Seasonality of Ecosystem Respiration and Gross Primary Production As Derived from FLUXNET Measurements
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Foliar and Ecosystem Respiration in an Old-Growth Tropical Rain Forest
Plant, Cell and Environment (2008) 31, 473–483 doi: 10.1111/j.1365-3040.2008.01775.x Foliar and ecosystem respiration in an old-growth tropical rain forest MOLLY A. CAVALERI1,2, STEVEN F. OBERBAUER3,4 & MICHAEL G. RYAN5,6 1Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO 80523, USA, 2Botany Department, University of Hawaii, Manoa, 3190 Maile Way, Honolulu, HI 96826, USA, 3Department of Biological Sciences, Florida International University, 11200 SW 8th Street, Miami, FL 33199, USA, 4Fairchild Tropical Botanic Garden, 11935 Old Cutler Road, Miami, FL 33156, USA, 5United States Department of Agriculture Forest Service, Rocky Mountain Research Station, 240 West Prospect RD, Fort Collins, CO 80526, USA and 6Graduate Degree Program in Ecology, Department of Forest, Rangeland, and Watershed Stewardship, Colorado State University, Fort Collins, CO 80523, USA ABSTRACT Chambers et al. 2004). Results vary widely about whether tropical forests are presently acting as carbon sources or Foliar respiration is a major component of ecosystem res- sinks, or how this may be affected by global warming. piration, yet extrapolations are often uncertain in tropical Several eddy flux studies have concluded that tropical rain forests because of indirect estimates of leaf area index forests are primarily acting as carbon sinks (Fan et al. 1990; (LAI). A portable tower was used to directly measure LAI Grace et al. 1995; Malhi et al. 1998; Loescher et al. 2003, and night-time foliar respiration from 52 vertical transects but see Saleska et al. 2003). Many atmosphere–biosphere throughout an old-growth tropical rain forest in Costa Rica. modelling studies, on the other hand, predict that tropical In this study, we (1) explored the effects of structural, func- forests will be an increased carbon source with global tional and environmental variables on foliar respiration; (2) warming (Kindermann, Würth & Kohlmaier 1996; Braswell extrapolated foliar respiration to the ecosystem; and (3) et al. -
Drought and Ecosystem Carbon Cycling
Agricultural and Forest Meteorology 151 (2011) 765–773 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Review Drought and ecosystem carbon cycling M.K. van der Molen a,b,∗, A.J. Dolman a, P. Ciais c, T. Eglin c, N. Gobron d, B.E. Law e, P. Meir f, W. Peters b, O.L. Phillips g, M. Reichstein h, T. Chen a, S.C. Dekker i, M. Doubková j, M.A. Friedl k, M. Jung h, B.J.J.M. van den Hurk l, R.A.M. de Jeu a, B. Kruijt m, T. Ohta n, K.T. Rebel i, S. Plummer o, S.I. Seneviratne p, S. Sitch g, A.J. Teuling p,r, G.R. van der Werf a, G. Wang a a Department of Hydrology and Geo-Environmental Sciences, Faculty of Earth and Life Sciences, VU-University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands b Meteorology and Air Quality Group, Wageningen University and Research Centre, P.O. box 47, 6700 AA Wageningen, The Netherlands c LSCE CEA-CNRS-UVSQ, Orme des Merisiers, F-91191 Gif-sur-Yvette, France d Institute for Environment and Sustainability, EC Joint Research Centre, TP 272, 2749 via E. Fermi, I-21027 Ispra, VA, Italy e College of Forestry, Oregon State University, Corvallis, OR 97331-5752 USA f School of Geosciences, University of Edinburgh, EH8 9XP Edinburgh, UK g School of Geography, University of Leeds, Leeds LS2 9JT, UK h Max Planck Institute for Biogeochemistry, PO Box 100164, D-07701 Jena, Germany i Department of Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht University, PO Box 80115, 3508 TC Utrecht, The Netherlands j Institute of Photogrammetry and Remote Sensing, Vienna University of Technology, Gusshausstraße 27-29, 1040 Vienna, Austria k Geography and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA 02215, USA l Department of Global Climate, Royal Netherlands Meteorological Institute, P.O. -
IPBES Global Assessment Chapter 4 - Supplementary Materials
