A case book of the Double Trouble State Park Wildfire (2002) Joseph J. Charney USDA Forest Service, Northern Research Station, East Lansing, MI Daniel.

Slides:



Advertisements
Similar presentations
Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA
Advertisements

Climatological Aspects of Ice Storms in the Northeastern U.S. Christopher M. Castellano, Lance F. Bosart, and Daniel Keyser Department of Atmospheric and.
Craig B. Clements 1, Sharon Zhong 2, Wenqing Yao 2, C. David Whiteman 3, and Tom Horst 4 1 University of Houston, Houston, TX, USA 2 Michigan State University,
Generation mechanism of strong winds in the left-rear quadrant of Typhoon MA-ON (2004) during its passage over the southern Kanto district, eastern Japan.
The Persistence and Dissipation of Lake Michigan-Crossing Mesoscale Convective Systems Nicholas D. Metz* and Lance F. Bosart # * Department of Geoscience,
Chapter 6 Section 6.4 Goals: Look at vertical distribution of geostrophic wind. Identify thermal advection, and backing and veering winds. Look at an example.
Matthew Vaughan, Brian Tang, and Lance Bosart Department of Atmospheric and Environmental Sciences University at Albany/SUNY Albany, NY NROW XV Nano-scale.
Modifications to the MYNN PBL and Surface Layer Scheme for WRF-ARW Joseph Olson1,2 John M. Brown1 1NOAA-ESRL/GSD/AMB 2Cooperative Institute for Research.
Fire Summary The simulations presented in this study represent the meteorological conditions associated with the Warren Grove Wildfire in south-central.
Skew-T Thermodynamic Diagram Global distribution of weather balloon stations.
The impact of mesoscale PBL parameterizations on the evolution of mixed-layer processes important for fire weather Joseph J. Charney USDA Forest Service,
Analysis of Precipitation Distributions Associated with Two Cool-Season Cutoff Cyclones Melissa Payer, Lance F. Bosart, Daniel Keyser Department of Atmospheric.
A Multiscale Analysis of the Inland Reintensification of Tropical Cyclone Danny (1997) within an Equatorward Jet-Entrance Region Matthew S. Potter, Lance.
The Inland Extent of Lake Effect Snow (LES) Bands Joseph P. Villani NOAA/NWS Albany, NY Michael L. Jurewicz, Sr. NOAA/NWS Binghamton, NY Jason Krekeler.
Predecessor Rain Events Ahead of TC Ike and TC Lowell on 11–14 September 2008 Lance F. Bosart, Thomas J. Galarneau, Jr., Jason M. Cordeira, and Benjamin.
EASTERLY WAVE STRUCTURAL EVOLUTION OVER WEST AFRICA AND THE EAST ATLANTIC Matthew A. Janiga Department of Atmospheric and Environmental Sciences, University.
Mike Evans NOAA/NWS Binghamton, NY Barry Lambert NOAA/NWS State College, Pa.
Hurricane Frances (2004) Hurricane Rita (2005) Hurricane Ike (2008) Supported by National Science Foundation grants , , , ,
Warm-Season Lake-/Sea-Breeze Severe Weather in the Northeast Patrick H. Wilson, Lance F. Bosart, and Daniel Keyser Department of Earth and Atmospheric.
300 hPa height (solid, dam), wind speed (shaded, m s −1 ), 300 hPa divergence (negative values dashed, 10 −6 s −1 ) n = 22 MSLP (solid, hPa),
Strong Polar Anticyclone Activity over the Northern Hemisphere and an Examination of the Alaskan Anticyclone Justin E. Jones, Lance F. Bosart, and Daniel.
Warm-Season Lake-/Sea-Breeze Severe Weather in the Northeast Patrick H. Wilson, Lance F. Bosart, and Daniel Keyser Department of Earth and Atmospheric.
Island Effects on Mei-Yu Jet/Front Systems and Rainfall Distribution during TIMREX IOP#3 Yi-Leng Chen and Chuan-Chi Tu Department of Meteorology SOEST,
Relationships between wind speed, humidity and precipitating shallow cumulus convection Louise Nuijens and Bjorn Stevens* UCLA - Department of Atmospheric.
Maintenance of a Mesoscale Convective System over Lake Michigan Nicholas D. Metz and Lance F. Bosart Department of Earth and Atmospheric Sciences University.
The Effects of Grid Nudging on Polar WRF Forecasts in Antarctica Daniel F. Steinhoff 1 and David H. Bromwich 1 1 Polar Meteorology Group, Byrd Polar Research.
Figure 1. Topography (m, shaded following inset scale) of the Intermountain West and adjoining region
High-Resolution Simulations of the 25 December 2002 Banded Snowstorm using Eta, MM5, and WRF David Novak NOAA/ NWS Eastern Region Headquarters, Scientific.
Upper-Level Precursors Associated with Subtropical Cyclone Formation in the North Atlantic Alicia M. Bentley, Daniel Keyser, and Lance F. Bosart University.
WILDFIRES BURNING IN THE WESTERN USA 42,933 WILDFIRES HAVE OCCURRED DURING 2012 AUGUST 16, 2012 Walter Hays, Global Alliance for Disaster Reduction, University.
Some Preliminary Modeling Results on the Upper-Level Outflow of Hurricane Sandy (2012) JungHoon Shin and Da-Lin Zhang Department of Atmospheric & Oceanic.
Coastal Meteorology and Atmospheric Prediction (COMAP) Research at Stony Brook University Michael Erickson, Brian A. Colle, Sara Ganetis, Nathan Korfe,
Assessment of the vertical exchange of heat, moisture, and momentum above a wildland fire using observations and mesoscale simulations Joseph J. Charney.
