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Rödenbeck C, Zaehle S, Keeling R, Heimann M. The European carbon cycle response to heat and drought as seen from atmospheric CO 2 data for 1999-2018. Philos Trans R Soc Lond B Biol Sci 2020; 375:20190506. [PMID: 32892730 PMCID: PMC7485106 DOI: 10.1098/rstb.2019.0506] [Citation(s) in RCA: 13] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/24/2022] Open
Abstract
In 2018, central and northern parts of Europe experienced heat and drought conditions over many months from spring to autumn, strongly affecting both natural ecosystems and crops. Besides their impact on nature and society, events like this can be used to study the impact of climate variations on the terrestrial carbon cycle, which is an important determinant of the future climate trajectory. Here, variations in the regional net ecosystem exchange (NEE) of CO2 between terrestrial ecosystems and the atmosphere were quantified from measurements of atmospheric CO2 mole fractions. Over Europe, several observational records have been maintained since at least 1999, giving us the opportunity to assess the 2018 anomaly in the context of at least two decades of variations, including the strong climate anomaly in 2003. In addition to an atmospheric inversion with temporally explicitly estimated anomalies, we use an inversion based on empirical statistical relations between anomalies in the local NEE and anomalies in local climate conditions. For our analysis period 1999–2018, we find that higher-than-usual NEE in hot and dry summers may tend to arise in Central Europe from enhanced ecosystem respiration due to the elevated temperatures, and in Southern Europe from reduced photosynthesis due to the reduced water availability. Despite concerns in the literature, the level of agreement between regression-based NEE anomalies and temporally explicitly estimated anomalies indicates that the atmospheric CO2 measurements from the relatively dense European station network do provide information about the year-to-year variations of Europe’s carbon sources and sinks, at least in summer. This article is part of the theme issue ‘Impacts of the 2018 severe drought and heatwave in Europe: from site to continental scale’.
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Affiliation(s)
- C Rödenbeck
- Max Planck Institute for Biogeochemistry, Jena, Germany
| | - S Zaehle
- Max Planck Institute for Biogeochemistry, Jena, Germany
| | - R Keeling
- Scripps Institution of Oceanography, University of California, San Diego, CA, USA
| | - M Heimann
- Max Planck Institute for Biogeochemistry, Jena, Germany.,Institute for Atmospheric and Earth System Research (INAR), Faculty of Science, University of Helsinki, Helsinki, Finland
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Bastos A, Fu Z, Ciais P, Friedlingstein P, Sitch S, Pongratz J, Weber U, Reichstein M, Anthoni P, Arneth A, Haverd V, Jain A, Joetzjer E, Knauer J, Lienert S, Loughran T, McGuire PC, Obermeier W, Padrón RS, Shi H, Tian H, Viovy N, Zaehle S. Impacts of extreme summers on European ecosystems: a comparative analysis of 2003, 2010 and 2018. Philos Trans R Soc Lond B Biol Sci 2020; 375:20190507. [PMID: 32892728 DOI: 10.1098/rstb.2019.0507] [Citation(s) in RCA: 22] [Impact Index Per Article: 5.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/12/2022] Open
Abstract
In Europe, three widespread extreme summer drought and heat (DH) events have occurred in 2003, 2010 and 2018. These events were comparable in magnitude but varied in their geographical distribution and biomes affected. In this study, we perform a comparative analysis of the impact of the DH events on ecosystem CO2 fluxes over Europe based on an ensemble of 11 dynamic global vegetation models (DGVMs), and the observation-based FLUXCOM product. We find that all DH events were associated with decreases in net ecosystem productivity (NEP), but the gross summer flux anomalies differ between DGVMs and FLUXCOM. At the annual scale, FLUXCOM and DGVMs indicate close to neutral or above-average land CO2 uptake in DH2003 and DH2018, due to increased productivity in spring and reduced respiration in autumn and winter compensating for less photosynthetic uptake in summer. Most DGVMs estimate lower gross primary production (GPP) sensitivity to soil moisture during extreme summers than FLUXCOM. Finally, we show that the different impacts of the DH events at continental-scale GPP are in part related to differences in vegetation composition of the regions affected and to regional compensating or offsetting effects from climate anomalies beyond the DH centres. This article is part of the theme issue 'Impacts of the 2018 severe drought and heatwave in Europe: from site to continental scale'.
