Book 2.indb - US Climate Change Science Program

The U.S. Climate Change Science ProgramHuber, M., L. Sloan, and C. Shellito, 2002: Early Paleogeneoceans and climate: A fully coupled modeling approach usingthe National Center for Atmospheric Research CommunityClimate System Model. In: Causes and Consequences of GloballyWarm Climates in the Early Paleogene [Wing, S.L., P.D.Gingerich, B. Schmitz, and E. Thomas (eds.)]. Geological Societyof America Special Paper 369, Boulder, CO, pp. 25–47.Jenkyns, H.C., 2003: Evidence for rapid climate change in theMesozoic-Palaeogene greenhouse world. Philosophical Transactionsof the Royal Society of London, Series A, MathematicalPhysical and Engineering Sciences, 361(1810), pp. 1885–1916.Joabsson, A. and T.R. Christensen, 2001: Methane emissionsfrom wetlands and their relationship with vascular plants: AnArctic example. Global Change Biology, 7, pp. 919–932.Jorgenson, M.T., C.H. Racine, J.C. Walters, and T.E. Osterkamp,2001: Permafrost degradation and ecological changes associatedwith a warming climate in central Alaska. Climatic Change,48, pp. 551–579.Jorgenson, M.T., Y.L. Shur, and E.R. Pullman, 2006: Abrupt increasein permafrost degradation in Arctic Alaska. GeophysicalResearch Letters, 33, L02503, doi:10.1029/2005GL024960.Kaplan, J.O., 2002: Wetlands at the Last Glacial Maximum: Distributionand methane emissions. Geopysical Research Letters,29, doi:10.1029/2001GL013366.Kaplan, J.O., G. Folberth, and D.A. Hauglustaine, 2006: Role ofmethane and biogenic volatile organic compound sources inlate glacial and Holocene fluctuations of atmospheric methaneconcentrations. Global Biogeochemical Cycles, 20, GB2016,doi:10.1029/2005GB002590.Kelly, M.J., R.L. Edwards, H. Cheng, D. Yuan, Y. Cai, M. Zhang,Y. Lin, and Z. An, 2006: High resolution characterization ofthe Asian Monsoon between 146,000 and 99,000 years B.P.from Dongge Cave, China and global correlation of eventssurrounding Termination II. Palaeogeography, Palaeoclimatology,Palaeoecology, 236, pp. 20–38, doi:10.1016/j.palaeo.2005.11.042.Kennett, J.P., K.G. Cannariato, I.L. Hendy, and R.J. Behl, 2000:Carbon isotopic evidence for methane hydrate instability duringQuaternary interstadials. Science, 288(5463), pp. 128–133,doi:10.1126/science.288.5463.128.Kennett, J.P., K.G. Cannariato, I.L. Hendy, and R.J. Behl, 2003:Methane Hydrates in Quaternary Climate Change: The ClathrateGun Hypothesis. AGU Press, Special Publication Vol. 54,216 pp.Kennett, J.P. and L.D. Stott, 1991: Abrupt deep sea warming, palaeoceanographicchanges and benthic extinctions at the end of thePaleocene. Nature, 353, pp. 319–322, doi:10.1038/353225a0.Kent, D.V., B.S. Cramer, L. Lanci, D. Wang, J.D. Wright, andR. Van der Voo, 2003: A case for a comet impact trigger forthe Paleocene/Eocene thermal maximum and carbon isotopeexcursion. Earth and Planetary Science Letters, 211(1-2),pp. 13–26, doi:10.1016/S0012-821X(03)00188-2.Keppler, F., J.T.G. Hamilton, M. Braß, and T. Röckman, 2006:Methane emissions from terrestrial plants under aerobic conditions.Nature, 439, pp. 187–191, doi:10.1038/nature04420.King, J.Y. and W.S. Reeburgh, 2002: A pulse-labeling experimentto determine the contribution of recent plant photosynthates tonet methane emission in arctic wet sedge tundra. Soil Biologyand Biochemistry, 34, pp. 173–180.King, J.Y., W.S. Reeburgh, and S.K. Regli, 1998: Methane emissionand transport by arctic sedges in Alaska: Results of a vegetationremoval experiment. Journal of Geophysical Research,103, pp. 29,083–29,092.Kobashi, T., J.P. Severinghaus, E.J. Brook, J.-M. Barnola, andA.M. Grachev, 2007: Precise timing and characterization ofabrupt climate change at 8200 years ago from air trapped inpolar ice. Quaternary Science Reviews, 26, pp. 1212–1222,doi:10.1016/j.quascirev.2007.01.009.Koch, P.L., J.C. Zachos, and P.D. Gingerich, 1992: Correlationbetween isotope records in marine and continental carbon reservoirsnear the Palaeocene/Eocene boundary. Nature, 358,pp. 319–322.Krason, J., 2000: Messoyakh gas field (W. Siberia): A model fordevelopment of the methane hydrate deposits of MackenzieDelta. In: Gas Hydrates: Challenges for the Future [Holder,G.D. and P.R. Bishnoi (eds.)]. Annals of the New York Academyof Sciences, v. 912, pp. 173–188.Kump, L.R. and M.A. Arthur, 1999: Interpreting carbon-isotopeexcursions: Carbonates and organic matter. Chemical Geology,161, pp. 181–198.Kvenvolden, K.A., 1993: Gas hydrates—Geological perspectiveand global change. Reviews of Geophysics, 31, pp. 173–187.Kvenvolden, K.A., 1999: Potential effects of gas hydrate on humanwelfare. Proceedings of the National Academy of Sciences,96, pp. 3420–3426.Kvenvolden, K.A, 2000: Gas hydrate and humans. In: Gas Hydrates:Challenges for the Future [Holder, G.D. and P.R. Bishnoi(eds.)]. Annals of the New York Academy of Sciences, 912,pp. 17–22.Kvenvolden, K.A. and T.D. Lorenson, 2001: The global occurrenceof natural gas hydrates. In: Natural Gas Hydrates: Occurrence,Distribution, and Detection [Paull, C.K. and W.P.Dillon (eds.)]. American Geophysical Union, GeophysicalMonograph, 124, pp. 3–18.Larson, R.L., 1991: Geological consequences of superplumes.Geology, 19, pp. 963–966.Lawrence, D.M. and A.G. Slater, 2005: A projection of severenear-surface permafrost degradation during the21st century. Geophysical Research Letters, 32, L24401,doi:10.1029/2005GL025080.Lawrence, D.M., A.G. Slater, V.E. Romanovsky, and D.J. Nicolsky,2008: The sensitivity of a model projection of near-surfacepermafrost degradation to soil column depth and inclusion ofsoil organic matter. Journal of Geophysical Research, 113,F02011, doi:10.1029/2007JF000883.Leifer, I., J.F. Clark, and R.F. Chen, 2000: Modifications of thelocal environment by natural marine hydrocarbon seeps. GeophysicalResearch Letters, 27(22), pp. 3711–3714.Leifer, I. and I. MacDonald, 2003: Dynamics of the gas flux fromshallow gas hydrate deposits: Interaction between oily hydratebubbles and the oceanic environment. Earth and PlanetaryScience Letters, 210(3-4), pp. 411–424.References234