Role of Ocean Emissions in the Mercury Budget Sarah Strode, Lyatt Jaeglé Department of Atmospheric Sciences, University of Washington Noelle Eckley Selin,

Slides:



Advertisements
Similar presentations
Earth Science & Climate Change, San Francisco, July 2014 Overview of Spatial and Temporal Distributions of Speciated Mercury Huiting Mao Department.
Advertisements

FRONTAL SYSTEMS CLIMATOLOGY OVER SOUTHEASTERN SOUTH AMERICA AND ASSOCIATED ATMOSPHERIC CIRCULATION IN A CLIMATE GCM SIMULATION Iracema FA Cavalcanti Luiz.
Development of a mechanistic model of Hg in the terrestrial biosphere Nicole Smith-Downey Harvard University GEOS-Chem Users Meting April 12, 2007.
 Similar picture from MODIS and MISR aerosol optical depth (AOD)  Both biomass and dust emissions in the Sahel during the winter season  Emissions.
Mercury & GCAP Nicole Smith-Downey, Noelle Eckley Selin, Chris Holmes, Bess Sturges, Daniel Jacob Harvard University Elsie Sunderland US EPA Sarah Strode,
What controls the climatological PBL depth? Brian Medeiros Alex Hall Bjorn Stevens UCLA Department of Atmospheric & Oceanic Sciences 16th Symposium on.
Lecture 7-8: Energy balance and temperature (Ch 3) the diurnal cycle in net radiation, temperature and stratification the friction layer local microclimates.
Mercury Chemistry in the Global Atmosphere: Constraints from Mercury Speciation Measurements Noelle Eckley Selin EPS Grad Student Seminar Series 14 February.
Building a Global Modeling Capability for Mercury with GEOS-CHEM Noelle Eckley Selin, Rokjin J. Park, Daniel J. Jacob Constraining the global budget of.
Transpacific transport of pollution as seen from space Funding: NASA, EPA, EPRI Daniel J. Jacob, Rokjin J. Park, Becky Alexander, T. Duncan Fairlie, Arlene.
Building a Global Modeling Capability for Mercury with GEOS-CHEM Noelle Eckley Selin GEOS-CHEM meeting 6 April 2005.
Sarah Strode, Lyatt Jaeglé, Dan Jaffe, Peter Weiss-Penzias, Phil Swartzendruber University of Washington Noelle Eckley Selin, Chris Holmes, Daniel Jacob.
U N I V E R S I T Y O F W A S H I N G T O N S C H O O L O F N U R S I N G Sensitivity of surface O 3 to soil NO x emissions over the U.S. Lyatt Jaeglé.
Discerning mercury-halogen chemistry from diurnal cycles of RGM Christopher Holmes, Daniel Jacob, Noelle Eckley Selin Harvard University Dan Jaffe, Phil.
5.7 PW5.9 PW The seasonal cycle of energy fluxes in the high latitudes Aaron Donohoe I.) How do the absorbed solar (ASR), outgoing longwave (OLR), and.
Global simulation of H 2 and HD with GEOS-CHEM Heather Price 1, Lyatt Jaeglé 1, Paul Quay 2, Andrew Rice 2, and Richard Gammon 2 University of Washington,
A Biogeochemical Model for Mercury in GEOS-Chem Noelle Eckley Selin GEOS-Chem 3rd Users’ Meeting April 12, 2007 Hg(0)Hg(II) MeHgHg(II) Why we care about.
ARM Atmospheric Radiation Measurement Program. 2 Improve the performance of general circulation models (GCMs) used for climate research and prediction.
NOCES meeting Plymouth, 2005 June Top-down v.s. bottom-up estimates of air-sea CO 2 fluxes : No winner so far … P. Bousquet, A. Idelkadi, C. Carouge,
Effects of Siberian forest fires on regional air quality and meteorology in May 2003 Rokjin J. Park with Daeok Youn, Jaein Jeong, Byung-Kwon Moon Seoul.
