the impact of mesoscale pbl parameterizations on the evolution of mixed-layer processes important...
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The impact of mesoscale PBL parameterizations
on the evolution of mixed-layer processes important for fire weather
Joseph J. CharneyUSDA Forest Service, Northern Research Station, East Lansing, MI
Daniel KeyserDepartment of Atmospheric and Environmental Sciences, University at
Albany, Albany, NY
1. Background
2. WRF model configuration
3. Double Trouble State Park (DTSP) wildfire case study
4. Summary and future work
Organization
• Mesoscale models are important tools for fire-weather forecasting and research applications.
• The surface-based mixed layer can profoundly influence fire–atmosphere interactions.
• Mixed-layer profiles of temperature, moisture, and wind strongly affect the evolution of a wildland fire.
• Mixed-layer processes are incorporated into mesoscale models through the planetary boundary layer (PBL) parameterization scheme.
Background
• WRF version 3.1
• 4 km nested grid
• 51 sigma levels, with 21 levels in the lowest 2000 m
• NARR data used for initial and boundary conditions
• Noah land-surface model
• RRTM radiation scheme
• MRF, YSU, MYJ, MYNN PBL schemes
WRF model configuration
PBL schemes
• MRF (Hong and Pan 1996): MRF PBL; predecessor to YSU scheme with implicit treatment of entrainment layer.
• YSU (Hong et al. 2006): update of MRF scheme; explicit entrainment layer, reduced mixing in high wind regimes, more realistic diurnal PBL growth.
• MYJ (Janjić 1990, 1994): TKE-based PBL prediction scheme used in Eta and MM5 models; Mellor–Yamada level 2.5 turbulence closure and local vertical mixing.
• MYNN (Nakanishi and Niino 2004): update to the MYJ scheme; deeper mixed layer, better representation of vertical moisture gradients.
WRF model configuration
Surface physics schemes
• MRF: MM5 similarity scheme
• YSU: MM5 similarity scheme
• MYJ: Eta similarity scheme
• MYNN: updated version of Eta similarity scheme
WRF model configuration
Surface physics schemes
• Simulations with the MYNN PBL scheme were rerun using the surface physics schemes for the MRF, YSU, and MYJ PBL schemes.
• Changing the surface physics scheme results in relatively minor differences compared with the differences that arise from changing the PBL scheme.
WRF model configuration
DTSP wildfire case study
DTSP wildfire event
• Occurred on 2 June 2002 in east-central NJ• An abandoned campfire grew into a major wildfire by
1800 UTC• Burned 1,300 acres• Forced closure of the Garden State Parkway• Damaged or destroyed 36 homes and outbuildings• Directly threatened over 200 homes• Forced evacuation of 500 homes• Caused ~$400,000 in property damage
DTSP wildfire event
Fire location
OKXupper air station
KWRI surface station
New Brunswick wind profiler
DTSP wildfire observations
Observed skew T–log p sounding at Upton, NY (OKX), valid at 0000 UTC 3 June 2002
Simulated skew T–log p sounding at OKX valid at 0000 UTC 3 June 2002
MRF
DTSP wildfire simulationsWRF simulations initialized at 1200 UTC 1 June 2002
Wind profiler observations at New Brunswick, NJ, from 1100 UTC to 2100 UTC 2 June 2002
DTSP wildfire observations
MRF
DTSP wildfire simulations
Simulated skew T–log p sounding at the fire location valid at 1800 UTC 2 June 2002
YSU
DTSP wildfire simulations
Simulated skew T–log p sounding at the fire location valid at 1800 UTC 2 June 2002
MYJ
DTSP wildfire simulations
Simulated skew T–log p sounding at the fire location valid at 1800 UTC 2 June 2002
MYNN
DTSP wildfire simulations
Simulated skew T–log p sounding at the fire location valid at 1800 UTC 2 June 2002
surface temperature (°C)
21.0022.00
23.0024.00
25.0026.00
27.0028.00
29.0030.00
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
MRF
YSU
MYNN
MYJ
OBS - McGuire AFB
DTSP wildfire simulations
Time series at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated surface temperature
surface mixing ratio (g kg−1)
0.00
2.00
4.00
6.00
8.00
10.00
12.00
14.00
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
MRF
YSU
MYNN
MYJ
OBS - McGuire AFB
DTSP wildfire simulations
Time series at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated surface mixing ratio
surface wind speed (m s−1)
0.001.002.003.004.005.006.007.008.009.00
10.00
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
MRF
YSU
MYNN
MYJ
OBS - McGuire AFB
DTSP wildfire simulations
Time series at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated surface wind speed
MRF temperature profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
temperature (°C)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature
YSU temperature profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
temperature (°C)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature
MYJ temperature profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
temperature (°C)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature
MYNN temperature profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
temperature (°C)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature
MRF mixing ratio profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 2.00 4.00 6.00 8.00 10.00 12.00
mixing ratio (g kg−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio
YSU mixing ratio profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 2.00 4.00 6.00 8.00 10.00 12.00
mixing ratio (g kg−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio
MYJ mixing ratio profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 2.00 4.00 6.00 8.00 10.00 12.00
mixing ratio (g kg−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio
MYNN mixing ratio profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 2.00 4.00 6.00 8.00 10.00 12.00
mixing ratio (g kg−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio
MRF wind speed profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
wind speed (m s−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated wind speed
YSU wind speed profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
wind speed (m s−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated wind speed
MYJ wind speed profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
wind speed (m s−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated wind speed
MYNN wind speed profiles
0
0.5
1
1.5
2
2.5
3
3.5
0.00 5.00 10.00 15.00 20.00 25.00 30.00
wind speed (m s−1)
he
igh
t (k
m)
1200
1300
1400
1500
1600
1700
1800
1900
2000
2100
DTSP wildfire simulations
Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated wind speed
• An intercomparison of the MRF, YSU, MYJ, and MYNN PBL schemes in WRF version 3.1 for the DTSP wildfire event indicates that the behavior of these schemes is consistent with that documented in the literature.
• The MRF and YSU schemes produce less directional wind shear than the MYJ and MYNN schemes.
• The diurnal growth of the mixed layer is more gradual in the YSU, MYJ, and MYNN schemes than in the MRF scheme.
• The YSU and MYNN PBL schemes exhibit a deeper mixed layer than the MYJ scheme.
Summary
Future work
• The methodology developed for the DTSP wildfire event will be extended to additional events.
• Candidates include the Warren Grove (NJ, 2007), Evans Road (NC, 2008), and Cottonville (WI, 2005) wildfires.
• Aspects to be examined for these events:
1) effects of the entrainment formulation on mixed-layer growth
2) sensitivity of mixing ratio profiles in the mixed layer to the choice of PBL scheme
3) performance of the PBL schemes in high-wind regimes