Thomas Wutzler

ORCID: 0000-0003-4159-5445
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About
Contact & Profiles
Research Areas
  • Soil Carbon and Nitrogen Dynamics
  • Plant Water Relations and Carbon Dynamics
  • Peatlands and Wetlands Ecology
  • Soil and Water Nutrient Dynamics
  • Atmospheric and Environmental Gas Dynamics
  • Forest ecology and management
  • Soil and Unsaturated Flow
  • Forest Management and Policy
  • Hydrology and Watershed Management Studies
  • Climate variability and models
  • Tree-ring climate responses
  • Microbial Community Ecology and Physiology
  • Remote Sensing in Agriculture
  • Fluid Dynamics and Turbulent Flows
  • Simulation Techniques and Applications
  • Remote Sensing and LiDAR Applications
  • Bioenergy crop production and management
  • Cryospheric studies and observations
  • Scientific Computing and Data Management
  • Soil Geostatistics and Mapping
  • Meteorological Phenomena and Simulations
  • Plant responses to elevated CO2
  • Aerodynamics and Acoustics in Jet Flows
  • Botany and Plant Ecology Studies
  • Plant Ecology and Soil Science

Max Planck Institute for Biogeochemistry
2015-2025

University of Edinburgh
2021

National Centre for Earth Observation
2021

Max Planck Society
2005-2013

Friedrich Schiller University Jena
2008

TU Dresden
2006

Abstract. With the eddy covariance (EC) technique, net fluxes of carbon dioxide (CO2) and other trace gases as well water energy can be measured at ecosystem level. These flux measurements are a main source for understanding biosphere–atmosphere interactions feedbacks through cross-site analysis, model–data integration, upscaling. The raw with EC technique require extensive laborious data processing. While there standard tools1 available in an open-source environment processing...

10.5194/bg-15-5015-2018 article EN cc-by Biogeosciences 2018-08-23

Abstract Aim To infer a forest carbon density map at 0.01° resolution from radar remote sensing product for the estimation of stocks in Northern Hemisphere boreal and temperate forests. Location The study area extends 30° N to 80° , covering three biomes – broadleaf mixed forests ( TBMF ), conifer TCF ) BFT over continents orth A merica, E urope sia). Methods This is based on recently available growing stock volume GSV retrieved synthetic aperture data. Forest biomass spatially explicit...

10.1111/geb.12125 article EN Global Ecology and Biogeography 2013-10-29

The effect of temperature and the influence fresh substrate addition on soil organic matter decomposition are two key factors we need to understand forecast carbon dynamics under climate change rising CO2 levels. Here perform a laboratory incubation experiment address following questions: 1) Does sensitivity differ between freshly added bulk carbon? 2) stimulate ("priming effect")? 3) If so, does this priming depend temperature? In our study, incubated sieved samples without with labelled...

10.1016/j.soilbio.2012.10.029 article EN cc-by-nc-nd Soil Biology and Biochemistry 2012-11-14

Sun-induced fluorescence (SIF) in the far-red region provides a new noninvasive measurement approach that has potential to quantify dynamic changes light-use efficiency and gross primary production (GPP). However, mechanistic link between GPP SIF is not completely understood. We analyzed structural functional factors controlling emission of at 760 nm (F760 ) Mediterranean grassland manipulated with nutrient addition nitrogen (N), phosphorous (P) or nitrogen-phosphorous (NP). Using...

10.1111/nph.14437 article EN New Phytologist 2017-02-09

Abstract Soil water content is a key variable for biogeochemical and atmospheric coupled processes. Its small‐scale heterogeneity impacts the partitioning of precipitation (e.g., deep percolation or transpiration) by triggering threshold processes connecting flow paths. Forest hydrologists frequently hypothesized that throughfall stemflow patterns induce soil heterogeneity, yet experimental validation limited. Here, we pursued pattern‐oriented approach to explore relationship between net...