IPBES Global assessment Chapter 4 - Supplementary materials Contents Appendix 4.1 – Supporting materials to section 1 .................................................................................. 2 A4.1.1 Methodology for Literature Search, Review and Analysis ...................................................... 2 General ............................................................................................................................................ 2 Literature Search and Supplementation ......................................................................................... 2 Literature metadata analysis .......................................................................................................... 4 A4.1.2 – Extended figures and tables to section 1............................................................................ 13 Appendix 4.2 - Supporting materials to section 2................................................................................. 15 A4.2.1 The main interrelations and feedbacks between hierarchical levels that are important for biodiversity future (extended materials, Box 4.2.1) ......................................................................... 15 INTRAPOPULATION and INTRASPECIFIC DIVERSITY ...................................................................... 15 INDIVIDUAL SPECIES...................................................................................................................... 17 SPECIES DIVERSITY ....................................................................................................................... -
Download the Annual Review PDF 2016-17
Annual Review 2016/17 Pushing at the frontiers of Knowledge Portrait of Dr Henry Odili Nwume (Brasenose) by Sarah Jane Moon – see The Full Picture, page 17. FOREWORD 2016/17 has been a memorable year for the country and for our University. In the ever-changing and deeply uncertain world around us, the University of Oxford continues to attract the most talented students and the most talented academics from across the globe. They convene here, as they have always done, to learn, to push at the frontiers of knowledge and to improve the world in which we find ourselves. One of the highlights of the past twelve months was that for the second consecutive year we were named the top university in the world by the Times Higher Education Global Rankings. While it is reasonable to be sceptical of the precise placements in these rankings, it is incontrovertible that we are universally acknowledged to be one of the greatest universities in the world. This is a privilege, a responsibility and a challenge. Other highlights include the opening of the world’s largest health big data institute, the Li Ka Shing Centre for Health Information and Discovery, and the launch of OSCAR – the Oxford Suzhou Centre for Advanced Research – a major new research centre in Suzhou near Shanghai. In addition, the Ashmolean’s success in raising £1.35 million to purchase King Alfred’s coins, which included support from over 800 members of the public, was a cause for celebration. The pages that follow detail just some of the extraordinary research being conducted here on perovskite solar cells, indestructible tardigrades and driverless cars. -
Grassland to Shrubland State Transitions Enhance Carbon Sequestration in the Northern Chihuahuan Desert
Global Change Biology Global Change Biology (2015) 21, 1226–1235, doi: 10.1111/gcb.12743 Grassland to shrubland state transitions enhance carbon sequestration in the northern Chihuahuan Desert M. D. PETRIE1 ,S.L.COLLINS1 ,A.M.SWANN2 ,P.L.FORD3 andM.E. LITVAK1 1Department of Biology, University of New Mexico, Albuquerque, New Mexico, USA, 2Department of Biology, Sevilleta LTER, University of New Mexico, Albuquerque, New Mexico, USA, 3USDA Forest Service, Rocky Mountain Research Station, Albuquerque, New Mexico, USA Abstract The replacement of native C4-dominated grassland by C3-dominated shrubland is considered an ecological state tran- sition where different ecological communities can exist under similar environmental conditions. These state transi- tions are occurring globally, and may be exacerbated by climate change. One consequence of the global increase in woody vegetation may be enhanced ecosystem carbon sequestration, although the responses of arid and semiarid ecosystems may be highly variable. During a drier than average period from 2007 to 2011 in the northern Chihuahuan À2 À1 Desert, we found established shrubland to sequester 49 g C m yr on average, while nearby native C4 grassland À À was a net source of 31 g C m 2 yr 1 over this same period. Differences in C exchange between these ecosystems were pronounced – grassland had similar productivity compared to shrubland but experienced higher C efflux via ecosys- tem respiration, while shrubland was a consistent C sink because of a longer growing season and lower ecosystem respiration. At daily timescales, rates of carbon exchange were more sensitive to soil moisture variation in grassland than shrubland, such that grassland had a net uptake of C when wet but lost C when dry. -
