fuss s 20150709_1730_upmc_jussieu_-_amphi_34

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The need for and limits to negative emissions Sabine Fuss & Pete Smith On behalf of 30+ collaborators from many institutes and GCP Mercator Research Institute on Global Commons and Climate Change, Berlin & Institute of Biological & Environmental Sciences, University of Aberdeen Our Common Future under Climate Change Conference, July 7-10 2015, Paris

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Page 1: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

The need for and limits to

negative emissions

Sabine Fuss & Pete Smith On behalf of 30+ collaborators from many institutes and GCP

Mercator Research Institute on Global Commons and Climate Change, Berlin

&

Institute of Biological & Environmental Sciences, University of Aberdeen

Our Common Future under Climate Change Conference, July 7-10 2015, Paris

Page 2: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

The need for negative emissions

• IPCC AR5: Achieving 2C is

still possible, but it entails

huge contributions from

bioenergy - in most scenarios

combined with Carbon

Capture & Storage to go

“negative“.

• BECCS need 2-10 Gt

CO2/yr in 2050 5–25% of

2010 CO2 emissions

• Current global mean removal

of CO2 by ocean and land

sinks is 9.2 ± 1.8 Gt CO2 and

10.3 ± 2.9 Gt CO2, resp.

2

Data: CDIAC/GCP/IPCC/Fuss et al 2014

Page 3: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

The need for negative emissions cont’d

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Based on Figure TS.17, IPCC, WG3, AR5, 2014.

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How can we go (net) negative?

The technology most widely used in climate stabilization

scenarios of AR5 is Bioenergy combined with CCS (BECCS).

4

Source: Applied Energy Handbook, Wiley.

Other negative emissions options:

• Afforestation (also in AR5, see next slide)

• Increases in soil carbon storage (biochar…)

• Direct air capture (coming up)

• Enhanced weathering (coming up)

Land-use and management changes:

• Saturation of CO2 removal over time

• Sequestration reversible (terrestrial carbon stocks inherently vulnerable to disturbance)

Geo-engineering options:

• Quicker and cheaper to ramp up

• Embody a much larger scale of mostly unknown risks

• Not able to deal with other consequences of increased CO2 concentrations such as ocean acidification

Page 5: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

Afforestation / Reforestation (AR)

Humpenöder et al. (2014)

Picture: http://en.wikipedia.org/wiki/File:Forest_ialoveni.jpg

Page 6: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

Summary of

the carbon

cycle impacts

of different

NETs

Smith et al. (2015)

Page 7: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

Factors potentially enhancing or limiting the global

capacity for NETs

Smith et al. (2015)

Page 8: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

Impact of NETs on

land, water,

nutrients, albedo,

energy and cost –

all expressed on a

per-t-C-eq. basis

Smith et al. (2015)

Page 9: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

NETs consistent with 2C target at 3.6 GtC-eq./yr in

2100 or mean (max) implementation

NET Global C

removal

(GtCeq./yr

in 2100)

Mean (max),

land

requirement

(Mha in

2100)

Estimated

energy

requirement

(EJ/yr in

2100)

Mean (max),

water

requirement

(km3/yr in

2100)

Nutrient

impact

(ktN/yr

in 2100)

Albedo

impact in

2100

Investment

needs

(BECCS

for

electricity /

BECCS for

biofuel;

B$/yr in

2050)

BECCS 3.6 310 -170 1910 Variable Variable 138 / 123

DAC 3.6 Very low

(unless solar

PV used for

energy)

170 10-330 None None >> BECCS

EW 0.2 (1.0) 2 (10) 46 0.3 (1.5) None None >BECCS

AR 1.1 (3.3) 320 (970) Very low 370 (1040) 2.2

(16.8)

Negative;

or

reduced

GHG

benefit

where not

negative

<<BECCS

Smith et al. (2015)

Page 10: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

Impact / limit summary for NETS

Main limits:

• DAC – cost, energy

• EW – vast areas – logistics

• Afforestation – albedo, water, competition for land

• BE/BECCS – water, competition for land Smith et al. (2015)

Page 11: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

Conclusions

• Negative emissions of 3.6 GtC-eq./yr in 2100 are possible with BECCS and DAC

• EW and AR can provide less negative emissions than this in 2100

• All NETs have limits / downsides and none is a magic bullet

• Need more R&D and pilot projects – then to see if technology is scalable Most probably will need to look into other NETs to complement BECCS and AR, e.g. DAC, EW

• Improve governance to ensure sustainable implementation of NETs

• Safe storage needed, in addition to storage from fossil CCS.

• An over-reliance on NETs in the future, if used as a means to allow continued use of fossil fuels in the present, is extremely risky since our ability to stabilise the climate at <2C declines as cumulative emissions increase (Kriegler et al., 2014, Luderer et al., 2012)

• A failure of NETs to deliver expected mitigation in the future, due to any combination of biophysical and economic limits examined here, leaves us with no “Plan B”

• “Plan A” must be to reduce GHG emissions aggressively now

Smith et al. (2015)

Page 12: Fuss s 20150709_1730_upmc_jussieu_-_amphi_34

Contact

Please also visit http://www.cger.nies.go.jp/gcp/magnet to learn more about GCP‘s research initiative „Managing Global Negative Emissions Technologies“

Sabine Fuss Mercator Research Institute on

Global Commons and Climate Change gGmbH

Torgauer Str. 12–15 | 10829 Berlin | Germany

tel +49 (0) 30 338 55 37 - 101

mail [email protected]

web www.mcc-berlin.net

Pete Smith Institute of Biological and Environmental Sciences, University of Aberdeen

23 St Machar Drive, Aberdeen, AB24 3UU, UK

tel +44 (0)1224 272702

mail [email protected]

web www.abdn.ac.uk/ibes/

people/profiles/pete.smith

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Backup Material

Dienstag, 25. August 2015 13

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The Extent of BECCS Use in IPCC AR5

Scenarios

• 101 of the 116 430-480ppm scenarios rely on BECCS.

• About 67% of these have a BECCS share in primary energy exceeding 20% in 2100.

• BUT: many uncertainties remain. Can we really bet on BECCS?

Source: Fuss et al. (2014), Nature Climate

Change.