Two-dimensional simulation of airflow and carbon dioxide transport over a forested mountain: Part II. Carbon dioxide budget analysis and advection effects

• Published in: Agricultural and forest meteorology Vol. 140; no. 1-4; pp. 352 - 364
• Main Authors: Sun, H, Clark, T.L, Stull, R.B, Black, T.A
• Format: Journal Article
• Language: English
• Published: 30.11.2006
• Subjects: advection; air temperature; atmospheric circulation; carbon dioxide; data analysis; diurnal variation; eddy covariance measurements; forest soils; gas exchange; height; mathematical models; montane forests; overstory; photosynthesis; simulation models; soil respiration; spatial variation; British Columbia; Canada, British Columbia, Vancouver I
• ISSN: 0168-1923; 1873-2240
• DOI: 10.1016/j.agrformet.2006.03.016

We apply a high-resolution atmospheric model to assess the influence of mesoscale advection of CO sub(2) on the estimation of net ecosystem exchange (NEE) using eddy-covariance CO sub(2) flux measurements at a Fluxnet-Canada forest site located on sloping terrain on Vancouver Island, Canada. The numerical simulation is performed for fair-weather conditions over an idealized two-dimensional mountain bounded by water. The model is enhanced to include a CO sub(2) budget with a treatment of canopy photosynthesis and soil respiration. The simulation captures the transport of CO sub(2) by nocturnal drainage flows and weak land breezes. The resulting vertical profiles and time evolution of CO sub(2) concentration show a significant variation near the ground, associated with stability changes in the atmospheric boundary layer. The simulated vertical CO sub(2) gradients are found to be large around sunset and sunrise. The decrease of CO sub(2) concentration over land after midnight and the CO sub(2) accumulation over the neighboring water surface indicate CO sub(2) advection. A CO sub(2) budget analysis of the numerical-model output shows that the mean horizontal and vertical advection have significant fluctuations and opposite signs during daytime, with the net result that they largely counteract each other. At night, mean advection results in the underestimation by 20% of the nocturnal respiration. The estimated NEE at night is dominated by sub-grid-scale vertical flux in this simulation. Further evaluation using 3D simulations with higher resolution is needed to see if our results hold where vertical fluxes are much better resolved.