Although these hydrological changes could potentially increase soil water availability in previously snow - covered regions during the cool low - ET season (34), this effect would likely be outweighed by the influence of warming temperatures (and
decreased runoff) during the warm high - ET season (36, 38), as well as by the increasing occurrence of consecutive years with low precipitation and high temperature (Fig. 4A).
Increased droughts and forest fires,
decreased runoff, loss of wildlife habitat, and rising air pollution are all signs of a climate out of control.
Temperature rise increases evaporation and
decreases runoff, but has been found to cause an increased rate of runoff in winter and a decrease in spring.
According to http://rsta.royalsocietypublishing.org/content/369/1934/85.full my area is likely to see 30 % lower precipitation in DJF (that's when it rains here) and warmer temperatures,
decreasing runoff more.
Not exact matches
Rules limiting nutrient
runoff from farms and wastewater treatment plants helped to
decrease nitrogen concentrations in the bay by 23 percent since 1984.
«Use of the nanoparticle increases soil diffusion while
decreasing the risk of leaching and
runoff, reducing the amount of chemical in food crops and reducing the cost to treat crops.»
This
decreases natural storm
runoff during high - flow winter months while contributing proportionately more water to streamflows during the drier months that make up about 80 percent of the region's calendar year.
The cores showed an increase in abundance of grass in the same sediments that showed a
decrease in surface
runoff.
To stave off a complete collapse of gulf fisheries and shrimp populations, Scavia finds, the dead zone must shrink drastically, to 2,000 square miles or less — and for that to happen, agricultural nitrogen
runoff will have to
decrease by at least 40 percent.
A 2016 report by the Bureau of Reclamation predicts that the basin's snowpack is likely to
decrease, stemming the flow of
runoff in spring and early summer.
Study team member Robert Dudley says global warming could be involved but that the aim of the study was only to determine whether snowmelt
runoff into rivers was increasing or
decreasing; it will be up to other scientists to examine what factors might be responsible for the trend they found.
Similarly, stormwater
runoff,
decreased evaporative cooling, and building damage from soil contraction and expansion are just a subset of how precipitation impacts will affect human systems.
* Over the last decade or two, rainfall has been markedly below average in our temperate south - west, south and east, and this along with increased average temperatures has caused a major
decrease in
runoff from our catchments.
Availability of resources such as usable water will also depend on changing rates of precipitation, with
decreased availability in many places but possible increases in
runoff and groundwater recharge in some regions like the high latitudes and wet tropics.
One of their greatest uses is in fact their ability to reduce the volume of surface
runoff which
decreases the risk of floods in case of heavy precipitation.
There was less rainfall over land, and a record
decrease in
runoff and ocean discharge into the ocean from October 1991 to September 1992, the scientists report this week in the journal Geophysical Research Letters.
However, almost all climate change projections predict increases in temperature and
decreases in Colorado River
runoff [Vano et al., 2014].
Quantifying the contribution of climate - and human - induced
runoff decrease in the Luanhe river basin, China
Average annual
runoff decreasing 20 - 40 percent in the Danube, Mississippi, Amazon and Murray Darling river basins
Decreased maize yields and
runoff, increased long - lasting drought and more favourable conditions for malaria transmission are greatest over drylands if global warming were to rise from 1.5 °C to 2.0 °C.
An ecoroof significantly
decreases stormwater
runoff, saves energy, reduces pollution and erosion, and helps preserve fish habitat.
The Canon del Plata hydropower project would experience a
decrease from 1540 gigawatt - hours to 1250 gigawatt - hours for a 50 % glacier
runoff reduction and decline to 970 gigawatt - hours for a 100 % glacier loss (Vergara et.
In Thunder Basin
runoff has in contrast
decreased negligibly, 4 %.
Eventually the resulting decline in glacier extent reduces the area available for melting causing a
decrease in glacier
runoff.
A continuing trend in glacier loss will seriously
decrease the water reserves stored as ice, reducing melt season
runoff.
However, a large majority of streams in glaciated basins in BC showed a statistically significant
decrease in August streamflow during 1976 to 1996, which suggests that these glaciers even with increased melt rates are providing less
runoff (Stahl and Moore, 2006).
Glacier
runoff does not increase or
decrease the long term
runoff for a basin, total
runoff over a period of several years is determined largely by annual precipitation.