10.1002/hyp.11274 article EN Hydrological Processes 2017-07-07
Ben Bond‐Lamberty Danielle Christianson Avni Malhotra Stephanie Pennington Debjani Sihi and 89 more Amir AghaKouchak Hassan Anjileli M. Altaf Arain Juan J. Armestó Samaneh Ashraf Mioko Ataka Dennis Baldocchi T. Andrew Black Nina Buchmann Mariah S. Carbone Shih‐Chieh Chang P. M. Crill Peter S. Curtis Eric A. Davidson Ankur R. Desai John E. Drake Tarek S. El‐Madany Michael Gavazzi Carolyn‐Monika Görres Christopher M. Gough Michael L. Goulden Jillian W. Gregg Omar Gutiérrez del Arroyo Jin He Takashi Hirano Anya M. Hopple Holly Hughes Järvi Järveoja Rachhpal S. Jassal Jinshi Jian Haiming Kan Jason P. Kaye Yuji Kominami Naishen Liang David A. Lipson Catriona A. Macdonald Kadmiel Maseyk Kayla Mathes Marguerite Mauritz Melanie A. Mayes Steven G. McNulty Guofang Miao Mirco Migliavacca S. D. Miller Chelcy Ford Miniat Jennifer Goedhart Nietz Mats B. Nilsson Asko Noormets H. Norouzi Christine S. O’Connell Bruce Osborne Cecilio Oyonarte Zhuo Pang Matthias Peichl Elise Pendall Jorge F. Pérez‐Quezada Claire L. Phillips Richard P. Phillips James W. Raich Alexandre A. Renchon Nadine K. Ruehr Enrique P. Sánchez‐Cañete Matthew Saunders K. E. Savage Marion Schrumpf Russell L. Scott Ulli Seibt Whendee L. Silver Wu Sun Daphne Szutu Kentaro Takagi Masahiro Takagi Munemasa Teramoto Mark G. Tjoelker Susan Trumbore Masahito Ueyama Rodrigo Vargas R. K. Varner Joseph Verfaillie Christoph S. Vogel Jinsong Wang G. Winston Tana E. Wood Juying Wu Thomas Wutzler Jiye Zeng Tianshan Zha Quan Zhang Junliang Zou

Abstract Globally, soils store two to three times as much carbon currently resides in the atmosphere, and it is critical understand how soil greenhouse gas (GHG) emissions uptake will respond ongoing climate change. In particular, soil‐to‐atmosphere CO 2 flux, commonly though imprecisely termed respiration ( R S ), one of largest fluxes Earth system. An increasing number high‐frequency measurements (typically, from an automated system with hourly sampling) have been made over last decades;...

10.1111/gcb.15353 article EN cc-by Global Change Biology 2020-10-07

The sensitivity of photosynthesis to environmental changes is essential for understanding carbon cycle responses global climate change and the development modeling approaches that explains its spatial temporal variability. We collected a large variety published functions gross primary productivity (GPP) different forcing variables assess response GPP factors. These include temperature; vapor pressure deficit, some which atmospheric CO2 concentrations; soil water availability (W); light...

10.1016/j.agrformet.2021.108708 article EN cc-by Agricultural and Forest Meteorology 2021-11-19

Abstract. Many projections of the soil carbon sink or source are based on kinetically defined pool models. Para\\-meters these models often determined in a way that steady state model matches observed stocks. The underlying simplifying assumption is stocks near equilibrium. This challenged by observations very old soils do still accumulate carbon. In this modelling study we explored consequences case where apart from Calculation equilibrium states currently accumulating small amounts were...

10.5194/bg-4-125-2007 article EN cc-by-nc-sa Biogeosciences 2007-02-15

This study provides a comprehensive set of functions for predicting biomass Common beech ( Fagus sylvatica L.) in Central Europe all major tree compartments. The equations are based on data stem, branch, timber, brushwood (wood with diameter below 5 or 7 cm), foliage, root, and total aboveground 443 trees from 13 studies. We used nonlinear mixed-effects models to assess the contribution fixed effects (tree dimensions, site descriptors), random (grouping according studies), residual variance...

10.1139/x07-194 article EN Canadian Journal of Forest Research 2008-06-01

Abstract. Decomposition of soil organic matter (SOM) is limited by both the available substrate and active decomposer community. The understanding this colimitation strongly affects feedbacks carbon to global warming its consequences. This study compares different formulations decomposition. We compiled from literature into groups according representation biomass on SOM decomposition rate a) non-explicit (substrate only), b) linear, c) non-linear. By varying equation in a basic simplified...

10.5194/bg-5-749-2008 article EN cc-by Biogeosciences 2008-05-13

Abstract. This study investigates the performances of different optical indices to estimate gross primary production (GPP) herbaceous stratum in a Mediterranean savanna with nitrogen (N) and phosphorous (P) availability. Sun-induced chlorophyll fluorescence yield computed at 760 nm (Fy760), scaled photochemical reflectance index (sPRI), MERIS terrestrial-chlorophyll (MTCI) normalized difference vegetation (NDVI) were from near-surface field spectroscopy measurements collected using high...

10.5194/bg-12-6351-2015 article EN cc-by Biogeosciences 2015-11-09

Abstract. Plant–soil interactions, such as the coupling of plants' below-ground biomass allocation with soil organic matter (SOM) decomposition, nutrient release and plant uptake, are essential to understand response carbon (C) cycling global changes. However, these processes poorly represented in current terrestrial biosphere models owing simple first-order approach SOM ignorance variations within a profile. While emerging microbially explicit C can better describe formation turnover, at...

10.5194/gmd-13-783-2020 article EN cc-by Geoscientific model development 2020-02-28

<ja:p>Countries need to assess changes in the carbon stocks of forest soils as a part national greenhouse gas (GHG) inventories under United Nations Framework Convention on Climate Change (UNFCCC) and Kyoto Protocol (KP). Since measuring these is expensive, it likely that many countries will use alternative methods prepare estimates. We reviewed seven well-known soil models from point view preparing country-scale C change first introduced explained how they incorporated most important input...