Multiscale Analyses of Tropical Cyclone-Midlatitude Jet Interactions: Camille (1969) and Danny (1997) Matthew S. Potter, Lance F. Bosart, and Daniel Keyser.
The IMPOWR (Improving the Mapping and Prediction of Offshore Wind Resources) project: Evaluation of WRF PBL Schemes Brian A. Colle and Matthew J. Sienkiewicz.
13th Cyclone Workshop 25 October 2005 Pacific Grove, CA1 A Study of the Effect of Horizontal Contrasts in Static Stability on Frontal Behavior Mark T.
Synoptic and Mesoscale Conditions associated with Persisting and Dissipating Mesoscale Convective Systems that Cross Lake Michigan Nicholas D. Metz and.
Observational and theoretical investigations of turbulent structures generated by low-Intensity prescribed fires in forested environments X. Bian, W. Heilman,
The diagnosis of mixed-layer depth above an eastern U.S. wildfire using a mesoscale numerical weather prediction model Joseph J. Charney USDA Forest Service,
Air Pressure and Winds. Atmospheric Pressure  What causes air pressure to change in the horizontal?  Why does the air pressure change at the surface?
Identification of side-door/back-door cold fronts for fire weather forecasting applications Joseph J. Charney USDA Forest Service Northern Research Station,
Simulation of Summertime Wind Speed at Turbine Hub Height: Model Sensitivities to Speed and Shear Characteristics Shannon L. Rabideau, Daniel A. Rajewski,
Figure sec mean topography (m, shaded following scale at upper left) of the Intermountain West and adjoining regions,
1 Longitudinally-dependent ozone recovery in the Antarctic polar vortex revealed by satellite-onboard ILAS-II observation in 2003 Kaoru Sato Department.
Research on the HWRF Model: Intensification and Uncertainties in Model Physics Research on the HWRF Model: Intensification and Uncertainties in Model Physics.
Validation of the Simulated Microphysical Structure within the Midlevel Inflow Region of a Tropical, Oceanic Squall Line Hannah C. Barnes, Robert A. Houze.
Meng, Z., F. Zhang, P. Markoswki, D. Wu, and K. Zhao, 2012: A modeling study on the development of a bowing structure and associated rear inflow within.
Figure 1. Schematic of factors contributing to high ozone concentrations. Potential temperature profile (red line) with stable layer trapping ozone precursors.
Kelley Murphy Earth & Atmospheric Sciences Department State University of New York at OneontaPhoto of snow crystals collected by Univ. of Utah during the.
Instability in Leapfrog and Forward-Backward Schemes by Wen-Yih Sun Department of Earth and Atmospheric Sciences Purdue University West Lafayette, IN.
The diagnosis of mixed-layer characteristics and their relationship to meteorological conditions above eastern U.S. wildland fires Joseph J. Charney USDA.
Numerical Simulation and Prediction of Supercell Tornadoes Ming Xue School of Meteorology and Center for Analysis and Prediction of Storms University of.
The diagnosis of mixed-layer characteristics and their relationship to meteorological conditions above eastern U.S. wildland fires Joseph J. Charney USDA.
11 Implementing a New Shallow Convection Scheme into WRF Aijun Deng and Brian Gaudet Penn State University Jimy Dudhia National Center for Atmospheric.
A Subtropical Cyclonic Gyre of Midlatitude Origin John Molinari and David Vollaro.
An Investigation of Model-Simulated Band Placement and Evolution in the 25 December 2002 Northeast U.S. Banded Snowstorm David Novak NOAA/ NWS Eastern.
Cheng-Zhong Zhang and Hiroshi Uyeda Hydroshperic Atmospheric Research Center, Nagoya University 1 November 2006 in Boulder, Colorado Possible Mechanism.
Upper-Level Precursors Associated with Subtropical Cyclone Formation in the North Atlantic Alicia M. Bentley, Daniel Keyser, and Lance F. Bosart University.
Climatological Aspects of Freezing Rain in the Eastern U.S. Christopher M. Castellano, Lance F. Bosart, and Daniel Keyser Department of Atmospheric and.
The sensitivity of fire-behavior and smoke-dispersion indices to the diagnosed mixed-layer depth Joseph J. Charney US Forest Service, Northern Research.
WRF-based rapid updating cycling system of BMB(BJ-RUC) and its performance during the Olympic Games 2008 Min Chen, Shui-yong Fan, Jiqin Zhong Institute.
Figure 1. NASA Blue Marble (i.e., true color) image of (a) the Intermountain West and (b) the Wasatch Front and adjoining region. Geographic features discussed.
Matt Vaughan Class Project ATM 621
An Investigation of the Skill of Week Two
Low level Jet.
Antecedent Environments Conducive to the Production of Extreme Temperature and Precipitation Events in the United States Andrew C. Winters, Daniel Keyser,
The November 26, 2014 banded snowfall case in southern NY
William Flamholtz, Brian Tang, and Lance Bosart
Ship observation and numerical simulation of the marine atmospheric boundary layer over the spring oceanic front in the northwestern South China Sea Rui.
New York State Mesoscale Weather Network
Presentation transcript:

