A 7-year record (1990-1996) of continuous atmospheric methane (CH4) me
asurements is presented from a remote midcontinental monitoring statio
n at Fraserdale, Ontario (49 degrees 53'N, 81 degrees 34'W). Ninety-si
x air samples per day were measured with a fully automated gas chromat
ograph with flame ionization detection. Five-day Lagrangian back traje
ctories over the 7-year period were used to establish a climatology in
the region of the station. The site is predominantly influenced by ai
r flow from northern and high-latitude regions and therefore uniquely
positioned to monitor wetland emissions. During winter, CH4 concentrat
ion time series from Fraserdale often match the short-term variability
observed at the high Arctic monitoring station at Alert, Northwest Te
rritories (82 degrees 27'N, 61 degrees 31'W). During summer, due to di
urnal changes of vertical mixing in the boundary layer, large diurnal
cycles in CH4 mixing ratio up to 150 ppb are observed. The data select
ed for the afternoon, when the boundary layer is well-mixed, are repre
sentative of a larger spatial scale. The mean annual cycle of CH4 at F
raserdale determined using these selected data is significantly differ
ent from annual cycles at other mid- and high-northern latitude sites
thus providing key information for global atmospheric CH4 models. In l
ate summer the annual cycle at Fraserdale shows a distinct secondary m
aximum in CH4. This is the result of advection of air with enhanced CH
4 due to emissions from the extensive wetland areas to the north and n
orthwest. The average growth rate (using selected data) for the period
was 5.6 ppb yr-l with a growth rate pattern that is slightly differen
t and out of phase with growth rate changes observed at other high-lat
itude observing sites by 2 to 6 months.