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The fractal nature of clouds in global storm-resolving models

Abstract:
Clouds in observations are fractals: they show self-similarity across scales ranging from one to 1000 km. This includes individual storms and large-scale cloud structures typical of organised convection. It is not known whether global storm-resolving models reproduce the observed fractal scaling laws for clouds and organised convection. We compute the fractal dimension of clouds using Himawari satellite data and compare this to global storm-resolving model simulations completed as part of the DYAMOND intercomparison project. We find cloud fields in these simulations are indeed fractal, and reproduce the observed fractal dimension to within 10%. We find the fractal dimension is sensitive to the choice of boundary layer parametrisation scheme used in each model simulation, and not to the convection parametrisation as might have been expected.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1029/2021gl095746

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Oxford college:
Wadham College
Role:
Author
ORCID:
0000-0001-8244-0218
More by this author
Role:
Author
ORCID:
0000-0003-4444-7376


Publisher:
American Geophysical Union
Journal:
Geophysical Research Letters More from this journal
Volume:
48
Issue:
23
Article number:
e2021GL095746
Publication date:
2021-11-19
Acceptance date:
2021-11-17
DOI:
EISSN:
1944-8007
ISSN:
0094-8276


Language:
English
Keywords:
Pubs id:
1211055
Local pid:
pubs:1211055
Deposit date:
2021-11-22

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