1. Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere 4.7 billion years ago:  The proto-Earth was a loosely-packed ball of “dirt” (primarily silicon, iron, nickel and their oxides), surrounded by a thin primordial atmosphere of hydrogen and helium (with traces of argon, neon and krypton). 4.7 billion years ago – 4.3 billion years ago:  The planet settled over 400 million years into a densely packed ball, with a molten core (due to pressure and high levels of radioactivity.  Most of the hydrogen and helium either “escaped” by absorption of solar radiation or was blown away by the “solar wind”.  The atmosphere grew even thinner, consisting solely of trace amounts of hydrogen, helium, argon, neon and krypton.

2. Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere 4.3 billion years ago – 4.0 billion years ago:  Through fissures in the Earth’s crust, “volcanic outgassing” spewed vast amounts of hydrogen (H 2 ), nitrogen (N 2 ), water (H 2 O), carbon monoxide (CO), carbon dioxide (CO 2 ), ammonia (NH 3 ) and methane (CH 4 ) into the atmosphere.  Most of the H 2 O vapor condensed to form the oceans.  As a result of three key processes (outlined on the next slide), the air ended up consisting primarily of N 2, CO 2 and CH 4, with traces of H 2, He, Ar, Ne, Kr, H 2 O, CO and NH 3.  There was still no oxygen gas (O 2 )!  Moreover, since CO 2 and CH 4 are “greenhouse” gases, the climate grew much warmer, thereby preventing freezing and accelerating surface “weathering”. Except for Oxygen, almost all of the Earth’s atmosphere today actually comes from the planet’s interior!

3. Process “Equation” Process “Equation” Disassociation of NH 3 2NH 3 + uv  N 2 + 3H 2 Conversion of some H 2 O and most CO H 2 O + CO + sunlight  H 2 + CO 2 (As most H 2 O condensed to create the oceans, rain, erosion and tides began “weathering” the Earth’s surface.) (As most H 2 O condensed to create the oceans, rain, erosion and tides began “weathering” the Earth’s surface.) Carbonate rock formationCaO + CO 2  CaCO 3 (limestone) (CO 2 absorption)MgO + CO 2  MgCO 3 (dolomite) Summary: most H 2 escaped; N 2 kept accumulating (since it didn’t react with anything else); most H 2 O was condensed or converted; most CO was converted; CO 2 accumulated, though a lot was absorbed in “weathering”; most NH 3 disassociated; and CH 4 accumulated (since it didn’t react with anything else at this point). Summary: most H 2 escaped; N 2 kept accumulating (since it didn’t react with anything else); most H 2 O was condensed or converted; most CO was converted; CO 2 accumulated, though a lot was absorbed in “weathering”; most NH 3 disassociated; and CH 4 accumulated (since it didn’t react with anything else at this point). Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere

4. 4.0 billion years ago – 3.8 billion years ago:  Volcanic outgassing slowed dramatically while carbonate rock formation increased, thereby lowering CO 2 levels somewhat.  N 2 and CH 4 continued to accumulate.  The Earth’s surface was still completely unsuitable for supporting life, due to the atmosphere’s high methane content and excessive levels of solar ultraviolet radiation.  However, a combination of solar ultraviolet radiation, lightning, radioactivity and meteorite bombardment of the surface created complex organic molecules (proteins, amino acids, maybe even DNA).  Ultimately, this led to the appearance ☻ of primitive one-celled aquatic organisms which could survive in the oceans. Life on Earth had begun, despite its inhospitable atmosphere! Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere

5. 3.8 billion years ago – 2.5 billion years ago:  Some of the one-celled organisms in the oceans developed the ability to conduct “photosynthesis”: Process “Equation” Process “Equation” Photosynthesis 6H 2 O + 6CO 2 + sunlight  C 6 H 12 O 6 + 6O 2 (This provided food, in the form of glucose, to these primitive aquatic plants, and very importantly, began the release of oxygen into the atmosphere!) Photosynthesis 6H 2 O + 6CO 2 + sunlight  C 6 H 12 O 6 + 6O 2 (This provided food, in the form of glucose, to these primitive aquatic plants, and very importantly, began the release of oxygen into the atmosphere!)  By 2.5 billion years ago, atmospheric oxygen accumulated to a level of about 1% (by volume). Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere

