Ecosystem-scale trade-offs between impacts of ozone and reactive nitrogen Ed Rowe, Felicity Hayes, Kasia Sawicka, Gina Mills, Laurence Jones, Filip Moldan,

Slides:



Advertisements
Similar presentations
Working Group on Soil Biodiversity Dr Jonathan Leake.
Advertisements

Air Pollution and Climate
WRAP Meeting Nov 11, 2009 Ozone and Nitrogen Concerns in Western National Parks Chris Shaver Air Resources Division National Park Service.
Ecological Perspectives on Critical Loads - Linkages between Biogeochemical Cycles and Ecosystem Change Differences and Similarities in N and S Cycling.
European Nitrogen Assessment: Supplementary Material: Powerpoint Graphics to Chapter 5. Source: Sutton, M.A., Howard, C.M., Erisman J.W., Bealey J.W.,
Nitrogen and Ecosystem Nutrient Cycling Nicole and Sarah Biogeochemistry of Northern Ecosystems March 2005.
It was known during the 18th century that air contains at least two gases, one of which supports combustion and life, and the other of which does not.
Carbon Cycle and Ecosystems Important Concerns: Potential greenhouse warming (CO 2, CH 4 ) and ecosystem interactions with climate Carbon management (e.g.,
Janet F. Bornman Co-Chair, Environmental Effects Assessment Panel (EEAP) of the Montreal Protocol Curtin University Perth, Western Australia 6845
Federal Department of the Environment, Transport, Energy and Communications DETEC Federal Office for the Environment FOEN CCE Call for Data , Swiss.
Modelling regional impacts of trends and policies on EU and global level: Integrating agriculture, land use, environmental and socio- economic aspects.
Development of a mechanistic model of Hg in the terrestrial biosphere Nicole Smith-Downey Harvard University GEOS-Chem Users Meting April 12, 2007.
Human Disruption of the Global Nitrogen Cycle Alan Townsend 7 December 2007 Guest Lecture – Soils Geography University of Colorado, Boulder.
Professor John Agard UWI Environment in Development.
Daily EQ: What is the ozone layer, where do you find it, and why is it important?
Simple Chemical modeling of ozone sensitivity
Modelling C and N dynamics with MAGIC model from annual to seasonal/monthly time step Filip Oulehle, Jack Cosby, Chris Evans, Jakub Hruška, Jiří Kopáček,
Chapter 15 Air Pollution and Stratospheric Ozone Depletion.
Air Pollution: Concepts that may be confusing. The concepts we’ll deal with today The difference between stratospheric and tropospheric ozone Photochemical.
Non-pollutant ecosystem stress impacts on defining a critical load Or why long-term critical loads estimates are likely too high Steven McNulty USDA Forest.
Modeling impacts of atmospheric nitrogen deposition on terrestrial ecosystems: Implications for climate change J.J. Reyes 1, J.C. Adam 1, C. L. Tague 2,
1 Nitrogen in the Environment David Gay 1 & Bob Hall 2 1 NADP Program Office, (217) U.S. Environmental.
Preliminary Results Study Area Model Description Building a biosphere-relevant Earth system modeling framework: Modeling impacts of atmospheric nitrogen.
Valuation of damage to ecosystems due to air pollution Preliminary findings ECLAIRE-project Rome, 7-10 April 2014 Rob Maas, TFIAM.
Clean Air The revision of the National Emission Ceilings Directive and agriculture FERTILIZERS FORUM 23 June 2015.
RoTAP Chapter 7 European and Global Perspective 4-5 December 2008.
LBG/LB 1 Working Group on Effects, ICPM&M-Coordination Center for Effects, J.-P.Hettelingh, Gothenburg, October 2004 New developments on air pollution.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 15: Biosphere and Nutrients Don Wuebbles Department of Atmospheric Sciences University.
Development of a new method for peat acidity critical loads in the UK Chris Evans, Jane Hall, Ed Rowe.
Potential Risk of Acidification in South Asia Kevin Hicks Stockholm Environment Institute (SEI)
Translation to the New TCO Panel Beverly Law Prof. Global Change Forest Science Science Chair, AmeriFlux Network Oregon State University.
Atmospheric Composition & Air Quality (MAQ-34806) Lecturers: Maarten Krol Wouter Peters.
24 Global Ecology. Global Biogeochemical Cycles Atmospheric CO 2 affects pH of the oceans by diffusing in and forming carbonic acid.
Malé Declaration 1 ST emissions inventory workshop AIT, Bangkok, 3rd – 5th July 2006 Part 1 – The air pollution problem and the need for emissions inventories.
Network for the support of European Policies on Air Pollution The assessment of European control measures and the effects of non-linearities.
Consultation meetings: Jan 2005, Brussels, consultation meeting on topics for FP7 2-3 Feb 06, Brussels, Symposium in memoriam Anver Ghazi 17 Feb 06, Text.
Integrated Assessment of Air Pollution and Greenhouse Gases Mitigation Janusz Cofala International Institute for Applied Systems Analysis (IIASA) Laxenburg,
Empirical determination of N critical loads for alpine vegetation William D. Bowman, Julia L. Gartner, Keri Holland, and Magdalena Wiedermann Department.
Potential Risk of Acidification in South Asia Kevin Hicks and Johan Kuylenstierna SEI
Chapter 16 Human Impact on Ecosystems
Attaining urban air quality objectives- links to transboundary air pollution Helen ApSimon, Tim Oxley and Marios Valiantis UK Centre for Integrated Assessment.
ATMOS 397G Presentation Long Cao April 19th, 2100.
Air Pollution What controls the level? –Amount of pollutants entering the air. –Amount of space into which the pollutants are dispersed. –Mechanisms that.
1 Trends in soil solution chemistry in temperate forests under on-going recovery from acidification and climate change in Flanders, Belgium Arne Verstraeten.
JEG DM: common work items Targets & ex post analysis Robustness Links with biodiversity Trends in selected modeled/measured parameters.
Ecological Perspectives on Critical Loads - Linkages between Emissions, Deposition and Biogeochemical Cycles J. N. Galloway Multi-Agency Critical Loads.
Air Pollution and Stratospheric Ozone Depletion
TF HTAP, TF IAM, Vienna, February HTAP-GAINS scenario analysis: preliminary exploration of emission scenarios with regard to the benefits of global.
Integrated Land Ecosystem Atmosphere Process Study Outgoing Co-Chair: Alex Guenther, UC Irvine Co-Chair: Hans C Hansson, Stockholm Univ. Incoming co-chair:
JEG DM: progress in DM dynamic models became a commonly used tool, several ICPs and national focal points use DM DM provide timescale to expected changes.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 18: Nitrogen Cycle Don Wuebbles Department of Atmospheric Sciences University of Illinois,
ECLAIRE: Effects of climate change on air pollution impacts and response strategies for European ecosystems.
Preliminary ECLAIRE findings Budapest, 2 October 2014 Rob Maas, RIVM.
Nitrous Oxide Focus Group Nitrous Oxide Focus Group launch event Friday February 22 nd, 2008 Dr Jan Kaiser Dr Parvadha Suntharalingam The stratospheric.
Alejandro Gallego Schmid Department of Chemical Engineering University of Santiago de Compostela (Spain) Boston, 30 th September 2009 Calculation of LCA.
NITROGEN OXIDES Formation and Relevance. WHERE DO NITROGEN OXIDES COME FROM? The most important forms of reactive nitrogen in the air are nitrogen monoxide.
Atmospheric Deposition Unit 4451 Research on Air Pollution Distribution and Effects in California Mountains Andrzej Bytnerowicz, Michael Arbaugh, Nancy.
Informed NPS Air Quality Management Decisions in Response to a Changing Climate.
Preparations for the Ozone Critical Levels Workshop (November, 2016)
Air Pollution and Stratospheric Ozone Depletion
Advanced Placement Environmental Science Teacher
Soil acidification affects carbon cycling more than nitrogen addition in European conifer and broadleaf forests Filip Oulehle, Karolina Tahovská, Tomáš.
Brooke Perry Rebecca Faust Jeff Bogutsky Donovan Sweet Leah Holleman
MOUNTAINS AT RISK.
Dr. Tanveer Iqbal Associate Professor,
DO NOW Pick up notes and Review #31..
Key Messages on Soils and Nutrient Cycling effects
Air Pollution and Stratospheric Ozone Depletion
Air Pollution and Stratospheric Ozone Depletion
Presentation transcript:

