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October 1 Magdalena Anguelova Ph.D. Candidate Advisor: Prof. Ferris Webster College of Marine Studies.

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Presentation on theme: "October 1 Magdalena Anguelova Ph.D. Candidate Advisor: Prof. Ferris Webster College of Marine Studies."— Presentation transcript:

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2 October 1 Magdalena Anguelova Ph.D. Candidate Advisor: Prof. Ferris Webster College of Marine Studies

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4 Bubble Bath Glenn Miller

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6 Bubbles in my beer Willie Nelson

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8 Bubbles naturally formed in the ocean Marine life Breaking waves

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11 Oceanic bubbles are associated with Oxygenic atmosphere Climate on the planet

12 Oxygenic atmosphere

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15 Archaean Earth  Ancient atmosphere of:  methane;  ammonia;  other gases.  Bacterial life.

16 Earth’s biogeologic clock

17 Stromatolite fossils 760 million years old, Arizona

18 Living stromatolites Shark Bay, Australia

19 Stromatolites

20 Cyanobacteria  3 billion individuals per sq. meter;  Use sediment and organic material;  Build stromatolites up to 1.5 m high

21 The Miracle Planet PBS Series

22 The Miracle Planet PBS Series o This cycle continued for eons o Cyanobacteria photosynthesized o Releasing tiny bubbles of oxygen o The water gradually saturated with O 2 o Then O 2 escaped into the air and o Transformed the atmosphere o To air we now breath o Then ozone layer formed against UV.

23 Life conquered the land

24 Oceanic bubbles mediated oxygenic atmosphere

25 Oceanic bubbles are associated with Oxygenic atmosphere Climate on the planet

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27 Oceanic whitecaps

28  As waves break,  air mixes into the water,  and forms clouds of bubbles. Wave Breaking

29  The small bubbles dissolve and disappear; The fate of the bubbles  The large bubbles rise to the surface,  Some bubbles join the ambient population of oceanic bubbles.

30  While floating on the surface, bubbles burst. Bursting of bubbles

31  Upon bursting, bubble caps shatter into thousands of small droplets. Film drops form. Film Drops

32  As the bubble cavity collapses... Jet drops form. Jet Drops

33  Under very high winds drops are torn from the wave crests and blown directly into the air. Spume drops form. Spume Drops

34  In the air, this sea spray: sea- salt aerosols.  evaporates,  shrinks,  and forms  So, whitecaps fill the air with film, jet, and spume drops. Sea Spray

35 What are Aerosols?  Aerosols are minute stable particles, solid or liquid, suspended in the atmosphere. Clean (rural/marine) air.Polluted (urban) air.

36 Tiny Particles  Cannot be seen with the naked eye.  Seen as...

37 A sunrise over the China Sea

38  The aerosols are:  Natural:  Man-made: Soil dust; Sea salt; Volcanic dust; Organic particles. Industrial; Burning biomass; Soot;  The most numerous are: Aerosol Types

39  Aerosols can influence climate:  Directly:  Indirectly: - by reflecting incoming sunlight back to space. - by modifying the properties and lifetime of the clouds. Why are Aerosols so Important?

40  More aerosols = more cloud droplets.  Reflect more sunlight.  Net result: cooling. Cloud Properties

41  Inhibit the growth of cloud droplets.  Rain delayed.  Net result: longer cloud lifetime. Cloud Lifetime

42  Oceans produce enormous amount of sea-salt aerosols.  For one year: 1.3  10 9 kg = 683 000 cars. Sea-salt aerosols

43  Sea-salt aerosols are the major contributor to sunlight reflection.  Sea-salt aerosols facilitate the formation of drops in marine clouds. Sea-Salt Aerosols and Climate

44 Oceanic bubbles link ocean and atmosphere

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