Huntley, Brian, Green, Rhys E., Collingham, Yvonne C., Hill, Jane K., Willis, Stephen G., Bartlein, Patrick J., ...
Species–climate 'envelope' models are widely used to evaluate potential climate change impacts upon species and biodiversity. Previous studies have used a variety of methods to fit models making it...
Barboni, Doris, Harrison, Sandy P., Bartlein, Patrick J., Jalut, G., New, M., Prentice, I. Colin, ...
Bigelow, N.H., Brubaker, Linda B., Edwards, M.E., Harrison, S.P., Prentice, I. Colin, Anderson, P.M., ...
A unified scheme to assign pollen samples to vegetation types was used to reconstruct vegetation patterns north of 55°N at the last glacial maximum (LGM) and mid-Holocene (6000 years B.P.). The...
Bigelow, N. H., Brubaker, L. B., Edwards, M. E., Harrison, Sandy P., Prentice, I. Colin, Anderson, P. M., ...
Kaplan, Jed O., Bigelow, N. H., Prentice, I. Colin, Harrison, Sandy P., Bartlein, Patrick J., Christensen, T. R., ...
Mid-Holocene climates of the americas: a dynamical response to changed seasonality (2003)
Harrison, Sandy P., Kutzbach, John E., Liu, Zhengyu, Bartlein, Patrick J., Otto-Bliesner, Bette, Muhs, Dan, ...
Global Change in Forests: Responses of Species, Communities, and Biomes (2001)
ANDREW J. HANSEN, RONALD P. NEILSON, VIRGINIA H. DALE, CURTIS H. FLATHER, LOUIS R. IVERSON, DAVID J. CURRIE, ...
Edwards, Mary E., Mock, Cary J., Finney, Bruce P., Barber, Valerie A., Bartlein, Patrick J.
The paleoclimatic history of a region can be viewed as a series of surface temperature and moisture anomalies through time. The effects of changes in large-scale climatic controls (e.g., insolation,...
Edwards, Mary E., Mock, Cary J., Finney, Bruce P., Barber, Valery A., Bartlein, Patrick J.
The paleoclimatic history of a region can be viewed as a series of surface temperature and moisture anomalies through time. The effects of changes in large-scale climatic controls (e.g., insolation,...
Edwards, Mary E., Mock, Cary J., Finney, Bruce P., Barber, Valery A., Bartlein, Patrick J.
The paleoclimatic history of a region can be viewed as a series of surface temperature and moisture anomalies through time. The effects of changes in large-scale climatic controls (e.g., insolation,...