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

Title: Impact of Resolution on Simulation of Closed Mesoscale Cellular Convection Identified by Dynamically Guided Watershed Segmentation

Journal Article · · Journal of Geophysical Research - Atmospheres
DOI:https://doi.org/10.1002/2014JD021962· OSTI ID:1166683
 [1];  [1];  [1];  [1]
  1. Pacific Northwest National Lab. (PNNL), Richland, WA (United States)

Organized mesoscale cellular convection (MCC) is a common feature of marine stratocumulus that forms in response to a balance between mesoscale dynamics and smaller scale processes such as cloud radiative cooling and microphysics. We use the Weather Research and Forecasting model with chemistry (WRF-Chem) and fully coupled cloud-aerosol interactions to simulate marine low clouds during the VOCALS-REx campaign over the southeast Pacific. A suite of experiments with 3- and 9-km grid spacing indicates resolution-dependent behavior. The simulations with finer grid spacing have smaller liquid water paths and cloud fractions, while cloud tops are higher. The observed diurnal cycle is reasonably well simulated. To isolate organized MCC characteristics we develop a new automated method, which uses a variation of the watershed segmentation technique that combines the detection of cloud boundaries with a test for coincident vertical velocity characteristics. This ensures that the detected cloud fields are dynamically consistent for closed MCC, the most common MCC type over the VOCALS-REx region. We demonstrate that the 3-km simulation is able to reproduce the scaling between horizontal cell size and boundary layer height seen in satellite observations. However, the 9-km simulation is unable to resolve smaller circulations corresponding to shallower boundary layers, instead producing invariant MCC horizontal scale for all simulated boundary layers depths. The results imply that climate models with grid spacing of roughly 3 km or smaller may be needed to properly simulate the MCC structure in the marine stratocumulus regions.

Research Organization:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC05-76RL01830
OSTI ID:
1166683
Report Number(s):
PNNL-SA-102353; 400402000
Journal Information:
Journal of Geophysical Research - Atmospheres, Vol. 119, Issue 22; ISSN 0747-7309
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English

Similar Records

Assessing regional scale predictions of aerosols, marine stratocumulus, and their interactions during VOCALS-REx using WRF-Chem
Journal Article · Fri Dec 02 00:00:00 EST 2011 · Atmospheric Chemistry and Physics · OSTI ID:1166683

Surface-based observations of mesoscale cumulus-stratocumulus interaction during ASTEX
Journal Article · Tue Aug 15 00:00:00 EDT 1995 · Journal of the Atmospheric Sciences · OSTI ID:1166683

Assessing regional scale predictions of aerosols, marine stratocumulus, and their interactions during VOCALS-REx using WRF-Chem
Journal Article · Fri Dec 02 00:00:00 EST 2011 · Atmospheric Chemistry and Physics · OSTI ID:1166683

Related Subjects