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

Title: Updraft Width Modulates Ambient Atmospheric Controls on Convective Cloud Depth

Journal Article · · Journal of Geophysical Research. Atmospheres

The depth of convective clouds affects vertical transport of atmospheric constituents, influencing downstream weather and climate. Atmospheric controls on the maximum depth reached by moist convection are investigated with radar-tracked convective cells tagged with sounding-derived atmospheric parameters from a field campaign in central Argentina. Regression analyses show that narrow (<12-km diameter) and wide (>16-km diameter) cell depths respond to disparate factors, where cell areas are defined using composite reflectivity signatures. Undiluted lifted parcel indices including convective available potential energy (CAPE) and level of neutral buoyancy (LNB) are top predictors of wide cell maximum depth while mid-tropospheric relative humidity is the top predictor of narrow cell maximum depth. Because narrow cells are more numerous than wide cells, the overall outcome of the full cell population does not strongly correlate with CAPE and LNB conditions. Tracked cells and atmospheric conditions in a simulation with 3-km grid spacing covering the field campaign produce similar results to those observed. Narrow cells that are relatively deep have a cooler and moister mid-troposphere with weaker free tropospheric subsidence, while relatively deep wide cells have much warmer and moister lower tropospheric conditions. These atmospheric differences are present 1 hr before cell initiation at both a fixed observing site and variable cell initiation locations. Simulated narrow cell maximum equivalent potential temperature decreases with height at a rate similar to the ambient vertical gradient, causing these cells to fall short of their LNB and supporting the view that entrainment-driven dilution is a dominant control on their depth.

Research Organization:
Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
Sponsoring Organization:
USDOE; USDOE Office of Science (SC), Basic Energy Sciences (BES). Scientific User Facilities (SUF); USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
AC02-05CH11231; AC05-76RL01830
OSTI ID:
2479797
Report Number(s):
PNNL-SA--199356
Journal Information:
Journal of Geophysical Research. Atmospheres, Journal Name: Journal of Geophysical Research. Atmospheres Journal Issue: 23 Vol. 129; ISSN 2169-897X
Publisher:
American Geophysical Union; WileyCopyright Statement
Country of Publication:
United States
Language:
English

References (59)

