Trapped-bubble records of concentrations of trace gases involved

Trapped-bubble records of concentrations of trace gases involved

Trapped-bubble records of concentrations of trace gases involved in global biogeochemical cycles Esther Pischel How does air become trapped? Snow falls and accumulates

Porous top layer exchanges air with the atmosphere Snow densifies at depth (50 150 m) and traps gas But The age of the air trapped in the ice is not the same as the ice itself Since air can freely exchange with the atmosphere in the porous upper zone of the ice sheet, it has a younger age than the ice itself

This age can be determined using steady-state or dynamic models Age difference is a function of temperature and snow accumulation rate Value is referred to as the gas age-ice age difference, or age Gas age timescale obtained by subtracting age from ice age timescale Another method for assessing gas age-ice age differences is a technique

based on the principle of thermal diffusion, which fractionates gas mixtures in a temperature gradient according to their mass Heavier 15N is concentrated with increasing depth Gases can be compared directly with gases, enabling a precise determination of the relative time of local temperature changes and atmospheric gas changes The trapped gas measured in Alley et al. is methane, CH4

Methane is used as a global climate proxy because the troposphere is well-mixed on decadal time scales Image source: http://chemwiki.ucdavis.edu/Inorganic_Chemistry/Case_Study:_Contrasting_Earth,_Mars_and_the_Moon's_Atmosphores Methane typically produced in an anaerobic environment generally associated with wetlands Modern wetlands methane emissions depend on Temperature Hydrologic balance

Net ecosystem productivity Warm, wet, and highly productive conditions are associated with higher methane emissions In ice cores: More methane = warmer Less methane = cooler Image source: http://wetlandsolutionsinc.com/ References:

Alley, R.B., Mayewski, P.A., Sowers, T., Stuiver, M., Taylor, K.C., and Clark, P.U., 1997, Holocence climatic instability: A prominent, widespread event 8200 yr ago, Geology, v. 25, no. 6, 3 p. Brook, E.J, Harder, S., Severinghaus, J., Steig, E.J., and Sucher, C.M., 2000, On the origin and timing of rapid changes in atmospheric methane during the last glacial period, Global Biogeochemical Cycles, v. 14, no. 12, 13 p. Schwander, J., Sowers, T., Barnola, J.M., Blunier, T., Fuchs, A. and Malaize, B., 1997, Age scale of the air in the summit ice: Implication for glacial-interglacial temperature change, Journal of Geophysical Research, v. 102, no. D16, 10 p. Severinghaus, J.P., Sowers, T., Brook, E.J., Alley, R.B., and Bender, M.L., 1998, Nature, v.

391, 5p. Sowers, T., Bender, M., Raynaud, D., and Korotkevich, Y.S., 1992, d 15N of N2 in air trapped in polar ice: A tracer of gas transport in the firn and a possible constraint on ice age-gas age differences, Journal of Geophysical Research, v. 97, no. D14, 14 p.

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