The purpose of this work is to test the methodology for modeling the conditions of formation of aircraft condensation trails (ACT), taking into account its application to regional climatic conditions. Examples of the formation of ACT based on known data from flight experiments are analyzed. An analysis of the conditions for the formation of ACT in the 1970s and 2010s in the Omsk and Moscow regions is carried out using a quantitative criterion for the theoretically possible maximum supersaturation of water vapor in an aircraft engine jet. The characteristics of aircraft engines of the D-30 and CFM56 families, which were widely used during these periods, were used for the estimates. Using the regional data averaged over 3 years from radiosonde observations of the atmosphere, conclusions were drawn about climate changes and the difference in the conditions of formation of ACT in the Omsk and Moscow regions. To control the influence of aviation on the formation of cirrus clouds and the radiation balance of the atmosphere, an approach has been proposed to assess the conditions for the formation of ACT based on current atmospheric sounding data in the region.
aircraft engine, axisymmetric nozzle, aircraft condensation trail, impact of aviation on the environment, heat transfer and jet gas dynamics
Апробация методики моделирования условий образования конденсационных следов самолетов на основе данных зондирования атмосферы
Целью данной работы является апробация методики моделирования условий образования конденсационных следов самолетов (КСС) с учетом ее применения к региональным климатическим условиям. Проанализированы примеры формирования КСС на основе известных данных летных экспериментов. Делается анализ условий формирования КСС в 1970-х и 2010-х годах в регионах Омск и Москва с помощью количественного критерия теоретически возможного максимального перенасыщения водяного пара в струе авиационного двигателя. Для оценок использованы характеристики авиационных двигателей семейств Д-30 и CFM56, которые массово использовались в эти периоды. С использованием осредненных за 3 года региональных данных радиозондовых наблюдений атмосферы сделаны выводы о климатических изменениях и различии условий образования КСС в регионах Омск и Москва. Для управления влиянием авиации на образование перистой облачности и радиационный баланс атмосферы предложен подход к оценке условий образования КСС на основе текущих данных зондирования атмосферы в регионе.
авиационный двигатель, осесимметричное сопло, конденсационный след самолета, влияние авиации на окружающую среду, теплообмен и газодинамика струи
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