Уважаемые коллеги, доброго времени суток! Представляем вам австрийское научное издание Meteorology and Atmospheric Physics. Журнал имеет третий квратиль, издается в Springer-Verlag Wien, его SJR за 2020 г. равен 0,634, пятилетний импакт-фактор - 2,209, печатный ISSN - 0177-7971, электронный - 1436-5065, предметная область Наука об атмосфере. Вот так выглядит обложка:
Редактором является Клеменс Зиммер, контактные данные - csimmer@uni-bonn.de.
Дополнительные публикационные контакты - pooja.ramesh.1@springernature.com, Kaaviya.Haribabu@springernature.com, journalpermissions@springernature.com, johanna.schwarz@springer.com.
К публикации принимаются оригинальные исследовательские работы в соответствии с рекомендациями экспертной комиссии. Акцент делается на следующих тематических областях:
- динамика атмосферы и общая циркуляция;
- синоптическая метеорология;
- погодные системы в определенных регионах, таких как тропики, полярные шапки, океаны;
- атмосферная энергетика;
- численное моделирование и прогнозирование;
- физические и химические процессы в атмосфере, включая радиацию, оптические эффекты, электричество, атмосферную турбулентность и процессы переноса;
- математические и статистические методы, применяемые к наборам метеорологических данных.
Также обсуждаются физические и химические процессы как в ясной, так и в облачной атмосфере, включая радиацию, оптические и электрические эффекты, осадки и микрофизику облаков.
Адрес издания - https://www.springer.com/journal/703
Пример статьи, название - A case study on the triggering mechanisms of localized warm-sector rainstorm. Заголовок (Abstract) - On the morning of July 21, 2017, a localized rainstorm event occurred in the Shijiazhuang area of Hebei Province, with the heavy rain mainly concentrating in the Shijiazhuang urban area and its eastern and northern parts. But this rainstorm process was omitted by both numerical and subjective forecasts. In this paper, the triggering mechanisms of the mesoscale convective systems that have caused this localized rainstorm are analyzed by using the intensified surface observation data, Doppler radar data, the four-dimensional variational Doppler radar analysis system (VDRAS), the National Centers for Environmental Prediction (NCEP) reanalysis data and the ERA5 reanalysis. The observation analysis shows that when the heavy rain was occurring, the Shijiazhuang area was controlled by the western Pacific subtropical high, and the high temperature and high humidity environment has provided favorable vapor, thermal and energy conditions for the rainfall. Three key factors are responsible for the triggering of this severe convective weather. First, the strong thunderstorm high pressure and cold pool formed in Qinhuangdao and Tangshan areas in the northeastern Hebei. The surface wind field was affected by the pressure-gradient force generated by the thunderstorm high pressure, and consequently the northeasterly wind gradually strengthened, which guided the tongue-shaped cold pool to gradually move southwestward to the northern Shijiazhuang. Thus, a long lasting cold-warm boundary (the leading edge of the cold tongue) was formed in the key precipitation area, which provided low-level convergence and the ascending motion for the occurrence and development of this severe convective weather. Second, the northeasterly wind in the east side of Taihang Mountain was forced to ascend by the topography of Taihang Mountain, which strengthened the upward motion. Third, as the direction of the Taihang Mountains shifts from a northeast–southwest direction to a northwest–southeast direction in the west side of Shijiazhuang, the surface northeasterly airflow is changed to a northwesterly airflow here, forming a convergence in the key area of precipitation in front of the mountain. Thus, an unstable vertical structure that features low-level convergence and middle-level divergence is formed. The above three factors work together in the region where the severe convections occurred, and triggered the release of the conditional instability energy, finally resulting in this short-time heavy rain. The results indicate that in the forecast of severe convections in midsummer, we should pay extra attention to the complex terrain and the effects of the cold pool.