Publications by authors named "Markus Reichstein"

The sensitivity of atmospheric CO growth rate to tropical temperature (γ) has almost doubled between 1959 and 2011, a trend that has been linked to increasing drought in the tropics. However, γ has declined since then. Understanding whether these variations in γ reflect forced changes or internal climate variability in the carbon cycle is crucial for future climate projections.

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  • Ecosystems act as both sources and sinks for atmospheric carbon (C), and their carbon use efficiency (CUE) is crucial for mitigating climate change.
  • Increased nitrogen (N) availability from human activities may lead to phosphorus (P) limitations in terrestrial ecosystems, affecting how plants and microorganisms utilize carbon.
  • In a Mediterranean tree-grass ecosystem study, it was found that wetter conditions and N fertilization improved CUE, but seasonal changes and potential longer dry summers could decrease CUE in the future.
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The response of vegetation physiology to drought at large spatial scales is poorly understood due to a lack of direct observations. Here, we study vegetation drought responses related to photosynthesis, evaporation, and vegetation water content using remotely sensed data, and we isolate physiological responses using a machine learning technique. We find that vegetation functional decreases are largely driven by the downregulation of vegetation physiology such as stomatal conductance and light use efficiency, with the strongest downregulation in water-limited regions.

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  • Scientists studied how plants use resources at the leaf level and wanted to see if similar patterns happen at the ecosystem level, which is a bigger area with lots of plants and animals.
  • They checked if three well-known theories about plant traits matched what happens in communities of plants and their ecosystems by analyzing data from many places.
  • They found that the patterns hold true at the ecosystem level, which could help create better models to predict how climate change affects nature.
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  • Soils are key carbon reservoirs, storing more carbon than other land ecosystems, but the mechanisms behind soil organic carbon (SOC) formation and persistence are still unclear, complicating predictions about their behavior in a changing climate.
  • Microorganisms are critical in influencing SOC through various processes, and microbial carbon use efficiency (CUE) serves as a key indicator of how these processes balance, impacting SOC storage.
  • Research suggests that CUE is significantly more important than other factors like carbon input or decomposition in determining SOC levels globally, and a better understanding of CUE and its environmental interactions could enhance predictions of SOC responses to climate change.
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Local studies and modeling experiments suggest that shallow groundwater and lateral redistribution of soil moisture, together with soil properties, can be highly important secondary water sources for vegetation in water-limited ecosystems. However, there is a lack of observation-based studies of these terrain-associated secondary water effects on vegetation over large spatial domains. Here, we quantify the role of terrain properties on the spatial variations of dry season vegetation decay rate across Africa obtained from geostationary satellite acquisitions to assess the large-scale relevance of secondary water effects.

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  • - This study focuses on how elevated atmospheric CO levels (eCO) affect plant carbon assimilation and water usage, impacting global carbon and water cycles.
  • - Researchers use a land surface model called QUINCY to simulate the effects of increasing CO on plant physiology and to develop a statistical method for detecting these effects amid natural variations in ecosystems.
  • - Findings show that eCO effects on carbon productivity can be detected at lower CO increases compared to their effects on water use, with stronger signals in forest ecosystems than in grasslands, providing insight for future observational studies.
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Extreme events, such as those caused by climate change, economic or geopolitical shocks, and pest or disease epidemics, threaten global food security. The complexity of causation, as well as the myriad ways that an event, or a sequence of events, creates cascading and systemic impacts, poses significant challenges to food systems research and policy alike. To identify priority food security risks and research opportunities, we asked experts from a range of fields and geographies to describe key threats to global food security over the next two decades and to suggest key research questions and gaps on this topic.

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Hydrological interactions between vegetation, soil, and topography are complex, and heterogeneous in semi-arid landscapes. This along with data scarcity poses challenges for large-scale modeling of vegetation-water interactions. Here, we exploit metrics derived from daily Meteosat data over Africa at ca.

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Global vegetation and associated ecosystem services critically depend on soil moisture availability which has decreased in many regions during the last three decades. While spatial patterns of vegetation sensitivity to global soil water have been recently investigated, long-term changes in vegetation sensitivity to soil water availability are still unclear. Here we assess global vegetation sensitivity to soil moisture during 1982-2017 by applying explainable machine learning with observation-based leaf area index (LAI) and hydro-climate anomaly data.

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Plant functional traits can predict community assembly and ecosystem functioning and are thus widely used in global models of vegetation dynamics and land-climate feedbacks. Still, we lack a global understanding of how land and climate affect plant traits. A previous global analysis of six traits observed two main axes of variation: (1) size variation at the organ and plant level and (2) leaf economics balancing leaf persistence against plant growth potential.

