A conceptual model for the link between Central American biomass burning aerosols and severe weather over the south central United States
Bibliographic Data
| ID | 15548328 |
|---|---|
| Authors | Jun Wang (0000-0003-4485-7201, University of Maryland, Baltimore County, corresponding author), Susan C van den Heever (0000-0001-9843-3864, Colorado State University), Jeffrey S Reid (0000-0002-5147-7955) |
| Year | 2009 |
| Volume | 4 |
| Issue | 1 |
| Pages | 015003-015003 |
| Publication date | 2009-01-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/4/1/015003 |
| OpenAlex | W2058057617 |
| Language | EN |
| Citations received | 3 |
| References cited | 24 |
Each spring, smoke particles from fires over the Yucatan Peninsula and south Mexico cross over the Gulf of Mexico into the United States (US) under the control of moist oceanic air flow from the southwestern branch of the subtropical (Bermuda) high. Smoke can be transported deep into the south central US, where dry lines and warm conveyor belts are frequently formed and cause deep convection and severe weather. Lyons et al (1998 Science 282 77–80) and Murray et al (2000 Geophys. Res. Lett. 27 2249–52) noticed a ∼50% increase of lightning along the smoke transport path over the south central US during the May 1998 Central American smoke episode. Here we present a conceptual model of coherent microphysical and meteorological mechanisms through which smoke may impact convective clouds and subsequently result in more severe weather over the south central US. The conceptual model depicts a chain of processes in which smoke particles are first activated as cloud condensation nuclei when they are entrained into the warm conveyor belt, a convective zone formed over the south central US as a result of the encounter between the mid-latitude trough and the subtropical Bermuda high. As the convection continues with deepening of the mid-latitude trough, the greater concentration of water cloud condensation nuclei delays the warm rain processes, enhances the development of ice clouds, and invigorates the updrafts, all of which contribute to the formation of severe weather such as hail and lightning. The conceptual model is based on the reasoning of physical mechanisms revealed in previous studies (over the tropical biomass region), and is supported here through the analysis of satellite data, ground observations, aerosol transport model results, and idealized cloud resolving simulations of a day in May 2003 when record tornado events occurred over the south central US. Further assessment of this conceptual model is discussed for future investigations
Aerosol · Atmospheric sciences · Chemical transport model · Climatology · Cloud condensation nuclei · Convection · Geography · Meteorology · Severe weather · Smoke · Storm · Subtropics · Tropical cyclone · Troposphere · Trough (economics · Atmospheric aerosols and clouds · Environmental Science · Fire effects on ecosystems · Meteorological Phenomena and Simulations · Geology
| Citations per year | 0.38 |
|---|---|
| Citation span | 2018 - 2025 (8) |
| Highly cited | No |