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Global Changes in Climate
Atmospheric effect Global Changes in Climate
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Fig 9
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Redistributing Energy from the Sun
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Differential heating of Earth
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Insolation
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Temperature at Surface
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Fig. 8C.
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Evaporation minus Precipitation
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Circulation Effect on Energy Balance
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Wind-driven surface ocean circulation
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Salinity at Surface
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Density of Water Ocean is stratified
Density increases with increasing salt content Density increases with decreasing temperature Temperature and salinity are set at the surface and are “conserved” in the deep ocean The ocean’s deep waters are COLD and thus deep waters were last at the surface at high latitudes At high latitudes, cooling is important for increasing water density and sending it to the bottom The “great ocean conveyor” acts as a giant heat pump in the Northern Atlantic
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Fig. 14.6A
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Atmosphere-Ocean Organization
ENSO NAO
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Normal State of the Pacific
Fig. 18.
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El Niño State of Pacific
Fig. 19.
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Ocean Response to Atmospheric Circulation
Fig. 7. Winds cause a general westward motion of tropical surface waters Winds also cause the warmest waters to “pile up” at the western Pacific (western Pacific warm pool)
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El Niño, after Ropelewski and Halpert 1987, MWR, 1606-1626.
Regions with consistent precipitation anomalies associated with El Niño, after Ropelewski and Halpert 1987, MWR,
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NAO+ NAO-
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Natural Causes of Climate Change on Long Timescales
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Geometry of Earth’s orbital variations and tilt
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60°N summer insolation minima coincide with glaciations
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The Carbon Cycle Fig
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Plate Tectonics
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Modern distribution of continents
Pangaea ~250 Ma Modern distribution of continents
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Before uplift After uplift
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Effect of uplift on climate
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d18O d13C 10 20 30 Age (Ma) 40 50 60 70 Zachos et al., 2001
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Inferring climate change far back in time
Proxies Inferring climate change far back in time
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What would we like to know?
Temperature Rainfall Evaporation Seasons Winds Ocean currents Deep ocean overturning
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