Ej. Cooter et Db. Schwede, Sensitivity of the National Oceanic and Atmospheric Administration multilayer model to instrument error and parameterization uncertainty, J GEO RES-A, 105(D5), 2000, pp. 6695-6707
The response of the National Oceanic and Atmospheric Administration multila
yer inferential dry deposition velocity model (NOAA-MLM) to error in meteor
ological inputs and model parameterization is reported. Monte Carlo simulat
ions were performed to assess the uncertainty in NOAA-MLM deposition veloci
ty V-d estimates for ozone (O-3), sulfur dioxide (SO2), and nitric acid (HN
O3) associated with measurements of meteorological variables (including tem
perature, humidity, radiation, wind speed, wind direction, and leaf area in
dex). Summer daylight scenarios for grass, corn, soybean, oak, and pine wer
e considered. Model sensitivity to uncertainty in the leaf area index (LAI)
, minimum stomatal resistance, and soil moisture parameterizations was expl
ored. For SO2 and HNO3, instrument error associated with the measurement of
wind speed and direction resulted in the greatest V-d error. Depending On
vegetation type, the most important source of uncertainty due to instrument
error for the V-d of O-3 was LAI. Of the model parameterizations studied,
accurate estimation of temporal aspects of the annual LAI profile and the c
haracterization of soil moisture supply and demand are most important to mo
del-estimated V-d uncertainty. Considered individually, these factors can r
esult in SO2 and HNO3 V-d estimate uncertainty of +/-25% and O-3 estimate u
ncertainty greater than 60%. For single plant species settings, reductions
in estimate uncertainty should be possible with minor algorithmic modificat
ion, inclusion of more species-appropriate LAI profiles, and careful applic
ation of remote sensing technology.