Journal article icon

Journal article

The impact of a land-sea contrast on convective aggregation in radiative-convective equilibrium

Abstract:

Convective aggregation is an important atmospheric phenomenon which frequently occurs in idealized models in radiative-convective equilibrium (RCE), where the effects of land, rotation, sea surface temperature gradients, and the diurnal cycle are often removed. This aggregation is often triggered and maintained by self-generated radiatively driven circulations, for which longwave feedbacks are essential. Many questions remain over how important the driving processes of aggregation in idealized models are in the real atmosphere. We approach this question by adding a continentally sized, idealized tropical rainforest island into an RCE model to investigate how land-sea contrasts impact convective aggregation and its mechanisms. We show that convection preferentially forms over the island persistently in our simulation. This is forced by a large-scale, thermally driven circulation. First, a sea-breeze circulation is triggered by the land-sea thermal contrast, driven by surface sensible heating. This sea-breeze circulation triggers convection which then generates longwave heating anomalies. Through mechanism denial tests we find that removing the longwave feedbacks reduces the large-scale effects of aggregation but does not prevent aggregation from occurring, and thus we highlight there must be another process aiding the aggregation of convection. We also show, by varying the island size, that the aggregated convective cluster appears to have a maximum spatial extent of O(10,000 km). These results highlight that the mechanisms of idealized aggregation remain relevant when land is included in the model, and therefore these mechanisms could help us understand convective organization in the real world.

Publication status:
Published
Peer review status:
Peer reviewed

Actions

Access Document

Files:
Publisher copy:
10.1029/2022ms003249

Authors

More by this author
Role:
Author
ORCID:
0000-0002-9831-9671
More by this author
Role:
Author
ORCID:
0000-0002-8391-6334
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Oxford college:
Oriel College
Role:
Author
ORCID:
0000-0002-1191-0128


More from this funder
Grant:
101003470
724602
821205


Publisher:
Wiley
Journal:
Journal of Advances in Modeling Earth Systems More from this journal
Volume:
15
Issue:
4
Article number:
e2022MS003249
Publication date:
2023-04-07
Acceptance date:
2023-03-24
DOI:
EISSN:
1942-2466


Language:
English
Keywords:
Pubs id:
1336856
Local pid:
pubs:1336856
Deposit date:
2023-04-10
ARK identifier:

Terms of use


Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP