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Development of a lightweight, portable, waterproof, and low power stem respiration system for trees

The Science
Stem respiration is a quantitatively important, but poorly understood component of ecosystem carbon cycling in terrestrial ecosystems. However, a dynamic stem gas exchange system for quantifying real-time stem carbon dioxide (CO2) efflux (Es) is not commercially available resulting in limited observations based on the static method where air is recirculated through a stem enclosure. The static method has limited temporal resolution, suffers from condensation issues, requires a leak-free enclosure, which is often difficult to verify in the field, and requires physically removing the chamber or flushing it with ambient air before starting each measurement. Here we present the design of a custom system for real-time off the grid monitoring of stem CO2 efflux from diverse tropical forests.

The Impact
The system is low cost, lightweight, and waterproof with low power requirements (1.2-2.4 W) for real-time monitoring of stem Esusing a 3D printed dynamic stem chamber and a 12V car battery. Great success was achieved with this system in the Amazon during the rainy season in 2022. This method allows for the use of real-time stem CO2 efflux measurements to evaluate diurnal patterns of growth and respiration in hyper diverse forests to help resolve some major uncertainties surrounding stem respiration. While temperature is assumed to stimulate growth and its associated respiratory processes, preliminary real-time diurnal data collected with the technique suggest that plant hydraulics are also key, with mid-day water stress in the dry season limiting plant growth and respiratory process. The deployment of the techniques to remote tropical forests in Brazil will allow us to link plant hydraulics and carbon metabolism in ecosystem demographics models like FATES.

Summary
Stem respiration is a quantitatively important, but poorly understood component of ecosystem carbon cycling in terrestrial ecosystems. However, a dynamic stem gas exchange system for quantifying real-time stem carbon dioxide (CO2) efflux (Es) is not commercially available resulting in limited observations based on the static method where air is recirculated through a stem enclosure. The static method has limited temporal resolution, suffers from condensation issues, requires a leak-free enclosure, which is often difficult to verify in the field, and requires physically removing the chamber or flushing it with ambient air before starting each measurement.

With the goal of improving our quantitative understanding of biophysical, physiological, biochemical, and environmental factors that influence diurnal Espatterns, here we present a custom system for quantifying real-time stem Esin remote tropical forests. The system is low cost, lightweight, and waterproof with low power requirements (1.2-2.4 W) for real-time monitoring of stem Esusing a 3D printed dynamic stem chamber and a 12V car battery. The design offers control over the flow rate through the stem chamber, eliminates the need for a pump to introduce air into the chamber, and water condensation issues by removing water vapor prior to CO2analysis. Following a simple CO2infrared gas analyzer (IRGA) calibration and match procedure with a 400-ppm standard, we quantified diurnal Esobservations over a 24-hours period during the summer growing season from an ash tree (Fraxinus sp.) in Fort Collins, Colorado. The results are consistent with previous laboratory and field studies that show Es can be suppressed during the day relative to the night.

Figure: Simplified diagram of the portable stem respiration system showing ambient air and stem gas flow, 12 VDC electrical circuit, and real-time CO2 concentration data from the stem chamber and ambient air buffer volume. Image credit: Kolby Jardine.

 

 

Contact: Kolby Jardine, Research Scientist, LBNL: Earth and Environmental Sciences Area, Ecology Department (kjjardine@lbl.gov)

Funding
Support for this research was provided as part of the Next Generation Ecosystem Experiments-Tropics (NGEE-Tropics) funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research through contract No. DE-AC02-05CH11231 to LBNL, as part of DOE’s Terrestrial Ecosystem Science Program. We kindly acknowledge Christina Wistrom for her support at the UC Berkeley Oxford Tract Greenhouse where the method was developed and Bryan Taylor at LBNL for support with computer systems and software.

Publication: Jardine, K., Augusto, E., Levine, S. D., Sunder, A., Som, S., & Chambers, J. (2023). Development of a lightweight, portable, waterproof, and low power stem respiration system for trees. MethodsX, 10, 101986. https://doi.org/10.1016/j.mex.2022.101986.

