Foliage temperature and latent heat flux of irrigated wheat

• Published in: Agricultural and forest meteorology Vol. 55; no. 1; pp. 133 - 147
• Main Authors: Dunin, F.X., Barrs, H.D., Meyer, W.S., Trevitt, A.C.F.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 1991; Oxford Elsevier; New York, NY
• Subjects: AGRICULTURA DE REGADIO; Agricultural and forest climatology and meteorology. Irrigation. Drainage; Agricultural and forest meteorology; Agronomy. Soil science and plant productions; Biological and medical sciences; BLE; CULTURE IRRIGUEE; FEUILLE; Fundamental and applied biological sciences. Psychology; General agronomy. Plant production; HOJAS; INFRARED RADIATION; IRRIGATED FARMING; LEAVES; RADIACION INFRARROJA; RAYONNEMENT INFRAROUGE; TEMPERATURA; TEMPERATURE; TRIGO; Water balance and requirements. Evapotranspiration; WHEATS; Australia; New South Wales; Oceania; Latent heat; Irrigation; Monocotyledones; Temperature; Heat flow; Evaporation; Cereal crop; Energy balance; Gramineae; Angiospermae; Foliage; Spermatophyta; Triticum aestivum
• ISSN: 0168-1923; 1873-2240
• DOI: 10.1016/0168-1923(91)90027-N

A series of 42 hourly measurements from a weighing lysimeter of foliage temperature provided a basis from which to evaluate the residual energy balance method for determining latent heat flux which incorporated foliage temperature measurements by an infrared thermometer. The measurements were taken regularly during daylight in a 2-ha field of irrigated wheat and covered a 14-day period ending at anthesis. The residual method ( λE T ) underestimated lysimeter latent heat loss ( λE L ) by 11% and accounted for 79% of the variance in λE L . Uncertainty in λE T ranged from overestimates of ∼ 35 W m −2 when advective effects were minimized with ∼ 95% profile adjustment to underestimates as high as 20% of λE L (approaching 200 W m −2) resulting from flux divergence in latent heat flux of comparable magnitude in causing advective enhancement of evaporation loss. This range in performance of λE T was explained in part owing to a variable fetch requirement, contributed to by atmospheric conditions of stability in influencing boundary layer development. The greatest uncertainty in λE T was observed during stable atmospheric conditions when foliage temperature lower than ambient accompanied significant local advective enhancement of crop evaporation.