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Ice Cores Very important paleoclimatic archives. Records of past atmospheric conditions. –Temperature –Humidity –Snow accumulation –Atmospheric composition –Volcanic activity –Tropospheric turbidity –Wind speed, wind direction –Atmospheric circulation
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Ice Core drilling
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Stable Isotopes-Concepts Name SymbolDefinition Atomic numberZ# protons (p + ) Neutron numberN# neutrons (n) Mass numberA# p + + n
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Abundance of stable isotopes of water IsotopeZAAbundance (%) Atomic wt. (amu) H1199.9851.007825 D120.0152.014102 16 O81699.76215.994915 18 O8180.20017.999160 17 O*8170.03816.999131
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Physical properties of water H 2 16 OH 2 18 O Density (g/cm 3 at 20°C )0.9971.1106 Melting point (°C at 760 torr)0.000.28 Boiling point (°C at 760 torr)100.00100.14 Vapor pressure (torr at 100°C)760.00758.07 Viscosity (centipoise at 20.2°C)1.0021.056
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Isotope effect and fractionation Isotopes undergo the same chemical and physical reactions. The rate of these reactions, however, could be different (isotope effect), resulting in the partitioning of isotopes (fractionation).
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Terminology =1000(R sample /R standard – 1) where R=heavy isotope/lighter isotope 18 O= 1000( 18 R sample / 18 R standard – 1) where 18 R= 18 O/ 16 O D= 1000( 2 R sample / 2 R standard – 1) where 2 R=D/H Standard is V-SMOW (Vienna-Standard Meteoric Ocean Water). 18 O V-SMOW = D V-SMOW = 0‰
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Temperature Altitude Distance from the source Latitude IAEA (2001). GNIP Maps and Animations.
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IAEA (2001). GNIP Maps and Animations
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Fricke and O’Neil, 1999
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Edwards et al., 2004
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d-excess Meteoric Water Line: D=8* 18 O+10 d-excess under “normal” conditions d= D-8* 18 O Increased relative humidity or lower sea-surface temperature (reduced evaporation rates) produces lower d-excess values.
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Dating Ice Cores Radio-isotopes Ice layers Ice flow models Reference horizons
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Volcanic markers provide additional time control
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Seasonal variations can be detected with microparticles and glacio-chemical data
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Antarctic Ice Cores
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Vostok Ice Core
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Epica Group, 2004
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Greenland
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MIS-5MIS-3MIS-1 MIS-4 Blunier and Brook, 2001, Science
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Warmer/Wetter? Colder/Drier?
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Range of 18 O values in the Kilimanjaro ice core
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