Page 18 - 《高原气象》2022年第6期

6 期 王卫国等：1979-2018年青藏高原不同地区积雪季极端降水水汽来源分析 1381
ricultural and Forest Meteorology， 298. DOI： 10. 1016/j. 52：181-196. DOI：10. 1007/s00382-018-4130-6.
agrformet. 2020. 108307. Qi W，Zhang B，Pang Y，et al，2013. TRMM data based spatial and
Drumond A，Gimeno L，Nieto R，et al，2017. Drought episodes in seasonal patterns of precipitation in the Qinghai Tibet Plateau［J］.
the climatological sinks of the Mediterranean moisture source： Scientia Geographica Sinica，33（8）：999-1005.
The role of moisture transport［J］. Global and Planetary Change， Qin H，Jiang D，Lang X，2018. Sources of moisture for different in‐
151：4-14. DOI：10. 1016/j. gloplacha. 2016. 12. 004. tensities of summer rainfall over the Chinese Loess Plateau during
Drumond A，Nieto R，Gimeno L，2011. Sources of moisture for Chi‐ 1979-2009［J］. International Journal of Climatology，38：1280-
na and their variations during drier and wetter conditions in 2000- 1287.
2004：a Lagrangian approach［J］. Climate Research，50：215- Qiu T，Huang W，Wright J S，et al，2019. Moisture sources for win‐
225. DOI：10. 3354/cr01043. tertime intense precipitation events over the three snowy subre‐
Gimeno-Sotelo L，Nieto R，Vazquez M，et al，2018. A new pattern of gions of the Tibetan Plateau［J］. Journal of Geophysical Research-
the moisture transport for precipitation related to the drastic de‐ Atmospheres， 124 （23） ： 12708-12725. DOI： 10. 1029/
cline in Arctic sea ice extent［J］. Earth System Dynamics，9（2）： 2019jd031110.
611-625. DOI：10. 5194/esd-9-611-2018. Qiu X，Yang X，Fang Y，et al，2018. Impacts of snow disaster on ru‐
Gocic M，Trajkovic S，2013. Analysis of changes in meteorological ral livelihoods in southern Tibet-Qinghai Plateau［J］. International
variables using Mann-Kendall and Sen's slope estimator statistical Journal of Disaster Risk Reduction，31：143-152.
tests in Serbia［J］. Global and Planetary Change，100：172-182. Saha S，Moorthi S，Wu X，et al，2014. The NCEP Climate Forecast
DOI：10. 1016/j. gloplacha. 2012. 10. 014. System Version 2［J］. Journal of Climate，27：2185-2208. DOI：
Guan X F，Yang L M，Zhang Y X，et al，2019. Spatial distribution， 10. 1175/JCLI-D-12-00823. 1.
temporal variation，and transport characteristics of atmospheric Sen P K，1968. Estimates of the regression coefficient based on Kend‐
water vapor over Central Asia and the arid region of China［J］. all's Tau［J］. Journal of the American Statistical Association，63：
Global and Planetary Change，172：159-178. DOI：10. 1016/j. 1379-1389. DOI：10. 1080/01621459. 1968. 10480934.
gloplacha. 2018. 06. 007. Sodemann H，Schwierz C，Wernli H，2008. Interannual variability of
He J，Yang K，Tang W，et al，2020. The first high-resolution meteoro‐ Greenland winter precipitation sources：Lagrangian moisture di‐
logical forcing dataset for land process studies over China［J］. Sci‐ agnostic and North Atlantic Oscillation influence［J］. Journal of
entific Data，7. DOI：10. 1038/s41597-020-0369-y. Geophysical Research-Atmospheres，113：D03107. DOI：10.
Huang W，Qiu T，Yang Z，et al，2018. On the formation mechanism 1029/2007jd008503.
for wintertime extreme precipitation events over the Southeastern Stohl A，James P，2004. A Lagrangian analysis of the atmospheric
Tibetan Plateau［J］. Journal of Geophysical Research：Atmo‐ branch of the global water cycle. Part I：Method description，vali‐
spheres，123（22）：12692-12714. DOI：12692-12714. 10. 1029/ dation，and demonstration for the August 2002 flooding in Cen‐
2018jd028921. tral Europe［J］. Journal of Hydrometeorology，5（4）：656-678.
Huang Y，Cui X，2015. Moisture sources of torrential rainfall events DOI： 10. 1175/1525-7541（2004）005<0656：ALAOTA>2. 0.
in the Sichuan Basin of China during summers of 2009-2013［J］. CO；2.
Journal of Hydrometeorology， 16 （4） ： 1906-1917. DOI： Stohl A，James P，2005. A Lagrangian analysis of the atmospheric
10. 1175/jhm-d-14-0220. 1. branch of the global water cycle. Part II：Moisture transports be‐
Immerzeel W W，van Beek L P H，Bierkens M F P J S，2010. Climate tween Earth's Ocean Basins and River Catchments［J］. Journal of
change will affect the Asian Water Towers［J］. Science，328 Hydrometeorology，6（6）：961-984. DOI：10. 1175/JHM470. 1.
（5984）：1382-1385. Sun B，Wang H J，2014. Moisture sources of semiarid grassland in
Liu F，Mao X，Zhang Y，et al，2014. Risk analysis of snow disaster China using the Lagrangian Particle Model FLEXPART［J］. Jour‐
in the pastoral areas of the Qinghai［Tibet Plateau［J］. Journal of nal of Climate，27（6）：2457-2474. DOI：10. 1175/jcli-d-13-
Geographical Sciences，24：411-426. 00517. 1.
Liu X D，Yin Z Y，2001. Spatial and temporal variation of summer Tian L，Yao T，MacClune K，et al，2007. Stable isotopic variations in
precipitation over the eastern Tibetan Plateau and the North Atlan‐ west China：A consideration of moisture sources［J］. Journal of
tic oscillation［J］. Journal of Climate，14（13）：2896-2909. DOI： Geophysical Research-Atmospheres，112：D10112. DOI：10.
10. 1175/1520-0442（2001）014<2896：satvos>2. 0. co；2. 1029/2006jd007718.
Mohsin T，Gough W A，2010. Trend analysis of long term tempera‐ Trenberth K E，1999. Atmospheric moisture recycling：Role of advec‐
ture time series in the Greater Toronto Area（GTA）［J］. Theoreti‐ tion and local evaporation［J］. Journal of Climate，12：1368-
cal and Applied Climatology，101：311-327. DOI：10. 1007/ 1381. DOI：10. 1175/1520-0442（1999）012<1368：Amrroa>2. 0.
s00704-009-0214-x. Co；2.
Pan C，Zhu B，Gao J，et al，2019. Quantitative identification of mois‐ Trenberth K E，2011. Changes in precipitation with climate change
ture sources over the Tibetan Plateau and the relationship between ［J］. Climate Research，47：123-138. DOI：10. 3354/cr00953.
thermal forcing and moisture transport［J］. Climate Dynamics， Vazquez M，Nieto R，Drumond A，et al，2016. Moisture transport in‐