Results 231 to 240 of about 170,268 (263)

Sorghum yield prediction based on remote sensing and machine learning in conflict affected South Sudan. [PDF]

Sci Rep
Karongo J, Mwaniki JI, Ndiritu J, Mokaya V.   +3 more
europepmc   +1 more source

A multi-proxy stalagmite record indicates a shift in forcing of twentieth century drought events in Normandy. [PDF]

Sci Rep
Bejarano-Arias I, Nehme C, Breitenbach SFM, Ionita M, Baldini J, Pons-Branchu E, Modestou S, Umbo S, Mouralis D.   +8 more
europepmc   +1 more source

Patterns and drivers of Holocene moisture variability in mid-latitude eastern North America. [PDF]

Nat Commun
Salonen JS, Schenk F, Williams JW, Shuman B, Lindroth Dauner AL, Wagner S, Jungclaus J, Zhang Q, Luoto M.   +8 more
europepmc   +1 more source

Phenological Adaptation of Wheat Varieties to Rising Temperatures: Implications for Yield Components and Grain Quality. [PDF]

Plants (Basel)
Gulino D, Lopes MS.
europepmc   +1 more source

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Comparison of evapotranspiration variables in Evapotranspiration Maps for Australia with commonly used evapotranspiration variables

Australasian Journal of Water Resources, 2003
AbstractThe Australia Bureau of Meteorology and the Cooperative Research Centre for Catchment Hydrology released a set of Evapotranspiration Maps for Australia in July 2001 as part of the Bureau’s Climatic Atlas Series. The maps give average monthly and annual values of three evapotranspiration (ET) variables: point potential evapotranspiration (PPET),
Francis H. S. Chiew, Christopher P Leahy
openaire   +2 more sources

Phenology and Evapotranspiration

2013
Many phenological models use ambient air temperature to estimate phenological stages during current and projected future climate conditions. However, the difference between ambient air temperature and plant-canopy temperature biases such estimates. Therefore, consideration of how energy balance factors affect evapotranspiration leads to more realistic ...
Richard L. Snyder, Donatella Spano, Donatella Spano   +2 more
openaire   +2 more sources

Evapotranspiration (ET) Covers

International Journal of Phytoremediation, 2012
Evapotranspiration (ET) cover systems are increasingly being used at municipal solid waste (MSW) landfills, hazardous waste landfills, at industrial monofills, and at mine sites. Conventional cover systems use materials with low hydraulic permeability (barrier layers) to minimize the downward migration of water from the surface to the waste ...
Bill Myers, Linda Fiedler, Steve Rock
openaire   +3 more sources

The Components of Evapotranspiration

2016
Evapotranspiration is the sum of evaporation from the soil surface and the plant surfaces, and transpiration. The evaporation from the soil in agronomy follows a two-stage process depending if the soil surface is wet after a rain or irrigation or has already dried up. When the soil surface is wet the rate of evaporation is potentially very high; that’s
Elias Fereres, Francisco J. Villalobos, Luca Testi   +2 more
openaire   +2 more sources

Precipitation and Evapotranspiration

2012
Local water budgets in arid regions are dominated by precipitation and evapotranspiration. Vadose zone interflow is a minor component of local water budgets and typically recharge rates are only a small percentage of rainfall. However, the paucity of vegetation and the occurrence of surface crusts in arid and semi-arid regions results in low soil ...
Thomas M. Missimer, Robert Maliva
openaire   +2 more sources

Potential evapotranspiration

2005
This chapter defines potential evapotranspiration (PET). The concept was put forth separately in 1948 by Thornthwaite in America and Penman in England. The factors that affect PET are discussed. They include fetch, crop height, crop cover, plant resistance to water flow, soil-water availability, and advection.
openaire   +3 more sources