«For a given wind farm, the inhibiting effect should be quantified by fully considering local background environmental factors (e.g., temperature and soil moisture) and the recovery of vegetation with
different vegetation conditions.
Not exact matches
It doesn't matter if one includes or excludes outliers due to upwind (
vegetation depleted) or downwind (volcanic increased)
conditions in the Mauna Loa data, or if one uses the data of the south pole, or Barrow, in all cases the trend doesn't differ with more than a few tenths of a ppmv... And the averages within one hemisphere are not more than 2 ppmv
different.
Using simulation results from five GCMs and the full range of RCPs, we have characterized the range of terrestrial
vegetation responses to future
conditions across seven
different global
vegetation model formulations.
The methanogenic community included genera capable of both AM and HM, indicating that methanogens could potentially use
different carbon substrates and thus acclimate to changing
conditions, for example
vegetation cover or hydrology, under a warmer climate.