DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Effects of a Simple Convective Organization Scheme in a Two‐Plume GCM

Abstract

Abstract A set of experiments is described with the Community Atmosphere Model (CAM5) using a two‐plume convection scheme. To represent the differences of organized convection from General Circulation Model (GCM) assumptions of isolated plumes in uniform environments, a dimensionless prognostic “organization” tracer Ω is invoked to lend the second plume a buoyancy advantage relative to the first, as described in Mapes and Neale (2016). When low‐entrainment plumes are unconditionally available (Ω = 1 everywhere), deep convection occurs too easily, with consequences including premature (upstream) rainfall in inflows to the deep tropics, excessive convective versus large‐scale rainfall, poor relationships to the vapor field, stable bias in the mean state, weak and poor tropical variability, and midday peak in diurnal rainfall over land. Some of these are shown to also be characteristic of CAM4 with its separated deep and shallow convection schemes. When low‐entrainment plumes are forbidden by setting Ω = 0 everywhere, some opposite problems can be discerned. In between those extreme cases, an interactive Ω driven by the evaporation of precipitation acts as a local positive feedback loop, concentrating deep convection: In areas of little recent rain, only highly entraining plumes can occur, unfavorable for rain production. This tunable mechanism steadily increases precipitation variancemore » in both space and time, as illustrated here with maps, time‐longitude series, and spectra, while avoiding some mean state biases as illustrated with process‐oriented diagnostics such as conserved variable profiles and vapor‐binned precipitation curves.« less

Authors:
ORCiD logo [1]; ORCiD logo [2]
  1. Department of Mathematics and Statistics Texas A&,M University at Corpus Christi Corpus Christi TX USA
  2. Rosenstiel School of Marine and Atmospheric Sciences University of Miami Miami FL USA
Publication Date:
Research Org.:
Univ. of Miami, FL (United States); Texas A & M Univ., Corpus Christi, TX (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER); Office of Naval Research (ONR) (United States)
OSTI Identifier:
1430570
Alternate Identifier(s):
OSTI ID: 1430572; OSTI ID: 1511568
Grant/Contract Number:  
DE‐SC0000823; DE‐SC0006806; SC0000823; SC0006806; N000141310704
Resource Type:
Published Article
Journal Name:
Journal of Advances in Modeling Earth Systems
Additional Journal Information:
Journal Name: Journal of Advances in Modeling Earth Systems Journal Volume: 10 Journal Issue: 3; Journal ID: ISSN 1942-2466
Publisher:
American Geophysical Union (AGU)
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; parameterization of convective organization; evaporation of precipitation; entrainment rate; mean state bias; variability

Citation Formats

Chen, Baohua, and Mapes, Brian E. Effects of a Simple Convective Organization Scheme in a Two‐Plume GCM. United States: N. p., 2018. Web. doi:10.1002/2017MS001106.
Chen, Baohua, & Mapes, Brian E. Effects of a Simple Convective Organization Scheme in a Two‐Plume GCM. United States. https://doi.org/10.1002/2017MS001106
Chen, Baohua, and Mapes, Brian E. Fri . "Effects of a Simple Convective Organization Scheme in a Two‐Plume GCM". United States. https://doi.org/10.1002/2017MS001106.
@article{osti_1430570,
title = {Effects of a Simple Convective Organization Scheme in a Two‐Plume GCM},
author = {Chen, Baohua and Mapes, Brian E.},
abstractNote = {Abstract A set of experiments is described with the Community Atmosphere Model (CAM5) using a two‐plume convection scheme. To represent the differences of organized convection from General Circulation Model (GCM) assumptions of isolated plumes in uniform environments, a dimensionless prognostic “organization” tracer Ω is invoked to lend the second plume a buoyancy advantage relative to the first, as described in Mapes and Neale (2016). When low‐entrainment plumes are unconditionally available (Ω = 1 everywhere), deep convection occurs too easily, with consequences including premature (upstream) rainfall in inflows to the deep tropics, excessive convective versus large‐scale rainfall, poor relationships to the vapor field, stable bias in the mean state, weak and poor tropical variability, and midday peak in diurnal rainfall over land. Some of these are shown to also be characteristic of CAM4 with its separated deep and shallow convection schemes. When low‐entrainment plumes are forbidden by setting Ω = 0 everywhere, some opposite problems can be discerned. In between those extreme cases, an interactive Ω driven by the evaporation of precipitation acts as a local positive feedback loop, concentrating deep convection: In areas of little recent rain, only highly entraining plumes can occur, unfavorable for rain production. This tunable mechanism steadily increases precipitation variance in both space and time, as illustrated here with maps, time‐longitude series, and spectra, while avoiding some mean state biases as illustrated with process‐oriented diagnostics such as conserved variable profiles and vapor‐binned precipitation curves.},
doi = {10.1002/2017MS001106},
journal = {Journal of Advances in Modeling Earth Systems},
number = 3,
volume = 10,
place = {United States},
year = {Fri Mar 30 00:00:00 EDT 2018},
month = {Fri Mar 30 00:00:00 EDT 2018}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
https://doi.org/10.1002/2017MS001106

