Baseline time accounting–reply to the letter to the
editor of Martin [Int J Life Cycle Assess (2013) 18(7):1279]
After becoming aware of a letter
to the editor from Martin (2013), we realize there is a need for further
elaboration of the baseline time accounting method laid out in Kløverpris and Mueller
(2013). In the following,we address Martin's comments. Martin states that our
method “does not eliminate the need to choose a timeframe.” This is correct and
inherent to any life cycle assessment (LCA) when it comes to the use of global warming
potentials (GWPs). Later, Martin states that we assert that our “approach
removes the need to consider arbitrary timeframes.” We are puzzled by this
statement since Sect. 2.3 of our paper explicitly acknowledges that the use of the
common 100-year GWP accounting period in LCA isindeed arbitrary. While we cannot
avoid this circumstance, our method does eliminate the need to consider an
arbitrary production period for biofuels (under the conditions described). We
will later get back to the fundamental difference between the GWP accounting
period and the assumed biofuels production period since the missing distinction
between these two time perspectives appears to be the primary basis of Martin's
critique. Martin states that the value of our insights “is diminished bythe
failure to include a full consideration of the importance of the timeframe of
the analysis .” While we (and the three reviewers) did not find it relevant to
include results other than GWP100 in our paper, the baseline time accounting
concept is not restricted to this metric. To accommodate Martin, Table 1 shows
results for GWP20 and (the more unusual) GWP30.1 As shown in the table, the applied
GWP accounting period is certainly of significance for the type of indirect
land use change (ILUC) called accelerated expansion. Meanwhile, the sensitivity
to the choice of GWP accounting period is not unique as indicated by the GWPs
for methane, also included in Table 1. For the type of ILUC called delayed
reversion, the GWP accounting period is without significance. We acknowledge that
this is due to the simplified assumption of constant carbon sequestration over
the GWP accounting period. In reality, there will be some sensitivity to the
choice of GWP accounting period for delayed reversion but not to the same
extent as for accelerated expansion. For additional discussion, we refer to
Sect. 4.1.2 in Electronic supplementary material 1 of Kløverpris and Mueller
(2013), particularly. Martin states that “The baseline time accounting approach
uses a 100-year timeframe,” but, as mentioned above, there is no conceptual or
methodological restriction on the chosen GWP accounting period. More correctly
stated, baseline time accounting converts a time shift in land use emissions
from a single batch of biofuels into an ILUC factor that is consistent with the
GWP concept, and the results presented by Kløverpris and Mueller (2013) are
based on a GWP accounting period of 100 years. The chosen GWP accounting period
ensures consistency with the common global warming metric used for greenhouse gas
(GHG) emissions. Since the ILUC factor is meant to be added to the GHG
emissions from the biofuels supply chain, consistency between addends is
necessary. Martin states that “It should come as no great surprise that changing
the denominator of a fraction from 30 to 100 reduces that number by 70 %.” While
this is universally true, it is not a proper way to explain the difference
between our results (based on a 100-year GWP accounting period) and theILUC
factors obtained with the 30-year annualization method. The key here is the
distinction between the biofuels productionperiod (ormore generally, the
temporal scope of an LCA) and the GWP accounting period applied for radiative
phenomena (be it GHG emissions, time shifts in land conversion, albedo change,
or something else). In many LCAs, production period assumptions are not of high
importance mainly because GHG emissions occur approximately at the same time.
For instance, the assessment of the climate impact of replacing a plastic
container with a metal container does not require elaborate considerations
about production periods because these would be relatively short. Still, the
GHG emissions from the two life cycles would typically be measured by
theirGWP100. In a slightly more complex example, consider the climate impact of
driving a car and the contribution from the steel in the car. In this case, you
would typically distribute the steel emissions over the entire service provided
by the car, i.e., the total numbers of kilometers driven over its lifespan, say
15 years. Still, theGHG emissionswould typically be measured by their GWP100.
As for the ILUC analyses by Searchinger et al. (2008) and Hertel et al. (2010),
they chose to look at 30 years of biofuels production and then distributed land
use emissions from an assumed one-time land conversion over the volume of
biofuels produced during those 30 years. Still, the resulting ILUC factors were
derived with the purpose of adding them to other GHG emissions from corn
ethanol, typically measured by their GWP100. The key point here is that there is
a fundamental difference between temporal considerations regarding lifespan or
production periods and the GWP accounting period applied for radiative
phenomena in an LCA. One of the main reasons is that an LCA typically considers
the longterm implications of the changes studied within a given temporal scope.
For the same reason, it is incorrect to assume that an ILUC factor derived with
the baseline time accounting method and based on a 30 year GWP accounting
period would be “consistent” with the Searchinger and Hertel analyses just because
they assume a 30-year production period. The only logical justification for
deriving an ILUC factor with the baseline time accounting method based on a
30-year GWP accounting period would be to use this ILUC factor in an LCA with GWP30
as the common metric for all biofuels emissions (and replaced fossil fuel
emissions, for that sake). We are not aware of any such LCAs.
Martin states that we justify our
“decision to use the global warming potential based on a 100 -year timeframe (GWP100)”
with “consistency between the ILUC factor estimation and the GWP concept .”
However, our paper repeatedly states that our method is based on consistency
with the GWP approach (regardless of the chosen accounting period), and that we
chose to present results as GWP100 because that seemed most relevant. Martin
states that “100 years is certainly not the only timeframe that is routinely
used in GWP analyses.” While the Intergovernmental Planet on Climate Change
publishes GWP values for GHGs with accounting periods of 20, 100, and 500
years, we are not aware of any major biofuels legislation that does not apply
the GWP100 metric for GHG emissions. This goes for the US Renewable Fuel
Standard, EU's Renewable Energy Directive, and California's Low Carbon Fuel
Standard. It also goes for the GREET Model (Argonne National Laboratory 2013),
the Greenhouse Gas Protocol (WRI/WBCSD 2011), PAS 2050 (BSI 2011), and many
other tools and standards.We have however, as already mentioned, presented results
in Table 1 for GWP20 and GWP30 to allow for analyses with short GWP accounting periods.
It is obviously important to keep in mind that such analyses ignore long-term
effects. In summary, it is necessary to ensure consistency between ILUC
emissions and other GHG emissions in an LCA. Hence, it is vital to apply consistent
GWP accounting periods for radiative phenomena and to distinguish this time
perspective from the biofuels production period assumed in the studies by Searchinger
et al. (2008) and Hertel et al. (2010). With baseline time accounting, production
period considerations become unnecessary under the conditions described in our
paper. Meanwhile, the choice of a general GWP accounting period remains
inherent to any LCA when it comes to global warming potentials.
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