Dry soils may amplify such extremes through feedbacks
with evapotranspiration.
Not exact matches
This company's specialized sensor system provides farmers
with data tracking
evapotranspiration to guide irrigation decisions.
Evapotranspiration is another way plants can communicate
with high - tech irrigation systems.
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.
Here it can be used by plants or evaporate directly,
with water loss from both processes combined called
evapotranspiration.
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.
Hence, in determining
evapotranspiration there is a trade - off between less solar radiation and increased surface wetness,
with the latter generally dominant.
Combined
with fuel loads, higher
evapotranspiration rates and resulting shifts in water balance may be the best predictor of increased fire risk and fire severity in the future under a changing climate (Littell and Gwozdz 2011; Abatzoglou and Kolden 2013).
To be sure, some of these effects (such as the impact of irrigation on surface water vapour, or land use changes on
evapotranspiration) are not easily dealt
with in terms of the tropospheric radiative forcing — a point that was well made in the National Academies report on radiative forcing (on which Dr. Pielke was an author).
Six Chinese scientists used remotely - sensed imaging data, including leaf area index (LAI), normalized difference vegetation index (NDVI), an enhanced vegetation index (EVI), gross primary production (GPP) and net primary production (NPP), coupled
with other data (temperature, soil moisture,
evapotranspiration, albedo and wind) over the period 2003 to 2014 to analyze the effects of a wind farm on summer vegetative growth in a region of northern China.
The role of vegetation in climate change is massive — and the above
evapotranspiration is a major player
with some reports of minus 0.6 C per year?
If the upper troposphere cools only by radiation (
with probably some convection across the tropopause), but the surface transfers energy to the upper troposphere via radiation, convection, and
evapotranspiration, why would the concurrent CO2 - induced warming be uniform?
Researchers in the historical Beaver Creek experiments hypothesized that lower tree densities associated
with thinning would reduce
evapotranspiration losses, and thereby allow more water to be available for soil moisture, groundwater recharge, and surface water runoff [29].
«Here we quantify the direct climate effects of sugar - cane expansion in the Brazilian Cerrado, on the basis of maps of recent sugar - cane expansion and natural - vegetation clearance combined
with remotely sensed temperature, albedo and
evapotranspiration over a 1.9 million km2 area.
Broad - scale changes in vegetation in general, and tree loss in particular, have pronounced effects on climate processes through biogeophysical mechanisms such as albedo,
evapotranspiration (ET), and carbon dioxide exchange
with the atmosphere [11].
Had the model started
with a higher warming figure, it would have resulted in a higher warming figure when
evapotranspiration was plugged in.»
«Furthermore, recent studies suggest that fragmenting the Amazon forest could disrupt regional rainfall by breaking down a «biotic pump», in which
evapotranspiration from forests creates low - pressure zones that draw in moisture - laden air from the Atlantic Ocean,» said William F. Laurance, a researcher at the Smithsonian Tropical Research Institute, who together
with Lovejoy, won the 2009 BBVA Foundation Frontiers of Knowledge Award in Ecology and Conservation Biology for their work in the Brazilian Amazon.
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.
There is little evidence for a human influence on precipitation deficits, but a lot of evidence for a human fingerprint on surface soil moisture deficits — starting
with increased
evapotranspiration caused by higher temperatures.
Key uncertainties involve: 1) the degree to which increases in
evapotranspiration versus permafrost thaw are leading to drier landscapes; 2) the degree to which it is these drier landscapes associated
with permafrost thaw, versus more severe fire weather associated
with climate change, that is leading to more wildfire; 3) the degree to which the costs of the maintenance of infrastructure are associated
with permafrost thaw caused by climate change versus disturbance of permafrost due to other human activities; and 4) the degree to which climate change is causing Alaska to be a sink versus a source of greenhouse gases to the atmosphere.
We have direct observation from ground - based instruments which measure downwelling and upwelling LWR separately and the results are entirely consistent
with Trenberth's energy budget cartoon, from whence it is we also find the surface fluxes for convection and
evapotranspiration.
Vegetation cover changes caused by land use can alter regional and global climate through both biogeochemical (emissions of greenhouse gases and aerosols) and biogeophysical (albedo,
evapotranspiration, and surface roughness) feedbacks
with the atmosphere,
with reverse effects following land abandonment, reforestation, and other vegetation recoveries (107).
A decrease in summertime precipitation, coupled
with increased
evapotranspiration, can lead to a reduction in inland freshwater levels at mid latitudes.
The team examined data on carbon - dioxide flux,
evapotranspiration, sensible heat, air temperature, net radiation and photosynthetic active radiation from five FLUXNET grassland sites in Canada, the US and Hungary, along
with leaf - area index information derived from satellite data.
Via the report: «The effects of climate change, primarily associated
with increasing temperatures and potential
evapotranspiration, are projected to significantly increase water demand across most of the United States.