Lisa C. Sloan
PUBLICATIONS 2005
LISA CIRBUS SLOAN
Endemic oaks, climate change, and regional conservation, Kueppers, L., Snyder, M.A., Sloan, L.C., Zavaleta, E. and Fulfrost, B., in press, Proc. National Academy Science, September 2005.
Come a little bit closer: A high-resolution climate study of the early Paleogene Laramide foreland, Sewall, J.O., and Sloan, L.C., in press, Geology, September 2005.
A framework for regional modeling of past climates, Sloan, L.C., accepted, Journal of Theoretical and Applied Climatology, July 2005.
Reconstructing a lost Eocene paradise, Part I: Simulating the change in global floral distribution at the Initial Eocene Thermal Maximum, Shellito, L. J., and Sloan, L. C., accepted, Global and Planetary Change, August 2005.
Reconstructing a lost Eocene paradise, Part II: On the utility of dynamic global vegetation models in Pre-Quaternary climate studies, Shellito, L. J., and Sloan, L. C., accepted, Global and Planetary Change, August 2005.
Transient future climate over the Western U.S. using a regional climate model, Snyder, M.A., and Sloan, L.C., Earth Interactions, 9, 1-21, 2005.
A method for using a fully-coupled climate system model to generate detailed surface boundary conditions for paleoclimate modeling investigations: An early Paleogene example, Sewall, J.O., Huber, M., and Sloan, L. Cirbus, Global and Planetary Change, 43, 173-182, 2004.
Modeled Regional Climate Change in the Hydrologic Regions of California: A CO2 Sensitivity Study, Snyder, M.A., Sloan, L.C., and Bell, J.L., Jour. American Water Resources Assoc., 591-601, 2004.
Mid-Holocene orbital forcing of regional-scale climate: A case study of western North America using a high-resolution RCM, Diffenbaugh, N.S., and Sloan, L.C., Jour. Climate, 17, 2927-2937, 2004.
Less ice, less tilt, less chill: The influence of a seasonally ice-free Arctic Ocean and reduced obliquity on early Paleogene climate, Sewall, J.O., and Sloan, L. Cirbus, Geology; June 2004; v. 32; no. 6; p. 477–480; doi: 10.1130/G20295.
Disappearing Arctic sea ice reduces available water in the American west, Sewall, J.O., and Sloan, L. Cirbus, Geophys. Res. Lett. 31 L06209, doi: 10.1029/2003GL019133, 2004.
Could land cover feedbacks alter near-shore upwelling regimes? , Diffenbaugh, N.S., Snyder, M.A., and Sloan. L.C., Proceedings of the National Academy of Sciences, 101, 27-31, 2004.
Regional changes in extreme climatic events, Bell, J.L., Sloan, L.C., and Snyder, M.A., Jour. Climate, 17, 81-87, 2004.
Regional climate change impacts: The role of institutional adaptability, Haddad, B. M., Sloan, L. C., Snyder, M.A., and Bell, J.L., International Journal of Sustainable Development, v. 6, 265-282, 2003.
Future climate change and upwelling in the California Current, Snyder, M.A., Sloan, L.C., Diffenbaugh, N.S., and. Bell, J.L., Geophys. Res. Lett.,30 (15), 1823, 10.1029/2003/GL017647, 2003.
Orbital suppression of wind driven upwelling in the California Current at 6 ka, Diffenbaugh, N.S., Sloan, L.C., and Snyder, M.A., Paleoceanography, 18 (2), 1051, 10.1029/2003PA000865, 2003.
Vegetation sensitivity to global anthropogenic carbon dioxide emissions in a topographically complex region, Diffenbaugh, N.S., Sloan, L. C., Snyder, M.A., Bell, J.L., Kaplan, J., Shafer, S.L., and Bartlein, P.J., Global Biogeochemical Cycles 17 (2), 1067.10.1029/200BG001974, 2003.
Chicxulub and climate: Effects of stratospheric injections of impact-produced S-bearing gases, Pierazzo, E., Hahmann, A., and Sloan, L. C., Astrobiology 3 (1), 99 – 118, Rubey Symposium Special Volume, 2003.
Evaluating pCO2 levels in the early-middle Paleogene, Shellito, L.J., Sloan, L. Cirbus, and Huber, M., Palaeogeog., Palaeoclim., Palaeoecol.,193, 112-123, 2003.
The relative importance of climate change and the physiological effects of CO2 on freezing tolerance for the future distribution of Yucca brevifolia, Dole, K.P., Loik, M., and Sloan, L. Cirbus, Global and Planetary Change, v. 36, p.137-146, 2003.
