Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Yinhuan Ao"'
Publikováno v:
Journal of Glaciology, Vol 67, Pp 91-106 (2021)
The Tibetan Plateau (TP) lakes are sensitive to climate change due to its seasonal ice cover, but few studies have paid attention to the freeze-thaw process of TP lakes and its key control parameters. By combining 216 simulation experiments using the
Externí odkaz:
https://doaj.org/article/b8d62d864b5c4aae8b4e6bade491d2d6
Publikováno v:
Remote Sensing, Vol 14, Iss 24, p 6283 (2022)
Evapotranspiration plays a decisive role in the whole oasis ecosystem and is an important factor to maintain the ecological stability of oases. To quantitatively analyze the evapotranspiration differences of oases at different scales and the expansio
Externí odkaz:
https://doaj.org/article/a4a3ddd8ba204c50b9aa98779398ce37
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
We investigated the relationship between the spring tropospheric temperature over the Tibetan Plateau (TPT) and summer precipitation in eastern China on an interannual timescale using the monthly mean ERA-Interim reanalysis dataset, the HadISST datas
Externí odkaz:
https://doaj.org/article/c60763c22bab46e2a767b36030f5ef90
Publikováno v:
Atmosphere, Vol 13, Iss 1, p 133 (2022)
Wind disasters are responsible for significant physical destruction, injury, loss of life, and economic damage. This study examined the extreme wind triggering mechanism over a typical mountain area with complex terrain, i.e., Dali city in Yunnan Pro
Externí odkaz:
https://doaj.org/article/27dda1ba10bb4859a7f10542159124b4
Publikováno v:
Atmosphere, Vol 12, Iss 12, p 1619 (2021)
The Loess Plateau is one land-atmosphere coupling hotspot. Soil moisture has an influence on atmospheric boundary layer development under specific early-morning atmospheric thermodynamic structures. This paper investigates the sensitivity of atmosphe
Externí odkaz:
https://doaj.org/article/47c58c6f26c94011a743e5fd9e1321a6
Autor:
ZHAOGUO LI, YINHUAN AO, SHIHUA LYU, JIAHE LANG, LIJUAN WEN, VICTOR STEPANENKO, XIANHONG MENG, LIN ZHAO
Publikováno v:
Journal of Glaciology, Vol 64, Pp 506-516 (2018)
The Tibetan Plateau (TP) lakes are sensitive to climate change due to ice-albedo feedback, but almost no study has paid attention to the ice albedo of TP lakes and its potential impacts. Here we present a recent field experiment for observing the lak
Externí odkaz:
https://doaj.org/article/2b3828c021ce43bbb4dac3b2d95425a7
Autor:
Lin Zhao, S.-Y. Simon Wang, Chi-Hua Wu, Sebastian Los, Shihua Lyu, Xianhong Meng, Lijuan Wen, Siqiong Luo, Yinhuan Ao, Zhaoguo Li
Publikováno v:
Atmosphere, Vol 11, Iss 1, p 105 (2020)
The characteristics of intense diurnal precipitation occurring beneath the South Asian High (SAH) are diagnosed in the summer monsoon season from 2010 to 2015 using observational data. The diagnostics indicate that summer nighttime rainfall events in
Externí odkaz:
https://doaj.org/article/4b0678fb99a84e59bb36b18f9612c19e
Publikováno v:
Advances in Meteorology, Vol 2017 (2017)
This paper reported a comprehensive analysis on the diurnal variation of the Atmospheric Boundary Layer (ABL) in summer of Badain Jaran Desert and discussed deeply the effect of surface thermal to ABL, including the Difference in Surface-Air Temperat
Externí odkaz:
https://doaj.org/article/038cd4b9a4b54c619974eb57a650ae1b
Autor:
Xianhong Meng, Shihua Lyu, Zhaoguo Li, Yinhuan Ao, Lijuan Wen, Lunyu Shang, Shaoying Wang, Mingshan Deng, Shaobo Zhang, Lin Zhao, Hao Chen, Di Ma, Suosuo Li, Lele Shu, Yingying An, Hanlin Niu
Publikováno v:
Advances in Atmospheric Sciences. 40:1142-1157
Thousands of lakes on the Tibetan Plateau (TP) play a critical role in the regional water cycle, weather, and climate. In recent years, the areas of TP lakes underwent drastic changes and have become a research hotspot. However, the characteristics o
Autor:
Zhaoguo, Li, Shaobo, Zhang, Xianhong, Meng, Shihua, Lyu, Xianyu, Yang, Yinhuan, Ao, Di, Ma, Lunyu, Shang, Lele, Shu, Yan, Chang
Publikováno v:
Science of The Total Environment. 859:160205
Extreme snowfall events have been increasing in the Tibetan Plateau, causing greater variations in the snow cover conditions. However, the soil water-heat transfer under different snow conditions has rarely been characterized in detail. Here, by usin