Changing Oceans

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38 Terms

1
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Heat balance

Heat absorbed by the Earth re-emitted as longwave radiation

2
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What are other long-wave radiation absorbed by?

-Co2

-Water vapour

-Nitrous oxides

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Insolation+

Radiation reaching surface

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Albedo=

Some of insolation is reflected by the surface

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Examples of high and low albedo?

High albedo=Snow

Low albedo=Soil

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What type of radiation is reflected back off to the atmosphere?

Infrared & longer wavelengths

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What 2 things strongly absorb infrared?

H2o vapour & CO2

8
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What caused CO2 levels to increase?

Industrial revolution

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What has accelerated CO2 levels recently?

-Greater industry activity (burning fossil fuels)

-Deforestation & land clearance

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Recent atmospheric CO2 changes?

From 1959 to 2011 there was increase of 24% atmospheric CO2

-Mauna Loa Observatory, Hawaii

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What is harder to measure CO” or global temperature?

Global temperature

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What is the effect of CO2 on the climate?

Mean global surface temperature increased by 0.74oC

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Direct Observations of recent Climate Change

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What is past climate characterised by?

High frequency and high amplitude cycles

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Past Climate features?

-High-mid latitudes: Glacial & Interglacial

-Lower latitude:Interpluvials & Pluvials

-Major changes in sea level

-Many cycles between warm & cold periods

-Milankovitch (1920): 3 astronomical

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Axial tilt

-Tilt of earths spin

-~21.5o to ~24.5o and back every 42k years

-More intense seasons in both hemispheres

<p>-Tilt of earths spin</p><p>-~21.5<span><sup>o </sup>to ~24.5</span><sup>o</sup><span> and back every 42k years</span></p><p><span>-More intense seasons in both hemispheres</span></p>
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Eccentricity of the Orbit

-Orbit circular, elliptical & back ~100k

-Weaker effects on seasonality than axial tilt

-Intensifies seasons in one hemisphere

-Moderates seasons in the other hemisphere

<p>-Orbit circular, elliptical &amp; back ~100k</p><p>-Weaker effects on seasonality than axial tilt</p><p>-Intensifies seasons in one hemisphere</p><p>-Moderates seasons in the other hemisphere</p>
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Precession of the Equinoxes

-Wobble of spin axis

-Interplay between the 1st two factors

<p>-Wobble of spin axis</p><p>-Interplay between the 1st two factors</p>
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What did the 3 factors that Milankovitch calculated control?

Sunshine reaching high North latitudes (20%)

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What is the problem with Milankovitch 3 factors?

No independent record of ice age timing

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What does the ratio of oxygen isotopes (¹⁸O/¹⁶O) in seawater indicate?

The ratio reflects ice volume changes on land

-During glacial periods, oceans become enriched in ¹⁸O as ice caps store snowfall depleted in ¹⁸O.

-Marine organisms, like foraminifera, incorporate this isotope ratio into their shells, which become sediment records of past climate.

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What did the records of ¹⁸O/¹⁶O from forams in deeps-sea cores:

Ratio fell & rose in accordance with Milankovitch cycles

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Ice volume every 100Ky:

Eccen of orbit

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Other 2 cycles (23Ky &m41 Ky):

Wrinkles

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What did analysed Co2 in ice core bubbles from Antarctica & Greenland?

-Very good correlation between CO2 & temperatures

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What can oceans regulate?

Atmospheric CO2

-Ocean can act as large CO2 sink & hold 50-60 times more CO2 than the atmosphere

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Thermohaline Conveyor features

-Begins in North Atlantic

-At latitude of Iceland water cools 10-2oC

-Gives off huge amount of heat

-Mild winters:North West Europe

-NaDW floods deep Atlantic, distributes around other oceans

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How much has CO2 has risen from the past 200 years?

150 ppm

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When was the last glaciation comparable rise?

5000 years

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Evidence atmospheric CO2 rising accelerates global warming

-Past 5 decades: increased freshening of Nordic seas

-Slowed NADW formation

-Overflowed decreased 20% since 1950

-Accelerated melting of Greenland ice sheet

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What is the percentage that models predict will happen with the Atlantic Thermohaline Circulation?

45% will collapse by 2100

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What are the amplifying factors in quaternary CO2 variations?

-Ocean Circulation

-Albedo feedback

-Atmospheric CO2

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Evidence of the oceans effectively pumping CO2 more efficiently during glacial periods:

-Enhanced PP & export during glacials

-More nutrients in surface mixed layer during glacials

-Increased aeolian Fe inputs

-Fe fertilised HNLC regions

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Does all anthropogenic CO2 remain in the atmosphere?

No

-past 100 years:~30% anthropogenic CO2 taken up by oceans

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Why does not all anthropogenic CO2 get absorbed?

-Increased atmospheric pCo2

-Increased PP & organic sedimentation

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