Articles | Volume 9, issue 12
Atmos. Chem. Phys., 9, 4039–4052, 2009
https://doi.org/10.5194/acp-9-4039-2009

Special issue: European Integrated Project on Aerosol-Cloud-Climate and Air...

Atmos. Chem. Phys., 9, 4039–4052, 2009
https://doi.org/10.5194/acp-9-4039-2009

  19 Jun 2009

19 Jun 2009

How important is the vertical structure for the representation of aerosol impacts on the diurnal cycle of marine stratocumulus?

I. Sandu et al.

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Subject: Clouds and Precipitation | Research Activity: Atmospheric Modelling | Altitude Range: Troposphere | Science Focus: Physics (physical properties and processes)
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Cited articles

Ackerman, A. S., Kirkpatrick, M. P., Stevens, D. E., and Toon, O. B.: The impact of humidity above stratiform clouds on indirect aerosol climate forcing, Nature, 432, 1014–1017, 2004.
Albrecht, B.: Effects of Precipitation on the Thermodynamic Structure of the Trade Wind Boundary Layer, J. Geophys. Res., 98(D4), 7327–7337, 1993.
Barker, H. and Davies, J. A.: Solar radiative fluxes for stochastic, scale-invariant broken cloud fields, J. Atmos. Sci., 49, 1115–1126, 1992.
Bougeault, P.: The diurnal cycle of marine stratocumulus: A higher order model study, J. Atmos. Sci., 42, 2826–2843, 1985.
Bretherton, C. S. and Wyant, M. C.: Moisture transport, lower-troposphere stability, and decoupling of cloud-topped boundary, J. Atmos. Sci., 54, 148–167, 1997.
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