The copyright line for this article was changed on 13 APR 2015 after original online publication.
Mechanism of tropical low-cloud response to surface warming using weather and climate simulations
Version of Record online: 30 MAY 2013
©2013. The Authors.
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Geophysical Research Letters
Volume 40, Issue 10, pages 2427–2432, 28 May 2013
How to Cite
2013), Mechanism of tropical low-cloud response to surface warming using weather and climate simulations, Geophys. Res. Lett., 40, 2427–2432, doi:10.1002/grl.50474., , and (
- Issue online: 1 JUL 2013
- Version of Record online: 30 MAY 2013
- Accepted manuscript online: 16 APR 2013 12:00AM EST
- Manuscript Accepted: 14 APR 2013
- Manuscript Revised: 12 APR 2013
- Manuscript Received: 21 MAR 2013
- Program for Risk Information on Climate Change (SOUSEI)
- Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan. Grant Numbers: 23310014, 23340137
|grl50474-sup-0001-demoto_cloud_GL055327R_auxiliary.doc||Word document||612K||Attached in auxiliary material are additional figures for summary and discussion of section 4. We show schematic diagram, results of the additional experiments, and analysis of changes in convective drying.|
|grl50474-sup-0002-55327fs01r.eps||PS document||16236K||Schematic of mechanisms controlling the decrease in low clouds over the subsidence regions.|
|grl50474-sup-0003-55327fs02r.eps||PS document||3149K||Same as Fig. 2d but for the 30 day runs (thick) together with the TAMIP experiments (thin).|
|grl50474-sup-0004-55327fs03r.doc||Word document||612K||Changes in convective drying due to the change in the vertical gradient of specific humidity (blue), due to the change in cumulus mass flux (red), and the sum of the two terms (black) in the TAMIP and AMIP experiments.|
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