4.6 Article

Examining the Regional Co-Variability of the Atmospheric Water and Energy Imbalances in Different Model Configurations-Linking Clouds and Circulation

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021MS002951

关键词

clouds; water budget; energy budget; circulation; tropics; climate change

资金

  1. Israeli Science Foundation [1419/21]
  2. European Research Council (ERC) project constRaining the EffeCts of Aerosols on Precipitation (RECAP) under the European Union [724602]
  3. FORCeS project under the European Union's Horizon 2020 research program [821205]
  4. Natural Environment Research Council (NERC), Oxford DTP [NE/L002612/1]
  5. NERC, Oxford DTP [NE/S007474/1]

向作者/读者索取更多资源

This study explores the co-variability of atmospheric energy and water budget imbalances in different global model configurations, proposing a framework that links cloud properties to large-scale tropical circulation and climate system.
Clouds are a key player in the global climate system, affecting the atmospheric water and energy budgets, and they are strongly coupled to the large-scale atmospheric circulation. Here, we examine the co-variability of the atmospheric energy and water budget imbalances in three different global model configurations-radiative-convective equilibrium, aqua-planet, and global simulations with land. The gradual increase in the level of complexity of the model configuration enables an investigation of the effects of rotation, meridional temperature gradient, land-sea contrast, and seasonal cycle on the co-variability of the water and energy imbalances. We demonstrate how this co-variability is linked to both the large-scale tropical atmospheric circulation and to cloud properties. Hence, we propose a co-variability-based framework that connects cloud properties to the large-scale tropical circulation and climate system and is directly linked to the top-down constrains on the system-the water and energy budgets. In addition, we examine how the water and energy budget imbalances co-variability depends on the temporal averaging scale, and explain its dependency on how stationary the circulation is in the different model configurations. Finally, we demonstrate the effect of an idealized global warming and convective aggregation on this co-variability.

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