Not exact matches
Gentine's team is the first to isolate the response of vegetation from the global warming
total complex response, which includes such variables for the water cycle as evapotranspiration (the water evaporated from the surface, both from plants and bare
soil)
soil moisture, and runoff.
Graphs show A) six - month winter (November to April) rainfall, B) annual temperature, C) annual
soil moisture, and D)
total population.
The amount of
soil moisture is estimated as «0.001 % of the
total water found on Earth,» but like the sweat it is critical to controlling temperature.
We find a close agreement between the CESM - based hindcasts and the Markov model, indicating that the largest contribution to the predictive skill of
soil water on interannual to decadal timescales in CESM can be attributed to the damped persistence, which is partly governed by the evapotranspiration (Delworth and Manabe 1988), the
total runoff, and the diffusion of
soil moisture into the deeper
soil levels as shown in the Eq.
In contrast, the dominant mode of
total water storage exhibits a large degree of redness, which translates into decadal predictability of depth integrated
soil moisture, particularly for the deep
soil layers.