«The stability of the rate of change justifies using higher carbon dioxide enrichment levels to interpret
soil water responses to currently observed carbon dioxide enrichment,» Wang said.
Determining the mechanisms of stronger
soil water responses in drylands will require further investigation.
Not exact matches
«Importantly, the observed
response lends weight to the hypothesis that any additional
soil water in the root zone is then available to facilitate vegetation growth and greening under enhanced carbon dioxide,» Wang said.
The researchers believe the greening is a
response to higher atmospheric carbon dioxide inducing decreases in plant stomatal conductance — the measure of the rate of passage of carbon dioxide entering, or
water vapor exiting, through the stomata of a leaf — and increases in
soil water, thus enhancing vegetation growth.
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.
«We designed a project to quantify the growth of Hibiscus acetosella «Panama Red» in
response to various
soil water content thresholds,» explained Bayer.
The original proposal of a 15 inch cap of borrow
soil, with agricultural limestone and a bactericide below and revegetation by shallow - rooting plants was determined to be «inadequate,... at the least, an additional layer must be added that will act as a barrier for
water, plant roots systems and burrowing animals».20 In
response Cyprus - Amax proposed, in January 1995, a typical cap section which added a 30 - mil PVC liner overlaid by a geoweb drainage mat with a fabric cover below the 15 inch
soil cap.
Above — And Below - Ground
Responses of C3 - C4 Species Mixtures to Elevated CO2 and
Soil Water Availability.
Samuelson et al. -LRB-[2004]-RRB- showed a lag effect in the
response of foliage to large changes in precipitation by correlating current growth of loblolly pine (Pinus taeda) with the previous year's LAI, and Sperry et al. -LRB-[2002]-RRB- explained how combinations of
soil texture and xylem can impose «hydraulic limits» on the ability of the foliage to maintain adequate pressure potentials to support a continuous
water column.
Based on 1705 field measurements from 21 distinct sites, a consistent and statistically significant increase in the availability of
soil water (11 %) was observed under elevated CO2 treatments in both drylands and non-drylands, with a statistically stronger
response over drylands (17 % vs. 9 %).
In order of seniority, the seven feedbacks that seem outstanding are:
Water vapour — rising by ~ 7 % per 1.0 C of warming; Albedo loss — due mostly to cryosphere decline; Microbial peat - bog decay — due to rising CO2 affecting ecological dynamics; Desiccation of tropical and temperate soils — due to SAT rise and droughts; Permafrost melt — due to SAT rise plus loss of snow cover, etc; Forest combustion — due to SAT rise, droughts, pest responses, etc; Methyl clathrates [aka methane hydrates] now threatened by rising sea - temperatures, increased water column mixing,
Water vapour — rising by ~ 7 % per 1.0 C of warming; Albedo loss — due mostly to cryosphere decline; Microbial peat - bog decay — due to rising CO2 affecting ecological dynamics; Desiccation of tropical and temperate
soils — due to SAT rise and droughts; Permafrost melt — due to SAT rise plus loss of snow cover, etc; Forest combustion — due to SAT rise, droughts, pest
responses, etc; Methyl clathrates [aka methane hydrates] now threatened by rising sea - temperatures, increased
water column mixing,
water column mixing, etc..