Present-day sources and past variability of mercury in the Arctic atmosphere and ocean AMAP Jenny A. Fisher University of Wollongong D. J. Jacob, A. L. Soerensen, H. M. Amos, E. D. Corbitt, D. G. Streets, Q. Wang, R. M. Yantosca, and E. M. Sunderland NASA Earth Observatory ACCESS XII 25-27 July 2013 Mercury in the Arctic Ocean: an ecological and human health concern Methylmercury is a potent neurotoxin that bioaccumulates in marine food webs. High mercury concentra:ons have been observed in Arc:c species that make up tradi:onal northern diets. Atmospheric transport brings mercury to the Arc:c, but atmosphere-‐ocean cycling is uncertain. Goal: Understand the factors contribu4ng to elevated mercury in the Arc4c atmosphere & ocean Jenny A. Fisher ([email protected]) AMAP 2011 ACCESS XII The atmosphere-ocean mercury cycle - an Arctic perspective Mid-‐la4tudes Arc4c 0 Hg HgII Snow/ice Hg0 II Hg Ocean subsurface Jenny A. Fisher ([email protected]) ACCESS XII The atmosphere-ocean mercury cycle - an Arctic perspective Mid-‐la4tudes Arc4c 0 Hg HgII Snow/ice Hg0 II Hg HgII Ocean subsurface Jenny A. Fisher ([email protected]) ACCESS XII The atmosphere-ocean mercury cycle - an Arctic perspective Mid-‐la4tudes Arc4c 0 Hg HgII Snow/ice Hg0 II Hg Hg0 HgII Ocean subsurface Jenny A. Fisher ([email protected]) ACCESS XII The atmosphere-ocean mercury cycle - an Arctic perspective Mid-‐la4tudes Arc4c 0 Hg HgII Snow/ice Hg0 II Hg Hg0 HgII Ocean subsurface Jenny A. Fisher ([email protected]) ACCESS XII The unique seasonal cycle of Arctic mercury summer maximum Observa4ons: mul>-‐year mean over three Arc>c sites (Alert, Amderma, Zeppelin) spring minimum: Atmospheric Mercury Deple:on Events Can we explain the summer peak using our standard understanding of mercury cycling? Jenny A. Fisher ([email protected]) ACCESS XII The GEOS-Chem biogeochemical mercury model The GEOS-‐Chem biogeochemical mercury model: • Global, gridded model • Driven by input meteorology from an assimilated GCM • 3-‐D atmosphere: emissions, chemistry, transport, and deposi:on • 2-‐D slab ocean mixed layer: chemistry, evasion, subsurface mixing and export • Cryospheric processes: AMDEs, snowpack re-‐emission, snowmelt delivery to ocean Represents our best a priori understanding of mercury sources & processes Jenny A. Fisher ([email protected]) ACCESS XII Testing our current understanding: model comparison to atmospheric observations summer maximum Observa4ons: mul>-‐year mean over three Arc>c sites spring minimum: Atmospheric Mercury Deple:on Events Can we explain the summer peak using our standard understanding of mercury cycling? Jenny A. Fisher ([email protected]) ACCESS XII Testing our current understanding: model comparison to atmospheric observations summer maximum Observa4ons: mul>-‐year mean over three Arc>c sites Model: GEOS-‐Chem at these sites in 2008 spring minimum: Atmospheric Mercury Deple:on Events Can we explain the summer peak using our standard understanding of mercury cycling? Jenny A. Fisher ([email protected]) ACCESS XII We test hypotheses using model sensitivity simulations 2.0 standard simula4on maximum oceanic reduc4on maximum snowpack reduc4on Hg0, ng.m-3 1.8 1.6 1.4 1.2 1.0 J F M A M J J A S O N D Month Atmospheric transport, snowpack processing, ocean chemistry cannot explain peak. Jenny A. Fisher ([email protected]) ACCESS XII We test hypotheses using model sensitivity simulations 2.0 Hg0, ng.m-3 1.8 standard simula4on + river/erosion source Arc4c Rivers 1.6 1.4 1.2 1.0 J F M A M J J A S O N D Month With a large river / coastal erosion source included, GEOS-‐Chem can reproduce the observed summer peak — a promising hypothesis, but more data are needed! Jenny A. Fisher ([email protected]) ACCESS XII Factors affecting Arctic mercury have changed dramatically Hg emissions growth: 1979-‐2010 Air temperature change: 1979-‐2010 May sea ice extent trend: 1979-‐2010 GISS NSIDC 2 Gg Asia USSR 0 Streets et al. (2011) What are the implica4ons for past — and future — variability in Arc4c Hg? Jenny A. Fisher ([email protected]) ACCESS XII Combined model-observation analysis lends insight Atmospheric [Hg0], 1995-‐2008 1. 30-‐year GEOS-‐Chem simula4on of Arc4c Hg (1979-‐2008) 2. Evaluated by long-‐term atmospheric observa4ons Alert, Canada (1995-‐2008) Zeppelin, Ny Ålesund (2000-‐2008) Pallas, Finland (1996-‐2008) 3. Extended to simula4on of surface ocean, where long-‐ term records unavailable Jenny A. Fisher ([email protected]) ACCESS XII We use interannual variability to identify drivers of change Focus on unique Arc:c signatures in spring and summer Atmospheric [Hg0] seasonal cycle Atmospheric [Hg0] 4me series Spring-‐summer trends are negligible, but IAV is large in observa4ons & model Jenny A. Fisher ([email protected]) ACCESS XII Atmospheric Hg variability governed by a combination of meteorological drivers Impacts of high T + low sea ice + high radia4on + shallow PBL SPRING SUMMER Environmental drivers of IAV iden:fied using a principal component analysis (PCA). Dominant mode explains 80% IAV in spring, 43% in summer. Jenny A. Fisher ([email protected]) ACCESS XII Surface ocean mercury driven by snowmelt & rivers pM Surface ocean [THg] Arc:c ocean mercury and IAV peak in summer 2.5 No trends in surface ocean mercury 2.0 J F M A M J J A S O N D Jenny A. Fisher ([email protected]) ACCESS XII Surface ocean mercury driven by snowmelt & rivers pM Surface ocean [THg] Arc:c ocean mercury and IAV peak in summer 2.5 No trends in surface ocean mercury 2.0 J F M A M J J A S O N D SUMMER Jenny A. Fisher Surface ocean inputs increase with: Meltwater • ⬆ summer solar radia:on (⬇ cloudiness) • ⬆ spring-‐summer T difference = ΔT Rivers • ⬆ May river flow Deposi4on • ⬆ summer wind speed ([email protected]) ACCESS XII Surface ocean mercury driven by snowmelt & rivers pM Surface ocean [THg] Arc:c ocean mercury and IAV peak in summer 2.5 No trends in surface ocean mercury 2.0 J F M A M J J A S O N D SUMMER Surface ocean inputs increase with: Meltwater • ⬆ summer solar radia:on (⬇ cloudiness) • ⬆ spring-‐summer T difference = ΔT Rivers • ⬆ May river flow Deposi4on • ⬆ summer wind speed GCMs predict future ⬆ cloudiness & ⬇ ΔT → less Hg may be added to the ArcDc Ocean in future! Jenny A. Fisher ([email protected]) ACCESS XII
© Copyright 2026 Paperzz