Model-Based Analysis of the Impact of Diffuse
Agricultural and Forest Meteorology 249 (2018) 377–389 Contents lists available at ScienceDirect Agricultural and Forest Meteorology journal homepage: www.elsevier.com/locate/agrformet Model-based analysis of the impact of diffuse radiation on CO2 exchange in a T temperate deciduous forest Min S. Leea, David Y. Hollingerb, Trevor F. Keenanc, Andrew P. Ouimetted, Scott V. Ollingerd, ⁎ Andrew D. Richardsona,e,f, a Harvard University, Department of Organismic and Evolutionary Biology, 26 Oxford Street, Cambridge, MA 02138, USA b USDA Forest Service, Northern Research Station, 271 Mast Rd, Durham, NH 03824, USA c Climate and Ecosystem Sciences Division, Lawrence Berkeley National Lab., 1 Cyclotron Rd., Berkeley, CA 94720, USA d University of New Hampshire, Earth Systems Research Center, 8 College Rd, Durham, NH 03824, USA e Northern Arizona University, School of Informatics, Computing and Cyber Systems, PO Box 5693, Flagstaff, AZ 86011, USA f Northern Arizona University, Center for Ecosystem Science and Society, PO Box 5620, Flagstaff, AZ 86011, USA ARTICLE INFO ABSTRACT Keywords: Clouds and aerosols increase the fraction of global solar irradiance that is diffuse light. This phenomenon is Diffuse radiation known to increase the photosynthetic light use efficiency (LUE) of closed-canopy vegetation by redistributing Light use efficiency photosynthetic photon flux density (400–700 nm) from saturated, sunlit leaves at the top of the canopy, to Eddy covariance shaded leaves deeper in the canopy. We combined a process-based carbon cycle model with 10 years of eddy Net ecosystem exchange covariance carbon flux measurements and other ancillary data sets to assess 1) how this LUE enhancement Deciduous forest influences interannual variation in carbon uptake, and 2) how errors in modeling diffuse fraction affect pre- Canopy photosynthesis dictions of carbon uptake. -
Respiration from a Tropical Forest Ecosystem: Partitioning of Sources and Low Carbon Use Efficiency
Ecological Applications, 14(4) Supplement, 2004, pp. S72±S88 q 2004 by the Ecological Society of America RESPIRATION FROM A TROPICAL FOREST ECOSYSTEM: PARTITIONING OF SOURCES AND LOW CARBON USE EFFICIENCY JEFFREY Q. CHAMBERS,1,2,4 EDGARD S. TRIBUZY,2 LIGIA C. TOLEDO,2 BIANCA F. C RISPIM,2 NIRO HIGUCHI,2 JOAQUIM DOS SANTOS,2 ALESSANDRO C. ARAUÂ JO,2 BART KRUIJT,3 ANTONIO D. NOBRE,2 AND SUSAN E. TRUMBORE1 1University of California, Earth System Sciences, Irvine, California 92697 USA 2Instituto Nacional de Pesquisas da AmazoÃnia, C.P. 478, Manaus, Amazonas, Brazil, 69011-970 3Alterra, University of Wageningen, Alterra, 6700 AA Wageningen, The Netherlands Abstract. Understanding how tropical forest carbon balance will respond to global change requires knowledge of individual heterotrophic and autotrophic respiratory sources, together with factors that control respiratory variability. We measured leaf, live wood, and soil respiration, along with additional environmental factors over a 1-yr period in a Central Amazon terra ®rme forest. Scaling these ¯uxes to the ecosystem, and combining our data with results from other studies, we estimated an average total ecosystem respiration (Reco) of 7.8 mmol´m22´s21. Average estimates (per unit ground area) for leaf, wood, soil, total heterotrophic, and total autotrophic respiration were 2.6, 1.1, 3.2, 5.6, and 2.2 mmol´m22´s21, respectively. Comparing autotrophic respiration with net primary production (NPP) esti- mates indicated that only ;30% of carbon assimilated in photosynthesis was used to con- struct new tissues, with the remaining 70% being respired back to the atmosphere as autotrophic respiration. -
Arxiv:1810.00224V2 [Q-Bio.PE] 7 Dec 2020 Humanity Is Increasingly Influencing Global Environments [195]
