the atmospheric boundary layer (abl) over mesoscale surface heterogeneity
DESCRIPTION
Research Review. The Atmospheric Boundary Layer (ABL) over Mesoscale Surface Heterogeneity. 25 June 2009 Song- Lak Kang. The ABL … . typically 1-2 km high. the lowest 10-20 % of the troposphere. directly influenced by the earth’s surface. Convective Boundary Layer. - PowerPoint PPT PresentationTRANSCRIPT
The Atmospheric Boundary Layer (ABL) over Mesoscale Surface Heterogeneity
25 June 2009Song-Lak Kang
Research Review
The ABL …
• typically 1-2 km high. • the lowest 10-20 % of the troposphere.• directly influenced by the earth’s surface.
Convective Boundary Layer
1700 MST ON 17 JUNE 2009
The sun’s ray heats the earth’s surface, which then heats and moistens the air above it.
Horizontally Homogeneous CBL
From Wyngaard (1990)
• Bottom-up (Surface heat and moisture fluxes) and• Top-down (entrainment from the free atmosphere) approaches.• The characteristic length scale of energy containing eddies is about height of the ABL
Mesoscale fluctuations in the CBL
Aircraft Observation at 33 m AGLFrom Mahrt et al. (1994)
Aircraft Observation at various levelsFrom LeMone et al. (2002)
Mesoscale and turbulent fluctuations coexist in the CBL
Does the spectral gap exists?
ln κ
ln E Mesoscale fluctuations
Turbulentfluctuations
Assumption of mesoscale modeling
Horizontal flows generated by mesoscale surface heat flux variation
U
7
Warm Cool
8
Horizontal flows generated by mesoscale surface heat flux variation
High-amplitude surface heat flux variation
Non-stationary flows
Low-amplitude surface heat flux variation
Quasi-stationary flows
w
zxu
tTemperature gradient increased
by divergence of vertical heat flux
w
zxu
tTemperature gradient reduced
by temperature advection
Why do the horizontal flows oscillate?Divergence of vertical heat flux .vs.
Temperature advection
9
Ramp event in wind power forecasting
The red solid lines represent observed wind speed and the blue solid lines wind power produced. From Cutler et al. (2007)
One of the most difficult issues that wind power forecasting system has encountered is a so-called ramp event. An unforeseen ramp event may be costly to balance the supply and demand of power and affect power system security (Cutler et al. 2007) .
The Ramp Event
Realistic surface heat flux variations
The diurnal cycle of surface heat flux variation
Multi-scale surface heat flux variation
Comparison of LES results with WRF results
Summary
• In the CBL, mesoscale horizontal flows generated by differential heating may temporally fluctuate.
• The temporal fluctuations are suggested as one of the reasons to cause the ramp event in horizontal wind speed.
• With more realistic conditions, LES experiments are being performed.
• The LES results are being compared with WRF results in order to improve the performance of wind power forecasting.