Intraseasonal variations in the surface layer heat balance of the central equatorial Indian Ocean: The importance of zonal advection and vertical mixing
Version of Record online: 6 JUN 2013
©2013. American Geophysical Union. All Rights Reserved.
Geophysical Research Letters
Volume 40, Issue 11, pages 2737–2741, 16 June 2013
How to Cite
2013), Intraseasonal variations in the surface layer heat balance of the central equatorial Indian Ocean: The importance of zonal advection and vertical mixing, Geophys. Res. Lett., 40, 2737–2741, doi:10.1002/grl.50536., and (
- Issue online: 3 JUL 2013
- Version of Record online: 6 JUN 2013
- Accepted manuscript online: 6 MAY 2013 12:00AM EST
- Manuscript Accepted: 3 MAY 2013
- Manuscript Revised: 2 MAY 2013
- Manuscript Received: 28 MAR 2013
Additional supporting information may be found in the online version of this article.
|2013gl056092fs01.eps||PS document||202K||Daily values of (a) shortwave radiation, (b) longwave radiation, (c) sensible heat flux, (d) latent heat flux, and (e) total net surface heat flux at the air-sea interface (in W m-2). Overplotted on latent heat flux is surface wind speed in (m s-1) as a red curve, with scale inverted.|
|2013gl056092fs02.eps||PS document||279K||Time longitude plot of outgoing longwave radiation (OLR) at the top of the atmosphere (in W m-2). Blues represent deep convection and rainy conditions while reds and yellows represent clear sky conditions. Ovals indicate eastward progression of variations associated with the Madden-Julian Oscillation for active phases (solid lines) and suppressed phases (dashed lines). Adapted from Climate Prediction Center (2013).|
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