Abstract:Abstract. Leaf transpiration and energy exchange are coupled processes that operate at small scales yet exert a significant influence on the terrestrial hydrological cycle and climate. Surprisingly, experimental capabilities required to quantify the energy-transpiration coupling at the leaf scale are lacking, challenging our ability to test basic questions of importance for resolving large-scale processes. The present study describes an experimental set-up for the simultaneous observation of transpiration rate… Show more
“…Model outputs were validated using a leaf replica with a known conductance to water vapor subjected to the same fluctuating conditions. Although leaf replicas have been used in the past to study the importance of mass transfer in leaf energy balance (Zwieniecki et al , 2016; Schymanski and Or, 2017; Schymanski et al , 2017), our results highlight the potential of the low-cost leaf replica and references to validate leaf temperature predictions obtained using energy balance equations. The ability to derive g sw from thermography under a fluctuating environment using a relatively simple set-up opens the way to field measurements in the future, but will require further improvements to take into consideration parameters such as leaf orientations and local variations in L d .…”
Spatiotemporal co-ordination of the stomatal response to light intensity over the lamina of different wheat leaves was assessed using a novel dynamic energy balance model.
“…Model outputs were validated using a leaf replica with a known conductance to water vapor subjected to the same fluctuating conditions. Although leaf replicas have been used in the past to study the importance of mass transfer in leaf energy balance (Zwieniecki et al , 2016; Schymanski and Or, 2017; Schymanski et al , 2017), our results highlight the potential of the low-cost leaf replica and references to validate leaf temperature predictions obtained using energy balance equations. The ability to derive g sw from thermography under a fluctuating environment using a relatively simple set-up opens the way to field measurements in the future, but will require further improvements to take into consideration parameters such as leaf orientations and local variations in L d .…”
Spatiotemporal co-ordination of the stomatal response to light intensity over the lamina of different wheat leaves was assessed using a novel dynamic energy balance model.
“…Such independent control may help to prevent excess water loss from the mesophyll positioned in close proximity of open stomata on the sunlit leaf side. Substantial differences in surface temperatures between sunlit (nontranspiring) and shaded transpiring sides of leaves have been found through detailed modelling of the leaf energy balance (0.2–0.3°C; Buckley et al ., ) and through experiments with leaf replicas (Schymanski et al ., ). The wider occurrence of independent control on adaxial vs abaxial stomatal conductance, as well as the potential benefit in terms of water‐use efficiency, remain to be determined.…”
Section: Prospective Future Researchmentioning
confidence: 97%
“…The interaction between stomatal distribution and leaf temperature also has the potential to influence photosynthetic efficiency under specific conditions. By spatially separating evaporative cooling from light absorption and photosynthesis, hypostomatous leaves could reduce transpiration, thereby increasing longwave and sensible heat emissions (Schymanski et al ., ) and, when leaf temperature is below optimal, slightly increase photosynthetic efficiency on the slightly warmer sun‐exposed leaf side. By contrast, the amphistomatous leaf morphology may achieve slight increases in photosynthetic efficiency when leaf temperature is above optimal (as is more likely in arid environments) by spatially coupling evaporative cooling to the photosynthetically active tissue.…”
Summary
Leaves with stomata on both upper and lower surfaces, termed amphistomatous, are relatively rare compared with hypostomatous leaves with stomata only on the lower surface. Amphistomaty occurs predominantly in fast‐growing herbaceous annuals and in slow‐growing perennial shrubs and trees. In this paper, we present the current understanding and hypotheses on the costs and benefits of amphistomaty related to water and CO2 transport in contrasting leaf morphologies. First, there is no evidence that amphistomatous species achieve higher stomatal densities on a projected leaf area basis than hypostomatous species, but two‐sided gas exchange is less limited by boundary layer effects. Second, amphistomaty may provide a specific advantage in thick leaves by shortening the pathway for CO2 transport between the atmosphere and the chloroplasts. In thin leaves of fast‐growing herbaceous annuals, in which both the adaxial and abaxial pathways are already short, amphistomaty enhances leaf–atmosphere gas‐exchange capacity. Third, amphistomaty may help to optimise the leaf‐interior water status for CO2 transport by reducing temperature gradients and so preventing the condensation of water that could limit CO2 diffusion. Fourth, a potential cost of amphistomaty is the need for additional investments in leaf water transport tissue to balance the water loss through the adaxial surface.
“…The standard deviations of the MODIS Aqua day-night overpass time over the study sites were found to be within 30-45 min (Sharifnezhadazizi et al, 2019), and the expected deviation in LST from the mean local time would be around ±0. 75 K (Sharifnezhadazizi et al, 2019).…”
Section: Possible Sources Of Errors In Seb Flux Evaluationmentioning
Abstract. One of the major undetermined problems in evaporation (ET) retrieval using thermal infrared remote sensing is the lack of a physically based ground
heat flux (G) model and its integration within the surface energy balance
(SEB) equation. Here, we present a novel approach based on coupling a
thermal inertia (TI)-based mechanistic G model with an analytical surface
energy balance model, Surface Temperature Initiated Closure (STIC, version
STIC1.2). The coupled model is named STIC-TI. The model is driven by
noon–night (13:30 and 01:30 local time) land surface temperature, surface albedo, and a vegetation index from MODIS Aqua in conjunction with a clear-sky net
radiation sub-model and ancillary meteorological information. SEB flux
estimates from STIC-TI were evaluated with respect to the in situ fluxes from eddy covariance measurements in diverse ecosystems of contrasting aridity in both
the Northern Hemisphere and Southern Hemisphere. Sensitivity analysis revealed substantial sensitivity of STIC-TI-derived fluxes due to the land surface temperature
uncertainty. An evaluation of noontime G (Gi) estimates showed 12 %–21 % error across six flux tower sites, and a comparison between STIC-TI versus empirical G models also revealed the substantially better performance
of the former. While the instantaneous noontime net radiation (RNi) and
latent heat flux (LEi) were overestimated (15 % and 25 %), sensible
heat flux (Hi) was underestimated (22 %). Overestimation
(underestimation) of LEi (Hi) was associated with the
overestimation of net available energy (RNi−Gi) and use of
unclosed surface energy balance flux measurements in LEi (Hi) validation. The mean percent deviations in Gi and Hi estimates were found to be
strongly correlated with satellite day–night view angle difference in
parabolic and linear pattern, and a relatively weak correlation was found
between day–night view angle difference versus LEi deviation. Findings
from this parameter-sparse coupled G–ET model can make a valuable contribution to mapping and monitoring the spatiotemporal variability of
ecosystem water stress and evaporation using noon–night thermal infrared observations from future Earth observation satellite missions such as
TRISHNA, LSTM, and SBG.
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