The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill Fire
The deadly shift of the Yarnell Hill, Arizona wildfire was associated with an environment exhibiting gusty wind patterns in response to organized convectively driven circulations. The observed synoptic (>2500 km) through meso-β (approximately 100 km) scale precursor environment that organized a m...
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| Format: | Article |
| Language: | English |
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MDPI AG
2021-11-01
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| Series: | Climate |
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| Online Access: | https://www.mdpi.com/2225-1154/9/12/170 |
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| author | Michael L. Kaplan Curtis N. James Jan Ising Mark R. Sinclair Yuh-Lang Lin Andrew Taylor Justin Riley Shak M. S. Karim Jackson Wiles |
| author_facet | Michael L. Kaplan Curtis N. James Jan Ising Mark R. Sinclair Yuh-Lang Lin Andrew Taylor Justin Riley Shak M. S. Karim Jackson Wiles |
| author_sort | Michael L. Kaplan |
| collection | DOAJ |
| description | The deadly shift of the Yarnell Hill, Arizona wildfire was associated with an environment exhibiting gusty wind patterns in response to organized convectively driven circulations. The observed synoptic (>2500 km) through meso-β (approximately 100 km) scale precursor environment that organized a mid-upper tropospheric cross-mountain mesoscale jet streak circulation and upslope thermally direct flow was examined. Numerical simulations and observations indicated that both circulations played a key role in focusing the upper-level divergence, ascent, downdraft potential, vertical wind shear favoring mobile convective gust fronts, and a microburst. This sequence was initiated at the synoptic scale by a cyclonic Rossby Wave Break (RWB) 72 h prior, followed by an anticyclonic RWB. These RWBs combined to produce a mid-continent baroclinic trough with two short waves ushering in cooler air with the amplifying polar jet. Cool air advection with the second trough and surface heating across the Intermountain West (IW) combined to increase the mesoscale pressure gradient, forcing a mid-upper tropospheric subsynoptic jet around the periphery of the upstream ridge over Southern Utah and Northern New Mexico. Convection was triggered by an unbalanced secondary jetlet circulation within the subsynoptic jet in association with a low-level upslope flow accompanying a mountain plains solenoidal circulation above the Mogollon Rim (MR) and downstream mountains. |
| first_indexed | 2024-03-10T04:23:26Z |
| format | Article |
| id | doaj.art-fdfa8b1bd5b74bb881a548c1526c8ead |
| institution | Directory Open Access Journal |
| issn | 2225-1154 |
| language | English |
| last_indexed | 2024-03-10T04:23:26Z |
| publishDate | 2021-11-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Climate |
| spelling | doaj.art-fdfa8b1bd5b74bb881a548c1526c8ead2023-11-23T07:44:59ZengMDPI AGClimate2225-11542021-11-0191217010.3390/cli9120170The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill FireMichael L. Kaplan0Curtis N. James1Jan Ising2Mark R. Sinclair3Yuh-Lang Lin4Andrew Taylor5Justin Riley6Shak M. S. Karim7Jackson Wiles8Department of Applied Aviation Sciences, Embry-Riddle Aeronautical University, Prescott, AZ 86301, USADepartment of Applied Aviation Sciences, Embry-Riddle Aeronautical University, Prescott, AZ 86301, USADepartment of Physics and Applied Science and Technology, North Carolina A&T University, Greensboro, NC 27405, USADepartment of Applied Aviation Sciences, Embry-Riddle Aeronautical University, Prescott, AZ 86301, USADepartment of Physics and Applied Science and Technology, North Carolina A&T University, Greensboro, NC 27405, USANational Weather Service, National Oceanic and Atmospheric Administration, Central Illinois Forecast Office, Lincoln, IL 62656, USADepartment of Physics and Applied Science and Technology, North Carolina A&T University, Greensboro, NC 27405, USADepartment of Physics and Applied Science and Technology, North Carolina A&T University, Greensboro, NC 27405, USADepartment of Physics and Applied Science and Technology, North Carolina A&T University, Greensboro, NC 27405, USAThe deadly shift of the Yarnell Hill, Arizona wildfire was associated with an environment exhibiting gusty wind patterns in response to organized convectively driven circulations. The observed synoptic (>2500 km) through meso-β (approximately 100 km) scale precursor environment that organized a mid-upper tropospheric cross-mountain mesoscale jet streak circulation and upslope thermally direct flow was examined. Numerical simulations and observations indicated that both circulations played a key role in focusing the upper-level divergence, ascent, downdraft potential, vertical wind shear favoring mobile convective gust fronts, and a microburst. This sequence was initiated at the synoptic scale by a cyclonic Rossby Wave Break (RWB) 72 h prior, followed by an anticyclonic RWB. These RWBs combined to produce a mid-continent baroclinic trough with two short waves ushering in cooler air with the amplifying polar jet. Cool air advection with the second trough and surface heating across the Intermountain West (IW) combined to increase the mesoscale pressure gradient, forcing a mid-upper tropospheric subsynoptic jet around the periphery of the upstream ridge over Southern Utah and Northern New Mexico. Convection was triggered by an unbalanced secondary jetlet circulation within the subsynoptic jet in association with a low-level upslope flow accompanying a mountain plains solenoidal circulation above the Mogollon Rim (MR) and downstream mountains.https://www.mdpi.com/2225-1154/9/12/170density currentRossby Wave Breakjetletdowndraft convective available potential energymicroburstwildfire |
| spellingShingle | Michael L. Kaplan Curtis N. James Jan Ising Mark R. Sinclair Yuh-Lang Lin Andrew Taylor Justin Riley Shak M. S. Karim Jackson Wiles The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill Fire Climate density current Rossby Wave Break jetlet downdraft convective available potential energy microburst wildfire |
| title | The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill Fire |
| title_full | The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill Fire |
| title_fullStr | The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill Fire |
| title_full_unstemmed | The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill Fire |
| title_short | The Multi-Scale Dynamics Organizing a Favorable Environment for Convective Density Currents That Redirected the Yarnell Hill Fire |
| title_sort | multi scale dynamics organizing a favorable environment for convective density currents that redirected the yarnell hill fire |
| topic | density current Rossby Wave Break jetlet downdraft convective available potential energy microburst wildfire |
| url | https://www.mdpi.com/2225-1154/9/12/170 |
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