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Affiliation(s)
- A Bastos
- Department of Geography, Ludwig Maximilians Universität, Luisenstrasse 37, 80333 Munich, Germany
| | - Z Fu
- Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA-CNRS-UVSQ, UMR8212, 91191 Gif-sur-Yvette, France
| | - P Ciais
- Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA-CNRS-UVSQ, UMR8212, 91191 Gif-sur-Yvette, France
| | - P Friedlingstein
- College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QF, UK
| | - S Sitch
- College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, UK
| | - J Pongratz
- Department of Geography, Ludwig Maximilians Universität, Luisenstrasse 37, 80333 Munich, Germany.,Max Planck Institute for Meteorology, 20146 Hamburg, Germany
| | - U Weber
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
| | - M Reichstein
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
| | - P Anthoni
- Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research / Atmospheric Environmental Research, 82467 Garmisch-Partenkirchen, Germany
| | - A Arneth
- Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research / Atmospheric Environmental Research, 82467 Garmisch-Partenkirchen, Germany
| | - V Haverd
- CSIRO Oceans and Atmosphere, Canberra 2601, Australia
| | - A Jain
- Department of Atmospheric Sciences, University of Illinois, Urbana, IL 61801, USA
| | - E Joetzjer
- Laboratoire Evolution et Diversite Biologique UMR 5174, CNRS Universite Paul Sabatier, Toulouse, France
| | - J Knauer
- CSIRO Oceans and Atmosphere, Canberra 2601, Australia
| | - S Lienert
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, Bern 3012, Switzerland
| | - T Loughran
- Department of Geography, Ludwig Maximilians Universität, Luisenstrasse 37, 80333 Munich, Germany
| | - P C McGuire
- Department of Meteorology, University of Reading, Earley Gate, Reading RG6 6BB, UK
| | - W Obermeier
- Department of Geography, Ludwig Maximilians Universität, Luisenstrasse 37, 80333 Munich, Germany
| | - R S Padrón
- Department of Environmental Systems Science, Institute for Atmospheric and Climate Science, ETH Zürich, Zürich, Switzerland
| | - H Shi
- International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, 602 Duncan Drive, Auburn, AL 36849, USA
| | - H Tian
- International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, 602 Duncan Drive, Auburn, AL 36849, USA
| | - N Viovy
- Laboratoire des Sciences du Climat et de l'Environnement (LSCE), CEA-CNRS-UVSQ, UMR8212, 91191 Gif-sur-Yvette, France
| | - S Zaehle
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
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Bastos A, Ciais P, Friedlingstein P, Sitch S, Pongratz J, Fan L, Wigneron JP, Weber U, Reichstein M, Fu Z, Anthoni P, Arneth A, Haverd V, Jain AK, Joetzjer E, Knauer J, Lienert S, Loughran T, McGuire PC, Tian H, Viovy N, Zaehle S. Direct and seasonal legacy effects of the 2018 heat wave and drought on European ecosystem productivity. Sci Adv 2020; 6:eaba2724. [PMID: 32577519 PMCID: PMC7286671 DOI: 10.1126/sciadv.aba2724] [Citation(s) in RCA: 68] [Impact Index Per Article: 17.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/19/2019] [Accepted: 04/14/2020] [Indexed: 05/23/2023]
Abstract
In summer 2018, central and northern Europe were stricken by extreme drought and heat (DH2018). The DH2018 differed from previous events in being preceded by extreme spring warming and brightening, but moderate rainfall deficits, yet registering the fastest transition between wet winter conditions and extreme summer drought. Using 11 vegetation models, we show that spring conditions promoted increased vegetation growth, which, in turn, contributed to fast soil moisture depletion, amplifying the summer drought. We find regional asymmetries in summer ecosystem carbon fluxes: increased (reduced) sink in the northern (southern) areas affected by drought. These asymmetries can be explained by distinct legacy effects of spring growth and of water-use efficiency dynamics mediated by vegetation composition, rather than by distinct ecosystem responses to summer heat/drought. The asymmetries in carbon and water exchanges during spring and summer 2018 suggest that future land-management strategies could influence patterns of summer heat waves and droughts under long-term warming.
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Affiliation(s)
- A. Bastos
- Department of Geography, Ludwig Maximilian University of Munich, Munich, Luisenstr. 37, 80333 Munich, Germany
| | - P. Ciais
- Laboratoire des Sciences du Climat et de l’Environnement (LSCE), CEA-CNRS-UVSQ, UMR8212, 91191 Gif-sur-Yvette, France
| | - P. Friedlingstein
- College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter EX4 4QF, UK
- LMD/IPSL, ENS, PSL Université, École Polytechnique, Institut Polytechnique de Paris, Sorbonne Université, CNRS, Paris, France
| | - S. Sitch
- College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, UK
| | - J. Pongratz
- Department of Geography, Ludwig Maximilian University of Munich, Munich, Luisenstr. 37, 80333 Munich, Germany
- Max Planck Institute for Meteorology, 20146 Hamburg, Germany
| | - L. Fan
- ISPA, UMR 1391, INRA Nouvelle-Aquitaine, Université de Bordeaux, Grande Ferrage, Villenave d’Ornon, France
| | - J. P. Wigneron
- ISPA, UMR 1391, INRA Nouvelle-Aquitaine, Université de Bordeaux, Grande Ferrage, Villenave d’Ornon, France
| | - U. Weber
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
| | - M. Reichstein
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
| | - Z. Fu
- Laboratoire des Sciences du Climat et de l’Environnement (LSCE), CEA-CNRS-UVSQ, UMR8212, 91191 Gif-sur-Yvette, France
| | - P. Anthoni
- Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research/Atmospheric Environmental Research, 82467 Garmisch-Partenkirchen, Germany
| | - A. Arneth
- Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research/Atmospheric Environmental Research, 82467 Garmisch-Partenkirchen, Germany
| | - V. Haverd
- CSIRO Oceans and Atmosphere, Canberra, ACT 2601, Australia
| | - A. K. Jain
- Department of Atmospheric Sciences, University of Illinois, Urbana, IL 61801, USA
| | - E. Joetzjer
- CNRM, Université de Toulouse, Météo-France, CNRS, Toulouse, France
| | - J. Knauer
- CSIRO Oceans and Atmosphere, Canberra, ACT 2601, Australia
| | - S. Lienert
- Climate and Environmental Physics, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, Bern CH-3012, Switzerland
| | - T. Loughran
- Department of Geography, Ludwig Maximilian University of Munich, Munich, Luisenstr. 37, 80333 Munich, Germany
| | - P. C. McGuire
- Department of Meteorology, Department of Geography & Environmental Science, and National Centre for Atmospheric Science, University of Reading, Earley Gate, RG66BB Reading, UK
| | - H. Tian
- International Center for Climate and Global Change Research, School of Forestry and Wildlife Sciences, Auburn University, 602 Duncan Drive, Auburn, AL 36849, USA
| | - N. Viovy
- Laboratoire des Sciences du Climat et de l’Environnement (LSCE), CEA-CNRS-UVSQ, UMR8212, 91191 Gif-sur-Yvette, France
| | - S. Zaehle
- Max Planck Institute for Biogeochemistry, 07745 Jena, Germany
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Rödenbeck C, Zaehle S, Keeling R, Heimann M. History of El Niño impacts on the global carbon cycle 1957-2017: a quantification from atmospheric CO 2 data. Philos Trans R Soc Lond B Biol Sci 2018; 373:rstb.2017.0303. [PMID: 30297464 PMCID: PMC6178444 DOI: 10.1098/rstb.2017.0303] [Citation(s) in RCA: 12] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Accepted: 08/16/2018] [Indexed: 11/12/2022] Open
Abstract
