skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Skill of ship‐following large‐eddy simulations in reproducing MAGIC observations across the northeast P acific stratocumulus to cumulus transition region

Journal Article · · Journal of Advances in Modeling Earth Systems
DOI:https://doi.org/10.1002/2017MS000924· OSTI ID:1351638

Abstract During the Marine ARM GPCI Investigation of Clouds (MAGIC) in October 2011 to September 2012, a container ship making periodic cruises between Los Angeles, CA, and Honolulu, HI, was instrumented with surface meteorological, aerosol and radiation instruments, a cloud radar and ceilometer, and radiosondes. Here large‐eddy simulation (LES) is performed in a ship‐following frame of reference for 13 four day transects from the MAGIC field campaign. The goal is to assess if LES can skillfully simulate the broad range of observed cloud characteristics and boundary layer structure across the subtropical stratocumulus to cumulus transition region sampled during different seasons and meteorological conditions. Results from Leg 15A, which sampled a particularly well‐defined stratocumulus to cumulus transition, demonstrate the approach. The LES reproduces the observed timing of decoupling and transition from stratocumulus to cumulus and matches the observed evolution of boundary layer structure, cloud fraction, liquid water path, and precipitation statistics remarkably well. Considering the simulations of all 13 cruises, the LES skillfully simulates the mean diurnal variation of key measured quantities, including liquid water path (LWP), cloud fraction, measures of decoupling, and cloud radar‐derived precipitation. The daily mean quantities are well represented, and daily mean LWP and cloud fraction show the expected correlation with estimated inversion strength. There is a −0.6 K low bias in LES near‐surface air temperature that results in a high bias of 5.6 W m −2 in sensible heat flux (SHF). Overall, these results build confidence in the ability of LES to represent the northeast Pacific stratocumulus to trade cumulus transition region.

Research Organization:
Univ. of Washington, Seattle, WA (United States)
Sponsoring Organization:
USDOE Office of Science (SC)
Grant/Contract Number:
DE‐SC0011602; SC0011602
OSTI ID:
1351638
Alternate ID(s):
OSTI ID: 1351640; OSTI ID: 1393515
Journal Information:
Journal of Advances in Modeling Earth Systems, Journal Name: Journal of Advances in Modeling Earth Systems Vol. 9 Journal Issue: 2; ISSN 1942-2466
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 26 works
Citation information provided by
Web of Science

References (27)

A Multipurpose Radar Simulation Package: QuickBeam journal November 2007
Cloud Resolving Modeling of the ARM Summer 1997 IOP: Model Formulation, Results, Uncertainties, and Sensitivities journal February 2003
Clouds, Precipitation, and Marine Boundary Layer Structure during the MAGIC Field Campaign journal March 2015
On the Structure of the Lower Troposphere in the Summertime Stratocumulus Regime of the Northeast Pacific journal March 2007
Confronting Models with Data: The GEWEX Cloud Systems Study: The GEWEX Cloud Systems Study journal April 2003
Methods for determining the height of the atmospheric boundary layer report February 1999
The Seasonal Cycle of Low Stratiform Clouds journal August 1993
On the Relationship between Stratiform Low Cloud Cover and Lower-Tropospheric Stability journal December 2006
Large-eddy simulation of the transient and near-equilibrium behavior of precipitating shallow convection: LES OF PRECIPITATING SHALLOW CONVECTION journal December 2015
Coupled vs. decoupled boundary layers in VOCALS-REx journal January 2011
Determining the Susceptibility of Cloud Albedo to Changes in Droplet Concentration with the Advanced Very High Resolution Radiometer journal March 1994
A New Double-Moment Microphysics Parameterization for Application in Cloud and Climate Models. Part I: Description journal June 2005
Assessment of MODIS cloud effective radius and optical thickness retrievals over the Southeast Pacific with VOCALS-REx in situ measurements: MODIS VALIDATION DURING VOCALS-REx journal December 2011
Evaluation of Large-Eddy Simulations via Observations of Nocturnal Marine Stratocumulus journal June 2005
Marine low cloud sensitivity to an idealized climate change: The CGILS LES intercomparison: CGILS LES Intercomparison journal May 2013
Steady-State Large-Eddy Simulations to Study the Stratocumulus to Shallow Cumulus Cloud Transition journal November 2012
Large-Eddy Simulations of EUCLIPSE–GASS Lagrangian Stratocumulus-to-Cumulus Transitions: Mean State, Turbulence, and Decoupling journal June 2016
A comparison of cloud-resolving model simulations of trade wind cumulus with aircraft observations taken during RICO journal January 2007
Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave journal July 1997
Aerosol variability, synoptic-scale processes, and their link to the cloud microphysics over the northeast Pacific during MAGIC: NE PACIFIC CCN AND CLOUD MICROPHYSICS journal May 2015
On the Fidelity of Large-Eddy Simulation of Shallow Precipitating Cumulus Convection journal September 2011
On the Factors Modulating the Stratocumulus to Cumulus Transitions journal September 2011
On the Relationships among Low-Cloud Structure, Sea Surface Temperature, and Atmospheric Circulation in the Summertime Northeast Pacific journal May 1995
The Epic 2001 Stratocumulus Study journal July 2004
The role of precipitation and spatial organization in the response of trade-wind clouds to warming: WARMING RESPONSE OF SHALLOW CONVECTION journal June 2016
The GASS/EUCLIPSE model intercomparison of the stratocumulus transition as observed during ASTEX: LES results: Astex SCU Transition-LES Results journal July 2013
Cloud Modeling Tests of the ULTIMATE–MACHO Scalar Advection Scheme journal October 2011