The intense diabatic heating over the Tibetan Plateau affects the movement of the
atmosphere over and around the Tibetan Plateau, which will have an important impact on …

利用青藏高原站点观测资料与ERA5, NCEP II, JRA55 和MERRA2 再分析资料, 对比分析了4
种再分析资料在青藏高原非绝热加热描述偏差的时空特征. 结果表明:(1) 4 种再分析资料在青藏 …

Based on the site data of the Tibetan Plateau (TP) from 1970 to 2015, the sensible heat
fluxes over the middle and eastern Tibetan Plateau were calculated by physical method …

Figure S1. Temperature anomaly evolution of independent warm day events (the first
column), independent warm night events (the second column), and the compound warm …

In this study, a parameterization method based on LANDDSAT7 ETM data and field
observations is described and tested for deriving the regional land surface variables …

伊朗高原和青藏高原热力作用对东亚区域气候具有重要影响. 基于1979—2014 年欧洲中心ERA-
interim 月平均再分析地表热通量资料, 分析了春, 夏季青藏高原与伊朗高原地表热通量的时 …

The high terrain of the Tibetan Plateau (TP) has a very important impact on the weather and
climate of China, East Asia, South Asia, and even the Northern Hemisphere. However, in …

Being the highest and largest land mass of the earth, the Tibetan Plateau has a strong
impact on the Asian climate especially on the Asian monsoon. With high downward solar …

Surface sensible and latent heat fluxes (SH and LE) over the Tibetan Plateau (TP) have
been under research since 1950s, especially for recent several years, by mainly using …

Using monthly reanalysis data of NCEP/NCAR from 1968 to 2009 and adopting reverse
computation method, the atmospheric heat source over east of the Tibetan Plateau in …