The characteristics of micrometeorology and the CO
2 flux of the Arctic wet tundra ecosystem were measured during the mid-summer of 1994 at Prudhoe Bay, Alaska. CO
2 flux was measured by the eddy correlation technique with a sonic anemometer and an open path IRGA.
Over the coastal Arctic tundra, the micrometeorology of the surface boundary layer changed remarkably according to wind direction. Wind from the Polar Sea brought cold and moist air, and southern wind brought warm and dry air with higher water vapor deficit, which resulted different CO
2 flux over the wet tundra ecosystem.
A simple canopy resistance model was applied in order to analyze the relationship between the CO
2 flux and the micrometeorology, in which parameters were determined using measured data. The ecosystem respiration increased with water temperature, and the rate was larger under higher wind speed. The photosynthesis rate decreased with water vapor deficit between leaves and the atmosphere, and its decrement was larger under higher wind speed conditions.
The effects of micrometeorology on the CO
2 flux were examined using the model, which showed that the level of ecosystem respiration due to high water temperature and that of photosynthetic decrease due to high water vapor deficit were the same orders as the potential of photosynthesis measured over the coastal Arctic tundra at Prudhou Bay, Alaska in mid summer. The magnitude of the ecosystem respiration and the decrement of photosynthesis were large enough to diminish the downward CO
2 flux to zero. The CO
2 budget over the coastal Arctic wet tundra was much affected by the ecosystem respiration and the contribution of water stress to plant photosynthesis caused by higher temperature and drying.
View full abstract