This map shows predicted increases in
runoff in blue, and
decreases in brown and red.
We summarized how important factors that are not directly modeled may increase or
decrease the range or
runoff due to thinning that is documented in this study in File S3.
The model predicted
runoff increases in a linear fashion with winter precipitation and basal area reductions, and
decreases linearly with years since treatment (Figure 3).
The effect is measurable: for example, reduced
runoff from snow melt has caused an annual 5 percent
decrease in the amount of water entering the Colorado River, which experts say already faces the risk of significantly drying up.
By mid-century, annual average river
runoff and water availability are projected to increase by 10 - 40 % at high latitudes and in some wet tropical areas, and
decrease by 10 - 30 % over some dry regions at mid-latitudes and in the dry tropics, some of which are presently water - stressed areas.
Bouraoui et al. (2004) showed, for southern Finland, that the observed increase in precipitation and temperature was responsible for a
decrease in snow cover and increase in winter
runoff, which resulted in an increase in modelled suspended sediment loads.
Where precipitation
decreases were projected, the results were more complex due largely to interactions between plant biomass,
runoff, and erosion, and either increases or
decreases in overall erosion could occur.
soil erodibility changes due to a
decrease in soil organic matter concentrations (which lead to a soil structure that is more susceptible to erosion) and to increased
runoff (due to increased soil surface sealing and crusting);
Snow
runoff (and the resulting
decrease in electricity prices) is a yearly event that usually awaits the spring thaw.
Increases in winter and early - spring stream flow — followed by
decreases in late spring, summer, and early fall — have already been observed over the past 50 years.6 Peak spring
runoff is occurring anywhere from a few days to 25 - 30 days earlier throughout the region.7
However, no anthropogenic influence can be detected for 1 - day and 3 - day surface
runoff, as increases in extreme precipitation in the present - day climate are offset by
decreased snow cover and lower frozen water content in soils during the May — June transition months, compared to pre-industrial climate.
It is perfectly conceivable, for example, to have annual precipitation increase 10 to 20 % at the same time that mean annual surface water
runoff decreases by 10 to 20 % (or even more).
3) Summer
runoff has
decreased markedly, 27 %, in the non-glacier Newhalem basin with the earlier melt of reduced winter snowpack.
Several studies focused on the Colorado River basin showed that annual
runoff reductions in a warmer western U.S. climate occur through a combination of evapotranspiration increases and precipitation
decreases, with the overall reduction in river flow exacerbated by human demands on the water supply.
What the report says about climate change and the Colorado River: The southwestern United States is projected to experience significant
decreases in surface water availability, leading to
runoff decreases in California, Nevada, Texas, and the Colorado River headwaters, even in the near term.
The eruption of Pinatubo was followed by a significant drop - off of rainfall over land and a record
decrease in
runoff and freshwater discharge into the ocean, according to a recent study by Trenberth and other scientists.
Shows that during the 1974 — 2004 period, the stability of the mean discharge on the main stem in Óbidos is explained by opposite regional features that principally involve Andean rivers: a
decrease in the low stage
runoff, particularly important in the southern regions, and an increase in the high stage
runoff in the northwestern region
Many basins in the tropical Andes have experienced an increase in
runoff in recent decades, while precipitation has remained almost constant or has shown a tendency to
decrease (Coudrain et al., 2005).
While these dead zones are often caused by fertilizer
runoff currently, it seems the
decreasing ability of the oceans to hold dissolved oxygen with continued warming will increasingly become a problem for marine ecosystems and fisheries in the coming decades.
This expansion of OMZs is due to nutrient
runoff makes the ocean more vulnerable to
decreasing solubility of O2 in a warmer ocean.
A wide variety of modeling efforts have yielded results that suggest, for each 1 °C increase in temperature,
runoff will
decrease from 2 — 8 % in the Colorado River basin (67).
The impacts of
runoff and soil moisture deficits associated with warm temperatures can be acute, including enhanced wildfire risk (21), land subsidence from excessive groundwater withdrawals (22),
decreased hydropower production (23), and damage to habitat of vulnerable riparian species (24).
What's more, our buildings can literally begin to come alive: green walls and rooftop gardens not only suck carbon out of the air, but they also can provide healthy local produce, can reduce storm water
runoff, and can
decrease the urban heat island effect.