Influence of Superparameterization and a Higher-Order Turbulence Closure on Rainfall Bias Over Amazonia in Community Atmosphere Model Version 5
Journal Article
·
· Journal of Geophysical Research: Atmospheres
- Univ. of Texas, Austin, TX (United States)
- Univ. of Texas, Austin, TX (United States); Univ. of California, Los Angeles, CA (United States)
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
- Nanjing Univ. (China); Collaborative Innovation Center of Climate Change, Nanjing (China)
- Centro Nacional de Monitoramento e Alertas aos Desastres Naturais, São Jose dos Campos (Brazil)
In this work, we evaluate the Community Atmosphere Model Version 5 (CAM5) with a higher-order turbulence closure scheme, named Cloud Layers Unified By Binomials (CLUBB), and a Multiscale Modeling Framework (MMF) with two different microphysics configurations to investigate their influences on rainfall simulations over Southern Amazonia. The two different microphysics configurations in MMF are the one-moment cloud microphysics without aerosol treatment (SAM1MOM) and two-moment cloud microphysics coupled with aerosol treatment (SAM2MOM). Results show that both MMF-SAM2MOM and CLUBB effectively reduce the low biases of rainfall, mainly during the wet season. The CLUBB reduces low biases of humidity in the lower troposphere with further reduced shallow clouds. The latter enables more surface solar flux, leading to stronger convection and more rainfall. MMF, especially MMF-SAM2MOM, unstablizes the atmosphere with more moisture and higher atmospheric temperatures in the atmospheric boundary layer, allowing the growth of more extreme convection and further generating more deep convection. MMF-SAM2MOM significantly increases rainfall in the afternoon, but it does not reduce the early bias of the diurnal rainfall peak; LUBB, on the other hand, delays the afternoon peak time and produces more precipitation in the early morning, due to more realistic gradual transition between shallow and deep convection. MMF appears to be able to realistically capture the observed increase of relative humidity prior to deep convection, especially with its two-moment configuration. In contrast, in CAM5 and CAM5 with CLUBB, occurrence of deep convection in these models appears to be a result of stronger heating rather than higher relative humidity.
- Research Organization:
- Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
- Sponsoring Organization:
- Fundação de Amparo à Pesquisa do Estado do Amazonas (FAPEAM) (Brazil); National Natural Science Foundation of China (NSFC); São Paulo Research Foundation (FAPESP) (Brazil); USDOE Office of Science (SC)
- Grant/Contract Number:
- AC05-76RL01830; AC06-76RL01830; SC0011117
- OSTI ID:
- 1406792
- Alternate ID(s):
- OSTI ID: 1393718
- Report Number(s):
- PNNL-SA--123731; KP1703010; KP1703040
- Journal Information:
- Journal of Geophysical Research: Atmospheres, Journal Name: Journal of Geophysical Research: Atmospheres Journal Issue: 18 Vol. 122; ISSN 2169-897X
- Publisher:
- American Geophysical UnionCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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A multiscale modeling framework model (superparameterized CAM5) with a higher‐order turbulence closure: Model description and low‐cloud simulations
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OSTI ID:1295973