Zobrazeno 1 - 10
of 131
pro vyhledávání: '"Pao K. Wang"'
Autor:
Pao K. Wang, Kuan-Hui Elaine Lin, Yu-Shiuan Lin, Ho-Jiunn Lin, Pi-Ling Pai, Wan-Ling Tseng, Hsin-Cheng Huang, Chung-Rui Lee
Publikováno v:
Scientific Data, Vol 11, Iss 1, Pp 1-16 (2024)
Abstract This study reports the methodology for reconstructing anomalous temperature index series of China in 1368–1911 based on the REACHES database which digitizes the Chinese records quoted in the Compendium of Meteorological Records of China in
Externí odkaz:
https://doaj.org/article/8437a91fe1a440caae79eb0234e87f83
Autor:
Yuri A. Dyakov, Sergey O. Adamson, Gennady V. Golubkov, Igor I. Morozov, Danil R. Nigmatullin, Oleg A. Olkhov, Pao K. Wang, Maxim G. Golubkov
Publikováno v:
Atoms, Vol 11, Iss 12, p 157 (2023)
Criegee intermediates, which are the products of the ozonolysis of alkenes, play a key role in many chemical and physical processes in the atmosphere. Their reactions with other atmospheric compounds are responsible for the formation of hydroxyl, met
Externí odkaz:
https://doaj.org/article/89e1cf9982d94be38781de0713bbbcfe
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 32, Iss 3, Pp 361-374 (2021)
We perform a sensitivity study on the ventilation effect of large hydrometeors, namely, raindrops, snow aggregates, and hail in a cloud-resolving model. The ventilation effect could accelerate the heat and mass transfer rates between vapor and fallin
Externí odkaz:
https://doaj.org/article/8c5a547a5cb94c52a65a06dc8f32a435
Autor:
Olga P. Borchevkina, Yuliya A. Kurdyaeva, Yurii A. Dyakov, Ivan V. Karpov, Gennady V. Golubkov, Pao K. Wang, Maxim G. Golubkov
Publikováno v:
Atmosphere, Vol 12, Iss 11, p 1384 (2021)
Determination of the physical mechanisms of energy transfer of tropospheric disturbances to the ionosphere is one of the fundamental problems of atmospheric physics. This article presents the results of observations carried out using two-wavelength l
Externí odkaz:
https://doaj.org/article/6ad30a6fd6db4ad8a8b7e6a4b38beee2
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 22, Iss 5, p 447 (2011)
Recent observational and numerical modeling studies of the mechanisms which transport moisture to the stratosphere by deep convective storms at mid-latitudes are reviewed. Observational evidence of the cross-tropopause transport of moisture by thunde
Externí odkaz:
https://doaj.org/article/b23534e73c93449990e99808f7350684
Autor:
Pao K. Wang
This key new textbook provides a state-of-the-art view of the physics of cloud and precipitation formation, covering the most important topics in the field: the microphysics, thermodynamics and cloud-scale dynamics. Highlights include: the condensati
Deep convective storms represent the fastest vertical transport mechanism of both momentum and chemical species from the surface to the middle atmosphere, and these transports may potentially impact strongly the global atmospheric and climate process
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c6914e3b3517bb8cb1c6991bf78e230
https://doi.org/10.5194/egusphere-egu23-12557
https://doi.org/10.5194/egusphere-egu23-12557
Autor:
Pao K. Wang
In addition to their tremendous power display and serious damages they often cause, convective storms also play important roles in the global atmospheric transport processes. In this presentation, I would like to discuss two aspects of these processe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75ee2ab13add9702e21a06f3442ef138
https://doi.org/10.5194/ecss2023-172
https://doi.org/10.5194/ecss2023-172
Autor:
Pao K. Wang
Atmospheric ice particles play crucial roles in cloud and storm dynamics, atmospheric chemistry, climatological processes, and other atmospheric processes. Ice Microdynamics introduces the elementary physics and dynamics of atmospheric ice particles
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 32, Iss 3, Pp 361-374 (2021)
We perform a sensitivity study on the ventilation effect of large hydrometeors, namely, raindrops, snow aggregates, and hail in a cloud-resolving model. The ventilation effect could accelerate the heat and mass transfer rates between vapor and fallin