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Related Concept Videos

Boundary Layer Characteristics01:18

Boundary Layer Characteristics

404
When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
404

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Measuring Spatially- and Directionally-varying Light Scattering from Biological Material
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Testing the Two-Layer Model for Correcting Near Cloud Reflectance Enhancement Using LES/SHDOM Simulated Radiances.

Guoyong Wen1,2, Alexander Marshak1, Tamás Várnai1,3

  • 1NASA Goddard Space Flight Center, Greenbelt, Maryland.

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|August 4, 2020
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Summary
This summary is machine-generated.

Simple models estimate radiation enhancement from clouds. A new model including cloud-surface interactions (CSI) captures nearly 80% of this enhancement, improving satellite data accuracy.

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Area of Science:

  • Atmospheric Science
  • Radiative Transfer
  • Remote Sensing

Background:

  • Clouds scatter solar radiation into clear sky regions, creating a transition zone.
  • Satellite observations show enhanced radiation near clouds, but 3D scattering is computationally expensive to model.
  • Existing models estimate radiation scattered via cloud-molecular interactions.

Purpose of the Study:

  • Develop a simple method to estimate cloud-induced radiation enhancement.
  • Incorporate cloud-surface interactions (CSI) into existing models.
  • Improve accuracy of satellite-based atmospheric retrievals.

Main Methods:

  • Developed a two-layer model (2LM) including cloud-surface interactions (CSI).
  • Compared model results to full 3D radiative transfer simulations (SHDOM).
  • Used realistic cumulus cloud fields from UCLA Large Eddy Simulation (LES) model.

Main Results:

  • The original 2LM (cloud-air molecule interactions) accounted for 64% of reflectance enhancement.
  • The new 2LM+CSI model accounted for nearly 80% of reflectance enhancement.
  • Remaining 20% may be explained by cloud-aerosol radiative interactions.

Conclusions:

  • Simple models can effectively estimate 3D cloud radiative effects.
  • Incorporating CSI significantly improves radiation enhancement estimates.
  • These models can reduce biases in satellite retrievals of aerosols and clear-sky properties.