isolating the impact of height dependence on cumulus entrainment
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Isolating the Impact of Height Dependence on Cumulus Entrainment. Walter Hannah May 25 th , 2011. EAPSI. 8 week visit (10 weeks or Japan) Myong -In Lee at Ulsan National Institute of Science and Technology in South Korea. Relaxed Arakawa-Schubert. Problems. - PowerPoint PPT PresentationTRANSCRIPT
Isolating the Impact of Height Dependence onCumulus Entrainment
Walter Hannah
May 25th, 2011
EAPSI
• 8 week visit (10 weeks or Japan)• Myong-In Lee at Ulsan National Institute of
Science and Technology in South Korea
Relaxed Arakawa-SchubertAssume form of normalized mass flux
Calculate λ based on MSE profile
Estimate the cloud work-function (i.e. CAPE)
Calculate the cloud-base mass flux
Calculate large-scale tendencies
Problems• Most cumulus schemes based on the “entraining plume”
are not sensitive enough to the environmental conditions• Precipitation occurs too often• Precipitation occurs too early• Tropical wave and MJO variability is unrealistic
• These problems are typically addressed with arbitrary trigger conditions
• Environmental Humidity (Wang and Schlesinger, 1999)• Entrainment (Tokioka et al, 1988)• Large scale vertical velocity (Kain and Fritsch, 1992)• Cloud base height (Lee et al, 2008)• Precipitation evaporation (Sud and Walker, 1993)• Convective inhibition (Kain and Fritsch, 1992)
Chikira and Sugiyama (2010)• Closure based on kinetic energy instead of mass flux• Entrainment rate is assumed to be inversely related to
vertical velocity• Improved performance is credited to having large
entrainment at low levels
Gregory (2001) Neggers et al. (2002) Pan and Randall (1998)
Height Dependent Entrainment
• RAS constant entrainment
• RAS linear entrainment
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The Normalized Mass Flux
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Chikira’s Test Case
• Input profile calculated from TOGA-COARE– Precipitation rate > 20 mm/day
SCM Results: GATE
SCM Results: TOGA-COARE
Diurnal Cycle Application• Lee et al. (2007) showed that only certain
trigger mechanisms can significantly effect the diurnal timing of precipitation– Height of starting level
• Defined as level of maximum MSE within 300 hPa from the surface
– Convective inhibition• The LFC is constrained to be within 150 hPa from the
starting level for convection to activate
• Can modifying the cloud base entrainment have the same effect?
Lee et al. (2007)
Diurnal Cycle Application
Lee et al. (2007)
Is Height Dependence Realistic?• Romps (2010) presented a
method for a direct measure of entrainment rate in LES models
• Entrainment and detrainment are sources and sinks of cloud air
Romps (2010)• Entrainment rate was found not to vary
significantly with height
• Entrainment did not scale with vertical velocity or buoyancy
Romps (2010)Cloud air defined by
moisture onlyCloud air defined by
moisture and vertical velocity
Questions?
Suggestions?