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Future Inhibition of Ecosystem Productivity by Increasing Wildfire Pollution Over Boreal North America Xu Yue, Susanna Strada, Nadine Unger, Aihui Wang

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Future Inhibition of Ecosystem Productivity by Increasing Wildfire Pollution Over Boreal North America Xu Yue, Susanna Strada, Nadine Unger, Aihui Wang Future inhibition of ecosystem productivity by increasing wildfire pollution over boreal North America Xu Yue, Susanna Strada, Nadine Unger, Aihui Wang To cite this version: Xu Yue, Susanna Strada, Nadine Unger, Aihui Wang. Future inhibition of ecosystem productivity by increasing wildfire pollution over boreal North America. Atmospheric Chemistry and Physics, Euro- pean Geosciences Union, 2017, 17 (22), pp.13699-13719. 10.5194/acp-17-13699-2017. hal-03226939 HAL Id: hal-03226939 https://hal.archives-ouvertes.fr/hal-03226939 Submitted on 16 May 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License Atmos. Chem. Phys., 17, 13699–13719, 2017 https://doi.org/10.5194/acp-17-13699-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Future inhibition of ecosystem productivity by increasing wildfire pollution over boreal North America Xu Yue1,2, Susanna Strada3, Nadine Unger4, and Aihui Wang2 1Climate Change Research Center, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 2Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 3Laboratoire des Sciences du Climat et de l’Environnement, L’Orme des Merisiers – Bat 712, 91191 Gif-Sur-Yvette, France 4College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, EX4 4QE, UK Correspondence to: Xu Yue ([email protected]) Received: 5 April 2017 – Discussion started: 23 June 2017 Revised: 11 October 2017 – Accepted: 12 October 2017 – Published: 17 November 2017 Abstract. Biomass burning is an important source of tropo- direct emissions increasing from 68 Tg C yr−1 at present day −1 spheric ozone (O3) and aerosols. These air pollutants can af- to 130 Tg C yr by mid-century but also through the bio- fect vegetation photosynthesis through stomatal uptake (for physical impacts of fire aerosols. O3) and light scattering and absorption (for aerosols). Wild- fire area burned is projected to increase significantly in bo- real North America by the mid-century, while little is known about the impacts of enhanced emissions on the terrestrial carbon budget. Here, combining site-level and satellite obser- 1 Introduction vations and a carbon–chemistry–climate model, we estimate the impacts of fire emitted O3 and aerosols on net primary The area burned by wildfire is increasing in recent decades productivity (NPP) over boreal North America. Fire emis- in North American boreal regions (Stocks et al., 2002; Ka- sions are calculated based on an ensemble projection from sischke and Turetsky, 2006). Fire activity is closely related 13 climate models. In the present day, wildfire enhances sur- to weather conditions and large-scale atmospheric oscilla- face O3 by 2 ppbv (7 %) and aerosol optical depth (AOD) tions (Gillett et al., 2004; Duffy et al., 2005) and is pro- at 550 nm by 0.03 (26 %) in the summer. By mid-century, jected to increase significantly in the future due to climatic area burned is predicted to increase by 66 % in boreal North changes (Flannigan et al., 2005; Balshi et al., 2009; de Groot America, contributing more O3 (13 %) and aerosols (37 %). et al., 2013; Wang et al., 2015). More area burned and the Fire O3 causes negligible impacts on NPP because ambient consequent fire emissions are accelerating carbon loss in O3 concentration (with fire contributions) is below the dam- boreal North America (Bond-Lamberty et al., 2007; Turet- age threshold of 40 ppbv for 90 % summer days. Fire aerosols sky et al., 2011). Meanwhile, fire-induced air pollution, in- reduce surface solar radiation but enhance atmospheric ab- cluding ozone (O3) and aerosols, is predicted to increase sorption, resulting in enhanced air stability and intensified in boreal and downwind regions by mid-century (Yue et regional drought. The domain of this drying is confined to the al., 2013, 2015). Wildfire emissions have large impacts on north in the present day but extends southward by 2050 due air quality (Wotawa and Trainer, 2000; Morris et al., 2006), to increased fire emissions. Consequently, wildfire aerosols weather and climate conditions (Randerson et al., 2006; Zhao enhance NPP by 72 Tg C yr−1 in the present day but decrease et al., 2014), and public health (Zu et al., 2016; Liu et NPP by 118 Tg C yr−1 in the future, mainly because of the al., 2017). However, little is known about how these pollu- soil moisture perturbations. Our results suggest that future tants affect ecosystem carbon assimilation and how this im- wildfire may accelerate boreal carbon loss, not only through pact will change with the increased wildfire activity in the future. Published by Copernicus Publications on behalf of the European Geosciences Union. 