potential impact of small scale supersonic …folie 1 volker grewe, dlr-oberpfaffenhofen, hisac...
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Folie 1Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Potential Impact of Small Scale Supersonic Transport Aircraft on the Atmosphere: Climate and Ozone Layer
Volker Grewe, DLR-Oberpfaffenhofen
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Folie 2Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Outline
• The physical basis of climate change
• The impact of air traffic on climate
• Assessments of supersonic transport: HSCT, IPCC, SCENIC
• Impact of small scale supersonic transport aircraft (S4TA)
• Conclusions
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Folie 3Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
The physical basis of climate change: IPCCScientific intergovernmental body set up by UN Consists of governments (review) and scientists (author+review)Aims at providing decision-makers and others interested in climate changewith an objective source of information about climate changeRegular reports 1990, 1995, 2001, 2007: ~550 authors ~400 reviewer per WG)Special reports (e.g. on air traffic 1999)3 working groups
FAQs
Detailed report
Technical summary
Summary for policymakers
The PhysicalScience Basis
FAQs
Detailed report
Technical summary
Summary for policymakers
Impacts,Adaptation& Vulnerability
FAQs
Detailed report
Technical summary
Summary for policymakers
Mitigation of Climate Change
2 stage expert & governmentreview
line-by-lineapproval
}}
www.ipcc.ch
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Folie 4Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Observed changes in global mean surface temperature, global mean sea level and Northern Hemisphere snow cover
IPCC, 2007, SPM
The 12 warmest years of the instrumental period:1998, 2005, 2003, 2002, 2004, 2006, 2001, 1997, 1995, 1999, 1990, 2000
Warminghappens !
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Folie 5Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
How sure are we that a warming happens?
IPCC, 2007, SPM
"very likely"
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Folie 6Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
ObservationsNatural Variability+ Anthropogenic
Impacts IPCC, 2007, SPM
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Folie 7Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Main results - Physical basis
Warming happens !GHGs increaseMost of the warming very likely caused by increase in GHGsProjected warming in 2100 compared to
pre-industrial 2000constant concentration 2000: 1.1°C 0.6°CA1B = rapid growth, global, new techs, fuel mix 3.3°C 2.8°C A2 = heterogeneous world, local approaches 4.1°C 3.6°CB2 = information economy, sustainable 2.9°C 2.4°CA1FI = A1, but only fossil fuels 4.5°C 4.0°C
IPCC, 2007, SPM
1=Global
2=Regional
A=Economic B=Ecological
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Folie 8Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Evolution of air traffic 1940 to 2005
Lee et al., 2009
More than linear increasein transport demand
Crises reduce air trafficfor a short time period.
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Folie 9Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Climate impact of current air traffic (2005)
Lee et al., 2009
Main contributors:CO2NOxContrails
3.5-5.0% of warmingattributed to air traffic
ACARE, 2008The findings of the IPCCpoint very clearly to theneed to do something butthere are areas of detail where more understandingis needed.
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Folie 10Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Supersonic transport: Fleets (Large/Small Aircraft) regarded in previous projects:
notcalculated
1-4<<2.41050015,17,192015BoeingNASA2002
DassaultAleniaSukhoi
Airbus
Boeing
Boeing
Concept
0.1
40
100
notcalculated
Climateimpact(RF)
[mW/m2]
0.4
62
137
82
Fuel
[109
kg/a]
1.6-1.8825015-162050HISAC2009
2.025050016-192050SCENIC2007
2.4309100017-202050IPCC 1999
2.4~30050018-212015HSRP1999
Speed
[Mach]
PAXNumberAircraft
MeanCruise Altitude
[km]
Timeof fullfleet
Project
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Folie 11Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
×3 !
Climate impact of large-scale supersonic transport
- Main contributors: H2O and CO2
- Large-Scale Supersonic Transport Aircrafthave a 6 time larger climate impact.
- Non-CO2 effect ranges from 5 (SCENIC) to 10 (IPCC99)
IPCC 99 SCENIC/ECATS
Grewe and Stenke, 2008
* RF/dT values to bemultiplied by 3
x6!
