The impact of the ice phase and radiation on a midlatitude squall line system

Journal Article · Tue Nov 15 04:00:00 EST 1994 · Journal of the Atmospheric Sciences

DOI:https://doi.org/10.1175/1520-0469(1994)051<3320:TIOTIP>2.0.CO;2· OSTI ID:57005

Chin, Hung-Neng S ^[1]

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1. Lawrence Livermore National Lab., CA (United States)

A two-dimensional cloud model is used to study the interrelationships among cloud microphysics, radiation, and dynamics in a midlatitude broken-line squall system. The impact of the ice phase, longwave and shortwave radiation on the dynamic and microphysical structures of this multicellular storm, the thermodynamic properties of the cloud ensemble, and their cloud-radiative feedback to the modeled squall line system is investigated in detail. In addition, partitioned heat, moisture, and water budgets are used to assess quantitatively the role of anvil clouds on the modeled squall line system. The major conclusions are as follows. (1) Both ice phase and radiation have little influence on the multicellular characters of the modeled squall line system. (2) The development of rear inflow in the modeled squall line system is attributed to the upshear tilt of the convective system. (3) For this type of squall line system, the ice phase and radiation do not considerably change the heating and drying profiles of the cloud ensemble (10% {approximately} 20% difference in the maximum heating and drying). (4) Horizontal transport of hydrometeors from deep convection is the primary source ({approximately} 2/3) of the water budget for anvil clouds in ice simulations; the rest ({approximately} 1/3) is contributed by the mesoscale lifting associated with the tilting convective system. (5) Longwave optical properties of anvils are insensitive to the ice phase. However, the ice phase can significantly impact shortwave optical properties of anvils. (6) Model simulations imply that the feedback of anvil clouds to the large-scale system is most likely dominated by radiative processes. Owing to the large coverage of convectively generated anvil clouds, the present study suggests that the missing physics of cumulus-anvil interactions in general circulation models may result in an underestimated cloud albedo and an overestimated surface insolation. 69 refs., 20 figs., 4 tabs.

• DOE Contract Number: W-7405-ENG-48
• OSTI ID: 57005
• Journal Information: Journal of the Atmospheric Sciences, Journal Name: Journal of the Atmospheric Sciences Journal Issue: 22 Vol. 51; ISSN 0022-4928; ISSN JAHSAK
• Country of Publication: United States
• Language: English

Related Subjects

54 ENVIRONMENTAL SCIENCES
CLOUDS
COUPLING
FEEDBACK
ICE
SOLAR RADIATION
STORMS