Mathematical modeling of surface forest fires transition into crown forest fires

Valeriy Afanasievich Perminov, Egor L. Loboda, Vladimir V. Reino

Результат исследований: Материалы для книги/типы отчетовМатериалы для конференции

4 Цитирования (Scopus)

Аннотация

It is developed mathematical model for description of heat and mass transfer processes at crown forest fire initiation. Mathematical model of forest fire was based on an analysis of experimental data and using concept and methods from reactive media mechanics. The paper suggested in the context of the general mathematical model of forest fires give a new mathematical setting and method of numerical solution of a problem of a forest fire modeling. The boundary-value problem is solved numerically using the method of splitting according to physical processes. In this paper the assignment and theoretical investigations of the problems of forest fire initiation were carried out.

Язык оригиналаАнглийский
Название основной публикации20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics
ИздательSPIE
Том9292
ISBN (электронное издание)9781628413762
DOI
СостояниеОпубликовано - 2014
Опубликовано для внешнего пользованияДа
Событие20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics - Novosibirsk, Российская Федерация
Продолжительность: 23 июн 201427 июн 2014

Конференция

Конференция20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics
СтранаРоссийская Федерация
ГородNovosibirsk
Период23.6.1427.6.14

ASJC Scopus subject areas

  • Applied Mathematics
  • Computer Science Applications
  • Electrical and Electronic Engineering
  • Electronic, Optical and Magnetic Materials
  • Condensed Matter Physics

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  • Цитировать

    Perminov, V. A., Loboda, E. L., & Reino, V. V. (2014). Mathematical modeling of surface forest fires transition into crown forest fires. В 20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics (Том 9292). [929225] SPIE. https://doi.org/10.1117/12.2086618