Oceanic Biogenic Volatile Organic Compounds (BVOCs): formation processes and ocean- atmosphere exchange Hang Qu Ruixiong Zhang April 16 2014.

Slides:



Advertisements
Similar presentations
DOGEE-SOLAS: The UK SOLAS Deep Ocean Gas Exchange Experiment Matt Salter.
Advertisements

Atmospheric inversion of CO 2 sources and sinks Northern Hemisphere sink Jay S. Gregg.
Emissions From The Oceans To The Atmosphere Deposition From The Atmosphere To The Oceans And The Interactions Between Them Tim Jickells Laboratory for.
Simulating the Impacts of Marine Organic Emissions on Global Atmospheric Chemistry and Climate using an Online-Coupled Meteorology and Chemistry Model.
Marine Ecosystems and Interdecadal climate variations Vidyunmala V. Ph.D Student, CAOS.
1 Biogenic Hydrocarbons Lecture AOSC 637 Atmospheric Chemistry Russell R. Dickerson Finlayson-Pitts Chapt. 6 & 9 Seinfeld Chapt. 6 OUTLINE History Nomenclature.
NOAA COARE Gas Transfer parameterization: Update Using Wave Parameters C. W. Fairall* NOAA Earth Science Research Laboratory, Boulder, CO, USA Ludovic.
Development of a Secondary Organic Aerosol Formation Mechanism: Comparison with Smog Chamber Experiments and Atmospheric Measurements Luis Olcese, Joyce.
Oxygen triple isotope composition for estimating photosynthesis rates Nir Krakauer June, 2006.
Effect of Variable Flux Footprint on Measurement of Air/Sea DMS Transfer Velocity A Southern Ocean Case Study Thomas Bell Presented by Mingxi Yang with.
Update on: 1. Secondary Organic Aerosol 2. Biogenic VOC emissions Colette L. Heald Chemistry Climate Working Group Meeting February.
Discussion Space Research Centre. Urbanization and Industrialization: in 2008, more than half of humans live in cities UN Population Report 2007.
THE ATMOSPHERE: OXIDIZING MEDIUM IN GLOBAL BIOGEOCHEMICAL CYCLES
The Contribution of Marine Organic Emissions to Coastal Air Quality Brett Gantt Advisor: Nicholas Meskhidze Co-Author: Annmarie Carlton (EPA) North Carolina.
SETTING THE STAGE FOR: BIOSPHERE, CHEMISTRY, CLIMATE INTERACTIONS.
METO 637 Lesson 16.
Air-Sea Exchange : 2 SOEE3410 : Lecture 5 Ian Brooks.
Evaluating the Role of the CO 2 Source from CO Oxidation P. Suntharalingam Harvard University TRANSCOM Meeting, Tsukuba June 14-18, 2004 Collaborators.
Havala Olson Taylor Pye April 11, 2007 Seinfeld Group Department of Chemical Engineering California Institute of Technology The Effect of Climate Change.
Ocean Water Chemistry. Figure 4.17a
Emissions of Volatile Organic Compounds by Plants Carbon Metabolism and Atmospheric Chemistry Kolby Jardine Amazon-PIRE Field Course June 2010.
GEOF236 CHEMICAL OCEANOGRAPHY (HØST 2012) Christoph Heinze University of Bergen, Geophysical Institute and Bjerknes Centre for Climate Research Prof. in.
The Air-Sea Gas Transfer Velocity - Approaching it from Multiple Angles Mingxi Yang, T. Bell, P. Nightingale, J. Shutler (Additional contributions from.
Estimates of global biogenic isoprene emissions from the terrestrial biosphere with varying levels of CO 2 David J. Wilton 1,2*, Kirsti Ashworth 2, Juliette.
Biosphere Atmosphere Exchange 1) Directly emitted GHGs CO 2, CH 4, N 2 O 2) Chemical sources of GHGs and SOA BVOCs  CO  CO 2 BVOC  aerosol 3) Effects.
Surface-Atmosphere Fluxes Part II Christine Wiedinmyer
Implications of observed surprisingly high atmospheric oxidizing capacity over tropical forest: the GABRIEL Campaign Laurens Ganzeveld 1,2, Tim Butler.
School of something FACULTY OF OTHER 1 Lecture 2: Aerosol sources and sinks Ken Carslaw.
The Other Carbon Dioxide Problem Ocean acidification is the term given to the chemical changes in the ocean as a result of carbon dioxide emissions.
Gas transfer coefficient : K = F / (pCO 2 ice - pCO 2 air ) = 2,5 mol m -2 d -1 atm -1 The study of air-ice CO 2 exchange emphasize the importance of gas.
Mapping isoprene emissions from space Dylan Millet with
The Diurnal Cycle of Salinity Kyla Drushka 1, Sarah Gille 2, Janet Sprintall 2 1. Applied Physics Lab, Univ. of Washington 2. Scripps.
Radiation Group 3: Manabe and Wetherald (1975) and Trenberth and Fasullo (2009) – What is the energy balance of the climate system? How is it altered by.
Air-side flux measurements UCI API CIMS (Proton transfer atmospheric pressure ionization) DMS, acetone (10 Hz) Sensitivity ~100 Hz/ppt DMS Currently being.
CHEMICAL CHARACTERISTICS OF NORTH AMERICAN OUTFLOW: INSIGHTS FROM CHEBOGUE POINT, NOVA SCOTIA Allen Goldstein, Dylan Millet, James Allan, Eben Cross, Rupert.
TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY Troposphere Stratosphere: 90% of total The many faces of atmospheric ozone: In stratosphere: UV shield In middle/upper.
Air / Water Gas Exchange The distribution of a chemical across the air-water interface between the atmospheric gas phase and the water dissolved phase.
TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY Troposphere Stratosphere: 90% of total The many faces of atmospheric ozone: In stratosphere: UV shield In middle/upper.
Where do these two models leave us? F = K ol * ( C w – C a / H) Whitman two film model un-measurable parameters: z w & z a Surface renewal model un-measurable.
The Surface Ocean - Lower Atmosphere Study Rob Upstill-Goddard University of Newcastle upon Tyne.
The GEOS-CHEM Simulation of Trace Gases over China Li ZHANG and Hong LIAO Institute of Atmospheric Physics Chinese Academy of Sciences April 24, 2008.
2006 OCRT Meeting, Providence Assessment of River Margin Air-Sea CO 2 Fluxes Steven E. Lohrenz, Wei-Jun Cai, Xiaogang Chen, Merritt Tuel, and Feizhou Chen.
Investigation of Mixed Layer Depth in the Southern Ocean by using a 1-D mixed layer model Chin-Ying Chien & Kevin Speer Geophysical Fluid Dynamics Institute,
Oxidant chemistry in the tropical troposphere: role of oxygenated VOCs and halogens, and implications for mercury Daniel J. Jacob with Kevin J. Wecht,
Status of MOZART-2 Larry W. Horowitz GFDL/NOAA MOZART Workshop November 29, 2001.
Dylan Millet Harvard University with D. Jacob (Harvard), D. Blake (UCI), T. Custer and J. Williams (MPI), J. de Gouw, C. Warneke, and J. Holloway (NOAA),
Global high-resolution marine isoprene emission derived from VIIRS-SNPP and MODIS-Aqua ocean color observations 1/25/2016Air Resources Laboratory1 Daniel.
Cooling - indirect light scattering by clouds CCN phytoplankton DMS sulphate aerosols dust particles cooling - direct light scattering by aerosols + iron.
Top Down Emission Analyses Theme 17 th GEIA Conference Nov. 19, 2015 Alex Guenther Department of Earth System Science University of California, Irvine.
AN ATMOSPHERIC CHEMIST’S VIEW OF THE WORLD FiresLand biosphere Human activity Lightning Ocean physics chemistry biology.
Spatial and temporal dynamics of atmospheric pollutants in London, UK. Carole Helfter, Eiko Nemitz, Chiara Di Marco, Ben Langford, Neil Mullinger, Ute.
Sensitivity of Biogenic Emissions to Climate Jihee Song Global Physical Climatology December 5, 2006.
Marine biogenic emissions, sulfate formation, and climate: Constraints from oxygen isotopes Becky Alexander Harvard University Department of Earth and.
Ally Lewis, University of York, U.K Data from Katie Read, Jim Hopkins, Jacqui Hamilton. NMHCs, & DMS measurements by GC-FID Remote automated NMHC, - simple.
Ten Year average of SeaWIFS ocean color data ( ) (NASA/MODIS ocean color NORTHEAST PACIFIC CARBON PROGRAM Investigating.
CVEN 5424 Environmental Organic Chemistry Lecture 8 – Henry’s Law Constant and Air-Water Exchange Kinetics.
Analysing and Modelling CO 2 fluxes across the air-sea boundary Anthony Bloom Project Supervisors: Ian Brooks, Conny Schwierz.
Measurement and modelling of reactive trace gas fluxes from the Amazonian rainforest (CLAIRE-UK) Amy Valach Supervised by Prof. Nick Hewitt et al. Lancaster.
Diurnal Variations in Near-Surface Salinity Kyla Drushka 1, Sarah Gille 2, Janet Sprintall 2 1. Applied Physics Lab, Univ. of Washington.
Precipitation Effects on Turbulence and Salinity Dilution in the Near Surface Ocean Christopher J. Zappa Lamont-Doherty Earth Observatory, Columbia University,
Ozone Budget From: Jacob. Ozone in the Atmosphere Lifetime: –~1 month –Highly variable – dependent on season, latitude, altitude, etc. Background concentrations:
3.3 Gas exchange Turbulent vertical motions in both the atmosphere and ocean are strongly suppressed near the air-sea interface.  STAGNANT FILM MODEL.
Ashok Luhar, Matthew Woodhouse, Ian Galbally 5 September 2017
Interactive C-cycle in Earth System models
Top-down constraints on emissions of biogenic trace gases from North America Dylan Millet with D.J. Jacob, R.C. Hudman, S. Turquety, C. Holmes (Harvard)
Organic Aerosol is Ubiquitous in the Atmosphere
Global Warming Problem
Aerosol Optical Thickness
Ocean Water Chemistry.
On-going developments of SinG: particles
Presentation transcript:

