摘要:Large lakes may constitute a significant component of regional surface–atmosphere fluxes, but few
efforts have been made to quantify these fluxes. Tracer-transport inverse models that infer the
CO2 flux
from the atmospheric concentration typically assume that the influence from large lakes is negligible.
CO2 observations from a tall tower in Wisconsin segregated by wind direction suggested a
CO2 signature from Lake Superior. To further investigate this difference, source–receptor
influence functions derived using a mesoscale transport model were applied and
results revealed that air masses sampled by the tower have a transit time over the
lake, primarily in winter when the total lake influence on the tower can exceed
20% of the total influence of the regional domain. When the influence functions
were convolved with air–lake fluxes estimated from a physical–biogeochemical
lake model, the overall total contribution of lake fluxes to the tall tower
CO2 were mostly negligible, but potentially detectable in certain periods of fall and winter when lake
carbon exchange can be strong and land carbon efflux weak. These findings suggest that large
oligotrophic lakes would not significantly influence inverse models that incorporate tall tower
CO2.