Cloud regimes as phase transitions

Abstract

Clouds are repeatedly identified as a leading source of uncertainty in future climate predictions. Of particular importance are stratocumulus clouds, which can appear as either (i) closed cells that reflect solar radiation back to space or (ii) open cells that allow solar radiation to reach the Earth's surface. Here we show that these clouds regimes—open versus closed cells—fit the paradigm of a phase transition. In addition, this paradigm characterizes pockets of open cells as the interface between the open‐ and closed‐cell regimes, and it identifies shallow cumulus clouds as a regime of higher variability. This behavior can be understood using an idealized model for the dynamics of atmospheric water as a stochastic diffusion process. With this new conceptual viewpoint, ideas from statistical mechanics could potentially be used for understanding uncertainties related to clouds in the climate system and climate predictions.

Document Details

Document Type
Pub Defense Publication
Publication Date
Jun 20, 2016
Source ID
10.1002/2016gl069396

Entities

People

  • Samuel N. Stechmann
  • Scott Hottovy

Organizations

  • Office of Naval Research
  • University of Wisconsin–Madison

Tags

Readers

  • Atmospheric Remote Sensing.
  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Theoretical Analysis.

Technology Areas

  • Space