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Folie 12Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Do supersonics avoid contrails?
Substitution Effect
No! Just a shift to the tropics! Stenke et al., 2008
Difference in flown kilometers
Substitution of subsonic large scale aircaft by supersonics:
Contrail coverage
SCENIC
replacedsubsonics
supersonics
replacedsubsonics= contrail avoidance
supersonics= contrails in the tropics
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Folie 13Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
20 km
15 km
10 km
5 km
Generell Circulation and Air Traffic Emissions
Residence time of speciesemitted by supersonictransport increases with
• increasing altitude• decreasing latitude
Residence time of a water vapour emission
Troposphere
Grewe and Stenke, 2008
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Folie 14Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
SCENIC: Impact on the ozone layer [ppbv]
Considerableozone depletionby the regardedSCENIC fleet
SCENIC: ~0.3 %
CFCs: ~3%
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Folie 15Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Description of HISAC S4TA
Low boom
Long range
Low weight
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Folie 16Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Methodology:
• 4 flight trajectories for 4 different geographical regions from Pole to Tropics
• Calculation of emissions along the flight trajectorieswith 2 combustion chamber technologies
• Calculation of concentration changes
• Calculation of climate impact
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Folie 17Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
HISAC fleet emissions
Fuel consumption NO2 emission EINOx
4.662.0-54-64SCENIC
10.60.441.77654.0C
11.90.3971.58952.6B
11.80.3961.58450.6A
EINOx(LPP)[g(NO2)/kg(fuel)]
Mean fleet fuelConsumption [Tg]
Mean fuel Consumption [t]
Mean flight altitude [kft]
Config
Theoretical
Based on experimental data
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Folie 18Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Atmospheric impact of a HISAC fleet
Water vapour [ppbv] Ozone [pptv]
HISAC
SCENICscaled toHISAC fuelconsumption
Non-CO2effects are a factor of 5-10
smaller than for the SCENIC fleet
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Folie 19Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Climate impact
50% reduction of the climate impactby reducing non-CO2 effects.
= impact of lower cruise altitudewrt SCENIC
CO2
-2
-1
0
1
2
3
4
5
6
7
War
min
g Po
tent
ial
HISAC
SCENIC
H2O
O3
Factor ~5
warming(non-CO2):warming(CO2)
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Folie 20Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Aircraft specifications impact on climate
Differences smallConfiguration A has minimal climate impactUncertainty range based on Monte-Carlo Simulation for uncertainties in atmospheric processes (residence time, radiation, climate sensitivity)
Ozone layer:Estimated depletion:CFCs: ~ 3%SCENIC: ~ 0.3 %HISAC: ~ 0.0005%
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Folie 21Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Direct intercomparison of sub- and supersonictransport
At low cruise altitudes a factor of 3 is achievable= 2 times more climate impact than respective subsonic aircraft
0 2 4 6 8 10 12 14 16
HISAC
Subsonic
SCENIC
Subsonic
IPCC
Subsonic
CO2
Non-CO2
7 mW/m2
7 mW/m2
~0.04 mW/m2
~14
~6
~3±0.4
Factor RF(Supersonic) : RF(subsonic)
Subsonics scaled to 1 Cruise altitude
17-20 km
16-19 km
15-16 km
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Folie 22Volker Grewe, DLR-Oberpfaffenhofen, HISAC Final Event Paris, 19 June 2009
Summary
Climate impact and ozone depletion of a fleet of Small Scale SupersonicAircraft are considerably smaller than for supersonic fleets consideredpreviously for 3 reasons (factor 400-1000):
Smaller fleet size (Factor 2-4)Smaller aircraft = less fuel consumption (Factor ~40) Lower flight altitude = smaller Non-CO2 effects (Factor ~5)
Climate impact and ozone depletion larger than for respective subsonic aircraft.
No explicit results available for a direct intercomparison of subsonic and supersonics ⇒ Estimates for the difference: Factor 3±0.4