Where are the degraded forests in the Amazon, and how much carbon do they lose?

Using high-resolution remote sensing and machine learning, researchers detected forest degradation, and found that forests lose 35% of carbon after fires

The Science
Forest degradation through fires and logging are widespread in the Amazon. Forest degradation changes the forest structure, but it is difficult to detect from space. A team of researchers used commercial satellites with very high resolution, and developed a machine learning system to automatically distinguish intact forests from logged or burned forests. They also used laser sensors on an aircraft to calculate how much carbon forests lose when they are degraded. To get the most precise impact of forest degradation on carbon stocks, the team considered that both their classification and their carbon stocks have uncertainties.

The Impact
The research team found that their machine learning method distinguishes degraded forests from intact forests in 86% of the cases. Sometimes the machine learning approach confuses logged forests with intact forests, but it is very good at identifying burnt areas. The team found that logged forests have almost the same amount of carbon as intact forests. However, forest fires can reduce the amount of carbon by 35%. The team also found that they needed to account for the confusion of the machine learning classification of forest degradation to correctly attribute carbon losses to forest degradation classes.

Summary
Forest degradation from logging and fires impacts large areas of tropical forests. However, the impact of degradation on carbon stocks remains uncertain because degradation is difficult to detect. This research used high resolution images from PlanetScope and produced a series of metrics that described the forest canopy texture. These metrics were then used to train a machine learning classifier that calculated the probability of forests being intact, burned or logged. The team also used biomass estimates from airborne lidar to calculate the impact of forest degradation on carbon stocks.

The classification approach has an accuracy between 0.69 and 0.93, depending on the site. This study found that changes in carbon stocks due to logging were small, but burned forests store 35% less carbon than intact forests. The team expected and found that uncertainty in carbon losses due to degradation increases when they account for the uncertainty in classification. However, they found that ignoring classification uncertainty could underestimate the impact of degradation on carbon stocks.

Figure: Examples of intact forests (left) and forests degraded by selective logging (middle) and fires (right) in the Amazon forest. Forest degradation changes forest structure that can be detected from high-resolution satellites. Photos by Marcos Longo.

 

Contact: Ekena Rangel Pinagé, College of Forestry, Oregon State University (rangelpe@oregonstate.edu)
Marcos Longo, Lawrence Berkeley National Laboratory, (mlongo@lbl.gov)

Funding
This research was funded by the NASA Land Cover and Land Use Change Program, and by the Next Generation Ecosystem Experiments-Tropics, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research. The research carried out at the Jet Propulsion Laboratory, California Institute of Technology, was under a contract with the National Aeronautics and Space Administration.

Publication: Pinagé, E. R., M. Keller, C. P. Peck, M. Longo, P. Duffy, and O. Csillik, 2023: Effects of forest degradation classification on the uncertainty of aboveground carbon estimates in the Amazon. Carbon Balance and Management, 18 (1), 2, doi:10.1186/s13021-023-00221-5.

Do small changes in topography influence tree characteristics in an Amazon forest?

ForestGEO scientists measured branch, leaf, and stomatal traits from one thousand trees to explore the sources of trait variability and dynamics among and within Amazon tree species.

The Science
Previous work in Amazon forests has shown significant variation in both tree species distribution and drought-induced tree mortality across small ridges and valleys. Forest ecologists measured 18 branch, leaf, and stomatal traits on 1,077 trees of 72 dominant species to identify the underlying functional traits driving such changes across topography while controlling for a highly documented source of trait variability within species—tree size. Researchers found large trait variability across trees within species (i.e., intraspecific) that was related to trees’ topographic location for leaf traits and tree size for branch and stomatal traits.

The Impact
This study demonstrates the importance of accounting for intraspecific trait variation when testing trait-environment relationships and suggests tree size as a critical source of variability to be included in mechanistic models aiming to predict forest dynamics. The next steps include quantifying physiological traits, functional rooting depths, and water table dynamics to comprehensively understand trees’ vulnerability to climatic drivers (e.g., droughts) and their implications for forest composition and ecosystem services.