Ecosystem-scale trade-offs between impacts of ozone and reactive nitrogen Ed Rowe, Felicity Hayes, Kasia Sawicka, Gina Mills, Laurence Jones, Filip Moldan, Sereina Bassin, Netty van Dijk & Chris Evans EGU, Vienna, 13th April 2015

Nitrogen is an acidifying pollutant Giant Mountains, Czech Republic, 2005 UK NO x emissions UK NH 3 emissions RoTAP report, CEH, 2012 Temporal deposition sequence from GANE project (Fowler et al 2004 WASP:Focus 4: 9-23) UK SO 2 emissions Many systems are recovering from ‘acid rain’ But reductions in reactive-nitrogen (NO x, NH y ) emissions have been small, compared to reductions in S emissions

Nitrogen is also a fertiliser End of the fertiliser bag, Mutare, Zimbabwe, 2002 Ammonium nitrate delivery, Gwynedd, UK, 2006 ‘Current Legislated [N] Emissions’ ‘Maximum Feasible [N] Reduction’ de Vries & Posch (2011) Env Poll 159: Additional European C sequestration due to N pollution

 not good for species that need ground-level light Hodgson et al. (2014) Functional Ecology 28: more N --> increasing productivity ground-level shade litterfall Drosera rotundifolia Urtica dioica Lotus corniculatus

