Lecture 4 CO 2 and Long Term Climate

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Lecture 4: CO 2 and Long Term Climate Change (Ch. 3)

Lecture 4: CO 2 and Long Term Climate Change (Ch. 3)

Atmospheric CO 2 Evolution

Atmospheric CO 2 Evolution

Why Venus is hotter than Earth? Venus (460 o. C) vs. Earth (15 o.

Why Venus is hotter than Earth? Venus (460 o. C) vs. Earth (15 o. C)

Why Venus (460 o. C) is hotter than the Earth (15 o. C) ?

Why Venus (460 o. C) is hotter than the Earth (15 o. C) ? Answer 1: Venus is closer to the Sun Distance to the sun: Venus/Earth=0. 72 radiation reach Venus/Earth = (12)/(0. 722)=1. 93 But, the albedo is 80% on Venus and 26% on Earth So the solar radiation received Venus/Earth = 1. 93 x (0. 20/0. 74)=0. 52 So, Venus should be colder than the earth? ? ?

Answer 2: The CO 2 GHG effect Venus vs. Earth The same amount of

Answer 2: The CO 2 GHG effect Venus vs. Earth The same amount of total carbon All carbon in the atmosphere Most carbon in rocks

Carbon reservoirs on the earth 0. 001% 0. 025% 0. 057% 99. 9%

Carbon reservoirs on the earth 0. 001% 0. 025% 0. 057% 99. 9%

Greenhouse Effect (1 - )S Tg 4 (1 - )S glass T 4 Heat

Greenhouse Effect (1 - )S Tg 4 (1 - )S glass T 4 Heat fluxes: surface = (1 -a)S + Tg 4 - T 4 =0 Top = (1 -a)S - Tg 4 = 0 (or radiation balance for the glass layer: 2 Tg 4 = T 4 ) Tg= ((1 -a)S/ )1/4 = Tcc=255 K , Tcg =21/4 Tg=288 o. K=15 o. C About right… Major GHG on earth: H 2 O!

Atmospheric CO 2 Evolution

Atmospheric CO 2 Evolution

Last 4. 5 Byr: Why the earth is not that cold? ---The faint young

Last 4. 5 Byr: Why the earth is not that cold? ---The faint young Sun Paradox

The faint young Sun paradox Assuming the same climate sensitivity: T~(S)1/4==> T 4 by/T

The faint young Sun paradox Assuming the same climate sensitivity: T~(S)1/4==> T 4 by/T 0 by~(S 4 by/S 0 by)1/4~(0. 7)1/4~0. 915 T 4 br=0. 915*T 0 br=0. 915*288 K=263 K= -10 o. C Would be frozen, But, incompatible with the evidence of premitive life found as far back as 3. 5 Ba, In spite of the much weaker Sun (30%) in the early stage of the earth, the earth has remained inhabitable, instead of largely frozen (a snowball earth). Something keeps the earth warmer! But, this factor must not be functioning today, which otherwise would heat the present earth inhabitable? (above 25 o. C, at least) a thermostat (temperature regulator) is functioning! Was the Earth more like the Venus in the past, with more carbon in rocks?

Carbon exchange

Carbon exchange

Carbon Source: Volcanic Eruption Renewal /depletion time: Atmosphere: 600/0. 15=4000 yr Combined surface reservoir:

Carbon Source: Volcanic Eruption Renewal /depletion time: Atmosphere: 600/0. 15=4000 yr Combined surface reservoir: 3700/0. 15=24, 700 yr Including deep ocean reservoir: 41, 700/0. 15=278, 000 yr, short compared with the history of the earth Volcanic flux is sufficient to provide carbon for the atmosphere (actually the entire surface earth system: atmos+soil+ocean) at long term 0. 15 GT/yr But, volcanic eruption of CO 2 has no direct feedback and therefore alone can’t form thermostat mechanism! Some feedback that feels the climate is needed.