10.14214/sf.290 article EN cc-by-sa Silva Fennica 2007-01-01

Abstract. The vertical distribution of soil organic matter (SOM) in the profile may constitute an important factor for carbon cycling. However, formation SOM is currently poorly understood due to equifinality, caused by entanglement several processes: input from roots, mixing bioturbation, and leaching. In this study we quantified contribution these three processes using Bayesian parameter estimation mechanistic model SOMPROF. Based on measurements, 13 parameters related decomposition...

10.5194/bg-10-399-2013 article EN cc-by Biogeosciences 2013-01-24

Abstract. Interactions between different qualities of soil organic matter (SOM) affecting their turnover are rarely represented in models. In this study, we propose three mathematical strategies at levels abstraction to represent those interactions. By implementing these into the Introductory Carbon Balance Model (ICBM) and applying them several scenarios litter input, show that applicable timescales. We present a simple one-parameter equation substrate limitation can straightforwardly be...

10.5194/bg-10-2089-2013 article EN cc-by Biogeosciences 2013-03-26

The inter-annual variability (IAV) of the terrestrial carbon cycle is tightly linked to semi-arid ecosystems. Thus, it utmost importance understand what main meteorological drivers for IAV such ecosystems are, and how they respond extreme events as droughts heatwaves. To shed light onto these questions, we analyse fluxes, its relation with variables, impact compound drought heatwave on two similar ecosystems, along a precipitation gradient. A four-year long dataset from 2016 2019 was used...

10.1098/rstb.2019.0519 article EN Philosophical Transactions of the Royal Society B Biological Sciences 2020-09-06

Abstract Nutrient availability, especially of nitrogen (N) and phosphorus (P), is major importance for every organism at a larger scale ecosystem functioning productivity. Changes in nutrient availability potential stoichiometric imbalance due to anthropogenic deposition might lead deficiency or alter various ways. In this study, we present 6 years (2014–2020) flux‐, plant‐, remote sensing data from large‐scale manipulation experiment conducted Mediterranean savanna‐type with an emphasis on...

10.1029/2020jg006005 article EN Journal of Geophysical Research Biogeosciences 2021-04-04

Abstract Temperate forest ecosystems have recently been identified as an important net sink in the global carbon budget. The factors responsible for strength of sinks and their permanence, however, are less evident. In this paper, we quantify present sequestration Thuringian managed coniferous forests. We effects indirect human‐induced environmental changes (increasing temperature, increasing atmospheric CO 2 concentration nitrogen fertilization), during last century using BIOME‐BGC, well...

10.1111/j.1365-2486.2005.00932.x article EN Global Change Biology 2005-04-05

Carbon dioxide (CO&amp;#8322;) flux partitioning involves separating net ecosystem exchange (NEE) into its gross primary production (GPP) and respiration (RECO) components. Despite 25 years of research abundant data from networks such as FLUXNET [1], the development validation new methods remain hindered by lack a standardized benchmark dataset evaluation protocol. Existing parametric methods, including nighttime (NT) [2] daytime (DT) [3] approaches, have become integral to products but face...

10.5194/egusphere-egu25-19561 preprint EN 2025-03-15

Heatwaves are well-documented drivers of adverse health outcomes and socio-economic disruptions, yet regional variations in risk, particularly the case multi-hazard scenarios, remain insufficiently understood. Understanding these is critical for development targeted strategies to mitigate outcomes. Most studies examining extreme heat terms associated mortality focus on temperature influence alone, often neglecting role coinciding environmental conditions, such as moisture. While those that...

10.22541/essoar.174282873.38972040/v1 preprint EN cc-by Authorea (Authorea) 2025-03-24

Abstract. With the eddy-covariance (EC) technique, net fluxes of carbon dioxide (CO2) and other greenhouse gases as well water energy can be measured at ecosystem level. These flux measurements are a main source for understanding biosphere-atmosphere interactions feedbacks by cross-site analysis, model-data integration, up-scaling. The raw with EC technique require an extensive laborious data processing. While there standard tools available in open environment processing high-frequency (10...

10.5194/bg-2018-56 preprint EN cc-by 2018-02-12

Abstract. Soils of temperate forests store significant amounts organic matter and are considered to be net sinks atmospheric CO2. Soil carbon (SOC) turnover has been studied using the Δ14C values bulk SOC or different fractions as observational constraints in models. Further, CO2 that evolved during incubation soil roots have widely used together with total respiration partition into heterotrophic (HR) rhizosphere respiration. However, these data not joint determine times. Thus, we focus on...

10.5194/bg-11-2147-2014 article EN cc-by Biogeosciences 2014-04-17
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