A Survey of Biodiversity Informatics: Concepts, Practices, and Challenges Luiz M. R. Gadelha Jr.1* Pedro C. de Siracusa1 Artur Ziviani1 Eduardo Couto Dalcin2 Helen Michelle Affe2 Marinez Ferreira de Siqueira2 Luís Alexandre Estevão da Silva2 Douglas A. Augusto3 Eduardo Krempser3 Marcia Chame3 Raquel Lopes Costa4 Pedro Milet Meirelles5 and Fabiano Thompson6 1National Laboratory for Scientific Computing, Petrópolis, Brazil 2Friedrich-Schiller-University Jena, Jena, Germany 2Rio de Janeiro Botanical Garden, Rio de Janeiro, Brazil 3Oswaldo Cruz Foundation, Rio de Janeiro, Brazil 4National Institute of Cancer, Rio de Janeiro, Brazil 5Federal University of Bahia, Salvador, Brazil 6Federal University of Rio de Janeiro, Rio de Janeiro, Brazil Abstract The unprecedented size of the human population, along with its associated economic activities, have an ever increasing impact on global environments. Across the world, countries are concerned about the growing resource consumption and the capacity of ecosystems to provide them. To effectively conserve biodiversity, it is essential to make indicators and knowledge openly available to decision-makers in ways that they can effectively use them. The development and deployment of mechanisms to produce these indicators depend on having access to trustworthy data from field surveys and automated sensors, biological collections, molec- ular data, and historic academic literature. The transformation of this raw data into synthesized information that is fit for use requires going through many refinement steps. The methodologies and techniques used to manage and analyze this data comprise an area often called biodiversity informatics (or e-Biodiversity). Bio- diversity data follows a life cycle consisting of planning, collection, certification, description, preservation, discovery, integration, and analysis. -
Curriculum Vitae 1
Curriculum Vitae Emily Boyd School of Archaeology, Geography and Environmental Sciences (SAGES) Reading, RG1 6AH, UK Phone: +44 (0)118 3787756; Fax: +44 (0)118 975 5865; email: [email protected] Present appointment Professor of Resilience Geography, School of Archaeology, Geography and Environmental Sciences (SAGES) University of Reading Research climate resilience, adaptation & mitigation, governance and development theory DEGREES 1999-2003 Ph.D. University of East Anglia, School of Development Studies Thesis title: Forests Post Kyoto: Global Priorities and Local Realities Supervisors: Prof. Katrina Brown & Prof. Neil Adger. External examiner: Tim Forsyth, LSE. 1997-1998 MSc. University of Oxford, School of Plant Sciences 2.1 Thesis title: A natural resource assessment: A case study of Ncaute village in Namibia. Supervisor: Prof. Jeff Burly 1994 BSc. University of East Anglia, School of Development Studies (Hons)(2.1) Development Studies, 1st Class Final Dissertation PROFESSIONAL APPOINTMENTS 2011-2013 Reader, University of Reading, School of Human and Environmental Sciences, 2010-11 Maternity leave 2009-11 Lecturer in Environment and Development, University of Leeds, School of Earth and Environment; Deputy Director, Global Development Centre, University of Leeds Research on adaptation & mitigation, climate change risk assessment UK, resilience theory, India, UK 2007-09 Leverhulme early career fellow, University of Oxford, Environmental Change Institute Research on resilience, CDM and sustainable development in India 2006-07 James -
Oriel College Record
Oriel College Record 2020 Oriel College Record 2020 A portrait of Saint John Henry Newman by Walter William Ouless Contents COLLEGE RECORD FEATURES The Provost, Fellows, Lecturers 6 Commemoration of Benefactors, Provost’s Notes 13 Sermon preached by the Treasurer 86 Treasurer’s Notes 19 The Canonisation of Chaplain’s Notes 22 John Henry Newman 90 Chapel Services 24 ‘Observing Narrowly’ – Preachers at Evensong 25 The Eighteenth Century World Development Director’s Notes 27 of Revd Gilbert White 92 Junior Common Room 28 How Does a Historian Start Middle Common Room 30 a New Book? She Goes Cycling! 95 New Members 2019-2020 32 Eugene Lee-Hamilton Prize 2020 100 Academic Record 2019-2020 40 Degrees and Examination Results 40 BOOK REVIEWS Awards and Prizes 48 Gonzalo Rodriguez-Pereyra, Leibniz: Graduate Scholars 48 Discourse on Metaphysics 104 Sports and Other Achievements 49 Robert Wainwright, Early Reformation College Library 51 Covenant Theology: English Outreach 53 Reception of Swiss Reformed Oriel Alumni Advisory Committee 55 Thought, 1520-1555 106 CLUBS, SOCIETIES NEWS AND ACTIVITIES Honours and Awards 110 Chapel Music 60 Fellows’ and Lecturers’ News 111 College Sports 63 Orielenses’ News 114 Tortoise Club 78 Obituaries 116 Oriel Women’s Network 80 Other Deaths notified since Oriel Alumni Golf 82 August 2019 135 DONORS TO ORIEL Provost’s Court 138 Raleigh Society 138 1326 Society 141 Tortoise Club Donors 143 Donors to Oriel During the Year 145 Diary 154 Notes 156 College Record 6 Oriel College Record 2020 VISITOR Her Majesty the Queen -
