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Marine Aerosols, Clouds and Climate

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Title: Marine Aerosols, Clouds and Climate


1
Marine Aerosols, Clouds and Climate
  • An Overview

2
Definition of Marine Aerosol?
  • Natural marine aerosol sea-salt, sulfates,
    organics
  • Advected marine aerosol soil-dust, sulfates,
    organics, black carbon, nitrates. Large amounts,
    some deposited to ocean and some transported long
    distances

From Husar et al. 1997
3
Distribution of Marine Aerosols
  • Northern Hemisphere marine environment is
    polluted, even away from major sources

From Heintzenberg et al. 2000
4
Marine Aerosols and Clouds
  • Clouds transport and transform marine aerosols,
    through chemical and physical processes
  • Marine clouds cool the surface by reflecting
    solar radiation

Modified from Hobbs 2000
5
Marine aerosols Sulfate
  • Dimethylsulfide gas from phytoplankton released
    to atmosphere produces SO2, H2SO4 eventually
    sulfate aerosol
  • New sulfate aerosol can act as cloud condensation
    nuclei, or CCN
  • Clouds w/ more drops reflect more light, cool
    surface--feedback??

CLAW hypothesis, courtesy M. Walkington
6
Marine aerosols Sulfate
  • New data suggests sea-salt or clouds scavenge
    much of the SO2 produced from DMS. Then converted
    to SO42- (internally mixed). Cloud drop N less
    affected. 
  • In regions w/ low sea-salt and clouds, new H2SO4
    particles can form (then partially neutralized)
  • A significant source of new particles is actually
    free troposphere near convection, where low
    particle surface area and cold temperatures favor
    new particle formation
  • New particles grow and are entrained into
    boundary layer, where they can act as new CCN

H2SO4
From Clement et al. 2001
7
New Particle Production in RICO
8
Marine Aerosols Sulfate
  • Limited S isotopic measurements of aerosol
    indicate less than 35 of S in No Hem is biogenic

From Heintzenberg et al. 2000
9
Marine aerosols Sea-salt
  • Sea-salt in various sizes produced by bubbles
    breaking waves
  • Hygroscopic, liquid at high humidity and can
    dominate light scattering in remote areas (direct
    effect)

From O'Dowd et al. 1997
10
Marine aerosols Sea-salt
  • Submicron sea-salt important in increasing
    number of droplets
  • Large and "giant" sea salt low in conc. but
    important in forming large cloud drops, which
    deplete water through drizzle

11
Sea-salt Effects of Giant Nuclei
  • Giant sea-salt particles produced by high wind
    speeds are predicted to dramatically increase
    rain rate

From Jensen, 2004
Anthropogenic giant nuclei?
12
Marine aerosols Sea-salt/Sulfate
  • SO2 is taken up by sea-salt aerosol and by cloud
    drops formed on sea-salt and is converted to
    sulfate ("non-sea-salt sulfate"). "Internally
    mixed" aerosol is mix of sea-salt and NSS-sulfate.
  • Smaller sea-salt particles have higher
    surface/volume ratio and so react more quickly w/
    avail. SO2
  • This reactivity is important for clouds and
    climate

.04 ?m
5 ?m
13
Marine aerosols Sea-salt/Sulfate
  • Internal mixing of sea-salt sulfate is
    important because it reduces the number of
    potential new aerosol particles, which reduces
    cloud drop number

From O'Dowd et al. 1999
14
Marine aerosols Organics
  • Large amount of aerosol mass may be organic, esp.
    in So Hem.
  • Wide open research area, speciation and
    cloud-forming abilities virtually unknown
  • Truth or fiction? Organic coatings on sea-salt
    or sulfate CCN may slow droplet growth and reduce
    cloud-forming ability

15
Marine Aerosols Organics
  • Some natural organics, by also produced by
    industry, biomass, transported long distances
  • Organics mix w/ sulfate in polluted regions

Courtesy Jim Anderson, ASU
16
Organics and Clouds
  • EELS reveals that some nuclei primarily C, with
    smaller amounts of N and S
  • Cloud droplets downwind of India evaporated and
    their nuclei analyzed by electron microscopy
  • At least some organic aerosols are good cloud
    nuclei, challenge is determining which ones and
    incorporating into models

17
Marine Aerosols Dust "The dust falls in such
quantities as to dirty everything on board, and
to hurt people's eyes vessels even have run on
shore owing to the obscurity of the atmosphere".
--Darwin, 1823
From Heintzenberg et al. 2000
18
Marine Aerosols Dust
  • Nutrients in soil dust (Fe, Mn) important for
    growth of ocean microorganisms
  • Pathogens may affect coral reefs
  • aspergillosis on sea fan
  • Dust transported long distances over oceans.
    African dust reaches Caribbean even US East
    Coast

19
Marine Aerosols Dust
  • Soil dust may act as a CCN (if coated w/ soluble
    substances) or an ice nucleus
  • Possible influence on tropical cloud systems?

From Dunion et al. 2004
20
Marine Aerosols, Clouds Climatefirst indirect
aerosol (Twomey) effect
  • Marine clouds naturally have low droplet number,
    large droplet size, drizzle a lot
  • Advected marine aerosols perturb this state
  • Aerosols act as CCN
  • more CCN --gt more, smaller droplets
  • Smaller drops reflect more sunlight (increase
    cloud reflectance or albedo), cool earth. Assumes
    constant liquid water path
  • One of largest uncertainties in prediction of
    global climate change

21
Marine Aerosols, Clouds ClimateIs indirect
effect valid for marine stratus?DYCOMS-II expt,
NE Pacific
22
DYCOMS-II Expt., NE Pacific
23
DYCOMS-II Expt., NE Pacific
  • Polluted clouds have smaller, more numerous
    drops, but are they more reflective?
  • Variations in liquid water path obscure cloud
    brightening effect of increased aerosol (Cotton
    seminar)

24
Summary
  • Ocean important source of sea-salt, sulfate
    aerosol, but advected aerosols dominate over much
    of Northern Hemisphere oceans
  • Atm. chemistry, ocean productivity and cloud
    properties are perturbed by these advected
    aerosols
  • Interactions between these aerosol types
    important
  • Increased aerosol DOES affect marine cloud
    properties (increase number, decrease size of
    drops). However, liquid water path differences
    may act to partially offset cooling effect on
    climate.

25
Areas Needing Research
  • Organic aerosols source (natural vs.
    anthropogenic), speciation, water solubility,
    mixing state, new particle formation
  • Sea-salt size distribution, mixing state w/
    sulfate and/or organics, giant nuclei N conc.
  • Sulfates source (isotopic measurements), mixing
    state w/ sea-salt, organics
  • Dust impact on cloud formation, amount deposited
    to oceans, role of different nutrients and impact
    on ocean productivity
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