4 research outputs found
Mode, Load, And Specific Climate Impact from Passenger Trips
The
climate impact from a long-distance trip can easily vary by
a factor of 10 per passenger depending on mode choice, vehicle efficiency,
and occupancy. In this paper we compare the <i>specific climate
impact</i> of long-distance car travel with coach, train, or
air trips. We account for both, CO<sub>2</sub> emissions and short-lived
climate forcers. This particularly affects the ranking of aircraft’s
climate impact relative to other modes. We calculate the specific
impact for the Global Warming Potential and the Global Temperature
Change Potential, considering time horizons between 20 and 100 years,
and compare with results accounting only for CO<sub>2</sub> emissions.
The car’s fuel efficiency and occupancy are central whether
the impact from a trip is as high as from air travel or as low as
from train travel. These results can be used for carbon-offsetting
schemes, mode choice and transportation planning for climate mitigation
Specific Climate Impact of Passenger and Freight Transport
Emissions of short-lived species contribute significantly to the climate impact of transportation. The magnitude of the effects varies over time for each transport mode. This paper compares first the absolute climate impacts of current passenger and freight transportation. Second, the impacts are normalized with the transport work performed and modes are compared. Calculations are performed for the integrated radiative forcing and mean temperature change, for different time horizons and various measures of transport work. An unambiguous ranking of the specific climate impact can be established for freight transportation, with shipping and rail having lowest and light trucks and air transport having highest specific impact for all cases calculated. Passenger travel with rail, coach or two- and three-wheelers has on average the lowest specific climate impact also on short time horizons. Air travel has the highest specific impact on short-term warming, while on long-term warming car travel has an equal or higher impact per passenger-kilometer
Climate Effects of Emission Standards: The Case for Gasoline and Diesel Cars
Passenger transport affects climate through various mechanisms
involving both long-lived and short-lived climate forcers. Because
diesel cars generally emit less CO<sub>2</sub> than gasoline cars,
CO<sub>2</sub> emission taxes for vehicle registrations and fuels
enhance the consumer preference for diesel cars over gasoline cars.
However, with the non-CO<sub>2</sub> components, which have been changed
and will be changed under the previous and upcoming vehicle emission
standards, what does the shift from gasoline to diesel cars mean for
the climate mitigation? By using a simple climate model, we demonstrate
that, under the earlier emissions standards (EURO 3 and 4), a diesel
car causes a larger warming up to a decade after the emissions than
a similar gasoline car due to the higher emissions of black carbon
and NO<sub>X</sub> (enhancing the O<sub>3</sub> production). Beyond
a decade, the warming caused by a diesel car becomes, however, weaker
because of the lower CO<sub>2</sub> emissions. As the latter emissions
standards (EURO 5 and 6) are phased in, the short-term warming due
to a diesel car becomes smaller primarily due to the lower black carbon
emissions. Thus, although results are subject to restrictive assumptions
and uncertainties, the switch from gasoline to diesel cars encouraged
by CO<sub>2</sub> taxes does not contradict with the climate mitigation
focusing on long-term consequences
Climate Penalty for Shifting Shipping to the Arctic
The
changing climate in the Arctic opens new shipping routes. A
shift to shorter Arctic transit will, however, incur a climate penalty
over the first one and a half centuries. We investigate the net climate
effect of diverting a segment of Europe–Asia container traffic
from the Suez to an Arctic transit route. We find an initial net warming
for the first one-and-a-half centuries, which gradually declines and
transitions to net cooling as the effects of CO<sub>2</sub> reductions
become dominant, resulting in climate mitigation only in the long
term. Thus, the possibilities for shifting shipping to the Arctic
confront policymakers with the question of how to weigh a century-scale
warming with large uncertainties versus a long-term climate benefit
from CO<sub>2</sub> reductions