Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/114356
DC FieldValueLanguage
dc.contributorDepartment of Mechanical Engineeringen_US
dc.contributorResearch Institute for Smart Energyen_US
dc.creatorDong, Pen_US
dc.creatorChang, Hen_US
dc.creatorDeng, Nen_US
dc.creatorGuo, Sen_US
dc.creatorLi, Men_US
dc.date.accessioned2025-07-25T06:13:49Z-
dc.date.available2025-07-25T06:13:49Z-
dc.identifier.issn1359-4311en_US
dc.identifier.urihttp://hdl.handle.net/10397/114356-
dc.language.isoenen_US
dc.publisherPergamon Pressen_US
dc.subject3-D multiphysics modelen_US
dc.subjectAir–water interface temperatureen_US
dc.subjectNatural convectionen_US
dc.subjectOpen-water evaporationen_US
dc.subjectRelative humidityen_US
dc.subjectRoll patternen_US
dc.titleMultiphysics modeling of open-water evaporation : quantifying the natural convection effects of wateren_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume278en_US
dc.identifier.doi10.1016/j.applthermaleng.2025.126964en_US
dcterms.abstractIn this study, we develop a three-dimensional (3-D) numerical model using COMSOL Multiphysics to estimate water evaporation from open-water bodies, rigorously validated against experimental data from the literature, demonstrating satisfactory accuracy. Through comprehensive simulations, we elucidate the evolving patterns of evaporation with natural convection in diverse environmental conditions, including temperature, wind speed, and relative humidity. Specifically, under windless conditions, the evaporation rate initially decreases due to moisture accumulation and subsequently increases, as determined by the temperature at the air–water interface. In contrast, under windy conditions, the evaporation rate consistently decreases, solely dictated by this temperature. In addition, our findings underscore the critical role of natural convection within the water body in influencing evaporation rates under both windy and windless conditions. Specifically: 1) Neglecting the contribution of natural convection within the water body results in significant discrepancies in evaporation rate estimations, over 2.5 times in windless conditions, 2.5 times at 2 m/s, and 1.5 times at 5 m/s, due to the lower heat transfer rate of conduction compared to convection. 2) In the absence of external heat input, the omission of natural convection reduces the evaporation rate by 2 times under windless conditions, 1.05 times at 2 m/s, and 1.02 times at 5 m/s. Finally, the roll pattern of Rayleigh–Bénard convection in a water body is analyzed, which is primarily dominant by external heat, even in windy conditions. Without external heat, the wind takes over as the main factor affecting the evaporation rate. In the absence of both external heat and wind, natural convection in the air becomes the dominant factor for evaporation. This numerical investigation expands the validity of current methods for estimating evaporation from open-water bodies under complex environmental conditions.en_US
dcterms.accessRightsembargoed accessen_US
dcterms.bibliographicCitationApplied thermal engineering, 1 Nov. 2025, v. 278, pt. A, 126964en_US
dcterms.isPartOfApplied thermal engineeringen_US
dcterms.issued2025-11-01-
dc.identifier.scopus2-s2.0-105008217861-
dc.identifier.eissn1873-5606en_US
dc.identifier.artn126964en_US
dc.description.validate202507 bchyen_US
dc.description.oaNot applicableen_US
dc.identifier.SubFormIDG000034/2025-07-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThe authors gratefully acknowledge the substantial support from Jiangsu Province Science and Technology Department (Project No. BZ2021057) and from the Research Grants Council of the Hong Kong Special Administrative Region, China (Project No. C6003-22Y).en_US
dc.description.pubStatusPublisheden_US
dc.date.embargo2027-11-01en_US
dc.description.oaCategoryGreen (AAM)en_US
Appears in Collections:Journal/Magazine Article
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Embargo End Date 2027-11-01
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