Zobrazeno 1 - 10
of 1 069
pro vyhledávání: '"Atmospheric gravity waves"'
Publikováno v:
Geodesy and Geodynamics, Vol 15, Iss 3, Pp 219-229 (2024)
It is commonly believed that the atmosphere is decoupled from the solid Earth. Thus, it is difficult for the seismic wave energy inside the Earth to propagate into the atmosphere, and atmospheric pressure wave signals excited by earthquakes are unlik
Externí odkaz:
https://doaj.org/article/f491de5b308049ddb106e0da9931c103
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 14, Pp n/a-n/a (2024)
Abstract The study presents (a) a 44‐year wintertime climatology of resolved gravity wave (GW) fluxes and forcing in the extratropical stratosphere using ERA5, and (b) their composite evolution around gradual (final warming) and abrupt (sudden warm
Externí odkaz:
https://doaj.org/article/af8350c261c149f5baf140f10a5bb9e7
Autor:
Wang Li, Fangsong Yang, Jiayi Yang, Renzhong Zhang, Juan Lin, Dongsheng Zhao, Craig M. Hancock
Publikováno v:
Remote Sensing, Vol 16, Iss 18, p 3375 (2024)
The atmospheric gravity waves (AGWs) generated by severe typhoons can facilitate the transfer of energy from the troposphere to the ionosphere, resulting in medium-scale traveling ionospheric disturbances (MSTIDs). However, the complex three-dimensio
Externí odkaz:
https://doaj.org/article/d0d6f938fa6b4fe4a57d1115a3b271e7
Autor:
Zhi‐Feng Xiu, Yu‐Zhang Ma, Qing‐He Zhang, Zan‐Yang Xing, Shun‐Rong Zhang, Yong‐Liang Zhang, Kjellmar Oksavik, Larry Lyons, Michael Lockwood, Yong Wang
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 1, Pp n/a-n/a (2024)
Abstract The space hurricane is a three‐dimensional magnetic vortex structure with strong flow shears and electron precipitation in the polar cap. This study investigates for the first time how a space hurricane disturbs the polar thermosphere. Dur
Externí odkaz:
https://doaj.org/article/97e11ff3286b4305a83d2a6114893faf
Autor:
JOSÉ VALENTIN BAGESTON, CRISTIANO MAX WRASSE, GABRIEL AUGUSTO GIONGO, EMÍLIA CORREIA, COSME ALEXANDRE O.B. FIGUEIREDO, DELANO GOBBI, HISAO TAKAHASHI, PAULO P. BATISTA, RICARDO A.B. DA COSTA
Publikováno v:
Anais da Academia Brasileira de Ciências, Vol 95, Iss suppl 3 (2023)
Abstract The thermal dynamics of the upper atmosphere, especially in the mesosphere, have been improving our understanding about the effects of climate change, as well as how the dynamics and general circulation in the upper atmosphere are driven by
Externí odkaz:
https://doaj.org/article/e74ea473e2e645f0b65b095606ea26a7
Publikováno v:
Earth and Planetary Physics, Vol 6, Iss 6, Pp 522-528 (2022)
Wavelike perturbations in the ionosphere of Titan, the largest satellite of Saturn, are explored based on the Cassini Ion Neutral Mass Spectrometer (INMS) measurements. Strong wavelike perturbations are identified for more than twenty ion species, fr
Externí odkaz:
https://doaj.org/article/029aa37171384286aed98102b508f5db
Autor:
Paul Prikryl, Vojto Rušin
Publikováno v:
Frontiers in Astronomy and Space Sciences, Vol 10 (2023)
A tendency of heavy rainfall-induced floods in Canada to follow arrivals of solar wind high-speed streams (HSSs) from coronal holes is observed. Precipitation events during the winter, including extreme freezing rain events in the province of New Bru
Externí odkaz:
https://doaj.org/article/c7d9febd03e645468814d88e9f16aa04
Autor:
Zhichao Liu, Chunhua Jiang, Tongxin Liu, Lehui Wei, Guobin Yang, Hua Shen, Wengeng Huang, Zhengyu Zhao
Publikováno v:
Remote Sensing, Vol 16, Iss 7, p 1142 (2024)
Spread F (SF) in the ionosphere can be observed frequently in mid-latitude regions. It is suggested that atmospheric gravity waves play a significant role for the seeding of mid-latitude SF. Previous research suggested that the source of travelling i
Externí odkaz:
https://doaj.org/article/9d6bbc6421934aa8afbb8b935709a927
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.