13700 X. Yue et al.: Inhibition of NPP by fire pollution Surface O3 causes damages to photosynthesis through stomatal uptake (Sitch et al., 2007). In the present climate state, fire-induced O3 enhancements are predicted to reduce net primary productivity (NPP) in the Amazon forest by −1 12 Aerosol s increase 230 Tg C yr (1 Tg D 10 g), a magnitude comparable to diffuse light and change T & P the direct release of CO2 from fires in South America (Paci- fico et al., 2015). The aerosol effects are more uncertain be- NOx, CO cause both positive and negative feedbacks occur. Appear- NMVOC ance of aerosols increases diffuse light, which is beneficial BVOC for shaded leaves in the lower canopy. Consequently, pho- tosynthesis of the whole ecosystem will increase as long as Ozone the total light availability is not compromised (Kanniah et Damaged plants al., 2012). Rap et al. (2015) estimated that biomass burning aerosols increase Amazon NPP by 78–156 Tg C yr−1, which Figure 1. Illustration of atmospheric chemistry and physics as offsets about half of the damage caused by fire O3 (Paci- . Illustration of atmospheric chemistry and physics, and biospheric processes well as biospheric processes investigated in the study. Carbona- fico et al., 2015). In contrast, strong light attenuation asso- fire plumes increase diffuse light and ceous aerosols from fire plumes increase diffuse light and change temperature and precipitation, influencing vegetation photosynthesis. Ozone ciated with high aerosol loading may decrease canopy pho- temperature (T) and precipitation (P), influencing vegetation pho- -emitted precursors (NOx, CO, and non-methane volatile tosynthesis (Cohan et al., 2002; Oliveira et al., 2007; Cirino tosynthesis. Ozone generated photochemically from fire-emitted (NMVOC)) and associated BVOC changes causes direct damage to plant et al., 2014). Furthermore, the aerosol radiative effects indi- precursors (NOx, CO, and non-methane volatile organic com- rectly influence ecosystem productivity through concomitant pounds,ynthesis. NMVOC) and associated biogenic volatile organic com- meteorological perturbations that are only beginning to be pound (BVOC) changes causes direct damage to plant photosyn- examined (Yue et al., 2017). thesis. Future wildfire activity is projected to increase over bo- real North America but with large uncertainties (Flannigan et al., 2005; Tymstra et al., 2007; Girardin and Mudelsee, that the wildfire emission increase by the 2050s would in- 2008; Nitschke and Innes, 2008; Amiro et al., 2009; Bal- crease mean summertime surface O3 by 5 ppbv in Alaska and shi et al., 2009; Bergeron et al., 2010; Wotton et al., 2010; 3 ppbv in Canada. The study found regional maximum O3 de Groot et al., 2013; Wang et al., 2016). For example, Amiro enhancements as high as 15 ppbv, suggesting the potential for et al. (2009) predicted an increase of 34 % in the area burned possible vegetation damage and land carbon loss due to the in Canada for a 2 × CO2 scenario (2040–2060) relative to enhanced boreal fire-related air pollution. Wildfire aerosols a 1 × CO2 condition (1975–1995), using the Canadian Fire are also expected to increase significantly but not predicted Weather Index (CFWI) and output from the Canadian Global in Yue et al. (2015). Climate Model (CGCM) version 1. Balshi et al. (2009) pro- In this study, we quantify the impacts of O3 and aerosols jected that area burned in boreal North America would dou- emitted from boreal wildfires on the land carbon uptake in ble by the year 2045–2050 relative to 1991–2000, using the North America in the present climate state and in the future Multivariate Adaptive Regression Splines (MARS) approach world at 2050, taking advantage of the ensemble projection and meteorological output from CGCM version 2. The in- of future wildfire emissions by Yue et al. (2015). The major creasing rate in Balshi et al. (2009) is higher than that in chain we investigate includes (i) generation of aerosols and Amiro et al. (2009), indicating substantial uncertainties in surface ozone from wildfire emissions and (ii) impact of fire- fire projections originating from both fire models and simu- emitted aerosols and ozone on plant photosynthesis through lated future climate. However, even with the same fire mod- physical and biogeochemical processes (Fig. 1). We first an- els and climate change scenario, large uncertainties (in both alyze relationships between gross primary production (GPP) magnitude and signs) are found in the projection of area and aerosol optical depth (AOD) at 550 nm over the boreal burned among individual climate models (Moritz et al., 2012; regions based on observations. We then perform a suite of Yue et al., 2013).
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