A case book of the Double Trouble State Park Wildfire (2002) Joseph J. Charney USDA Forest Service, Northern Research Station, East Lansing, MI Daniel Keyser Department of Atmospheric and Environmental Sciences, University at Albany, Albany, NY

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 OKX upper air station KWRI surface station New Brunswick wind profiler

Time (UTC)Activity reported 1415 fire tower weather: wind west at 4 m s P −1 P, gusting to 9 m s P −1 P ; temperature 24°C; relative humidity 62% 1700Estimated start time of fire 1709Fire reported by fire tower 1714Direct attack on fire by NJFFS firefighters begins 1725 fire tower reports winds greater than 18 m s P −1 P ; direct attack abandoned 1726Backfiring operations begin north and east of the fire 1731Request submitted for to be closed 1735Backfiring operations begin south of the fire 1747Request submitted for aerial support for fighting the fire 1751Fire jumps and approaches the 1800Fire is officially declared to be a major fire 1801Fire has crossed the 1808First report of a house being burned 1818Wind shift reported on the fire line 1823Fire crews prepare for structure protection 1851Wind shift to the north reported; former right flank of the fire becomes the head fire 1857 fire tower reports winds north at 16 m s P −1 P 1936Big wind shift reported on the fire line 1937fire tower reports winds shifting to the east, northeast 1938Right flank becomes head fire 1953Fire has been diverted south of the line of homes located just east of the 1959Wind shift reported on fire line; electric lines down on roadway 2001House on fire 2004Evacuation order issued for homes in the area 2010Wind shift reported on fire line 2024Wind shift reported on fire line; wind shift causes fire to spread rapidly towards the south directly towards a crew 2055East flank of fire reported to be growing; fire crews respond to quell 2113Fire west of the reported to be contained 2136Fire declared to be under control 2148 fire tower reports winds diminishing to less than 9 m s P −1 P Table 1. Sequence of events during the Double Trouble State Park wildfire from 1415 UTC to 2148 UTC 2 June 2002 [adapted from NJFFS (2003)]

Fig. 3. Surface analyses of potential temperature (contour interval 4°C, solid), mixing ratio (value indicated in g kg −1 at station location; contour interval 5 g kg −1, dashed, shaded as indicated in legend), and wind (full barb 5 m s −1 ) valid at (a) 1200 UTC 2 June 2002, (b) 1800 UTC 2 June 2002, and (c) 0000 UTC 3 June Adapted from surface analyses generated and archived in the Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York.

