The copyright line for this article was changed on 23 MAR 2015 after original online publication.
Precipitation scaling with temperature in warm and cold climates: An analysis of CMIP5 simulations
Article first published online: 2 AUG 2013
©2013. The Authors.
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Geophysical Research Letters
Volume 40, Issue 15, pages 4018–4024, 16 August 2013
How to Cite
2013), Precipitation scaling with temperature in warm and cold climates: An analysis of CMIP5 simulations, Geophys. Res. Lett., 40, 4018–4024, doi:10.1002/grl.50730., , , , and (
- Issue published online: 28 AUG 2013
- Article first published online: 2 AUG 2013
- Accepted manuscript online: 12 JUL 2013 08:53AM EST
- Manuscript Accepted: 9 JUL 2013
- Manuscript Revised: 3 JUL 2013
- Manuscript Received: 10 MAY 2013
- Australian Research Council. Grant Number: DP1201100343
- U.S. National Science Foundation. Grant Number: ATM-0602409
|SI_fig1.pdf||PDF document||2934K||Simulated temperature and precipitation changes in past, present, and projected climates. The values shown are ensemble averages of the outputs from six CMIP5 models (IPSL-CM5A-LR, MPI-ESM-P, MIROC-ESM, CCSM4, MRI-CGCM3, and GISS E2 R). The plots show the anomalies (experiment minus piControl) of mean annual temperature (MAT) and mean annual precipitation (MAP) at the Last Glacial Maximum (lgm) from the historical run (average for period 1979 to 2005), the 1% CO2 run (1pctCO2, average for the period model years 86–115), and the 4xCO2 run (abrupt4xCO2).|
|SI_fig2.pdf||PDF document||14K||Simulated changes in (left) temperature and (right) precipitation during the historical period (1850–2005). The simulated changes can be compared with the average values obtained in the preindustrial (pi) simulation of each model (black dot).|
|Auxilliary_Material_table.docx||Word 2007 document||22K||Supporting information|
|Auxilliary_Material_figure_caption.docx||Word 2007 document||14K||Supporting information|
|README.txt||plain text document||1K||Supporting information|
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