Summary
Tropical forest responses to variation in water availability, which are critical for understanding and predicting the effects of climate change, depend on trait variation among trees. ForestGEO scientists quantified interspecific (among species) and intraspecific (across trees within species) variation in 18 branch, leaf and stomatal traits for 72 dominant tree species along a local topographic gradient in an aseasonal Amazon terra firme forest. They used these sampling design to test trait relationships with tree size, elevation, and species’ topographic associations as well as trait correlations. Intraspecific trait variation was substantial and exceeded interspecific variation in 10 of 18 traits. For leaf acquisition traits, intraspecific variation was mainly related to tree topographic elevation, while most of the variation in branch, leaf and stomatal traits was related to tree size. Interspecific variation showed no clear relationships with species’ habitat association. Although trait correlations and coordinations were generally maintained among trees and among species, bivariate relationships varied among trees within species, across habitat association classes and across tree size classes. These results demonstrate the magnitude and importance of intraspecific trait variation in tropical trees, especially as related to tree size. Furthermore, these results indicate that previous findings relating interspecific variation with topographic association in seasonal forests do not necessarily generalize to aseasonal forests.

Figure: Some of the hundred thousand trees monitored in the Amacayacu Forest Dynamics Plot, Northwestern Amazon. Image courtesy of Daniel Zuleta; Photo credit Sebastian Ramirez.

 

 

 

Contact: Daniel Zuleta, Forest Global Earth Observatory, Smithsonian Tropical Research Institute (dfzuleta@gmail.com)

Funding
D. Zuleta was supported by the National Doctoral Scholarship COLCIENCIAS-Colombia (647, 2015-II), the Smithsonian Tropical Research Institute Short-Term Fellowships and the Next Generation Ecosystem Experiments-Tropics, funded by the US Department of Energy, Office of Science, Office of Biological and Environmental Research (https://ngee-tropics.lbl.gov/). Data collection was supported by the Forest Global Earth Observatory (ForestGEO) of the Smithsonian Institution and Universidad Nacional de Colombia.

Publications
Zuleta, D., Muller-Landau, H.C., Duque, A., Caro, N., Cardenas, D., Castaño, N., León-Peláez, J.D., and Feeley, K.J. “Interspecific and intraspecific variation of tree branch, leaf and stomatal traits in relation to topography in an aseasonal Amazon forest.” Functional Ecology 36, 2955– 2968 (2022). [DOI: 10.1111/1365-2435.14199]

Related Links
https://functionalecologists.com/2022/12/08/daniel-zuleta-do-small-scale-changes-in-topography-affect-functional-trait-variability-in-an-aseasonal-amazon-forest/

https://fesummaries.wordpress.com/2022/10/12/from-ridge-to-valleys-do-trees-have-different-characteristics-along-a-short-topographic-gradient-in-an-aseasonal-amazon-forest/

Climate Change likely to cause more windthrows in the Amazon

The connection between convective storms and tree mortality in the Amazon projects a large increase in future windthrow events.

The Science
A leading cause of tree mortality in the Amazon is windthrow, i.e., tree broken or uprooted by high winds and heavy rainfall in an extreme storm. Here we built a linkage between extreme storms in the atmosphere and forest mortality on the land surface. Global warming makes extreme storms more intense, and using this linkage, the projected storms are likely to make tree mortality by windthrow commonplace over about 50% more of the Amazon by the end of the century.

The Impact
Amazon forests play important roles in regulating global carbon cycle, but variable natural disturbances increase the uncertainty of the carbon capacity. Extreme storms are important drivers of tree mortality in the Amazon region. In this study, we provide a framework for representing the coupling between forest mortality on the land surface and extreme storms in the atmosphere. This analysis highlights the potential for predicting the rate of future storm-driven tree mortality, a driver of tree mortality that currently is not included in global models and emphasizes the need to improve land-atmosphere relationship in models.