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  • Sun-induced fluorescence (SIF) is a valuable tool for assessing vegetation's gross primary production (GPP), but its effectiveness can be compromised during extreme weather events like heatwaves.
  • The 2018 European heatwave led to a reversal in the typical GPP-SIF relationship in evergreen broadleaved trees, primarily due to nonphotochemical quenching (NPQ) that protects plants from high light intensity.
  • This study reveals that extreme heat stress alters the energy allocation in plants, impacting the NPQ-SIF-GPP dynamics, highlighting limitations in current models that don't fully capture these complex interactions.
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The leaf economics spectrum and the global spectrum of plant forms and functions revealed fundamental axes of variation in plant traits, which represent different ecological strategies that are shaped by the evolutionary development of plant species. Ecosystem functions depend on environmental conditions and the traits of species that comprise the ecological communities. However, the axes of variation of ecosystem functions are largely unknown, which limits our understanding of how ecosystems respond as a whole to anthropogenic drivers, climate and environmental variability.

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Year-to-year changes in carbon uptake by terrestrial ecosystems have an essential role in determining atmospheric carbon dioxide concentrations. It remains uncertain to what extent temperature and water availability can explain these variations at the global scale. Here we use factorial climate model simulations and show that variability in soil moisture drives 90 per cent of the inter-annual variability in global land carbon uptake, mainly through its impact on photosynthesis.

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Empirical vegetation indices derived from spectral reflectance data are widely used in remote sensing of the biosphere, as they represent robust proxies for canopy structure, leaf pigment content, and, subsequently, plant photosynthetic potential. Here, we generalize the broad family of commonly used vegetation indices by exploiting all higher-order relations between the spectral channels involved. This results in a higher sensitivity to vegetation biophysical and physiological parameters.

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  • - The study compares three methods for estimating ecosystem transpiration from eddy covariance data across 251 FLUXNET sites worldwide, highlighting their high correlation (R between .89 and .94) despite differing in magnitude (T/ET ranging from 45% to 77%).
  • - The analysis shows that the estimated transpiration is more closely related to sap flow measurements than to other evapotranspiration estimates and that the transpiration-to-evapotranspiration ratio tends to increase with factors like drought conditions and leaf area index.
  • - Findings reveal that the main drivers of spatial variability in the transpiration-to-evapotranspiration ratio are vegetation and soil characteristics rather than climate, marking a significant improvement in understanding ecosystem transp
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The CONterminous United States (CONUS) presents a large range of climate conditions and biomes where terrestrial primary productivity and its inter-annual variability are controlled regionally by rainfall and/or temperature. Here, the response of ecosystem productivity to those climate variables was investigated across different biomes from 2010 to 2018 using three climate datasets of precipitation, air temperature or drought severity, combined with several proxies of ecosystem productivity: a remote sensing product of aboveground biomass, an net primary productivity (NPP) remote sensing product, an NPP model-based product and four gross primary productivity products. We used an asymmetry index (AI) where positive AI indicates a greater increase of ecosystem productivity in wet years compared to the decline in dry years, and negative AI indicates a greater decline of ecosystem productivity in dry years compared to the increase in wet years.

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  • The terrestrial carbon cycle's inter-annual variability (IAV) is closely connected to semi-arid ecosystems, making it critical to identify meteorological factors affecting these ecosystems and their responses to extreme events like droughts and heatwaves.
  • A four-year analysis of carbon fluxes at two FLUXNET sites in Spain revealed that the wetter ecosystem was less affected by soil water changes, while the drier site became a CO2 sink during wetter years.
  • The study indicates that the timing of droughts significantly impacts yearly carbon fluxes, emphasizing that drought events in spring or autumn are more crucial than summertime heatwaves.
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  • - The FLUXNET2015 dataset encompasses ecosystem-scale data on carbon dioxide, water, and energy exchange, collected from 212 global sites contributing over 1500 site-years of data until 2014.
  • - The dataset was systematically quality controlled and processed, facilitating consistency for various applications in ecophysiology, remote sensing, and ecosystem modeling.
  • - For the first time, derived data products such as time series, ecosystem respiration, and photosynthesis estimates are included, and 206 sites are made accessible under a Creative Commons license, with the processing methods available as open-source codes.
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The eddy covariance (EC) technique is used to measure the net ecosystem exchange (NEE) of CO between ecosystems and the atmosphere, offering a unique opportunity to study ecosystem responses to climate change. NEE is the difference between the total CO release due to all respiration processes (RECO), and the gross carbon uptake by photosynthesis (GPP). These two gross CO fluxes are derived from EC measurements by applying partitioning methods that rely on physiologically based functional relationships with a limited number of environmental drivers.

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Anthropogenic nitrogen (N) deposition and resulting differences in ecosystem N and phosphorus (P) ratios are expected to impact photosynthetic capacity, that is, maximum gross primary productivity (GPP ). However, the interplay between N and P availability with other critical resources on seasonal dynamics of ecosystem productivity remains largely unknown. In a Mediterranean tree-grass ecosystem, we established three landscape-level (24 ha) nutrient addition treatments: N addition (NT), N and P addition (NPT), and a control site (CT).

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