Carbon sink: Chemical Weathering I Hydrolysis: CO 2+H 2 O in the atmosphere removes

Carbon sink: Chemical Weathering I Hydrolysis: CO 2+H 2 O in the atmosphere removes CO 2 from the atmosphere and is incorporated into ground water to form H 2 CO 3 in soil, which attaches rocks and dissolve ions, and transported into the ocean in river, and store in the shells of marine plankton which eventually is deposited into the ocean bottom Hydrolysis : H 2 O (rain)+CO 2 (air) Ca. Si. O 3 +H 2 CO 3 Silicate rock Carbonic acid (Continent) soil Ca. CO 3 +Si. O 2 +H 2 O shells of organism

Carbon sink: Chemical Weathering II Dissolution: CO 2+H 2 O in the atmosphere removes

Carbon sink: Chemical Weathering II Dissolution: CO 2+H 2 O in the atmosphere removes CO 2 from the atmosphere and forms H 2 CO 3 which attacks limestone caves, and the dissolved ions flow to the ocean in rivers. Dissolution : H 2 O (rain)+CO 2 (air) Ca. CO 3 +H 2 CO 3 Limestone rock in soil Ca. CO 3 +H 2 O + CO 2 shells of organism return to air Different from hydrolysis Dissolution much faster but leads to no net removal of CO 2 from the atmosphere So does not contribute to the lowering of CO 2 in the long run

Chemical weathering: earth’s thermostat through a higher temperature, rainfall and vegetation higher temperature increasing

Chemical weathering: earth’s thermostat through a higher temperature, rainfall and vegetation higher temperature increasing weather rate (10 o. C double rate) higher precipitation raise ground water level in the soil increasing weather rate Increase vege photosynthesis removal CO 2 delivers into the soil where it combines with ground water to form H 2 CO 3, increasing weather rate

Chemical weathering forms the earth’s thermostat through T, P, V Chemical weathering is an

Chemical weathering forms the earth’s thermostat through T, P, V Chemical weathering is an excellent candidate for Earth’s thermostat

A negative feedback mechanism for the fainted young Sun paradox: Weaker Sun => cooler/less

A negative feedback mechanism for the fainted young Sun paradox: Weaker Sun => cooler/less P/less vege => less chemical weathering => More CO 2 left in the atmosphere => stronger greenhouse effect =>compensates the weaker Sun. Chemical weathering is an excellent candidate for Earth’s thermostat (James Walker, Paul Hays and James Kastings) In contrast to chemical weathering, water vapor feedback is a positive feedback

The Gaia Hypothesis The ultimate control of climate: Life itself has been responsible for

The Gaia Hypothesis The ultimate control of climate: Life itself has been responsible for regulating earth’s climate (J. Lovelock and L. Margulis, 1980) life is involved in the weathering process (vegetation, plankton shell…) warmer more plants/plankton takes CO 2 down cooling

Life and CO 2 Organic carbon cycle, accounts for 20% of carbon fluxes

Life and CO 2 Organic carbon cycle, accounts for 20% of carbon fluxes

Primitive system ineffective in the removal of atmospheric CO 2 Root system effective removal

Primitive system ineffective in the removal of atmospheric CO 2 Root system effective removal of atmospheric CO 2 Evolution of Life and CO 2 removal efficiency

The Debate on Gaia Hypothesis life is involved in the weathering process (vegetation, plankton

The Debate on Gaia Hypothesis life is involved in the weathering process (vegetation, plankton shell…) (warmer more plants/plankton takes CO 2 down cooling • Critics: early life too primitive to play an significant role in weathering, modern plants (root system) developed last 540 Ma marine shells develop after 540 Ma (before chemical precip in shallow tropical seas…), • Support: bacteria in early time can help reduce CO 2 too life evolution matches the earth’s need for progressively greater chemical weather through time. Later, more complex life leads to stronger weathering, reducing more CO 2.

Thermostat Malfunction: A Snowball Earth? 2 -4 times glacial deposits, at least once in

Thermostat Malfunction: A Snowball Earth? 2 -4 times glacial deposits, at least once in the tropics Chemical weathering not working: a 6% reduction of insolation, not cold enough Assuming the same climate sensitivity: T~(S)1/4==> T 8 Ma/T 0 Ma~(S 8 Ma/S 0 Ma)1/4~(0. 94)1/4~0. 985 T 8 Ma=0. 985*T 0 Ma=0. 985*288 K=283 K= 10 o. C So, a lower CO 2 is needed (according to climate models). But, with chemical weathering thermostat, cooling reduced weathering higher CO 2

Reading Material for L 4 • Hoffman P. and D. Schrag, 2002: The snowball

Reading Material for L 4 • Hoffman P. and D. Schrag, 2002: The snowball Earth hypothesis: testing the limits of global change. Terra Nova, 14, 129 -155 • Schrag, D. Berner, R. , P. Hoffman and G. Halverson, 2002: On the initiation of a snowball Earth. Geocheistry, Geophysics, Geosystems, 3, 10. 1029/2001 GC 000219

The End

The End