Summary
Forest mortality caused by convective storms (windthrow) is a major disturbance in the Amazon. However, the linkage between windthrows at the surface and convective storms in the atmosphere remains unclear. In addition, the current Earth system models (ESMs) lack mechanistic links between convective wind events and tree mortality. In this study, we manually map 1012 large windthrow events encompassing 30 years from 1990-2019 and generate hourly convective available potential energy (CAPE, which represents the environment to produce storms) from ERA5 reanalysis data. Here we find an empirical relationship that maps CAPE, which is well simulated by ESMs, to the spatial pattern of large windthrow events. This relationship builds connections between strong convective storms and forest dynamics in the Amazon. Based on the relationship, our model projects a 51% ± 20% increase in the area favorable to extreme storms, and a 43 ± 17% increase in windthrow density within the Amazon by the end of this century under the high-emission scenario (SSP 585). These results indicate significant changes in tropical forest composition and carbon-cycle dynamics under climate change.

Figure. The spatial pattern of windthrows matches well with the meteorological variable, convective available potential energy (CAPE), which represents the favorable environment to produce storms. Image courtesy of Yanlei Feng, UC Berkeley

 

 

Contact
Yanlei Feng, University of California, Berkeley, ylfeng@berkeley.edu
Jeffrey Chambers, Lawrence Berkeley National Lab, jchambers@lbl.gov

Funding
This research was supported as part of the Next Generation Ecosystem Experiments-Tropics, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research under contract number DE-AC02-05CH11231. We acknowledge the World Climate Research Programme, which, through its Working Group on Coupled Modelling, coordinated and promoted CMIP6. We thank the climate modeling groups for producing and making available their model output, the Earth System Grid Federation (ESGF) for archiving the data and providing access, and the multiple funding agencies who support CMIP6 and ESGF.

Publications
Feng, Y., et al., “Amazon windthrow disturbances are likely to increase with storm frequency under global warming”. Nature Communications, 14(1), pp.1-8, (2023), [DOI: 10.1038/s41467-022-35570-1]

Related Links
Climate Change Likely to Uproot More Amazon Trees, News from Berkeley Lab
Storms are a major source of forest mortality in the Amazon, Earth.com
Thunderstorms Caused by Climate Change Will Most Likely Increase the Number of Large Windthrow Events in the Amazon, Nature World News

Tree Leaves Act as Bottlenecks to Water Flow in the Transpiration Stream

Disproportionate resistance to water flow in leaves helps trees maintain their vascular function, but the effect declines as trees grow larger.

Image courtesy of Edwin Andrade.

Researchers used cranes to access tree crowns for measurements of pressure gradients within trees, which were used to assess the constriction of water flow within leaves. Image courtesy of Edwin Andrade. Researchers used cranes to access tree crowns for measurements of pressure gradients within trees, which were used to assess the constriction of water flow within leaves.

The Science
Trees move large quantities of water from soil to the atmosphere in the transpiration stream, forming a major component in Earth’s water cycle. Water in the transpiration stream is pulled through trees under tension (i.e., negative pressure) in specialized conduits. When tension is excessive, vascular disfunction occurs. Compared to conduits in roots and stems, leaf conduits constrict water flow. This constriction reduces tension upstream, protecting stem and leaves from vascular disfunction. Variation among trees in this constriction is not well resolved. This study assessed variation in the extent to which tree leaves constrict water flow in the transpiration stream.

The Impact
Results showed that, on average, about half the total resistance to water flow within trees is located within leaves. This indicates that tree leaves are generally highly constrictive to water flow in the transpiration stream. Larger trees tended to have a lower proportion of total resistance to water flow within their leaves. This suggests that leaves in larger trees are less effective at protecting stems and roots from vascular disfunction associated with high water tension. These results help to understand and predict transpiration rates and tree mortality during droughts and heat waves.

