Drought
causes dry soils causes higher surface temperatures.
This result suggests that the reduced precipitation has
caused drier soils, which in turn have enhanced the warming owing to reduced cooling by evaporation.
Not exact matches
Another
cause of
drying is evaporation from the top of the
soil, which can be controlled with a mulch of grass clippings — but then it's hard to see how wet the
soil is.
When the
soil (and the wood)
dry out again, the wood contracts, the rubber hose opens and lets water drip, just enough to
cause the simple valve to close again.
Another theory: oxidation of organic matter — as permafrost thawed, as peaty
soils burned or as a seaway
dried up — may have
caused the Paleocene - Eocene warming.
Nolan was influenced by the real - life ecological disaster of the Dust Bowl in 1930s North America, when the rich top
soil essential to farming
dried out and blew away, desolating vast areas and
causing famine and mass human displacement — a situation that could yet happen again with the severe, ongoing US drought in the US.
«From a policy perspective, we have to recognize that we have been trending toward
drier conditions over the last 1,500 years and the warming in Nevada is only going to exacerbate that trend,» he said, noting that «warmer temperatures
cause more
soil moisture to evaporate so you amplify the effects of drought when climate is warming.
Therefore, the current evidence suggests that permafrost thaw in
dry soils will
cause a stronger permafrost carbon — climate feedback than in water - saturated
soils 1,7.
This
causes land uplift that has changed the sea bottom into
dry soil since the end of the ice age.
This
causes the precipitating convection to move over the
dry soils and reverses the polarity of the circulation.
Natural processes changed the timing and magnitude of
soil moisture, streamflow, and groundwater deficits by up to several years, and
caused the amplification of rainfall declines in streamflow to be greater than in normal
dry years.
For example, studies of temperatures in Arizona and Mexico have shown that lost vegetation from severe overgrazing and other careless practices
caused the
soil surface to
dry.
Combined with diminished precipitation, high temperatures in California are
causing soils and vegetation to lose moisture earlier in the spring and stay
dry later in the fall, meaning the landscape is flammable for more of the year.
A prominent example of massive
soil drying was the «Dust Bowl» in the 1930s (Woodhouse and Overpeck 1998), which
caused massive crop failures and other large - scale socio - economic impacts (Schubert et al. 2004; Cook et al. 2009).
Two processes can disrupt this system and
cause a transition to a less dense transitional forest or to fire - adapted vegetation: (1) damage to canopy trees by fires fueled by
dry understory vegetation; or (2) depletion of deep stores of
soil moisture.
Increased rainfall variability was more significant than rainfall amount for tall - grass prairie productivity (Fay et al., 2000, 2002), with a 50 % increase in
dry - spell duration
causing 10 % reduction in NPP (Fay et al., 2003) and a 13 % reduction in
soil respiration (Harper et al., 2005).
Further, the United Nations Convention to Combat Desertification (UNCCD) defines land degradation as a reduction or loss in arid, semi-arid, and
dry sub-humid areas of the biological or economic productivity and complexity of rain - fed cropland, irrigated cropland, or range, pasture, forest and woodlands resulting from land uses or from a process or combination of processes, including those arising from human activities and habitation patterns, such as: (i)
soil erosion
caused by wind and / or water; (ii) deterioration of the physical, chemical, and biological or economic properties of
soil; and (iii) long - term loss of natural vegetation.
The United Nations Convention to Combat Desertification defines land degradation as a reduction or loss in arid, semi-arid, and
dry sub-humid areas, of the biological or economic productivity and complexity of rain - fed cropland, irrigated cropland, or range, pasture, forest, and woodlands resulting from land uses or from a process or combination of processes, including processes arising from human activities and habitation patterns, such as (i)
soil erosion
caused by wind and / or water; (ii) deterioration of the physical, chemical and biological or economic properties of
soil; and (iii) long - term loss of natural vegetation.
The areas with enhanced warming over the USA may also be
caused by
drier soils from reduced precipitation, although the poor model agreement in precipitation changes for this region means this conclusion is uncertain.
Subsidence is
caused by
soil shrinkage and movement, and is increasingly becoming a risk to property owners due to cracks in the earth
caused by prolonged
dry spells which alter
soil conditions.
A
dry summer in 2013 would
cause heavy damage to property in areas with high levels of clay in the
soil.
He's discovered a number of problems that can lurk: oversaturation of
soil; tree branches hanging over a home that can damage roofs and allow pests access; broken or misaligned sprinklers that can lead to
dry rot or termites; inefficient rain gutters that
cause drainage problems; and lawn slopes that drain toward the house rather than away, setting the scene for flooding issues.
Bitter Cucumbers A bitter taste in cucumbers may be
caused by extreme
dry or hot temperatures, overwatered
soils or poor fertility.
Too much water can
cause the plant to rot, so it is advisable to allow the
soil to
dry out somewhat between watering.