6. 2.5 billion years ago – 600 million years ago:  Slowly but steadily, the evolutionary process and photosynthesis continued.  Multi-celled organisms appeared, and some of these evolved into soft-bodied worm-like animals with a variety of organs, and still later into the first hard-shelled creatures capable of leaving fossils.  Oxygen continued to accumulate in the atmosphere, reaching about 10% by volume.  Life above the water was still not possible, due to strong solar ultraviolet radiation and high levels of methane. Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere

7. 600 million years ago – 3 million years ago:  Volcanic outgassing slowed to a relative trickle, but two more key processes (outlined on the next slide) completely altered the atmosphere, enabling plants and animals to leave the oceans, and survive and evolve on land.  Between 450 million years ago and 350 million years ago, land plants and amphibian animals began to appear, and oxygen levels approached today’s value of nearly 21% by volume.  By the end of this period, the atmosphere contained much less CO 2 than before (280 ppm) and very little CH 4 (800 ppb), and the critically important protective ozone layer was in place.  Plants and animals flourished in continuing diversity, despite occasional mass extinction events. Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere

8. Process “Equation” Process “Equation” Conversion of most CH 4 2CH 4 + 3O 2  4H 2 O + 2CO (This eliminated most of the atmospheric methane, which would have been toxic to surface-dwelling animals.) Ozone production 3O 2 + uv  2O 3 (This created the “ozone layer” high in the atmosphere, which blocked solar uv from reaching the ground and made it possible for plants and animals to survive above the ocean surface.) Ozone production 3O 2 + uv  2O 3 (This created the “ozone layer” high in the atmosphere, which blocked solar uv from reaching the ground and made it possible for plants and animals to survive above the ocean surface.) Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere

9. 3.0 million years ago - 200 years ago:  The first hominids (human-like creatures) appeared roughly 3 million years ago.  Over time, humankind emerged ☻ as the dominant species and a number of “advanced” civilizations developed (and, in some cases, disappeared).  Agriculture and the domestication of animals for human consumption, as well as metallurgy, became well established practices.  By 200 years ago, the industrial age, with its demand for fossil fuels, was getting underway.  The impact of people on the atmosphere was about to become noticeable! Evolution of the Earth and its Atmosphere Evolution of the Earth and its Atmosphere

10. The Earth and its Atmosphere Today Planetary Composition SectionComponents% by WtTotal % CrustSiO 2 & misc other 1 1 MantleSiO 2 30 MgO20 FeO 6 Fe 2 O 3 6 Al 2 O 3 2 CaO 2 66 CoreFe 24 Ni 4 Si 432 99

11. The Earth and its Atmosphere Today Atmospheric Composition (excluding H 2 O) GasFormula% by Volume NitrogenN 2 78.08 OxygenO 2 20.95 ArgonAr.93 Carbon DioxideCO 2.035 Carbon DioxideCO 2.035 Hydrogen, Helium, H 2, He Neon, Krypton, Ne, Kr Carbon Monoxide, CO Ammonia, NH 3.005 Sulphur Dioxide,SO 2 Methane, Ozone CH 4, O 3 Nitrous Oxide, N 2 O CFC’s, etc _______ Hydrogen, Helium, H 2, He Neon, Krypton, Ne, Kr Carbon Monoxide, CO Ammonia, NH 3.005 Sulphur Dioxide,SO 2 Methane, Ozone CH 4, O 3 Nitrous Oxide, N 2 O CFC’s, etc _______ 100.000 100.000 Gases in green are “greenhouse” gases!