Interannual variations in the large-scale net ecosystem exchange (NEE) of CO2 between the terrestrial biosphere and the atmosphere were estimated for 1957-2017 from sustained measurements of atmospheric CO2 mixing ratios. As the observations are sparse in the early decades, available records were combined into a 'quasi-homogeneous' dataset based on similarity in their signals, to minimize spurious variations from beginning or ending data records. During El Niño events, CO2 is anomalously released from the tropical band, and a few months later also in the northern extratropical band. This behaviour can approximately be represented by a linear relationship of the NEE anomalies and local air temperature anomalies, with sensitivity coefficients depending on geographical location and season. The apparent climate sensitivity of global total NEE against variations in pan-tropically averaged annual air temperature slowly changed over time during the 1957-2017 period, first increasing (though less strongly than in previous studies) but then decreasing again. However, only part of this change can be attributed to actual changes in local physiological or ecosystem processes, the rest probably arising from shifts in the geographical area of dominating temperature variations.This article is part of a discussion meeting issue 'The impact of the 2015/2016 El Niño on the terrestrial tropical carbon cycle: patterns, mechanisms and implications'.
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Affiliation(s)
- C Rödenbeck
- Max Planck Institute for Biogeochemistry, Jena, Germany
| | - S Zaehle
- Max Planck Institute for Biogeochemistry, Jena, Germany
| | - R Keeling
- Scripps Institution of Oceanography, University of California, San Diego, CA, USA
| | - M Heimann
- Max Planck Institute for Biogeochemistry, Jena, Germany.,Institute for Atmospheric and Earth System Research (INAR), Faculty of Science, University of Helsinki, Helsinki, Finland
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Norby RJ, De Kauwe MG, Walker AP, Werner C, Zaehle S, Zak DR. Comment on “Mycorrhizal association as a primary control of the CO
2
fertilization effect”. Science 2017; 355:358. [DOI: 10.1126/science.aai7976] [Citation(s) in RCA: 14] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/12/2016] [Accepted: 11/28/2016] [Indexed: 11/02/2022]
Affiliation(s)
- R. J. Norby
- Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, TN 37831-6301, USA
| | - M. G. De Kauwe
- Macquarie University, Department of Biological Sciences, North Ryde, New South Wales 2109, Australia
| | - A. P. Walker
- Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, TN 37831-6301, USA
| | - C. Werner
- Senckenberg Biodiversity and Climate Research Centre (BiK-F), D-60325 Frankfurt am Main, Germany
| | - S. Zaehle
- Biogeochemical Integration Department, Max Planck Institute for Biogeochemistry, D-07701 Jena, Germany
| | - D. R. Zak
- School of Natural Resources and Environment, University of Michigan, Ann Arbor, MI 48109-1041, USA
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Forkel M, Carvalhais N, Rodenbeck C, Keeling R, Heimann M, Thonicke K, Zaehle S, Reichstein M. Enhanced seasonal CO2 exchange caused by amplified plant productivity in northern ecosystems. Science 2016; 351:696-9. [DOI: 10.1126/science.aac4971] [Citation(s) in RCA: 250] [Impact Index Per Article: 31.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/04/2015] [Accepted: 01/11/2016] [Indexed: 02/05/2023]
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Ahlstrom A, Raupach MR, Schurgers G, Smith B, Arneth A, Jung M, Reichstein M, Canadell JG, Friedlingstein P, Jain AK, Kato E, Poulter B, Sitch S, Stocker BD, Viovy N, Wang YP, Wiltshire A, Zaehle S, Zeng N. The dominant role of semi-arid ecosystems in the trend and variability of the land CO2 sink. Science 2015; 348:895-9. [DOI: 10.1126/science.aaa1668] [Citation(s) in RCA: 765] [Impact Index Per Article: 85.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/26/2014] [Accepted: 04/24/2015] [Indexed: 11/02/2022]
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Abstract
