References - Ice Ages and Interglacials: Measurements, Interpretation, and Models - page 385

Sime, L.C., E.W. Wolff, K.I.C. Oliver, and J.C. Tindall (2009), ''Evidence for warmer

interglacials in East Antarctic ice cores,'' Nature, 462, 342-346.
Singer, S.F. and D.T. Avery (2007), Unstoppable Global Warming: Every 1500 Years, Rowman
& Littlefield, Lanham, MD.
Skinner, L.C. (2006), Glacial interglacial atmospheric CO 2 change: A simple hypsometric
effect on deep-ocean carbon sequestration? Climate of the Past Discussions, 2, 711-743
( http://www.clim-past-discuss.net/2/711/2006/ ).
Smith, A.G. and K.T. Pickering (2003), ''Oceanic gateways as a critical factor to initiate
icehouse Earth,'' Journal of the Geological Society, London, 160, 337-340.
Soon, W. (2007) ''Quantitative implications of the secondary role of carbon dioxide climate
forcing in the past glacial-interglacial cycles for the likely future climatic impacts of
anthropogenic greenhouse-gas forcings,'' Physical Geography, 28, 97-125.
Soon, W. and S. Baliunas (2003a), Lessons and Limits of Climate History: Was the 20th
Century Climate Unusual? (informal report), George C. Marshall Institute,

Washington, D.C.
Soon, W. and S. Baliunas (2003b), ''Reconstructing climatic and environmental changes of the
past 1000 years: A reappraisal,'' Energy and Environment, 14, 233-299.
Sowers, T. and M. Bender (1995), ''Climate records covering the last deglaciation,'' Science,
269, 210-214.
Spencer, R.W., W.D. Braswell, J.R. Christy, and J. Hnilo (2007), ''Cloud and radiation
budget changes associated with tropical intraseasonal oscillations,'' Geophysical

Research Letters, 34, L15707-L15711.
Spotl, C., A. Mangini, N. Frank, R. Eichstadter, and S.J. Burns (2002), ''Start of the last
interglacial period at 135 ka: Evidence from a high Alpine speleothem,'' Geology, 30,
815-818.
Steph, S., R. Tiedemann, M. Prange, J. Groeneveld, M. Schulz, A. Timmermann,
D. Nu¨ rnberg, C. Ru¨ hlemann, C. Saukel, and G.H. Haug (2010), ''Early Pliocene increase
in thermohaline overturning: A precondition for the development of the modern equator-
ial Pacific cold tongue,'' Paleoceanography, 25, PA2202.
Stephens, B.B. and R.F. Keeling (2000), ''The influence of Antarctic sea ice on glacial/
interglacial CO 2 variations,'' Nature, 404, 171-174.
Stott, L. (2010) ''No signs of Southern Ocean CO 2 ,'' Nature Geoscience, 3, 153-154.
Stott, L. and A. Timmermann (2011), ''Hypothesized link between glacial/interglacial
atmospheric CO 2 cycles and storage/release CO 2 -rich fluids from deep sea sediments,''
Geophysical Monograph Series, 193, 123-128.
Stott, L., A. Timmermann, and R. Thunell (2007), ''Southern Hemisphere and deep-sea
warming led deglacial atmospheric CO 2 rise and tropical warming,'' Science, 318,
435-439.
Svensmark, H. (2000), ''Cosmic rays and Earth's climate,'' Space Science Reviews, 93, 155-166
( http://www.junkscience.com/Greenhouse/influence-of-cosmic-rays-on-the-earth.pdf ).
Svensmark, H. (2007), ''Cosmoclimatology: A new theory emerges,'' Astronomy and
Geophysics, 48, 1.18-1.24.
Svensmark, H. and Friis-Christensen, E. (1997), ''Variation of cosmic ray flux and global
cloud coverage: A missing link in solar-climate relationships,'' Journal of Atmospheric
and Solar-Terrestrial Physics, 59, 1225-1232.
Svensmark, H. and E. Friis-Christensen (2007), Reply to Lockwood and Fro¨hlich: The
Persistent Role of the Sun in Climate Forcing (Danish National Space Center Scientific
Report, March) ( http://www.spacecenter.dk/publications/scientific-report-series/Scient_

No._3.pdf/view ) .