A new project to modify Boeing 787 aircraft has started in February 2021.
We plan to develop new CME and ASE instruments and install them into 787 aircrafts
operated by Japan Airlines. The coming observations provided by 787 flights
will strongly sustain the current CONTRAIL observation network.
Japan Airlines' Boeing 787 aircraft
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Estimation of fire-induced carbon emission from Equatorial Asia in 2015
May 2021
The inverse analysis was used to estimate the fire carbon emission in Equatorial Asia
induced by the big El Niño in 2015. This inverse analysis is unique
because it extensively used high-precision atmospheric mole fraction data
of carbon dioxide (CO2) from the commercial aircraft observation project.
By comparisons with independent shipboard observations, especially carbon monoxide (CO) data,
the validity of the estimated fire-induced carbon emission was elucidated.
The best estimate, which used both aircraft and shipboard CO2 observations,
indicated 273 Tg C for fire emission during September–October 2015.
This two-month-long emission accounts for 75 % of the annual total fire emission
and 45 % of the annual total net carbon flux within the region,
indicating that fire emission is a dominant driving force of interannual variations
of carbon fluxes in Equatorial Asia. Several sensitivity experiments demonstrated
that aircraft observations could measure fire signals, though they showed
a certain degree of sensitivity to prior fire-emission data. The inversions
coherently estimated smaller fire emissions than the priors,
partially because of the small contribution of peatland fires,
indicated by enhancement ratios of CO and CO2 observed by the ship.
In the future warmer climate condition, Equatorial Asia would experience more severe droughts
and have risks for releasing a large amount of carbon into the atmosphere.
Therefore, the continuation of aircraft and shipboard observations is fruitful
for reliable monitoring of carbon fluxes in Equatorial Asia.
CO2 mole fractions in the free troposphere around Equatorial Asia observed by CONTRAIL (a) and their corresponding prior (GG)(b) and posterior (C_GG) (c) model values deviated from the observations. Each upper panel presents a time-latitude cross-section from cruising mode data(~11 km above sea level) within the longitude range of 90°–130°E, and the lower one shows a time-altitude cross-section from ascending/descending data over Singapore.Prior (a) and posterior (b: C_GG, e: C_NO) surface CO2 flux distributions averaged for September 2015. Differences between prior and posterior fluxes(c,f) and prior fire emissions (d) are also shown.