Oceanic Biogenic Volatile Organic Compounds (BVOCs): formation processes and ocean- atmosphere exchange Hang Qu Ruixiong Zhang April

Outline Introduction OVOCs formation processes Ocean-atmosphere exchange

What is inside the oceans? Antioxidant/metabolite/...

Dimethyl sulfide (DMS) Nitrogen-containing gases:N 2 O, ammonia and amines Carbon Monoxide VOCs Methane Non-methane VOCs (NMVOCs) Terpenes: Isoprene, monoterpene Halocarbons: CHBr 3, CHBr 2, CHCl 3, CH 3 Cl... Oxygenated VOCs (OVOCs) Methanol, ethanol, propanol Acetaldehyde Acetone What does the ocean emit? Aerosol GHG, aerosol Atmospheric chemistry GHG SOA precursors Atmospheric chemistry SOA precursors

OH O2O2 O2O2 CH 3 OHCH 3 O CH 2 OHHCHO Chemical depletion of OVOCs CH 3 CHO hνhν CH 4 +CO CH 3 +HCO OH CH 2 CHOCH 3 CO O2O2 CH 3 C(O)O 2 HC(O)CHO O2O2 HCHO+CO CH 2 O 2 CHO CH 2 CO O2O2 CH 3 O 2 O2O2 CO 5% 95% 10% 90% M Almost 100% CH 3 C(O)CH 3 hνhν CH 3 +CH 3 CO OH CH 3 C(O)CH 2 O2O2 CH 3 C(O)CH 2 O 2 23% 40%