Summary
Researchers compiled new and previously published measurements into a multibiome dataset to assess variation among trees in the fraction of whole-tree hydraulic resistance that is in leaves (fRleaf). The measurements relied on pressure differences between leaves, stems, and roots in transpiring trees. Among 80 samples, fRleaf averaged 0.51, was consistent among biomes, and declined with tree height. The results show that leaves play an important role in controlling the flow rate and tension of water in the transpiration stream. Because higher fRleaf protects stems from vascular disfunction and fRleaf declines with tree height, taller trees may be at greater risk of vascular disfunction during droughts. This effect may contribute to the disproportionate drought mortality that has been observed among tall trees.

Contact
Brett Wolfe
Louisiana State University Agricultural Center
wolfe1@lsu.edu 

Funding
Next-Generation Ecosystem Experiments‐Tropics funded by the US Department of Energy, Office of Science, Office of Biological and Environmental Research; United States Department of Energy contract to Brookhaven National Laboratory; Smithsonian Tropical Research Institute post-doctoral fellowship; National Institute of Food and Agriculture, US Department of Agriculture, McIntire Stennis Project; Innovation and Technology Fund (funding support to State Key Laboratories in Hong Kong of Agrobiotechnology) of the HKSAR, China; US National Science Foundation; USDA NIFA Hatch Project through the Maine Agricultural and Forest Experiment Station. 

Publications
Wolfe, B. T. et al. Leaves as bottlenecks: The contribution of tree leaves to hydraulic resistance within the soil−plant−atmosphere continuum. Plant, Cell & Environment 46, 736–746 (2023). [DOI: 10.1111/pce.14524]

Windthrows Characteristics and their Regional Association with Rainfall, Soil and Surface elevation in the Amazon

Amazon windthrows characteristics driven by environmental variables

The Science
Windthrows (trees uprooted and broken by winds) are common across the Amazon and affect forest dynamics, composition, structure, and carbon balance. Yet, the current understanding of the spatial variability of windthrows is limited. We present the first study to examine the occurrence, area, and direction of windthrows and the control that environmental variables exert on them across the whole Amazon.

The Impact
We found that windthrows are more frequent and larger in the northwestern and the central Amazon. The predominant direction of windthrows is westward. Rainfall, surface elevation, and soil characteristics explain the variability of windthrows but their effects vary regionally. A better understanding of the spatial dynamics of windthrows will improve understanding of the functioning of Amazon forests.

Summary
A total of 392 Landsat 8 images covering the entire Amazon were used and 1116 windthrows were identified based on their shape and spectral characteristics over a 30-year period. Windthrows were integrated with environmental data in a geospatial analysis framework.

Figure. Characteristics of windthrows in the Amazon and their regional distribution in the Amazon.  The Amazon region is represented by the green contour line. Kernel density map for windthrow occurrence. Windthrow density map used a kernel of 1° radius and was resampled at 0.1°. Black dots represent the observed windthrows. Selected environmental variables include mean annual rainfall, surface elevation and soil organic carbon. Windthrows density and environmental variables were used to determine Regions of Windthrows determined by a regionalization analysis. The regionalization analysis used the Queen weighting method. The number of windthrows in Regions 1 to 4 are 390, 291, 297, and 44, respectively.

Contact
Robinson Negron-Juarez, Lawrence Berkeley National Lab, Staff Scientist (robinson.inj@lbl.gov)

Funding
This study was supported by the Office of Science, Office of Biological and Environmental Research of the US Department of Energy, Agreement grant. DE-AC02-05CH11231, Next Generation Ecosystem Experiments-Tropics, and the Office of Science’s Regional and Global Model Analysis of the US Department of Energy, Agreement grant. DE-AC02-05CH11231, Reducing Uncertainties in Biogeochemical Interactions through Synthesis Computation Scientific Focus Area (RUBISCO SFA).

Publications
Negron-Juarez, R.I., Marra, D., Feng, Y., Urquiza-Muñoz, J.D., Riley, W.J., Chambers, J.Q. Windthrows characteristics and their regional association with rainfall, soil and surface elevation in the Amazon (2022) Environ. Res. Lett. https://doi.org/10.1088/1748-9326/acaf10

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