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Low-level warm marine boundary layer MBL clouds cover large regions of Earth's surface.


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They have a significant role in Earth's radiative energy balance Klein and Hartmann, and hydrological cycle. Despite the fundamental role of low-level warm water clouds in climate, our understanding of these clouds is still limited. In particular, connections between their properties e.

Modeling these clouds in climate models remains a challenging problem. As a result, the influece of aerosols on these clouds in the past and future, and the potential impacts of these clouds on global warming remain open questions leading to substantial uncertainty in climate projections. To improve our understanding of these clouds, we need continuous observations of cloud properties on both a global scale and over a long enough timescale for climate studies.

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At present, satellite-based remote sensing is the only means of providing such observations. Publication Abstracts Zhang et al.

15 editions of this work

AU - Platnick, S. Gorodnichev, Sergei V. Ivliev, Alexander I.

LIGHT SCATTERING REVIEWS 8

Kuzovlev 8. On the application of the invariant embedding method and the radiative transfer equation codes for surface state analysis Victor P. Afanas'ev, Dmitry S. Efremenko and Alexander V.

Journal of Biomedical Photonics & Engineering

Lubenchenko 9. On some trends in the progress of astrophysical radiative transfer Arthur G. Nikoghosian A review of fast radiative transfer techniques Vijay Natraj Dependence of direct aerosol radiative forcing on the optical properties of atmospheric aerosol and underlying surface Claudio Tomasi, Christian Lanconelli, Angelo Lupi, and Mauro Mazzola.


  • Online Light Scattering Reviews 8 Radiative Transfer And Light Scattering 2013.
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