Citation Metrics:
Cited by: 12 works
Citation information provided by
Web of Science

Save / Share:

Works referenced in this record:

Moisture Vertical Structure, Column Water Vapor, and Tropical Deep Convection
journal, June 2009

  • Holloway, Christopher E.; Neelin, J. David
  • Journal of the Atmospheric Sciences, Vol. 66, Issue 6
  • DOI: 10.1175/2008JAS2806.1

The Impacts of Convective Parameterization and Moisture Triggering on AGCM-Simulated Convectively Coupled Equatorial Waves
journal, March 2008


A cumulus parameterization with a prognostic closure
journal, April 1998

  • Pan, Dzong-Ming; Randall, Davi D. A.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 124, Issue 547
  • DOI: 10.1002/qj.49712454714

Parameterization of the Vertical Velocity Equation for Shallow Cumulus Clouds
journal, August 2012

  • de Roode, Stephan R.; Siebesma, A. Pier; Jonker, Harm J. J.
  • Monthly Weather Review, Vol. 140, Issue 8
  • DOI: 10.1175/MWR-D-11-00277.1

Critical Roles of the Stratiform Rainfall in Sustaining the Madden–Julian Oscillation: GCM Experiments
journal, July 2009


High-Resolution Simulation of Shallow-to-Deep Convection Transition over Land
journal, December 2006

  • Khairoutdinov, Marat; Randall, David
  • Journal of the Atmospheric Sciences, Vol. 63, Issue 12
  • DOI: 10.1175/JAS3810.1

Rain-Profiling Algorithm for the TRMM Precipitation Radar
journal, December 2000


The evolution of the tropical western Pacific atmosphere-ocean system following the arrival of a dry intrusion
journal, January 2000

  • Parsons, David B.; Redelsperger, Jean-Luc; Yoneyama, Kunio
  • Quarterly Journal of the Royal Meteorological Society, Vol. 126, Issue 563
  • DOI: 10.1002/qj.49712656307

Thermodynamic control of tropical rainfall
journal, April 2000

  • Raymond, D. J.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 126, Issue 564
  • DOI: 10.1002/qj.49712656406

The Tropical Dynamical Response to Latent Heating Estimates Derived from the TRMM Precipitation Radar
journal, June 2004


Intraseasonal oscillations in 15 atmospheric general circulation models: results from an AMIP diagnostic subproject
journal, April 1996

  • Slingo, J. M.; Sperber, K. R.; Boyle, J. S.
  • Climate Dynamics, Vol. 12, Issue 5
  • DOI: 10.1007/BF00231106

Global Precipitation: A 17-Year Monthly Analysis Based on Gauge Observations, Satellite Estimates, and Numerical Model Outputs
journal, November 1997


Convectively coupled equatorial waves
journal, January 2009

  • Kiladis, George N.; Wheeler, Matthew C.; Haertel, Patrick T.
  • Reviews of Geophysics, Vol. 47, Issue 2
  • DOI: 10.1029/2008RG000266

Process-Oriented MJO Simulation Diagnostic: Moisture Sensitivity of Simulated Convection
journal, July 2014


A Unified Convection Scheme (UNICON). Part I: Formulation
journal, November 2014


Large-eddy simulation of organized precipitating trade wind cumulus clouds
journal, January 2013


The Role of Convective Moistening in the Madden–Julian Oscillation
journal, November 2009

  • Thayer-Calder, Katherine; Randall, David A.
  • Journal of the Atmospheric Sciences, Vol. 66, Issue 11
  • DOI: 10.1175/2009JAS3081.1

