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Spontaneous Aggregation of Convective Storms

  • Caroline Muller
  • Da Yang
  • George Craig
  • Timothy Cronin
  • Benjamin Fildier
  • Jan O. Haerter
  • Cathy Hohenegger
  • Brian Mapes
  • David Randall
  • Sara Shamekh
  • Steven C. Sherwood
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Abstract

Idealized simulations of the tropical atmosphere have predicted that clouds can spontaneously clump together in space, despite perfectly homogeneous settings. This phenomenon has been called self-aggregation, and it results in a state where a moist cloudy region with intense deep convective storms is surrounded by extremely dry subsiding air devoid of deep clouds. We review here the main findings from theoretical work and idealized models of this phenomenon, highlighting the physical processes believed to play a key role in convective self-aggregation. We also review the growing literature on the importance and implications of this phenomenon for the tropical atmosphere, notably, for the hydrological cycle and for precipitation extremes, in our current and in a warming climate.

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Muller C., Yang D., Craig G., Cronin T., Fildier B., Haerter J.O., Hohenegger C., Mapes B., Randall D., Shamekh S. and Sherwood S.C. (2021) Spontaneous Aggregation of Convective Storms. Annual Review of Fluid Mechanics 54(1). 10.1146/annurev-fluid-022421-011319

Details

Forschungsschwerpunkte
Datum 23.09.2021
Journal Annual Review of Fluid Mechanics
Issue 1
Volume 54
Open Access Closed Access
Open Access Status Closed Access
Eprints_link https://cris.leibniz-zmt.de/id/eprint/4743
Peer-Reviewed

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