Dlugokencky, E. J., R. C. Myers,
P. M. Lang,
K. A. Masarie,
A. M. Crotwell,
K. W. Thoning,
B. D. Hall,
J. W. Elkins and L. P. Steele, (2005),
Conversion of NOAA atmospheric dry air CH4 mole fractions to a gravimetrically prepared standard scale,
JGR-Atmospheres, 110, D18, doi:10.1029/2005JD006035
Sixteen mixtures of methane (CH4) in dry air were prepared using a gravimetric technique to define a CH4 standard gas scale covering the
nominal range 300-2600 nmol mol(-1). It is designed to be suitable for
measurements of methane in air ranging from those extracted from
glacial ice to contemporary background atmospheric conditions. All
standards were prepared in passivated, 5.9 L high-pressure aluminum
cylinders. Methane dry air mole fractions were determined by gas
chromatography with flame ionization detection, where the repeatability
of the measurement is typically better than 0.1% (<= 1.5 nmol mol(-1))
for ambient CH4 levels. Once a correction was made for 5 nmol mol(-1)
CH4 in the diluent air, the scale was used to verify the linearity of
our analytical system over the nominal range 300-2600 nmol mol(-1). The
gravimetrically prepared standards were analyzed against CH4 in air
standards that define the Climate Monitoring and Diagnostics Laboratory
(CMDL) CMDL83 CH4 in air scale, showing that CH4 mole fractions in the
new scale are a factor of (1.0124 +/- 0.0007) greater than those
expressed in the CMDL83 scale. All CMDL measurements of atmospheric CH4
have been adjusted to this new scale, which has also been accepted as
the World Meteorological Organization (WMO) CH4 standard scale; all
laboratories participating in the WMO Global Atmosphere Watch program
should report atmospheric CH4 measurements to the world data center on
this scale.