Along the boundary,
soil moisture showed «a sharp transition,» as did the type of vegetation likely to grow there in the absence of human activity, the scientists noted.
Corresponding time series of
soil moisture show a similar drying.
Soil moisture shows a decreasing trend over the 1979 - 2017 period and all seasons of 2017 showed below average values.
Not exact matches
Studies including Wang's earlier work in Africa have
shown that even small changes in
soil moisture in drylands could be significant enough to cause large changes in vegetation productivity.
DeLaune said previous field studies from the Rolling Plains and adjacent High Plains demonstrated mixed results, with some
showing a reduction in
soil moisture and cash crop yield due to cover crops and others indicating no significant impact of cover crops on subsequent fiber yield.
Soil moisture sensors
show, over time, how much water has gone into the ground, and how much has left, either from drainage or in the form of evapotranspiration from plants.
Control experiments have
shown that water held in the zeolite increases the
moisture content of
soil in desert conditions.
Results
showed that the bioplastics and biofabrics increased
soil moisture relative to bare
soil.
Analyses
showed that high - frequency irrigation resulted in higher root zone
soil moisture content relative to low - frequency irrigation despite reduced evaporative demand during part of the growing season.
Cultivars «Radicans» and «August Beauty» were used in a study that
showed that
soil moisture sensor technology can be effective for controlling growth of the cultivars.
-- Research
shows that wheat crops benefit from a preceding legume pulse crop through the addition of
soil organic matter leading to conservation of
soil moisture and the addition of nitrogen (Miller et al 2002; Miller et al 2003; Cutforth et al 2007).
«The study
showed soil amendment using lignite - derived humic substances improved the condition of plants exposed to water stress by reducing
moisture loss,» he said.
Studies
show that
soil moisture retention in most years did not significantly decrease with the presence of these crops (Miller et al. 2006; Miller and Holmes 2012), suggesting that this revenue - generating crop can replace a fallow year without incurring a
moisture deficit.
Graphs
show A) six - month winter (November to April) rainfall, B) annual temperature, C) annual
soil moisture, and D) total population.
The decreasing rainfall (
shown in the top graph below) combined with rising temperatures (second graph) resulted in a decline in
soil moisture (third graph), the researchers say.
At the same time, other research
shows that increased heat will be detrimental to many domesticated cereal crops, plus it will promote increased loss of
soil moisture, both of which will promote reduced crop yields.
Although data are not complete, and sometimes contradictory, the weight of evidence from past studies
shows on a global scale that precipitation, runoff, atmospheric water vapor,
soil moisture, evapotranspiration, growing season length, and wintertime mountain glacier mass are all increasing.
Charts
showing the timing of floods (green) alongside the peaks in their main drivers — 7 - day maximum rainfall (purple), peak snowmelt (orange) and maximum
soil moisture (blue)-- for six regions in Europe from 1960 to 2010.
You can see this illustrated in the charts below, which
show the timing of floods (green lines) as well as the peaks of each of their drivers — rainfall (purple), orange (snowmelt) and
soil moisture (blue)-- for six flooding «hotspots» in Europe.
Previous research has
shown that
soil moisture plays a critical part in both permafrost thaw and carbon exchange with the atmosphere — as the permafrost breaks down, surface water may drain away to deeper
soil layers, leaving the topsoil high and dry.
The Palmer Drought Severity Index, which is a measure of
soil moisture using precipitation measurements and rough estimates of changes in evaporation, has
shown that from 1900 to 2002, the Sahel region of Africa has been experiencing harsher drought conditions.
Maps
show most recent daily, monthly and 12 - month calculated
soil moisture, anomalies and percentiles.
Moreover, we
show that multidecadal variations exist in other hydrological variables (evapotranspiration, snow cover, and
soil moisture).
These seasonal changes contribute to an annual increase in GPP with simultaneous wNA + Amazon forest loss due to release from
soil moisture limitation (not
shown).
The ERA - Interim analyses of
soil moisture are included in the monthly summaries to provide a qualitative picture of major anomalies and to
show the consistency with other variables.
The averages for the last 12 months
show dry conditions over most regions within a large belt stretching across parts of both Europe and Asia, with below average precipitation and
soil moisture and much below average relative humidity, starting in south - western Europe and ending near Japan.
The four months to March 2018 for SE Europe also
showed negative anomalies for both relative humidity and
soil moisture.
Murry Salby who is suggesting that ocean and
soil moisture data
shows that the observed rise in atmospheric CO2 might well be entirely from natural causes and Roy Spencer who suggests that variations in oceans and sun affecting global cloudiness make it impossible to verify the sign of the climate system response to more CO2 in the air.
The darker grey shading denotes where
soil moisture is not
shown due to ice cover or climatologically low precipitation.
Soil moisture is included in the monthly summaries to provide a qualitative picture of the major anomalies and to
show its consistency with the other variables.
In 2004, new rainfall data
showed that half of the forest area of the Amazon Basin had either fallen below, or was very close to, the critical level of
soil moisture below which trees begin to die (Nepstad et al. 2004).
Bill Gray has a favorite diagram, taken from a 1985 climate model,
showing little nodules in the center with such labels as «thermal inertia» and «net energy balance» and «latent heat flux» and «subsurface heat storage» and «absorbed heat radiation» and so on, and they are emitting arrows that curve and loop in all directions, bumping into yet more jargon, like «
soil moisture» and «surface roughness» and «vertical wind» and «meltwater» and «volcanoes.»
The four months to January 2018 for SE Europe also
showed large negative anomalies for both relative humidity and
soil moisture.
The ERA - Interim analyses of
soil moisture are included here to provide a qualitative picture of major anomalies and to
show the consistency with other variables.
In the results section both data records are thus
shown with respect to their «native» climatology, mainly in order to more directly relate the ERA - Interim
soil moisture with other ERA - Interim variables.
The three main variables that are used for the analysis are precipitation,
soil moisture and relative humidity of surface air, though the latter is not
shown.
Relative humidity of surface air is not
shown, but referred to when it provides complementary information to the precipitation and
soil moisture analysis.
The higher resolution of E-OBS
shows a large positive precipitation anomaly over the Alps and the satellite
soil moisture product
shows above average
soil moisture for a larger region than ERA - Interim.
The seasons with the largest negative anomalies were the spring and the summer, which both had the third largest negative
soil moisture anomaly for the respective season in the ERA - Interim record, while regionally autumn
showed the largest anomalies.
Evaluation of C3S satellite
soil moisture against sets of ground - based measurements
shows that it captures temporal dynamics, but with large variations in quality through space and time (Dorigo et al. 2017, Dorigo et.
«Our results
show that increasing temperatures have a large effect on carbon release from permafrost, but that changes in
soil moisture conditions have an even greater effect,» Dr Schädel says.
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.
FIGURE 2.17 Colors
show volumetric
soil moisture content, where blue is more moist and red is drier.
«The models also
showed that modest global warming may produce a higher CH4 emission, but that this effect may be reversed by larger increases in temperature, due to the effect of
soil moisture depletion.»
Blue depicts areas with higher
soil moisture than usual, while brown
shows lower
soil moisture than usual for this time of the year.
The image
shows soil moisture anomalies in the United States and the Gulf of Mexico for the last 10 days of August 2017.
The four months to April 2018 for SE Europe also
showed negative anomalies for both relative humidity and
soil moisture.
Their various climate simulations do
show differences in
soil moisture, as well as in the land - atmosphere interactions that contribute to
soil - drying evaporation.