Evaluating the Role of the CO 2 Source from CO Oxidation P. Suntharalingam Harvard University TRANSCOM Meeting, Tsukuba June 14-18, 2004 Collaborators.
3 rd GEOS-Chem Users’ Meeting April 12, 2007 Elsie Sunderland U.S. Environmental Protection Agency Office of Research & Development National Center for.
WP4 Tropospheric composition Reeves, Coe, Heard, Lewis, Monks, Pyle In the case of WP4 the objectives have been subdivided so that individual groups (first-
Building a Global Modeling Capability for Mercury with GEOS-CHEM Noelle Eckley Selin, Rokjin J. Park, Daniel J. Jacob Constraining the global budget of.
Mercury Source Attribution at Global, Regional and Local Scales Christian Seigneur, Krish Vijayaraghavan, Kristen Lohman, and Prakash Karamchandani AER.
SOURCE ATTRIBUTION OF MERCURY EXPOSURE FOR U.S. SEAFOOD CONSUMERS: IMPLICATIONS FOR POLICY Noelle Eckley Selin Joint Program on the Science and Policy.
MERCURY IN THE ATMOSPHERE, BIOSPHERE, AND POLICY SPHERE: MERCURY IN THE ATMOSPHERE, BIOSPHERE, AND POLICY SPHERE: Constraints from a global 3D land-ocean-atmosphere.
Pacific vs. Indian Ocean warming: How does it matter for global and regional climate change? Joseph J. Barsugli Sang-Ik Shin Prashant D. Sardeshmukh NOAA-CIRES.
Potential temperature ( o C, Levitus 1994) Surface Global zonal mean.
Challenges in Global Mercury Modeling Ashu Dastoor Meteorological Service of Canada Environment Canada Acknowledgements: Didier Davignon and Arturo Quintanar.
Interannual variability across sites: Bridging the gap between flux towers and flasks Goals Obtain a mechanistic understanding of tower-scale interannual.
NEW PERSPECTIVES ON ATMOSPHERIC MERCURY Daniel J. Jacob with Noelle E. Selin and Christopher D. Holmes Supported by NSF, EPA and Sarah Strode and Lyatt.
U N I V E R S I T Y O F W A S H I N G T O N S C H O O L O F N U R S I N G U N I V E R S I T Y O F W A S H I N G T O N DEPARTMENT OF ATMOSPHERIC SCIENCES.
The Large-Scale Energy Budget of the Arctic Mark C. Serreze National Snow and Ice Data Center (NSIDC) Cooperative Institute for Research in Environmental.
Linking sea surface temperature, surface flux, and heat content in the North Atlantic: what can we learn about predictability? LuAnne Thompson School of.
OMI HCHO columns Jan 2006Jul 2006 Policy-relevant background (PRB) ozone calculations for the EPA ISA and REA Zhang, L., D.J. Jacob, N.V. Smith-Downey,
The Influence of Tropical-Extratropical Interactions on ENSO Variability Michael Alexander NOAA/Earth System Research Lab.
Global Modeling of Mercury in the Atmosphere using the GEOS-CHEM model Noelle Eckley, Rokjin Park, Daniel Jacob 30 January 2004.
Human fingerprints on our changing climate Neil Leary Changing Planet Study Group June 28 – July 1, 2011 Cooling the Liberal Arts Curriculum A NASA-GCCE.
Building a Global Modeling Capability for Mercury with GEOS-CHEM Noelle Eckley Selin EPS Day 12 March 2005.
Mean 20 o C isotherm (unit: meter) The thermocline zone is sometimes characterized by the depth at which the temperature gradient is a maximum (the “thermocline.
Approach: Assimilation Efficiencies The Carbon based model calculates mixed layer NPP (mg m -3 ) as a function of carbon and phytoplankton growth rate:
1 Improving the parameterization of land-surface exchange in the GEOS-Chem Hg model Shaojie Song and Noelle Selin Massachusetts Institute of Technology.
