img

QQ Group

img

Wechat

Plateau Meteorology
Adv search
Online submission Peer review Office work
  • Impact of High-Resolution Atmospheric Forcing and Plant Functional Types Datasets on Soil Temperature Simulation in the Qinghai-Tibetan Plateau

    Impact of High-Resolution Atmospheric Forcing and Plant Functional Types Datasets on Soil Temperature Simulation in the Qinghai-Tibetan Plateau

    SHEN Runping, GUO Qian, CHEN Pingping, LI Xinhui, WANG Shaowu, SHI Chunxiang

    Plateau Meteorology, 2019 38 (6): 1129-1139.

    Soil temperature is a key physical quantity in the land-atmosphere interaction, and also an important parameter in the research of land surface model simulation. However, it is very difficult to obtain the spatiotemporal. . .

     
  • Numerical Simulation of the Variation of the Turbulent Fluxes on the Qinghai-Tibetan Plateau and its Surrounding Area from 2004 to 2013

    Numerical Simulation of the Variation of the Turbulent Fluxes on the Qinghai-Tibetan Plateau and its Surrounding Area from 2004 to 2013

    LI Maoshan, YIN Shucheng, LIU Xiaoran, Lü Zhao, SONG Xingyu, MA Yaoming, SUN Fanglin

    Plateau Meteorology, 2019 38 (6): 1140-1148.

    The mesoscale model WRF with improved surface roughness is used to simulate the variation characteristics of surface turbulent flux over the Qinghai-Tibetan Plateau and its surrounding areas from 2004 to 2013. The result. . .

     
  • The Variation Characteristics of Planetary Boundary Layer Height in Northwest China: Based on Radiosonde and ERA-Interim Reanalysis Data

    The Variation Characteristics of Planetary Boundary Layer Height in Northwest China: Based on Radiosonde and ERA-Interim Reanalysis Data

    ZHAO Cailing, LI Yaohui, LIU Yuanpu, ZHOU Ganlin, ZHANG Tiejun, SUN Xuying

    Plateau Meteorology, 2019 38 (6): 1181-1193.

    The planetary boundary layer height (PBLH) are calculated by using the radiosonde sounding data of 38 L-band operational sites during September 2015 to August 2016 in Northwest China. The radiosonde sounding data of 6 in. . .

     
Current issueArchiveHighlightSpecial issue
2020, Vol.39 No.3  No.2 No.1
2019, Vol.38 No.6  No.5 No.4 No.3 No.2 No.1
2018, Vol.37 No.6  No.5 No.4 No.3 No.2 No.1
2017, Vol.36 No.6  No.5 No.4 No.3 No.2 No.1
2016, Vol.35 No.6  No.5 No.4 No.3 No.2 No.1
2015, Vol.34 No.6  No.5 No.4 No.3 No.2 No.1
2014, Vol.33 No.6  No.5 No.4 No.3 No.2 No.1
2013, Vol.32 No.6  No.5 No.4 No.3 No.2 No.1
2012, Vol.31 No.6  No.5 No.4 No.3 No.2 No.1
2011, Vol.30 No.6  No.5 No.4 No.3 No.2 No.1
2010, Vol.29 No.6  No.5 No.4 No.3 No.2 No.1
2009, Vol.28 No.6  No.5 No.4 No.3 No.2 No.1
2008, Vol.27 No.6  No.5 No.4 No.3 No.2 No.1
No.增刊
2007, Vol.26 No.6  No.5 No.4 No.3 No.2 No.1
2006, Vol.25 No.6  No.5 No.4 No.3 No.2 No.1
2005, Vol.24 No.6  No.5 No.4 No.3 No.2 No.1
2004, Vol.23 No.s1  No.6 No.5 No.4 No.3 No.2
No.1
2003, Vol.22 No.s1  No.6 No.5 No.4 No.3 No.2
No.1
2002, Vol.21 No.6  No.5 No.4 No.3 No.2 No.1
2001, Vol.20 No.4  No.3 No.2 No.1
2000, Vol.19 No.4  No.3 No.2 No.1
1999, Vol.18 No.4  No.3 No.2 No.1
1998, Vol.17 No.4  No.3 No.2 No.1
1997, Vol.16 No.4  No.3 No.2 No.1
1996, Vol.15 No.4  No.3 No.2 No.1
1995, Vol.14 No.4  No.3 No.2 No.1
1994, Vol.13 No.4  No.3 No.2 No.1
1993, Vol.12 No.4  No.3 No.2 No.1
1992, Vol.11 No.4  No.3 No.2 No.1
1991, Vol.10 No.4  No.3 No.2 No.1
1990, Vol.9 No.4  No.3 No.2 No.1
1989, Vol.8 No.4  No.3 No.2 No.1
1988, Vol.7 No.4  No.3 No.2 No.1
1987, Vol.6 No.s1  No.4 No.3 No.2 No.1
1986, Vol.5 No.4  No.3 No.2 No.1
1985, Vol.4 No.s1  No.s2 No.4 No.3 No.2 No.1
1984, Vol.3 No.4  No.3 No.2 No.1
1983, Vol.2 No.4  No.3 No.2 No.1
1982, Vol.1 No.4  No.3 No.2 No.1
1900, Vol.29 No.1 
Topics
The newsDownloadExpress informationVideo information
Links CNKI WanFang Data

©2018Plateau Meteorology

Tel：0931-8260935；0931-8261524

Email：gybjb@lzb.ac.cn

Support:Magtech