N deposition reduces species-richness Acid grassland, UK Heathland, UK Stevens et al. (2004) Science 303: Maskell et al. (2010) Global Change Biol.16: 671–679 kg N ha -1 y -1 Number of species Number of species

Global reactive-N deposition Dentener et al Global Biogeochem Cycles 20: GB4003 mg N m -2 yr -1 “For terrestrial ecosystems, land-use change probably will have the largest effect [on biodiversity], followed by climate change, nitrogen deposition, biotic exchange, and elevated carbon dioxide concentration.” Sala et al 2000, Science 287: kg N ha -1 yr

Predicting effects of N and S (MADOC) N14C: Tipping et al Ecological Modelling 247:11-26 VSD: Posch & Reinds 2009 Env Modelling and Software 24: DyDOC: Michalzik et al Biogeochemistry 66, N14C: vegetation growth and soil organic matter development VSD: cation exchange and pH DyDOC: dissolution of organic matter MADOC: dynamic integration, allowing feedback between pH and DOC

MADOC passes some plausibility tests Rowe et al Environmental Pollution 184, Calibration dataset (EHFI acidification / alkalisation experiment) Independent dataset (Acid Waters Monitoring Network sites)

Predicting effects on plant species and biodiversity Floristic response MultiMOVE Vegetation and soil biogeochemistry MADOC Total N deposition Indicators of environmental conditions e.g. pH, mineral N, light Habitat suitability for individual species Other drivers Biogeochemistry Plant ecology Quantity Model Key: Other drivers Rhynchospora alba Smart et al J Veg Sci 21: 643:656 Henrys et al. New J Bot in prep.

Summarising effects on ‘biodiversity’ Rowe et al. (submitted) Ecological Indicators

How will ozone pollution interact? Ozone in the stratosphere protects the planet from ultraviolet radiation …but tropospheric i.e. ‘ground-level’ ozone is a problem. Formed in reactions involving nitrogen oxides and Volatile Organic Compounds European NO x and VOC emissions controls  decreasing peak concentrations Hemispheric transport  increasing background concentrations Effects on human health Damage to plants  increasing crop losses Photo: Gina Mills Tropospheric ozone formation diagram:

Ozone effects supported by evidence 1.Decreasing plant productivity (NPP) at greater ozone concs.  reduced productivity, reduced carbon inputs 2.Reduced translocation of N out of senescing leaves at greater ozone concs.  more potential for N loss e.g. leaching, N 2 O

Ozone effects added into MADOC 1.Reduction in NPP with increasing ozone concentration

Ozone effects added into MADOC 2. Reduced translocation of N out of senescing leaves with increasing ozone conc.

Sites simulated LlynBrianne Montseny Alpflix Brandbjerg Whim Grizedale Sourhope Gårdsjøn Clocaenog Kiskunsag Klausen Oldebroek Sites modelled in ECLAIRE

Responses to N treatments Whim Moss Scotland heath exposed to dry NH 3 or wet NaNO 3 or wet NH 4 Cl Symbols = Modelled Lines = observed

Responses to N treatments Gårdsjön Sweden coniferous forest subcatchments Treatments: Control; +40 kg N ha -1 yr -1 (wet NH 4 NO 3 ) Symbols = Modelled Lines = observed

Responses to N x O 3 treatments AlpFlix Switzerland Alpine grassland, extremely low N deposition, but chronically exposed to ozone Experimental responses (circles): Strong productivity response to N No significant productivity response to ozone Bassin et al (2007) New Phytologist 175, Modelled responses (lines): responses to N and ozone negative interaction (ozone limits response to N, and vice versa) Symbols = Modelled Lines = observed

Sensitivity of productivity to N and Ozone i.e. ozone reduces plant productivity by a greater proportion at greater N deposition  Could it be said that ozone pollution moderates the effects of N pollution?

Direct ozone effects on biodiversity Hayes et al. (unpublished) Effect of ozone exposure on cover of Campanula rotundifolia in calcareous grassland

Conclusions We need more ecosystem-level experiments on N-ozone interactions Simulations are the best available basis for assessing ecosystem effects of O 3 and N N is likely to increase productivity  benefits for agriculture and forestry, C storage  disbenefits for biodiversity Ozone is likely to decrease productivity  benefits for biodiversity?  likely to be outweighed by direct adverse effects of O 3 N and ozone together are likely to increase soil N cycling rates  disbenefits due to N leaching and NOx emissions Acknowledgements This work was funded by the UK Government (Defra) and by the European Union (FP7 ECLAIRE project)