Evaluation of cloud-resolving and limited area model intercomparison simulations using TWP-ICE observations: 1. Deep convective updraft properties: Eval. of TWP-ICE CRMs and LAMs Pt. 1 journal December 2014
The relative influence of environmental characteristics on tropical deep convective morphology as observed by CloudSat: MORPHOLOGICAL SENSITIVITY TO ENVIRONMENT journal May 2015
Transport of chemical tracers from the boundary layer to stratosphere associated with the dynamics of the Asian summer monsoon: CHEMICAL TRANSPORT BY THE ASIAN MONSOON journal December 2016
Linear theory of shallow convection in deep, vertically sheared atmospheres journal August 2019
On the sensitivity of deep‐convection initiation to horizontal grid resolution journal January 2020
The ERA5 global reanalysis journal June 2020
Organized Convective Systems: Archetypal Dynamical Models, Mass and Momentum Flux Theory, and Parametrization journal July 1992
An Integrated View of the 1987 Australian Monsoon and Its Mesoscale Convective Systems. I: Horizontal Structure journal July 1992
Sources and distributions of dust aerosols simulated with the GOCART model journal September 2001
Moisture plumes above thunderstorm anvils and their contributions to cross‐tropopause transport of water vapor in midlatitudes journal March 2003
Factors responsible for the vertical development of tropical oceanic cumulus convection: FACTORS FOR TROPICAL CUMULUS DEVELOPMENT journal June 2004
Effect of convection on the summertime extratropical lower stratosphere journal December 2004
Radiative forcing by long-lived greenhouse gases: Calculations with the AER radiative transfer models journal January 2008
Where is the level of neutral buoyancy for deep convection?: LNB FOR DEEP CONVECTION journal August 2012
The Relationship of Cloud Number and Size With Their Large‐Scale Environment in Deep Tropical Convection journal August 2019
Updraft and Downdraft Core Size and Intensity as Revealed by Radar Wind Profilers: MCS Observations and Idealized Model Comparisons journal June 2020
Revisiting the Entrainment Relationship of Convective Plumes: A Perspective From Global Observations journal March 2021
An Observational Comparison of Level of Neutral Buoyancy and Level of Maximum Detrainment in Tropical Deep Convective Clouds journal August 2020
Interpreting the Diurnal Cycle of Clouds and Precipitation in the ARM GoAmazon Observations: Shallow to Deep Convection Transition journal March 2021
The Relation of Environmental Conditions With Charge Structure in Central Argentina Thunderstorms journal May 2022
How Does LCL Height Influence Deep Convective Updraft Width? journal July 2021
Invigoration or Enervation of Convective Clouds by Aerosols? journal August 2021
Revisiting the Land‐Ocean Contrasts in Deep Convective Cloud Intensity Using Global Satellite Observations journal March 2023
Peak Rain Rate Sensitivity to Observed Cloud Condensation Nuclei and Turbulence in Continental Warm Shallow Clouds During CACTI journal August 2022
Entrainment Makes Pollution More Likely to Weaken Deep Convective Updrafts Than Invigorate Them journal June 2023
The Effects of Shallow Cumulus Cloud Shape on Interactions Among Clouds and Mixing With Near‐Cloud Environments journal December 2023
Dependencies of Simulated Convective Cell and System Growth Biases on Atmospheric Instability and Model Resolution journal November 2024
Sensitivity of organized convective storms to model grid spacing in current and future climates
  • Prein, A. F.; Rasmussen, R. M.; Wang, D.
  • Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, Vol. 379, Issue 2195 https://doi.org/10.1098/rsta.2019.0546
journal March 2021
Retrieving Liquid Wat0er Path and Precipitable Water Vapor From the Atmospheric Radiation Measurement (ARM) Microwave Radiometers journal November 2007
Global Cloud Detection for CERES Edition 4 Using Terra and Aqua MODIS Data journal November 2019
CERES MODIS Cloud Product Retrievals for Edition 4--Part I: Algorithm Changes journal January 2020
CERES MODIS Cloud Product Retrievals for Edition 4—Part II: Comparisons to CloudSat and CALIPSO journal May 2021
The future of Earth system prediction: Advances in model-data fusion journal April 2022
Thunderstorms: An Important Mechanism in the Transport of Air Pollutants journal January 1987
Equivalent Radar Reflectivity Factors for Snow and Ice Particles journal August 1984
Variability of Midtropospheric Moisture and Its Effect on Cloud-Top Height Distribution during TOGA COARE* journal December 1997
What Controls the Transition from Shallow to Deep Convection? journal June 2009
Mechanisms Affecting the Transition from Shallow to Deep Convection over Land: Inferences from Observations of the Diurnal Cycle Collected at the ARM Southern Great Plains Site journal September 2010
Cloud-Resolving Simulations of Deep Convection over a Heated Mountain journal February 2011
Life Cycle of Numerically Simulated Shallow Cumulus Clouds. Part II: Mixing Dynamics journal May 2005
The Structure of Thermals in Cumulus from Airborne Dual-Doppler Radar Observations journal May 2006
A Mass-Flux Scheme View of a High-Resolution Simulation of a Transition from Shallow to Deep Cumulus Convection journal July 2006
High-Resolution Simulation of Shallow-to-Deep Convection Transition over Land journal December 2006
Slippery Thermals and the Cumulus Entrainment Paradox* journal August 2013
Observations of Convection Initiation “Failure” from the 12 June 2002 IHOP Deployment journal January 2006
The Sensitivity of Convective Initiation to the Lapse Rate of the Active Cloud-Bearing Layer journal September 2007
Sensitivity of a Simulated Squall Line to Horizontal Resolution and Parameterization of Microphysics journal January 2012
Sensitivity of moist convection to environmental humidity journal October 2004
The role of stability and moisture in the diurnal cycle of convection over land
  • Chaboureau, J. -P.; Guichard, F.; Redelsperger, J. -L.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 130, Issue 604 https://doi.org/10.1256/qj.03.132
journal October 2004
A study of thermals in cumulus clouds
  • Blyth, Alan M.; Lasher-Trapp, Sonia G.; Cooper, William A.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 131, Issue 607 https://doi.org/10.1256/qj.03.180
journal April 2005
Daytime convective development over land: A model intercomparison based on LBA observations journal January 2006
Development of an Improved Turbulence Closure Model for the Atmospheric Boundary Layer journal January 2009
Interpolated Sounding and Gridded Sounding Value-Added Products report September 2021
MWRRET Value-Added Product: The Retrieval of Liquid Water Path and Precipitable Water Vapor from Microwave Radiometer (MWR) Data Sets report July 2011
Raindrop Size Spectrum in Deep Convective Regions of the Americas journal July 2021
Microphysical and Kinematic Characteristics of Anomalous Charge Structure Thunderstorms in Cordoba, Argentina journal August 2022
Drop Size Distribution Variability in Central Argentina during RELAMPAGO-CACTI journal May 2021
Data and Code for "Updraft Width Modulates Ambient Atmospheric Controls on Convective Cloud Depth" by Varble et al. (2024) dataset January 2024
The Python ARM Radar Toolkit (Py-ART), a Library for Working with Weather Radar Data in the Python Programming Language journal July 2016