018

• Fen in a river valley mire system, drainage began early 1700s, re-wetting 2000• Peat depth up to 10 m, MAT 8.7 °C, mean annual precipitation: 584 mm

Polder Zarnekow, Peenetal (DE-Zrk)

Map: Bennet Juhls

Page 9: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 925. September 2018

Rewetted peatland study sites

Polder Zarnekow

Page 10: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1025. September 2018

Degradation classes (Schumann & Joosten)

Source: Timmermann et al. 2009, modified

Page 11: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1125. September 2018

Polder Zarnekow 2015

Picture: 12.11.2015

Page 12: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1225. September 2018

Polder Zarnekow August 2018

Page 13: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1325. September 2018

Polder Zarnekow throughout the years

2013 2014 2015

2016 2017 2018

Page 14: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1425. September 2018

Note the water level fluctuations! (not obviously related to precipitation…)

Weather at Zarnekow

Page 15: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1525. September 2018

• All years were warmer than the long-term average:

• 2017 was much wetter than average,2014, 2016, and 2018 much drier:

Meteorology and climate at Zarnekow

Page 16: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1625. September 2018

• 2D wind speed & direction Gill WindSonic• 3D sonic anemometer Gill HS-50• Closed path H2O/CO2/CH4 Los Gatos FGGA-EP• Enclosed H2O/CO2 LI-7200• Open path CH4 LI-7700• Temperature / humidity Vaisala HMP155• Pressure Young Model 61302V• 4 component radiation Kipp & Zonen CNR4• PAR LI-190SL• Precipitation Young 52203 tipping bucket• Water temperatures• Sediment temperatures UMS Th3• Heat flux plates Hukseflux HFP01SC• O2 sensors

Instrumentation

Page 17: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1725. September 2018

Footprint – what do we “see”?

• Two main surface types Open water Emergent vegetation (Typha latifolia)

• Surface type fractions based on Göckede et al. (2004)• Source area based on Kormann & Meixner (2001)• Footprint climatology based on Chen et al. (2011)

• Peak contribution 18 m from the tower mainly from the open water area

• Open water covered on average 62.5% of source area

Franz et al. (2016) Biogeosciences

Page 18: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1825. September 2018

Large CO2 loss July/ Aug 2018 vs. damped CO2 loss in wet 2017

Significant CO2 uptake in 2018 compared to previous years

Monthly ecosystem respiration (CO2 loss)

Page 19: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 1925. September 2018

• Much more photosynthesis in 2018, followed by dry year 2016 Does temporal drying enhance vegetation growth and thus CO2 uptake?

• Respiration also clearly increased in dry years 2016/2018, lowest in wet 2017 High water level supresses respiration (known, that‘s why we re-wet)

Annual cumulative photosynthesis & respiration

Page 20: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 2025. September 2018

Annual total fluxes

• Unclear trends: Slowly decreasing CH4 source? Transition from CO2 source to sink?

Page 21: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 2125. September 2018

Summary and to do list

• Substantial and slowly decreasing CH4 and CO2 source First CO2 sink year in 2018

• Increasing respiration, unclear trend in photosynthesis May depend on re-analysis of suspicious 2015 data Dry years appear to enhance photosynthesis

• Climate impact dominated by CH4 release

• To do: 2015 data possibly biased towards respiration re-analysis to verify/falsify unusal Sept flux

Involve hydrologists (lateral transport) (continued) biogeochemical and micro-biological

investigations - why are CH4 oxidizers missing? Investigate spatial representativeness

based on aircraft and UAV measurements

Page 22: Treibhausgasdynamik & Klimawirksamkeit wiedervernässter Moore

[email protected] 2225. September 2018

Thank you for your attention!