Mineral aerosols: A comparison of the last glacial maximum and preindustrial Holocene

Canadian Journal of Earth Sciences

Volumn 37, Issue 5, 2000, Pages 751-767

  Reader, M C ^a   Fung, I ^b   McFarlane, N ^c  

^a UNIVERSITY OF VICTORIA   (Canada)

^b UNIVERSITY OF CALIFORNIA   (United States)

^c ENVIRONMENT CANADA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC MODELING; ATMOSPHERIC MOTION; COMPARATIVE STUDY; DUST; HOLOCENE; ICE CORE; LAST GLACIAL MAXIMUM;

EID: 0033859307     PISSN: 00084077     EISSN: None     Source Type: Journal    
DOI: 10.1139/e99-109     Document Type: Article

References (26)

1. Alexander, R.C., and Mobley, R.L. 1976. Monthly average sea surface temperatures and ice pack limits on a 1° global grid. Monthly Weather Review, 104: 143-148.
2. CLIMAP. 1981. Seasonal reconstructions of the Earth's surface at the last glacial maximum. Geological Society of America, Map Chart Series MC-36.
3. De Angelis, M., Barkov, N.I., and Petrov, V.N. 1987. Aerosol concentrations over the last climatic cycle (160 kyr) from an Antarctic ice core. Nature (London), 325: 318-321.
4. Denning, A.S., Holzer, M., Gurney, K.R., Heimann, M., Law, R.M., Rayner, P.J., Fung, I. Y., Fan, S., Taguchi, S., Friedlingstein, P., Balkanski, Y., Maiss M., and Levin, I. 1999. Three-dimensional transport and concentration of SF6: A model intercomparison study (transcom 2). Tellus, 51B: 266-297.
5. Genthon, C. 1992. Simulations of desert dust and sea salt aerosols in Antarctica with a general circulation model of the atmosphere. Tellus, 44: 371-389.
6. Holzer, M. 1999. Analysis of passive tracer transport as modelled by an atmospheric general circulation model. Journal of Climate, 12: 1659-1684.
7. Joussaume, S. 1993. Simulation of the desert dust cycle at 18 kyr B.P. Journal of Geophysical Research, 98: 2767-2805.
8. Mahowald, N., Kohfeld, K.E., Hansson, M., Balkanski, Y., Harrison, S.P., Prentice, I.P., Schulz M., and Rodhe, H. 1999. Dust sources and deposition during the last glacial maximum and current climate: a comparison of model results with paleodata from ice cores and marine sediments. Journal of Geophysical Research, 104(D13): 15895-15916.
9. 2 change: The iron hypothesis. Paleoceanography, 5 (1): 1-13.
10. Mayewski, P.A., Meeker, L.D., Whitlow, M., Twickler, M.S., Morrison, M.C., Bloomfield, P., Bond, G.C., Alley, R.B., Gow, A.J., Grootes, P.M., Meese, D.A., Ram, M., Taylor, K.C., and Wumkes, W. 1994. Changes in atmospheric circulation and ocean ice cover over the North Atlantic during the last 41 000 years. Science, 263: 1747-1751.
11. McFarlane, N.A., Boer, G.J., Blanchet, J.-P., and Lazare, M. 1992. The Canadian Climate Centre second-generation general circulation model and its equilibrium climate. Journal of Climate, 5: 1013-1044.
12. Miller, R.L., and Tegen, I. 1998. Climate response to soil dust aerosols. Journal of Climate, 11: 3247-3267.
13. Petit, J.-R., Briat, M., and Royer, A. 1981. Ice age aerosol content from East Antarctic ice core samples and past wind strength. Nature (London), 293: 391-394.
14. Petit, J.-R., Mounier, L., Jouzel, J., Korotkevich, Y.S., Kotlyakov, V.I., and Lorius, C. 1990. Paleoclimatological and chronological implications of the Vostok core dust record. Nature (London), 343: 56-58.
15. Ram, M., Gayley, R.I., and Petit, J.-R. 1988. Insoluble particles in Antarctic ice: background aerosol size distribution and diatom concentration. Journal of Geophysical Research, 93 (D7): 8378-8382.
16. Reader, M.C., Fung, I., and McFarlane, N. 1999a. Correction to "the mineral dust aerosol cycle during the last glacial maximum." Journal of Geophysical Research, 104(D 18): 22319-22320.
17. Reader, M.C., Fung, I., and McFarlane, N. 1999b. The mineral dust aerosol cycle during the last glacial maximum. Journal of Geophysical Research, 104(D8): 9381-9398.
18. Seinfeld, J.H. 1986. Atmospheric chemistry and physics of air pollution. John Wiley and Sons, Inc., New York.
19. Steffensen, J.P. 1997. The size distribution of microparticles from selected segments of the Greenland Ice Core Project ice core representing different climatic periods. Journal of Geophysical Research, 102(C12): 26755-26763.
20. Stowe, L.L., Ignatov, A.M., and Singh, R.R. 1997. Development, validation, and potential enhancements to the second-generation operational aerosol product at the National Environmental Satellite, Data and Information Service of the National Oceanic and Atmospheric Administration. Journal of Geophysical Research, 102: 16923-16934.
21. Swap, R.M., Garstang, M., Greco, S., Talbot R., and Kallberg, P. 1992. Saharan dust in the Amazon basin. Tellus, 44B: 133-148.
22. Tegen, I., and Fung, I. 1994. Modeling of mineral dust in the atmosphere: sources, transport and optical thickness. Journal of Geophysical Research, 99: 22897-22914.
23. Tegen, I., and Fung, I. 1995. Contribution to the mineral aerosol load from land surface modification. Journal of Geophysical Research, 100: 18707-18725.
24. Thompson, L.G., and Mosley-Thompson, E. 1981. Microparticle concentration variation linked with climatic change: evidence from polar ice cores. Science, 212: 812-815.
25. Thompson, L.G., Yao, T., Davis, M.E., Henderson, K.A., Mosley-Thompson, E., Lin, P-N., Beer, J., Synal, H.-A., Cole-Dai, J., and Bolzan, J.F. 1997. Tropical climate instability: the last glacial cycle from a Qinghai-Tibetan ice core. Science, 276: 1821-1825.
26. Vettoretti, G., Peltier, W.R., and McFarlane, N.A. 2000. Global water balance and atmospheric water vapour transport at last glacial maximum: climate simulations with the CCCma atmospheric general circulation model. Canadian Journal of Earth Sciences, 37: 695-723.