Fig. 4. NARR upper-air analyses of (a) geopotential height (contour interval 30 m, solid), temperature (°C, color shaded as indicated in legend), and wind (maximum vector 25 m s P −1 P ) at 1200 UTC 2 June 2002 at 850 hPa, (b) geopotential height (contour interval 120 m, solid), wind speed (m s P −1 P, color shaded as indicated in legend), and wind (maximum vector 75 m s P −1 P ) at 1200 UTC 2 June 2002 at 300 hPa, (c) as in (a) except for 0000 UTC 3 June 2002, and (d) as in (b) except for 0000 UTC 3 June 2002.

Fig. 6. Skew T–log p soundings at Upton, NY (OKX), valid at (a) 1200 UTC 2 June 2002 and (b) 0000 UTC 3 June Adapted from the University of Wyoming weather web page ( TU UT ). TU UT

DTSP wildfire observations Observed skew T–log p sounding at Upton, NY (OKX), valid at 0000 UTC 3 June 2002

Wind profiler observations at New Brunswick, NJ, from 1100 UTC to 2100 UTC 2 June 2002 DTSP wildfire observations

Fig. 8. Surface meteograms from 0000 UTC to 2300 UTC 2 June 2002 for (a) McGuire Air Force Base, NJ (WRI), and (b) Atlantic City, NJ (ACY). Adapted from the Plymouth State Weather Center web page ( TU UT ). TU UT

Fig. 12. Northwest– southeast-oriented vertical cross section of simulated relative humidity (%, color shaded as indicated in legend) and pressure-coordinate vertical velocity (contour interval 10 dPa s −1, solid, starting at 10 dPa s −1 ) valid at (a) 1500 UTC 2 June 2002, (b) 1600 UTC 2 June 2002, (c) 1700 UTC 2 June 2002, and (d) 1800 UTC 2 June The fire location is indicated by the fire icon at 208 km on the abscissa of the cross section. The location of the cross section is indicated by the thick black line in Fig. 10.

Fig. 13. Time series at the fire location valid from 1200 UTC 2 June 2002 to 0000 UTC 3 June 2002 of simulated (a) surface relative humidity (%), (b) surface wind speed (m s P −1 P ), and (c) PBL depth (m). The fire location is indicated by the fire icon in Fig. 10.

Fig. 14. Time–height cross section at the fire location valid from 1200 UTC 2 June 2002 to 0000 UTC 3 June 2002 of simulated (a) relative humidity (%, color shaded as indicated in legend) and (b) wind speed (m s P −1 P, color shaded as indicated in legend). The fire location is indicated by the fire icon in Fig. 10.

Fig. 9. Simulated surface relative humidity (%, color shaded as indicated in legend) and surface wind (full barb 5 m s P −1 P ) valid at 1800 UTC 2 June Fig. 10. Simulated relative humidity (%, color shaded as indicated in legend) at 700 hPa valid at 1800 UTC 2 June The fire icon indicates the fire location and the thick black line shows the orientation of the vertical cross section in Fig. 12.

Simulated skew T–log p sounding at OKX valid at 0000 UTC 3 June 2002 MRF DTSP wildfire simulations WRF simulations initialized at 1200 UTC 1 June 2002

Simulated skew T–log p sounding at OKX valid at 0000 UTC 3 June 2002 YSU DTSP wildfire simulations

MYJ Simulated skew T–log p sounding at OKX valid at 0000 UTC 3 June 2002 DTSP wildfire simulations

MYNN Simulated skew T–log p sounding at OKX valid at 0000 UTC 3 June 2002 DTSP wildfire simulations

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

DTSP wildfire simulations Time series at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated surface temperature

DTSP wildfire simulations Time series at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated surface mixing ratio

DTSP wildfire simulations Time series at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated surface wind speed

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated temperature

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated mixing ratio

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated wind speed

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated wind speed

DTSP wildfire simulations Vertical profiles at fire location valid from 1200 UTC to 2100 UTC 2 June 2002 of simulated wind speed

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