Interactions between the terrestrial nitrogen (N) and carbon (C) cycles shape the response of ecosystems to global change. However, the global distribution of nitrogen availability and its importance in global biogeochemistry and biogeochemical interactions with the climate system remain uncertain. Based on projections of a terrestrial biosphere model scaling ecological understanding of nitrogen-carbon cycle interactions to global scales, anthropogenic nitrogen additions since 1860 are estimated to have enriched the terrestrial biosphere by 1.3 Pg N, supporting the sequestration of 11.2 Pg C. Over the same time period, CO2 fertilization has increased terrestrial carbon storage by 134.0 Pg C, increasing the terrestrial nitrogen stock by 1.2 Pg N. In 2001-2010, terrestrial ecosystems sequestered an estimated total of 27 Tg N yr(-1) (1.9 Pg C yr(-1)), of which 10 Tg N yr(-1) (0.2 Pg C yr(-1)) are due to anthropogenic nitrogen deposition. Nitrogen availability already limits terrestrial carbon sequestration in the boreal and temperate zone, and will constrain future carbon sequestration in response to CO2 fertilization (regionally by up to 70% compared with an estimate without considering nitrogen-carbon interactions). This reduced terrestrial carbon uptake will probably dominate the role of the terrestrial nitrogen cycle in the climate system, as it accelerates the accumulation of anthropogenic CO2 in the atmosphere. However, increases of N2O emissions owing to anthropogenic nitrogen and climate change (at a rate of approx. 0.5 Tg N yr(-1) per 1°C degree climate warming) will add an important long-term climate forcing.
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Affiliation(s)
- S Zaehle
- Department of Biogeochemical Integration, Max Planck Institute for Biogeochemistry, Hans-Knöll-Strasse 10, 07745 Jena, Germany.
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Mahecha MD, Reichstein M, Jung M, Seneviratne SI, Zaehle S, Beer C, Braakhekke MC, Carvalhais N, Lange H, Le Maire G, Moors E. Comparing observations and process-based simulations of biosphere-atmosphere exchanges on multiple timescales. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2009jg001016] [Citation(s) in RCA: 62] [Impact Index Per Article: 4.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
Affiliation(s)
- M. D. Mahecha
- Biogeochemical Model-Data Integration Group; Max-Planck-Institut für Biogeochemie; Jena Germany
- Department of Environmental Sciences; ETH Zurich; Zurich Switzerland
| | - M. Reichstein
- Biogeochemical Model-Data Integration Group; Max-Planck-Institut für Biogeochemie; Jena Germany
| | - M. Jung
- Biogeochemical Model-Data Integration Group; Max-Planck-Institut für Biogeochemie; Jena Germany
| | - S. I. Seneviratne
- Department of Environmental Sciences; ETH Zurich; Zurich Switzerland
| | - S. Zaehle
- Biogeochemical Model-Data Integration Group; Max-Planck-Institut für Biogeochemie; Jena Germany
| | - C. Beer
- Biogeochemical Model-Data Integration Group; Max-Planck-Institut für Biogeochemie; Jena Germany
| | - M. C. Braakhekke
- Biogeochemical Model-Data Integration Group; Max-Planck-Institut für Biogeochemie; Jena Germany
| | - N. Carvalhais
- Biogeochemical Model-Data Integration Group; Max-Planck-Institut für Biogeochemie; Jena Germany
- Faculdade de Ciência e Tecnologia; Universidade Nova de Lisboa; Caparica Portugal
| | - H. Lange
- Norsk Institutt for Skog og Landskap; Ås Norway
| | - G. Le Maire
- CIRAD, UPR Fonctionnement et pilotage des écosystèmes de plantations; UPR 80; Montpellier France
- LSCE, UMR; CEA-CNRS-UVSQ; Gif-sur-Yvette France
| | - E. Moors
- Alterra; Wageningen University and Research Centre; Wageningen Netherlands
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