Ocean-atmosphere exchange: two-file resistance model CwCw CgCg Total mass transfer coefficient (Liss and Slater et al., 1974)

Water-side transfer velocity, k w Disturbing molecular diffusion layer will increase sea-atmosphere transfer IMPORTANT when wind is weak coolercooler Evaporation (cooling effect)

Water-side transfer velocity, k w White capping bubbles breaking waves would bring: 1.transfer of gases through bubble wall 2.increase instability IMPORTANT for less soluble gases when wind is strong (Wanninkhof et al., 2009)

Air-side transfer velocity, k a Lack of measurement/ validation Large uncertainty (especially for soluble gases) (Johnson et al., 2010)

NOAA COARE gas transfer algorithm (Johnson et al., 2010; Fairall et al., 2011) (molecular turbulence)

Spatial Distribution Beale et al. (2013)

LatitudeMethanolAcetaldehydeAcetone 30N to 50N N to 30N S to 10N S to 10S12157 Light DepthMethanolAcetaldehydeAcetone 97%(5m) %(10-30m) %(20-60m) %(50-150m) %(200m)< <0.3-7 Oligotrophic Northern Atlantic Gyre Decrease with light strength Increase with light strength

Concentrations of OVOCs following a phytoplankton bloom V. Sinha et al. (2007)

Air-Sea Fluxes of OVOCs Tg/yr MethanolAcetaldehydeAcetone Sea Glob. 206 (Jacob, 2005) 213 (Millet, 2010) 82 (Fischer 2012) Perc.4.4%17.1%2.4%

Thank you!

Reference Liss, P. S. and Slater, P. G.: Flux of Gases across the Air-Sea Interface, Nature, 247, 181–184, doi: /247181a0, , 268, 284 Carpenter, L. J., Archer, S. D., and Beale, R.: Ocean-atmosphere trace gas exchange, Chemical Society Reviews, 41, , /c2cs35121h, Wanninkhof, R., Asher, W. E., Ho, D. T., Sweeney, C. S., and McGillis, W. R.: Advances in quantifying air-sea gas exchange and environmental forcing, Ann. Rev. Mar. Sci., 1, 213–244, doi: /annurev.marine , Fairall, C. W., Yang, M., Bariteau, L., Edson, J. B., Helmig, D., McGillis, W., Pezoa, S., Hare, J. E., Huebert, B., and Blomquist, B.: Implementation of the Coupled Ocean-Atmosphere Response Experiment flux algorithm with CO2, dimethyl sulfide, and O3, Journal of Geophysical Research: Oceans, 116, C00F09, /2010JC006884, Johnson, M. T.: A numerical scheme to calculate temperature and salinity dependent air-water transfer velocities for any gas, Ocean Sci., 6, 913–932, doi: /os , 2010.

Reference V. Sinha et al., Air-sea fluxes of methanol, acetone, acetaldehyde, isoprene and DMS from a Norwegian fjord following a phytoplankton bloom in a mesocosm experiment, Atmos. Chem. Phys., 7, , D. B. Millet et al., Clobla atmospheric budget of acetaldehyde: 2-D model analysis and constraints from in-situ and satellite observations, Atmos. Chem. Phys., 10, , 2010 L. J. Carpenter et al., Ocean-atmosphere trace gas exchange, Chem. Soc. Rev., 41, , 2012 E. V. Fischer et al., The role of the ocean in the global atmospheric budget of acetone, Geophys. Res. Lett., 39, L01807, 2012 J. L. Dixon et al., Production of methanol, acetaldehyde, and acetone in the Atlantic Ocean, Geophys. Res. Lett., 40, , 2013 D. J. Jacob et al., Global budget of methanol: Constraints from atmospheric observations, J. Geophys. Res., 110, D08303, 2005 R. Beale et al., Methanol, acetaldehyde, and acetone in the surface waters of the Atlantic Ocean, J. Geophys. Res., 118, , 2013