Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Renran Zhou"'
Publikováno v:
Remote Sensing, Vol 16, Iss 7, p 1230 (2024)
Mêdog is located at the entrance of the water vapor channel of the Yarlung Tsangpo Great Canyon on the southeastern Tibetan Plateau (TP). In this study, the seasonal variation in the microphysical vertical structure of stratiform precipitation at th
Externí odkaz:
https://doaj.org/article/269b561e9b0543ab85230f7329e5515d
Publikováno v:
Remote Sensing, Vol 15, Iss 15, p 3731 (2023)
Mêdog and Nagqu are two typical climate regions of the Tibetan Plateau, with different atmospheric conditions and local orography. This may lead to different diurnal variation patterns of clouds and precipitation. This paper investigates the diurnal
Externí odkaz:
https://doaj.org/article/ef72259611354f74a77198322a6b8d1e
Publikováno v:
Remote Sensing, Vol 14, Iss 13, p 3149 (2022)
Mêdog is located at the entrance of the water vapor channel in the Yarlung Zangbo Grand Canyon (YGC). This area has the largest annual accumulated rainfall totals and precipitation frequency on the Tibetan Plateau (TP). This paper investigates the s
Externí odkaz:
https://doaj.org/article/0e698741aa7a476789de487b166ab0fb
Publikováno v:
Journal of Meteorological Research. 37:90-106
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::158b98b295d85f65835559f230fc5f17
https://doi.org/10.1007/s13351-023-2108-8
https://doi.org/10.1007/s13351-023-2108-8
Publikováno v:
Advances in Atmospheric Sciences. 39:1062-1078
Motuo and Naqu are two typical regions of the Tibetan Plateau with different geographical locations and climate regimes. These differences may lead to discrepancies in the raindrop size distributions (DSDs) and precipitation microphysical processes b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb8d57309f913ffbfe2f499676da1b13
https://doi.org/10.1007/s00376-021-1135-6
https://doi.org/10.1007/s00376-021-1135-6
Publikováno v:
Atmospheric Research. 258:105629
The southeastern Tibetan Plateau (TP) is the critical region of water vapor transport over the TP. Ground-based Ka-band cloud radar (KaCR) measurements collected at the Motuo National Climate Observatory in 2019 were used to analyze the physical prop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22be6e26587bfd9147882345ca4ba048
https://doi.org/10.1016/j.atmosres.2021.105629
https://doi.org/10.1016/j.atmosres.2021.105629
Publikováno v:
Atmospheric Research. 249:105311
As part of the Second Tibetan Plateau Scientific Expedition and Research (STEP) field campaign, raindrop size distribution (DSD) measurements were conducted with a laser optical particle size velocity disdrometer in Motuo on the Tibetan Plateau (TP).
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f54e3c3e6a1c894fb03aba81ba20a709
https://doi.org/10.1016/j.atmosres.2020.105311
https://doi.org/10.1016/j.atmosres.2020.105311