Deep moist atmospheric convection in a subkilometer global simulation

Deep moist atmospheric convection is a key element of the weather and climate system for transporting mass, momentum, and thermal energy. It has been challenging to simulate convection realistically in global atmospheric models because of the large gap in spatial scales between convection (100 km) a...

Full description

Saved in:
Bibliographic Details
Published inGeophysical research letters Vol. 40; no. 18; pp. 4922 - 4926
Main Authors Miyamoto, Yoshiaki, Kajikawa, Yoshiyuki, Yoshida, Ryuji, Yamaura, Tsuyoshi, Yashiro, Hisashi, Tomita, Hirofumi
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 28.09.2013
American Geophysical Union
John Wiley & Sons, Inc
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Deep moist atmospheric convection is a key element of the weather and climate system for transporting mass, momentum, and thermal energy. It has been challenging to simulate convection realistically in global atmospheric models because of the large gap in spatial scales between convection (100 km) and global motions (104 km). We conducted the first ever subkilometer global simulation and described the features of convection. Through a series of grid‐refinement resolution testing, we found that an essential change for convection statistics occurred around 2 km grid spacing. The convection structure, number of convective cells, and distance to the nearest convective cell dramatically changed at this resolution. The convection core was resolved using multiple grids in simulations with grid spacings less than 2.0 km. Key Points Subkilometer global simulation is first successfully conductedThe global features of deep moist convection are presentedThe necessary resolution for simulating convection in global models is 2 km
Bibliography:ArticleID:GRL50944
Supporting InformationSupporting Information
istex:7A6E0F6DF7D2FE3D48ED4BDF71B111B3F0662F0F
ark:/67375/WNG-CNN6QC56-L
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1002/grl.50944