Oceanic mixed layer heat budget in the Eastern Equatorial Atlantic using ARGO floats and PIRATA buoys M. Wade (1,2,3), G. Caniaux (1) and Y. du Penhoat.
SOURCE ATTRIBUTION OF MERCURY EXPOSURE FOR U.S. SEAFOOD CONSUMERS: IMPLICATIONS FOR POLICY Noelle Eckley Selin Joint Program on the Science and Policy.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 14: Methane and CO Don Wuebbles Department of Atmospheric Sciences University of Illinois,
04/12/011 The contribution of Earth degassing to the atmospheric sulfur budget By Hans-F. Graf, Baerbel Langmann, Johann Feichter From Chemical Geology.
Tom Breider, Loretta Mickley, Daniel Jacob, Cui Ge, Jun Wang, Melissa Payer, Betty Croft, David Ridley, Sangeeta Sharma, Kostas Eleftheriadis, Joe McConnell,
An Observationally-Constrained Global Dust Aerosol Optical Depth (AOD) DAVID A. RIDLEY 1, COLETTE L. HEALD 1, JASPER F. KOK 2, CHUN ZHAO 3 1. CIVIL AND.
GEOS-CHEM Activities at NIA Hongyu Liu National Institute of Aerospace (NIA) at NASA LaRC June 2, 2003.
Examining Fresh Water Flux over Global Oceans in the NCEP GDAS, CDAS, CDAS2, GFS, and CFS P. Xie 1), M. Chen 1), J.E. Janowiak 1), W. Wang 1), C. Huang.
MICHAEL A. ALEXANDER, ILEANA BLADE, MATTHEW NEWMAN, JOHN R. LANZANTE AND NGAR-CHEUNG LAU, JAMES D. SCOTT Mike Groenke (Atmospheric Sciences Major)
THE ATMOSPHERIC CYCLE OF MERCURY AND THE ROLE OF COAL-BASED EMISSIONS Noelle Eckley Selin Harvard University Department of Earth and Planetary Sciences.
Sea Ice, Solar Radiation, and SH High-latitude Climate Sensitivity Alex Hall UCLA Department of Atmospheric and Oceanic Sciences SOWG meeting January 13-14,
Global-scale Mercury Modeling: Status and Improvements Daniel J. Jacob with Noelle E. Selin 1, Christopher D. Holmes, Nicole V. Downey, Elizabeth D. Sturges.
The Solar Radiation Budget, and High-latitude Climate Sensitivity Alex Hall UCLA Department of Atmospheric and Oceanic Sciences University of Arizona October.
Background ozone in surface air over the United States Arlene M. Fiore Daniel J. Jacob US EPA Workshop on Developing Criteria for the Chemistry and Physics.
Nitrous Oxide Focus Group Nitrous Oxide Focus Group launch event Friday February 22 nd, 2008 Dr Jan Kaiser Dr Parvadha Suntharalingam The stratospheric.
Trends in atmospheric mercury and implications for past and future mercury accumulation in surface reservoirs Daniel J. Jacob with Anne Sørensen, Hannah.
CONSTRAINTS FROM RGM MEASUREMENTS ON GLOBAL MERCURY CHEMISTRY Noelle Eckley Selin 1 Daniel J. Jacob 1, Rokjin J. Park 1, Robert M. Yantosca 1, Sarah Strode,
Issues surrounding NH high- latitude climate change Alex Hall UCLA Department of Atmospheric and Oceanic Sciences.
The role of Arctic sea ice in defining European extreme winters
GLOBAL CYCLING OF MERCURY
Annual cycle of cloud fraction and surface radiative cloud forcing in the South-East Pacific Stratocumulus region Virendra P. Ghate and Bruce A. Albrecht.
Daniel J. Jacob Harvard University
Building a Global Modeling Capability for Mercury with GEOS-CHEM
+ = Climate Responses to Biomass Burning Aerosols over South Africa
From hemispheric to local scale air pollution: Mercury
Extratropical Climate and Variability in CCSM3
From hemispheric to local scale air pollution: Mercury
Presentation transcript:

