Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Shunwu Zhou"'
Publikováno v:
暴雨灾害, Vol 42, Iss 2, Pp 144-149 (2023)
In the summer of 2012 and 2013, two northeastward-moving Tibetan Plateau vortices (referred to as TPV) moved out of the Tibetan Plateau (referred to as plateau), and then caused heavy rain in the northwest region. In 2013, The moving path of TPV was
Externí odkaz:
https://doaj.org/article/8b0978054b7f4038a5b41d339d76c26a
Publikováno v:
Remote Sensing, Vol 16, Iss 4, p 619 (2024)
Antarctic Total Column Ozone (TCO) gradually began to recover around 2000, and a large number of studies have pointed out that the recovery of the Antarctic TCO is most significant in the austral early spring (September). Based on the Bodeker Scienti
Externí odkaz:
https://doaj.org/article/26a9142f9ab3498c83d79eea33283eaf
Publikováno v:
Frontiers in Environmental Science, Vol 11 (2023)
Externí odkaz:
https://doaj.org/article/5da38e406ef24c99a2ad13c3ff34d6fe
Publikováno v:
Frontiers in Environmental Science, Vol 11 (2023)
This study aims to investigate the impacts of the spring sensible heat (SH) over the Tibetan Plateau (TP) and the El Niño–Southern Oscillation (ENSO) in the preceding wintertime on midsummer (July–August) precipitation over South China under the
Externí odkaz:
https://doaj.org/article/a784c0a7cd7245088a94d4d97c65f319
Publikováno v:
Remote Sensing, Vol 15, Iss 23, p 5587 (2023)
Recent years have witnessed contrasting trends in summer total rainfall (STR) over the Tibetan Plateau (TP), with an increase in the northern and a decrease in the southern TP. This study identifies four significant centers of rainfall trends: easter
Externí odkaz:
https://doaj.org/article/7cdc951b63aa493c857a0805efc09fad
Publikováno v:
Atmosphere, Vol 14, Iss 5, p 812 (2023)
The spring sensible heating (SSH) over the Tibetan Plateau (TP), which can significantly affect the precipitation in China, has experienced three different stages of change, showing significant increasing (1961–1979, Stage I), decreasing (1980–20
Externí odkaz:
https://doaj.org/article/b3858d7072c646e7b8056a1d06834482
Publikováno v:
Atmosphere, Vol 13, Iss 5, p 689 (2022)
The Tibetan Plateau (TP) vortex (TPV), one of the crucial weather systems triggering rainfall, plays a key role in modulating precipitation over TP and downstream regions. The role of atmospheric heat source in TPV development is explored by a case s
Externí odkaz:
https://doaj.org/article/89a09b7489a3479182ded6b38945ab34
Publikováno v:
Atmosphere, Vol 11, Iss 2, p 215 (2020)
A persistent strong cold surge occurred in East Asia in late January 2018, causing mean near-surface air temperature in China to hit the second lowest since 1984. Moreover, the daily mean air temperature remained persistently negative for more than 2
Externí odkaz:
https://doaj.org/article/4ca53e71a66d483b83ef56c4b228f5b9
Publikováno v:
Advances in Meteorology, Vol 2017 (2017)
Local climate effects of Tibetan Plateau Ozone Valley (OVTP) were investigated by numerical simulations using Community Atmosphere Model version 5.1.1 (CAM5). After a 20-year spin-up period, two additional 10-year experiments were conducted. CAM5 was
Externí odkaz:
https://doaj.org/article/21095e23623a4ac2abe0d25a72795e29
Autor:
Meirong Wang, Jun Wang, Deliang Chen, Anmin Duan, Yimin Liu, Shunwu Zhou, Dong Guo, Hengmao Wang, Weimin Ju
Publikováno v:
Environmental Research Letters, Vol 14, Iss 12, p 124066 (2019)
The spring sensible heating (SH) over the Tibetan Plateau (TP) serves as a huge ‘air pump’, significantly influencing the Asian summer monsoon, has experienced a decreasing trend. However, it remains unclear whether this decline will continue. Th
Externí odkaz:
https://doaj.org/article/b492cc1b9d8745408c4c53f12e6ec747