Abstract

Clouds affect our daily life in many ways. They dominate our perception of weather and, thus, have an enormous influence on our everyday activities and our health. This fact is completely at odds with our knowledge about clouds, their representation in climate and weather forecast models, and our ability to predict clouds. It is their high variability in time and space that makes clouds both hard to monitor and to model. Clouds are the major concern in the climate modeling community, as stated by the Intergovernmental Panel on Climate Change (IPCC; information available online at www.ipcc.ch) “the most urgent scientific problems requiring attention to determine the rate and magnitude of climate change and sea level rise are the factors controlling the distribution of clouds and their radiative characteristics.” A similar conclusion was obtained within the Atmospheric Model Intercomparison Project (AMIP; e.g., Gates et al. 1999). The great challenge of climate research is to correctly account for the fact that the global state of our climate system is largely driven by various small-scale processes and their interaction with each other. Clouds are the most visible examples of this situation. On a global scale, clouds have a strong cooling effect on our climate: more solar radiation is reflected back to space than thermal surface radiation is trapped in the atmosphere. However, because radiation reacts on the instantaneous cloudy atmosphere and not on some climatological mean, the physical processes leading to the overall radiative effect strongly depend on the spatial distribution and structure of clouds.

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