Rain Reevaporation, Boundary Layer–Convection Interactions, and Pacific Rainfall Patterns in an AGCM
journal, December 2006

  • Bacmeister, Julio T.; Suarez, Max J.; Robertson, Franklin R.
  • Journal of the Atmospheric Sciences, Vol. 63, Issue 12
  • DOI: 10.1175/JAS3791.1

Sensitivity of moist convection to environmental humidity
journal, October 2004

  • Derbyshire, S. H.; Beau, I.; Bechtold, P.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 130, Issue 604
  • DOI: 10.1256/qj.03.130

A Unified Convection Scheme (UNICON). Part II: Simulation
journal, November 2014


Precipitation Characteristics in Eighteen Coupled Climate Models
journal, September 2006


Structure and Dynamics of a Tropical Squall–Line System
journal, December 1977


Recovery Processes and Factors Limiting Cloud-Top Height following the Arrival of a Dry Intrusion Observed during TOGA COARE
journal, August 2002


Evaluating Boundary Layer–Based Mass Flux Closures Using Cloud-Resolving Model Simulations of Deep Convection
journal, July 2010

  • Fletcher, Jennifer K.; Bretherton, Christopher S.
  • Journal of the Atmospheric Sciences, Vol. 67, Issue 7
  • DOI: 10.1175/2010JAS3328.1

Parameterizing Convective Organization to Escape the Entrainment Dilemma: PARAMETERIZING CONVECTIVE ORGANIZATION
journal, February 2011

  • Mapes, Brian; Neale, Richard
  • Journal of Advances in Modeling Earth Systems, Vol. 3, Issue 2
  • DOI: 10.1029/2011MS000042

A Cumulus Parameterization Including Mass Fluxes, Vertical Momentum Dynamics, and Mesoscale Effects
journal, March 1993


Gravity Waves, Compensating Subsidence and Detrainment around Cumulus Clouds
journal, March 1989


Uncertainties in the Rain Profiling Algorithm for the TRMM Precipitation Radar
journal, January 2009

  • Iguchi, Toshio; Kozu, Toshiaki; Kwiatkowski, John
  • Journal of the Meteorological Society of Japan, Vol. 87A
  • DOI: 10.2151/jmsj.87A.1

Representing the Sensitivity of Convective Cloud Systems to Tropospheric Humidity in General Circulation Models
journal, September 2011


Tropical Intraseasonal Variability in 14 IPCC AR4 Climate Models. Part I: Convective Signals
journal, June 2006

  • Lin, Jia-Lin; Kiladis, George N.; Mapes, Brian E.
  • Journal of Climate, Vol. 19, Issue 12
  • DOI: 10.1175/JCLI3735.1

The ERA-Interim reanalysis: configuration and performance of the data assimilation system
journal, April 2011

  • Dee, D. P.; Uppala, S. M.; Simmons, A. J.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 137, Issue 656
  • DOI: 10.1002/qj.828

Factors for the Simulation of Convectively Coupled Kelvin Waves
journal, May 2012


The Cumulus Parameterization Problem: Past, Present, and Future
journal, July 2004


Impacts of Cumulus Convection Parameterization on Aqua-planet AGCM Simulations of Tropical Intraseasonal Variability
journal, January 2003

  • Lee¹, Myong-In; Kang, In-Sik; Mapes, Brian E.
  • Journal of the Meteorological Society of Japan, Vol. 81, Issue 5
  • DOI: 10.2151/jmsj.81.963

Understanding advances in the simulation of intraseasonal variability in the ECMWF model. Part I: The representation of the MJO
journal, November 2012

  • Hirons, L. C.; Inness, P.; Vitart, F.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 139, Issue 675
  • DOI: 10.1002/qj.2060

Analyzing the Climate Sensitivity of the HadSM3 Climate Model Using Ensembles from Different but Related Experiments
journal, July 2009

  • Rougier, Jonathan; Sexton, David M. H.; Murphy, James M.
  • Journal of Climate, Vol. 22, Issue 13
  • DOI: 10.1175/2008JCLI2533.1

A Mass-Flux Scheme View of a High-Resolution Simulation of a Transition from Shallow to Deep Cumulus Convection
journal, July 2006

  • Kuang, Zhiming; Bretherton, Christopher S.
  • Journal of the Atmospheric Sciences, Vol. 63, Issue 7
  • DOI: 10.1175/JAS3723.1