Ozone impact on the forest in the Tanzawa Mountains has been recognized for many years. In order to understand the forest decline, the hourly stomatal O
3 flux and the accumulated Phytotoxic Ozone Dose (POD
y: y means a threshold) were estimated using two numerical models. The numerical models (meteorological model: MM5 and air quality model: CMAQ) were executed to estimate the hourly O
3 concentration and the meteorological elements (air temperature, specific humidity, insolation and wind speed) from April to October including the leafing time to the leaf-fall time. We compared the POD
1( 26.2 mmol/m
2 )based on observation and the POD
1 ( 27.7 mmol/m
2 ) based on the output of numerical models at the Inukoeji station in the Tanzawa Mountains, and these POD
1 values were comparable. It shows the possibility of an application of numerical models for an O
3 impact study in the Tanzawa Mountains. The horizontal distribution of the POD
1 showed that the POD
1 exceeded the critical level in the Tanzawa Mountains. The POD
1 depends on the altitude and reaches higher values at the top of the mountains, because the stomatal O
3 conductance parameters on temperature and humidity depend on the altitude and are higher values on top of the mountains.
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