Circling in on Convective Self-Aggregation

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Circling in on Convective Self-Aggregation. / Nissen, Silas Boye; Härter, Jan Olaf Mirko.

I: Journal of Geophysical Research: Atmospheres, Bind 126, Nr. 20, e2021JD035331, 24.09.2021.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Nissen, SB & Härter, JOM 2021, 'Circling in on Convective Self-Aggregation', Journal of Geophysical Research: Atmospheres, bind 126, nr. 20, e2021JD035331. https://doi.org/10.1029/2021JD035331

APA

Nissen, S. B., & Härter, J. O. M. (2021). Circling in on Convective Self-Aggregation. Journal of Geophysical Research: Atmospheres, 126(20), [e2021JD035331]. https://doi.org/10.1029/2021JD035331

Vancouver

Nissen SB, Härter JOM. Circling in on Convective Self-Aggregation. Journal of Geophysical Research: Atmospheres. 2021 sep. 24;126(20). e2021JD035331. https://doi.org/10.1029/2021JD035331

Author

Nissen, Silas Boye ; Härter, Jan Olaf Mirko. / Circling in on Convective Self-Aggregation. I: Journal of Geophysical Research: Atmospheres. 2021 ; Bind 126, Nr. 20.

Bibtex

@article{31849d8f47344c87a00a18e06d2af6d4,
title = "Circling in on Convective Self-Aggregation",
abstract = "In radiative-convective equilibrium simulations, convective self-aggregation (CSA) is the spontaneous organization into segregated cloudy and cloud-free regions. Evidence exists for how CSA is stabilized, but how it arises favorably on large domains is not settled. Using large-eddy simulations, we link the spatial organization emerging from the interaction of cold pools (CPs) to CSA. We systematically weaken simulated rain evaporation to reduce maximal CP radii, R_{max}, and find reducing R_{max} causes CSA to occur earlier. We further identify a typical rain cell generation time and a minimum radius, R_{min}, around a given rain cell, within which the formation of subsequent rain cells is suppressed. Incorporating R_{min} and R_{max}, we propose a toy model that captures how CSA arises earlier on large domains: when two CPs of radii r_i,r_j ∈ [R_{min}, R_{max}] collide, they form a new convective event. These findings imply that interactions between CPs may explain the initial stages of CSA.",
author = "Nissen, {Silas Boye} and H{\"a}rter, {Jan Olaf Mirko}",
year = "2021",
month = sep,
day = "24",
doi = "10.1029/2021JD035331",
language = "English",
volume = "126",
journal = "Journal of Geophysical Research: Solid Earth",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "20",

}

RIS

TY - JOUR

T1 - Circling in on Convective Self-Aggregation

AU - Nissen, Silas Boye

AU - Härter, Jan Olaf Mirko

PY - 2021/9/24

Y1 - 2021/9/24

N2 - In radiative-convective equilibrium simulations, convective self-aggregation (CSA) is the spontaneous organization into segregated cloudy and cloud-free regions. Evidence exists for how CSA is stabilized, but how it arises favorably on large domains is not settled. Using large-eddy simulations, we link the spatial organization emerging from the interaction of cold pools (CPs) to CSA. We systematically weaken simulated rain evaporation to reduce maximal CP radii, R_{max}, and find reducing R_{max} causes CSA to occur earlier. We further identify a typical rain cell generation time and a minimum radius, R_{min}, around a given rain cell, within which the formation of subsequent rain cells is suppressed. Incorporating R_{min} and R_{max}, we propose a toy model that captures how CSA arises earlier on large domains: when two CPs of radii r_i,r_j ∈ [R_{min}, R_{max}] collide, they form a new convective event. These findings imply that interactions between CPs may explain the initial stages of CSA.

AB - In radiative-convective equilibrium simulations, convective self-aggregation (CSA) is the spontaneous organization into segregated cloudy and cloud-free regions. Evidence exists for how CSA is stabilized, but how it arises favorably on large domains is not settled. Using large-eddy simulations, we link the spatial organization emerging from the interaction of cold pools (CPs) to CSA. We systematically weaken simulated rain evaporation to reduce maximal CP radii, R_{max}, and find reducing R_{max} causes CSA to occur earlier. We further identify a typical rain cell generation time and a minimum radius, R_{min}, around a given rain cell, within which the formation of subsequent rain cells is suppressed. Incorporating R_{min} and R_{max}, we propose a toy model that captures how CSA arises earlier on large domains: when two CPs of radii r_i,r_j ∈ [R_{min}, R_{max}] collide, they form a new convective event. These findings imply that interactions between CPs may explain the initial stages of CSA.

U2 - 10.1029/2021JD035331

DO - 10.1029/2021JD035331

M3 - Journal article

VL - 126

JO - Journal of Geophysical Research: Solid Earth

JF - Journal of Geophysical Research: Solid Earth

SN - 0148-0227

IS - 20

M1 - e2021JD035331

ER -

ID: 281669956