Terrestrial climatic response to precessional orbital forcing in the Eocene, Lawrence, K.T., Sloan, L. Cirbus, and Sewall, J.O., Geological Society of America Special Volume 369, Causes and consequences of globally warm climates in the early Paleogene (eds. Wing, S.L., Gingerich, P.D., Schmitz, B., and Thomas, E.), pp 65-77, 2003.
Early Paleogene oceans and climate: A fully coupled modeling approach using the NCAR CCSM, Huber, M., Sloan, L. C., and Shellito, L.J., Geological Society of America Special Volume 369, Causes and consequences of globally warm climates in the early Paleogene, (eds. Wing, S.L., Gingerich, P.D., Schmitz, B., and Thomas, E.), pp 65-77, 2003.
Evaluation of Northern Hemisphere natural climate variability in multiple temperature reconstructions and global climate model simulations, Bell, J.L., Sloan, L. Cirbus, Revenaugh, J., and Duffy, P.B., Global and Planetary Change, 37, 2003; doi: 10.1016/S0921-8181(02)000189-3.
Climate responses to a doubling of atmospheric carbon dioxide for a climatically vulnerable region, Snyder, M.A., Bell, J.L., Sloan, L. Cirbus, Duffy, P. B., and Govindasamy, B., Geophys. Res. Letters, 7 June 2002 (vol.29, 10.1029/2001GL014431, 2002).
Global climate sensitivity to land surface change: The Mid Holocene revisited, Diffenbaugh, N. S., and Sloan, L. Cirbus, Geophys. Res. Letters, 30 May 2002 (vol. 29, 10.1029/2002/GL014880, 2002).
Equable Paleogene climates: The result of a stable, positive Arctic Oscillation?, Sewall, J.O., and Sloan, L. Cirbus, Geophys. Res. Letters, v. 28, 3693-3696, 2001.
Heat transport, deep waters, and temperature gradients: Coupled simulation of an Eocene “Greenhouse” climate, Huber, M., Sloan, L. Cirbus, Geophys. Res. Letters, v. 28, 3481-3484, 2001.
Modeling orbital forcing of lake level change: Lake Gosiute (Eocene), North America, Morrill, C., Small, E. E., and Sloan, L. Cirbus, Global and Planetary Change, v. 29, 57-76, 2001.
Trends, rhythms, and aberrations in global climate 65 Ma to present, Zachos, J., Pagani, M., Sloan, L. C., Thomas, E., and Billups, K., Science, v. 292, 686-693, 2001.
Effect of sea surface temperature configuration on model simulations of “equable” climate in the early Eocene, Sloan, L. Cirbus, Huber, M., Crowley, T.J., Sewall, J.O., and Baum, S., Palaeogeography, Palaeoclimatology, Palaeoecology, v.167, 321-335, 2001.
Eocene Oceanic Responses to Orbital Forcing on Precessional Time Scales, Sloan, L. Cirbus, and Huber, M., Paleoceanography, v. 16, 101-111, 2001.
Changes in surface air temperature caused by desiccation of the Aral Sea, Small, E. E., Sloan, L. Cirbus, and Nychka, D., Jour. Climate, v. 14, p. 284-299, 2001.
The effects of desiccation and climatic change on the hydrology of the Aral Sea, Small, E.E., Giorgi, F., Sloan, L. Cirbus, and Hostetler, S., Jour. Climate, v. 14, p. 300-322, 2001.
Climate sensitivity to changes in land surface characteristics, Sewall, J.O., Sloan, L. Cirbus, Huber, M., and Wing, S., Global and Planetary Change v. 26, p. 445-465, 2000,
High concentrations of greenhouse gases and polar stratospheric clouds: A possible solution to high latitude faunal migration at the Latest Paleocene Thermal Maximum, Peters, R. B., and Sloan, L. Cirbus, Geology, v. 28, p. 979-982, 2000.
Modeling the Paleogene, Part I: Paleogene terrestrial climate change predicted from climate modeling studies, Sloan, L. Cirbus, Huber, M., Peters, R., and Ewing, A., GFF, (Geological Society of Sweden), v. 122, p. 146-147, 2000.
Modeling the Paleogene, Part II: Paleogene wind-driven ocean circulation changes predicted from climate modeling studies, Huber, M, and Sloan, L. Cirbus, GFF (Geological Society of Sweden), v. 122, p. 80-81, 2000.
Climatic responses to tropical sea surface temperature changes on a “greenhouse” Earth, Huber, M, and Sloan, L. Cirbus, Paleoceanography, v. 15, 443-450, 2000.
Effect of flux adjustments on temperature variability in climate models, Duffy, P.B., Bell, J., Covey, C., Sloan, L., and the CMIP investigators, Geophys. Res. Lett., v. 27, p. 763-766, 2000.
Comparison of temperature variability in observations and sixteen climate model simulations, Bell, J., Duffy, P., Covey, C., and Sloan, L. Cirbus, and the CMIP investigators, Geophys. Res. Lett., v. 27, p. 261-264, 2000.
Early Paleogene Warm Climates and Biosphere Dynamics: Meeting in Göteborg Makes Progress in Deciphering the Dynamics of Past Greenhouse Worlds , Sloan, L. Cirbus, Schmitz, B., Aubry, M.-P., and Zachos, J., Paleoceanography, v. 14, p. 559-560, 1999.
Warm Climate Transitions: A General Circulation Modeling Study of the Late Paleocene Thermal Maximum (~56 Ma), Huber, M., and Sloan, L. Cirbus, Jour. Geophys.Research, v. 104, p.16633-16655, 1999.
Simulating the water balance of the Aral Sea with a coupled modeling system, Small, E.E., Sloan, L. Cirbus, Hostetler, S. and Giorgi, F.,Jour. Geophys. Research, v. 104, p.6583-6602, 1999.
Regional climate model simulation of precipitation in central Asia: Mean and interannual variability, Small, E.E., Giorgi, F., and Sloan, L. Cirbus, Jour. Geophys. Research, v. 104, p.6563-6582, 1999.
Orbital Forcing and Eocene Continental Temperatures, Sloan, L. Cirbus and Morrill, C., Palaeogeography, Palaeoclimatology, Palaeoecology, v. 144, p. 21-35, 1998.
Polar stratospheric clouds: a high latitude winter warming mechanism in an ancient greenhouse world, Sloan, L. Cirbus, and Pollard, D., Geophysical Research Letters, v. 25, p. 3517-3520, 1998.
A comparison of spatially-resolved and global mean reconstructions of continental denudation under ice-free and present conditions, Sloan, L. Cirbus, Bluth, G. J. S., and Filippelli, G., Paleoceanography, v. 12, p. 147-160, 1997.
Paleoclimate data constraints on climate sensitivity: The paleocalibration method, Covey, C., Sloan, L. Cirbus, and Hoffert, M. I., Clim. Change, v. 32, p. 1-20, 1996.
Modeling of Middle Pliocene climate with the NCAR Genesis general circulation model, Sloan, L. Cirbus, Crowley, T. J., and Pollard, D., Marine Micropaleontology, v. 27, p. 51-61, 1996.
Climates and climate variability of the Pliocene, Poore, R. Z. and Sloan, L. Cirbus, Marine Micropaleontology, v. 27, p. 1-2, 1996.
The role of oceanic heat transport in early Eocene climate, Sloan, L. Cirbus, Walker, J. C. G., and Moore, Jr., T.C., Paleoceanography, v. 10, p. 347-356, 1995.
Atmospheric carbon dioxide and early Eocene climate: A general circulation modeling sensitivity study, Sloan, L. Cirbus, and Rea, D. K., Palaeogeography, Palaeoclimatology, Palaeoecology, v. 119, p. 275-292, 1995.
Model-model and data-model comparisons: Applications to the PRISM project, Sloan, L. Cirbus, U.S. Geological Survey Open File Report 94-23, R. S. Thompson, ed., p. 69-70, 1994.
"Equable" climates during the early Eocene: Significance of regional paleogeography for North American climate, Sloan, L. Cirbus, Geology, v. 22, p. 881-884, 1994.
Modeling of Mid-Pliocene climate with the NCAR Genesis GCM, Sloan, L. C., U. S. Geological Survey Open File Report 94-588, S. E. Ishman, ed., p. 24, 1994.
Possible methane-induced polar warming in the early Eocene Sloan, L. Cirbus, J. C. G. Walker, Moore, T.C. ,Jr., Rea, D. K., and Zachos, J. C., Nature, v. 357, p. 320-322, 1992.
A comparison of Eocene climate model results to quantified to paleoclimatic interpretations, Sloan, L. Cirbus and Barron, E. J., Palaeogeography, Palaeoclimatology, Palaeoecology, v.93, p.183-202, 1992.
Paleoclimate of the Kimmeridgian/Tithonian (Late Jurassic) world: II, Sensitivity tests comparing three different paleotopographic settings, Moore, G. T., Sloan, L. Cirbus, Hayashida, D.N., and Umrigar, N.P., Palaeogeography, Palaeoclimatology, Palaeoecology, v. 95, p. 229-252, 1992.
Something is wrong with climate theory, Walker, J. C. G. and Sloan, L. Cirbus, Geotimes, June 1992, p. 16-18, 1992.
Reply to comments on "Equable" climates during Earth history?, Sloan, L. Cirbus and Barron, E. J., Geology, v. 19, p. 540-542, 1991.
"Equable" climates during Earth history?, Sloan, L. Cirbus and Barron, E. J.,, Geology, v. 18, p. 489-492, 1990.