Interpreting, Measuring, and Modeling Soil Respiration
Biogeochemistry (2005) 73: 3–27 Ó Springer 2005 DOI 10.1007/s10533-004-5167-7 -1 Interpreting, measuring, and modeling soil respiration MICHAEL G. RYAN1,2,* and BEVERLY E. LAW3 1US Department of Agriculture-Forest Service, Rocky Mountain Research Station, 240 West Pros- pect Street, Fort Collins, CO 80526, USA; 2Affiliate Faculty, Department of Forest, Rangeland and Watershed Stewardship and Graduate Degree Program in Ecology, Colorado State University Fort Collins, CO 80523, USA; 3Department of Forest Science, Oregon State University, 328 Richardson Hall, Corvallis, OR 97331, USA; *Author for correspondence (e-mail: [email protected]) Key words: Belowground carbon allocation, Carbon cycling, Carbon dioxide, CO2, Infrared gas analyzers, Methods, Soil carbon, Terrestrial ecosystems Abstract. This paper reviews the role of soil respiration in determining ecosystem carbon balance, and the conceptual basis for measuring and modeling soil respiration. We developed it to provide background and context for this special issue on soil respiration and to synthesize the presentations and discussions at the workshop. Soil respiration is the largest component of ecosystem respiration. Because autotrophic and heterotrophic activity belowground is controlled by substrate availability, soil respiration is strongly linked to plant metabolism, photosynthesis and litterfall. This link dominates both base rates and short-term fluctuations in soil respiration and suggests many roles for soil respiration as an indicator of ecosystem metabolism. However, the strong links between above and belowground processes complicate using soil respiration to understand changes in ecosystem carbon storage. Root and associated mycorrhizal respiration produce roughly half of soil respiration, with much of the remainder derived from decomposition of recently produced root and leaf litter. -
Global Satellite-Driven Estimates of Heterotrophic Respiration
Biogeosciences, 16, 2269–2284, 2019 https://doi.org/10.5194/bg-16-2269-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Global satellite-driven estimates of heterotrophic respiration Alexandra G. Konings1, A. Anthony Bloom2, Junjie Liu2, Nicholas C. Parazoo2, David S. Schimel2, and Kevin W. Bowman2 1Department of Earth System Science, Stanford University, Stanford, CA 94305, USA 2NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA Correspondence: Alexandra G. Konings ([email protected]) Received: 31 October 2018 – Discussion started: 15 November 2018 Revised: 4 April 2019 – Accepted: 10 May 2019 – Published: 4 June 2019 Abstract. While heterotrophic respiration (Rh) makes up to bottom-up estimates of annual heterotrophic respiration, about a quarter of gross global terrestrial carbon fluxes, using new uncertainty estimates that partially account for it remains among the least-observed carbon fluxes, partic- sampling and model errors. Top-down heterotrophic respira- ularly outside the midlatitudes. In situ measurements col- tion estimates are higher than those from bottom-up upscal- lected in the Soil Respiration Database (SRDB) number only ing everywhere except at high latitudes and are 30 % greater a few hundred worldwide. Similarly, only a single data- overall (43.6 Pg C yr−1 vs. 33.4 Pg C yr−1). The uncertainty driven wall-to-wall estimate of annual average heterotrophic ranges of both methods are comparable, except poleward of respiration exists, based on bottom-up upscaling of SRDB 45◦ N, where bottom-up uncertainties are greater. The ra- measurements using an assumed functional form to account tio of top-down heterotrophic to total ecosystem respiration for climate variability.