Results 71 to 80 of about 21,909 (264)

Evaluation of six empirical evapotranspiration equations - case study: Campos dos Goytacazes/RJ Avaliação de seis equações empíricas de evapotranspiração diária - estudo de caso: Campos dos Goytacazes/RJ

open access: yesRevista Brasileira de Meteorologia, 2012
The evapotranspiration is a component of the water balance constituting a major challenge in its quantification. The complex physical processes involved in its effective determination on a large scale have spurred scientists to often make use of ...
Lázaro Costa Fernandes   +2 more
doaj   +1 more source

Critical analysis of the contemporary methods for estimating reference evapotranspiration [PDF]

open access: yesGlasnik Šumarskog Fakulteta: Univerzitet u Beogradu, 2012
Evapotranspiration is one of the most important processes within the hydrological cycle whose reliable assessment is essential in the planning and managing of land and water resources.
Đukić Vesna, Mihailović Vladislava
doaj   +1 more source

Field‐Scale Soil Moisture Predictions in Real Time Using In Situ Sensor Measurements in an Inverse Modeling Framework: SWIM2

open access: yesWater Resources Research, Volume 62, Issue 2, February 2026.
Abstract Affordable autonomous soil sensors and IoT technology enable real‐time soil moisture monitoring, which offers opportunities for real‐time model calibration and irrigation optimization. We introduce an irrigation decision support system SWIM2 (Sensor Wielded Inverse Modeling of a Soil Water Irrigation Model), a digital twin that integrates ...
Marit G. A. Hendrickx   +7 more
wiley   +1 more source

Evapotranspiração de referência com base na radiação solar global estimada pelo método de Bristow-Campbell Reference evapotranspiration based on solar radiation estimated by the Bristow-Campbell model

open access: yesEngenharia Agrícola, 2010
A quantidade de água a ser aplicada em sistemas de irrigação é normalmente calculada com base na evapotranspiração de referência (ETo) da região. Vários métodos podem ser empregados para o cálculo de ETo, sendo o de Hargreaves um dos mais adotados.
Marco A. F. Conceição
doaj   +1 more source

Diversification and intensification of irrigated maize‐based cropping systems under Mediterranean conditions

open access: yesAgronomy Journal, Volume 118, Issue 1, January/February 2026.
Abstract Under Mediterranean irrigated conditions cover cropping (CC) and double cropping (DC) are diversification/intensification strategies that can increase grain yield and resource use efficiency of the traditional winter fallow‐maize (Zea mays L.) system.
I. Zugasti‐López, R. Isla, J. Cavero
wiley   +1 more source

Hydro-PE: gridded datasets of historical and future Penman–Monteith potential evaporation for the United Kingdom [PDF]

open access: gold, 2023
E. L. Robinson   +6 more
openalex   +1 more source

Effects of barley‐pea intercropping on soil carbon, crop productivity, and grain quality in a low‐input temperate agroecosystem

open access: yesAgronomy Journal, Volume 118, Issue 1, January/February 2026.
Abstract Intercropping has the potential to help adapt arable agriculture to climate change, but its effects on soil carbon and crop production in temperate agroecosystems remain uncertain. This study examined the effects of temperate intercropping systems on soil carbon and crop productivity.
Oludare S. Durodola   +5 more
wiley   +1 more source

Modification of FAO Penman–Monteith equation for minor components of energy [PDF]

open access: yesHydrology Research, 2018
AbstractThe conventional Food and Agriculture Organization of the United Nations (FAO) Penman–Monteith (P-M) equation requires knowledge of the available energy to estimate reference evapotranspiration (ETo); however, it is common to ignore the minor energy components (MECs). This study was conducted to determine the effect of not including the MECs in
John H. Prueger   +2 more
openaire   +1 more source

FAO crop coefficient and plant‐available water: Do soil and plant hydraulic properties matter?

open access: yesAgronomy Journal, Volume 118, Issue 1, January/February 2026.
Abstract How to ensure that “the availability of soil water does not limit plant growth or transpiration?” Determining the so‐called crop coefficient (Kc) relies on this assumption of optimal or non‐limiting soil water conditions, which, in turn, is understood as the soil water content at field capacity, a parameter with, de facto, no relation to ...
Marina Luciana Abreu de Melo   +3 more
wiley   +1 more source

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