Role of Ocean Emissions in the Mercury Budget Sarah Strode, Lyatt Jaeglé Department of Atmospheric Sciences, University of Washington Noelle Eckley Selin, Rokjin Park, Daniel Jacob Noelle Eckley Selin, Rokjin Park, Daniel Jacob Department of Earth and Planetary Sciences, Harvard University

The ocean in the global Hg budget From Mason and Sheu, 2002 The ocean represents about a third of the total source to the atmosphere The magnitude, seasonality, and distribution of the flux are still uncertain reemits deposited mercury  role in global transport

Ocean-atmosphere cycling of Hg 0 Hg 0 Hg II Surface ocean Evasion (T,wind) deposition transport P(light,biology) reduction Hg 0 Hg II Marine Boundary Layer oxidation Loss Reduction proportional to radiation and net primary productivity (MODIS 2003) Reduction proportional to radiation and net primary productivity (MODIS 2003) d[Hg II ] aq /dt = deposition – Kl*[Hg II ] aq – Kr*[Hg II ] aq d[Hg II ] aq /dt = deposition – Kl*[Hg II ] aq – Kr*[Hg II ] aq d[Hg 0 ] aq /dt = Kr*[Hg II ] aq – Kw([Hg 0 ] aq – H*[Hg 0 ] atmos ) d[Hg 0 ] aq /dt = Kr*[Hg II ] aq – Kw([Hg 0 ] aq – H*[Hg 0 ] atmos ) Evasion based on kw=f(T,u 10 2 ) and H=f(T) Evasion based on kw=f(T,u 10 2 ) and H=f(T) Loss and reduction scaled together to yield total flux=2000 Mg/yr Loss and reduction scaled together to yield total flux=2000 Mg/yr MLD from NRL mixedlayer depth climatology  =7 months  =7 months (4-79 months)

Observed & modeled total aqueous Hg June-AugSept-Oct March-MayDec-Feb pM Observations from: Coquery & Cossa 1995, Cossa et al. 2004, Dalziel 1995, Ferrara et al. 2003, Gill & Fitgerald 1987, Kim & Fitgerald 1986, Laurier et al. 2004, Mason & Fitgerald 1993, Mason et al. 1998, Mason et al. 2001, Mason & Sullivan 1999

Comparison to Observations DGM (pM)Ocean Flux (ng/m 2 /h) Med. Sea N. Atl. N. Atl. Baltic Pacific JJA SON JJA MAM MAM Med. Sea N. Atl. eq. Pac Baltic eq. Pac N. Atl. JJA JJA JJA MAM DJF SON Observation Model Observations from: Baeyens & Leermakers 1998, Coquery & Cossa 1995, Gardfeldt et al. 2003, Kim & Fitzgerald 1986, Laurier et al. 2003, Mason & Fitzgerald 1994, Mason et al. 1998, Wangberg et al. 2001

Ocean flux distribution & seasonality kg July ocean flux Jan. ocean flux latitude Jan. July Higher flux in tropics due to high temperature and radiation Higher flux in tropics due to high temperature and radiation High flux in regions of high deposition High flux in regions of high deposition Seasonality due to temperature, npp, radiation, and mixed layer depth Seasonality due to temperature, npp, radiation, and mixed layer depth

Effect of Ocean Flux Ocean source: 40-50% of surface Hg0 over the southern ocean 15-35% over northern continents Seasonal variability due to seasonality of ocean source Annual Hg 0 surface concentration Contribution of Ocean Source % Monthly ocean source contribution S. Pacific Europe N. America % ng/m 3 %

Summary Model captures some of the spatial and temporal variability in ocean mercury concentrations and fluxes, but misses the extreme values seen in observations Model captures some of the spatial and temporal variability in ocean mercury concentrations and fluxes, but misses the extreme values seen in observations The ocean flux shows a large seasonal cycle and spatial variability due to the variability in mixed layer depth, radiation, npp, temperature, and deposition The ocean flux shows a large seasonal cycle and spatial variability due to the variability in mixed layer depth, radiation, npp, temperature, and deposition Future work: continue comparing model seasonality to observations of atmospheric concentrations at coastal sites Future work: continue comparing model seasonality to observations of atmospheric concentrations at coastal sites

Flux Parameters & Observations Ocean Flux (ng/m 2 /h) Med. Sea N. Atl. N. Atl. Baltic Pacific JJA SON JJA MAM MAM Observations from: Baeyens & Leermakers 1998, Gardfeldt et al. 2003, Laurier et al N. Atlantic flux with controlling parameters Observation Model

Flux and mixed layer depth Jan. ocean fluxJuly ocean flux kg Jan. mixed layer depthJuly mixed layer depth m