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. 2024 Apr 15:6:0169.
doi: 10.34133/plantphenomics.0169. eCollection 2024.

Practical Considerations and Limitations of Using Leaf and Canopy Temperature Measurements as a Stomatal Conductance Proxy: Sensitivity across Environmental Conditions, Scale, and Sample Size

Affiliations

Practical Considerations and Limitations of Using Leaf and Canopy Temperature Measurements as a Stomatal Conductance Proxy: Sensitivity across Environmental Conditions, Scale, and Sample Size

Ismael K Mayanja et al. Plant Phenomics. .

Abstract

Stomatal conductance (gs) is a crucial component of plant physiology, as it links plant productivity and water loss through transpiration. Estimating gs indirectly through leaf temperature (Tl) measurement is common for reducing the high labor cost associated with direct gs measurement. However, the relationship between observed Tl and gs can be notably affected by local environmental conditions, canopy structure, measurement scale, sample size, and gs itself. To better understand and quantify the variation in the relationship between Tl measurements to gs, this study analyzed the sensitivity of Tl to gs using a high-resolution three-dimensional model that resolves interactions between microclimate and canopy structure. The model was used to simulate the sensitivity of Tl to gs across different environmental conditions, aggregation scales (point measurement, infrared thermometer, and thermographic image), and sample sizes. Results showed that leaf-level sensitivity of Tl to gs was highest under conditions of high net radiation flux, high vapor pressure deficit, and low boundary layer conductance. The study findings also highlighted the trade-off between measurement scale and sample size to maximize sensitivity. Smaller scale measurements (e.g., thermocouple) provided maximal sensitivity because they allow for exclusion of shaded leaves and the ground, which have low sensitivity. However, large sample sizes (up to 50 to 75) may be needed to differentiate genotypes. Larger-scale measurements (e.g., thermal camera) reduced sample size requirements but include low-sensitivity elements in the measurement. This work provides a means of estimating leaf-level sensitivity and offers quantitative guidance for balancing scale and sample size issues.

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Conflict of interest statement

Competing interests: The authors declare that they have no competing interests.

Figures

Fig. 1.
Fig. 1.
Typical response of leaf temperature (Tl) to varying stomatal conductance (gs). As gs increases, the sensitivity of Tl to gs (or slope of the curve) decreases. Tdry is the leaf temperature when gs is 0, Twet is the leaf temperature of an equivalent wet surface with unlimited supply of free water, and TΔ is the difference between Tdry and Twet.
Fig. 2.
Fig. 2.
Schematic diagram showing the different levels of aggregation used in simulated Tl measurement, scaling with an increase in the level of complexity from a single isolated leaf parallel to the ground, to a single-layer canopy of leaves randomly orientated with no self-shading, to a canopy average, and an image average representative of an aerial thermal image of the homogeneous canopy.
Fig. 3.
Fig. 3.
Field and simulated data for (A) Tl and (B) gs averaged across each genotype. The simulated Tl and gs are in an acceptable range with measured field data, which shows that the developed sorghum geometry can reliably produce acceptable simulations. The hat operator denotes a spatial average.
Fig. 4.
Fig. 4.
Variation in the sensitivity (S) of leaf temperature to stomatal conductance with changes in ambient conditions and stomatal conductance (gs). Each subplot represents different combinations of relative humidity (Rh) ranging from 0.2 to 0.8 and air temperature (Tair) varying from 10 to 40C. The columns correspond to different gs ranging from 0 to 1  mol  m−2  s−1. (A to F) Conditions for a sunlit leaf (RSW = 300  W  m−2). (G to L) Shaded leaf (RSW = 50  W  m−2). The wind speed (U) remains constant within each row, with (A) to (C) and (G) to (I) having U of 1  m  s−1, and (D) to (F) and (J) to (L) having U of 5  m  s−1. To interpret this plot, a subplot is selected based on ambient radiation level, wind speed, and expected stomatal conductance. The S value can be determined by matching the surface color at the given ambient air temperature and humidity to the associated value in the color bar.
Fig. 5.
Fig. 5.
Relationship between Tl and gs for different levels of aggregation at constant ambient conditions of 30C  (Tair), 0.5  (Rh), and 1  m  s−1  (U). (A) Trend of an isolated single leaf with absorbed radiation flux RSW of 50, 300, and 600 W  m−2. The line plots of the single leaf were replotted in (B) to (D) to show how the single leaf Tl − gs trend relates when scaling at a canopy level. Each spike shown in (B) (single layer), (C) (canopy average with sunlit leaves), and (D) (canopy average with shaded leaves) is a single Em value, which was set in the stomatal conductance model to vary the gs values. (D and F) Aerial thermal image (image average) of the homogeneous canopy for sunlit and shaded thermal pixels, respectively. The brighter yellow colors in (D) and (F) shows the highest density of thermal pixel data points.
Fig. 6.
Fig. 6.
The fraction of sunlit leaves (fsun) with varying LAI is shown for (A) canopy average and (B) image average, which also includes how much of the ground is viewed in a thermal image (fground) for different LAI (fground does not change with solar zenith angle). Variation in average S with varying gs, LAI, solar zenith, and aggregation scale is shown in (C) to (I): (C) single-layer canopy, (D) canopy average with LAI = 0.5, (E) canopy average with LAI = 1.5, (F) canopy average with LAI = 3, (G) image average with LAI = 0.5, (H) image average with LAI = 1.5, and (I) image average with LAI = 3. The single layer generally has the highest S because there are no shaded leaves. For the canopy averages, S decreases with an increase in LAI due to the increase in the fraction of shaded leaves. For the image averages, S increases with an increase in LAI due to the decrease in ground exposure. The hat operator denotes a spatial average.
Fig. 7.
Fig. 7.
(A) Visualization of 3D model sorghum canopy. (B) Example of simulated aerial thermal images captured by the thermal camera for five sorghum genotypes under conditions of high S (favorable) and low S (unfavorable). Images show the difference between surface temperature and ambient air temperature (Tair = 40.3C for favorable, and Tair = 14.1C for unfavorable) in order to increase contrast.
Fig. 8.
Fig. 8.
Ability of the thermal camera to detect a difference in average stomatal conductance among sorghum genotypes for varying camera viewing angles and environmental conditions. (A) to (C) compare different viewing angles at environmental conditions with moderate sensitivity: (A) 0, (B) 15, and (C) 30 between the thermal camera viewing direct and sun direction. (D) Results for a viewing direction of 0, but unfavorable conditions. Error bars indicate standard deviation. Groups sharing the same letter are not statistically different from each other at a significance level of α= 0.05, based on Dunn’s post hoc analysis following Kruskal–Wallis test. S had the same significance designations as Tl, and gs is significantly different across genotypes for all cases. The hat operator denotes a spatial average.
Fig. 9.
Fig. 9.
Violin plots showing the Tl distribution across genotypes for (A) thermocouple and (B) IR thermometer conducted under favorable conditions (Tair = 40.3C, Rh = 0.18, U = 2.77 m s−1). gs of the genotypes decreases from left to right, and the horizontal dotted lines represent the air temperature. The hat operator on T^l denotes that average values of Tl were considered in this scenario.

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