So it seems quite clear that there is a potential connection, in a statistical sense, between human - caused global warming, declining Arctic sea ice, and the anomalous blocking pattern this winter that has added to other factors we know are tied to human - caused climate change (warmer temperatures and
increased soil evaporation, and decreased winter snowpack and freshwater runoff) to produce the unprecedented drought this year in California.
Not exact matches
Increased temperatures trigger more
evaporation from reservoirs, and accelerate water loss from
soils needed for agricultural production — all factors that boost demand for water, he added.
Global warming is desiccating the region in two ways: higher temperatures that
increase evaporation in already parched
soils, and weaker winds that bring less rain from the Mediterranean Sea during the wet season (November to April).
The apparent rise in evapotranspiration — the process by which water is transferred from the land to the atmosphere by
evaporation from plants and
soil — is
increasing potential drought risk with rising temperature trends, especially during periodic drought cycles that have been linked with strong El Nino events.
They found that
evaporation of water from the
soil surface significantly decreased with
increasing aggregate mulch thickness.
Not only does this limit the land available for use in agriculture, but in land that has been used for generations, the combination of irrigation and
evaporation gradually leads to
increasing soil salinity.
Those high temperatures have helped allow drought to flourish in the Northeast and Southeast, as they
increase the amount of
evaporation from
soils and transpiration from trees.
However, in many of the same places, actual evapotranspiration inferred from surface water balance exhibits an
increase in association with enhanced
soil wetness from
increased precipitation, as the actual evapotranspiration becomes closer to the potential
evaporation measured by the pans.
In a world warming from
increasing greenhouse gases,
evaporation from oceans, lakes and
soils also
increases.
Plant die - off means carbon dioxide is released and more
soil is exposed,
increasing evaporation, and thus drying out the
soil for neighboring plants.
Still more
evaporation from the
soil and an
increased risk of drought.
Like we mentioned above, as temperatures rise,
evaporation increases and
soils dry out.
But going into spring and summer,
soil should dry out more quickly (and it has been) given a decreased warm month precipitation and
increased rate of
evaporation.
Even in areas where precipitation does not decrease, these
increases in surface
evaporation and loss of water from plants lead to more rapid drying of
soils if the effects of higher temperatures are not offset by other changes (such as reduced wind speed or
increased humidity).5 As
soil dries out, a larger proportion of the incoming heat from the sun goes into heating the
soil and adjacent air rather than evaporating its moisture, resulting in hotter summers under drier climatic conditions.6
At the local scale, high temperatures may lead to
increased evaporation and decreased
soil moisture, resulting in an «agricultural drought».
Warm temperatures
increase the rate of
evaporation from parched
soils and critically dry rivers, lakes, and streams — exacerbating the impacts of existing precipitation deficits.
On average, lakes have decreased in area in the last 50 years in the southern two - thirds of Alaska, 102,103,87,88 due to a combination of permafrost thaw, greater
evaporation in a warmer climate, and
increased soil organic accumulation during a longer season for plant growth.
Fires: We know that higher temperatures lead to
increased rates of
evaporation, leading to rapid drying of
soils.
Since the
soil moisture in permafrost regions in the warm period is already very high,
evaporation would not necessarily
increase.
Warmer temperatures also
increase evaporation in
soil, which affects plant life and can reduce rainfall even more.
With
increased temperatures comes
increased evaporation from the surface, be it water or
soil.
One of the most well - known effects of global warming is an intensification of the water cycle, with higher air temperatures leading to
increased evaporation from the seas and
soils, and more atmospheric water vapor contributing to more frequent heavy precipitation events.
Warmer temperatures can directly
increase evaporation rates, and also affect the water vapour transport within
soils themselves, further adding to the evaporative demand.
«Warming will
increase evaporation so the
soils will be drier, even if the precipitation remains the same.»