12. The Earth and its Atmosphere Today Atmospheric Distribution Above 40 km, the stratosphere continues to about 50 km (where the temperature rises to 0  C).Above 40 km, the stratosphere continues to about 50 km (where the temperature rises to 0  C). The mesosphere extends from 50 km to 80 km (where the temperature drops to -90  C).The mesosphere extends from 50 km to 80 km (where the temperature drops to -90  C). The thermosphere extends from 80 km to 160 km with the ionosphere above that, but the “air” is so “thin” as to be virtually nonexistent.The thermosphere extends from 80 km to 160 km with the ionosphere above that, but the “air” is so “thin” as to be virtually nonexistent.

13. Danger in the Air Carbon Dioxide (CO 2 )  After decreasing quite steadily for billions of years, carbon dioxide levels have grown by 25%, from 280 ppm to 350 ppm, in the last 200 years; moreover this increase is accelerating.  While some of this increase may be natural (e.g. forest fires started by lightning), most of it may be traced directly to human activity, with deforestation for any purpose and fossil fuel burning being the two primary causes.  Since CO 2 is the most abundant greenhouse gas, its increase is contributing significantly to global warming.  In fact, the 8 warmest years on record have occurred in the past 12 years.

14. Danger in the Air Methane (CH 4 )  Once very abundant, methane levels dropped dramatically for almost 2 billions years, but in the last 200 years have essentially doubled, from about 800 ppb to roughly 1600 ppb.  Most of this increase is a direct result of human activity, including agriculture (e.g. rice paddies, livestock), sewage treatment, landfill development and wood burning.  CH 4 is another greenhouse gas, whose increase thus contributes to global warming.  Specifically, though much less abundant than carbon dioxide, each molecule of CH 4 can absorb 25 times more heat than a molecule of CO 2.

15. Danger in the Air Ozone (O 3 )  Ozone is both “good” and “bad”; the “good” ozone found in the stratospheric ozone layer protects all life on Earth by blocking dangerous solar ultraviolet radiation.  Unfortunately, the ozone layer is being threatened by our development and use of CFCs (as discussed in the next slide).  On the other hand, low altitude ozone is a “bad” thing.  While also occurring naturally as a byproduct of lightning, the increase in low altitude ozone is primarily due to the burning of fossil fuels, a human activity.  Low level ozone is not only a greenhouse gas, whose increase contributes to global warming, but also a key constituent of urban smog.

16. Danger in the Air Chlorofluorocarbons (CFCs)  Chlorofluorocarbons are a class of synthetic compounds which are—or were, before being banned—used in a variety of industrial applications: refrigerants, aerosol propellants, frothing compounds, solvents and fire extinguishers.  Almost unheard of in the 1950’s, CFC concentrations have more than quadrupled from.8 ppb to 3.5 ppb in the last 40 years, largely because they can take decades to break down once released into the air.  At low altitudes, they act as “greenhouse” gases and contribute to global warming.  At high altitudes, CFCs break down, releasing chlorine gas which is responsible for the thinning of the ozone layer, through the so-called “chlorine cycle”: Cl 2 + 2O 3  2ClO + 2O 2 and2ClO + O 2  Cl 2 +2O 2

17. Danger in the Air Nitrous Oxide (N 2 O)  In the last 200 years, nitrous oxide concentrations in the atmosphere have increased by 10%, from about 280 ppb to about 310 ppb.  This growth is a product of both fossil fuel combustion and the increasingly widespread use of nitrogen-based chemical fertilizers for lawns, gardens and agriculture.  The increase, while small, is significant, since a molecule of N 2 O can absorb 320 times more heat than a molecule of CO 2, making it a substantial contributor to global warming.  Moreover, N 2 O can further exacerbate global warming through deforestation resulting from acid rain.  Finally, as a pollutant, N 2 O contributes to urban smog.

18. Danger in the Air Sulphur Dioxide (SO 2 )  Sulphur dioxide is a byproduct of the burning of wood or fossil fuels.  While not a greenhouse gas, it can nevertheless contribute indirectly to global warming through deforestation brought about by acid rain: H 2 O + SO 2  H 2 SO 3 (sulphurous acid)  Also, as a pollutant, SO 2 contributes to urban smog.