Increased Global Land Carbon Sink Due to Aerosol‐Induced Cooling

15823 10 87094 4 247453 document 87094 2018GB006051.pdf application/pdf 70f3fc9a5ca97573567ee93775252c06 MD5 2397704 2019-04-01 06:20:44 https://pure.iiasa.ac.at/id/eprint/15823/1/2018GB006051.pdf 15823 1 1 application/pdf text en public cc_by_nc_4

2018GB006051.pdf

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http://eprints.org/relation/isVersionOf https://pure.iiasa.ac.at/id/document/87094 http://eprints.org/relation/isVolatileVersionOf https://pure.iiasa.ac.at/id/document/87094 http://eprints.org/relation/issmallThumbnailVersionOf https://pure.iiasa.ac.at/id/document/87094 archive 353 disk0/00/01/58/23 2019-04-01 06:24:25 2021-08-27 17:31:35 2019-04-01 06:24:25 article show Zhang Y. Goll D. Bastos A. Balkanski Y. Boucher O. Cescatti A. Collier M. Gasser T. 2136 0000-0003-4882-2647 Ghattas J. Li L. Piao S. Viovy N. Zhu D. Ciais P. Increased Global Land Carbon Sink Due to Aerosol‐Induced Cooling pub prog_esm aerosols; climate sensitivity; CMIP5 climate; land carbon cycle; NBP; ORCHIDEE Anthropogenic aerosols have contributed to historical climate change through their interactions with radiation and clouds. In turn, climate change due to aerosols has impacted the C cycle. Here we use a set of offline simulations made with the Organising Carbon and Hydrology In Dynamic Ecosystems (ORCHIDEE) land surface model driven by bias-corrected climate fields from simulations of three Coupled Model Intercomparison Project Phase 5 (CMIP5) Earth system models (ESMs; IPSL-CM5A-LR, CSIRO-Mk3.6.0, and GISS-E2-R) to quantify the climate-related impacts of aerosols on land carbon fluxes during 1860–2005. We found that climate change from anthropogenic aerosols (CCAA) globally cooled the climate, and increased land carbon storage, or cumulative net biome production (NBP), by 11.6–41.8 PgC between 1860 and 2005. The increase in NBP from CCAA mainly occurs in the tropics and northern midlatitudes, primarily due to aerosol-induced cooling. At high latitudes, cooling caused stronger decrease in gross primary production (GPP) than in total ecosystem respiration (TER), leading to lower NBP. At midlatitudes, cooling-induced decrease in TER is stronger than that of GPP, resulting in NBP increase. At low latitudes, NBP was also enhanced due to the cooling-induced GPP increase, but precipitation decline from CCAA may negate the effect of temperature. The three ESMs show large divergence in low-latitude CCAA precipitation response to aerosols, which results in considerable uncertainties in regional estimations of CCAA effects on carbon fluxes. Our results suggest that better understanding and simulation of how anthropogenic aerosols affect precipitation in ESMs is required for a more accurate attribution of aerosol effects on the terrestrial carbon cycle. 2019-03 published American Geophysical Union 10.1029/2018GB006051 2885 public Global Biogeochemical Cycles 33 3 439-457 TRUE 1944-9224 Effects of phosphorus limitations on Life, Earth system and Society (IMBALANCE-P, FP7 610028) FALSE yes info:eu-repo/grantAgreement/EC/FP7/610028/EU/Effects of phosphorus limitations on Life, Earth system and Society/IMBALANCE-P info:eu-repo/semantics/article info:eu-repo/semantics/embargoedAccess