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                 1079. DOI:10. 1175/JAM2500. 1.                    290. DOI:10. 1175/2007JAMC1547. 1.
             Li M,Liu X,Shu L,et al,2021. Variations in surface roughness of  Yang K,Chen Y Y,Qin J,2009. Some practical notes on the land sur‐
                 heterogeneous surfaces in the Nagqu area of the Tibetan Plateau  face modeling in the Tibetan Plateau[J]. Hydrology and Earth
                [J]. Hydrology and Earth System Sciences,25(5):2915-2930.  System Sciences,13,5(2009-05-27),13(5):687-701. DOI:
                 DOI:10. 5194/hess-25-2915-2021.                   10. 5194/hess-13-687-2009.
             Ma Y,Fan S,Ishikawa H,et al,2005. Diurnal and inter-monthly  Zeng X,Barlage M,Dickinson R E,et al,2005. Treatment of under‐
                 variation of land surface heat fluxes over the central Tibetan Pla‐  canopy turbulence in land models[J]. Journal of Climate,18
                 teau area[J]. Theoretical and Applied Climatology,80(2-4):  (23):5086-5094. DOI:10. 1175/JCLI3595. 1.
                 259-273. DOI:10. 1007/s00704-004-0104-1.       Zeng X,Dickinson R E,1998. Effect of surface sublayer on surface
             Massman W J,Weil J C,1999. An analytical one-dimensional second-  skin temperature and fluxes[J]. Journal of Climate,11(4):537-
                 order closure model of turbulence statistics and the Lagrangian  550. DOI: 10. 1175/1520-0442(1998)011<0537: EOSSOS>
                 time scale within and above plant canopies of arbitrary structure  2. 0. CO;2.
                [J]. Boundary-Layer Meteorology,91(1):81-107. DOI:10.  Zeng X,Wang A,2007. Consistent parameterization of roughness
                 1023/A:1001810204560.                             length and displacement height for sparse and dense canopies in
             Niu G Y,Yang Z L,Mitchell K E,et al,2011. The community Noah  land models[J]. Journal of Hydrometeorology,8(4):730-737.
                 land surface model with multiparameterization options(Noah ‐  DOI:10. 1175/JHM607. 1.
                 MP):1. Model description and evaluation with local‐scale mea‐  Zeng X,Wang Z,Wang A,2012. Surface skin temperature and the in‐
                 surements[J]. Journal of Geophysical Research:Atmospheres,  terplay between sensible and ground heat fluxes over arid regions
                 116(D12). DOI:10. 1029/2010JD015139.             [J]. Journal of Hydrometeorology,13(4):1359-1370. DOI:
             Sun G,Hu Z,Wang J,et al,2016. Upscaling analysis of aerodynam‐  10. 1175/JHM-D-11-0117. 1.
                 ic roughness length based on in situ data at different spatial scales  Zheng D,Van Der Velde R,Su Z,et al,2014. Assessment of rough‐
                 and remote sensing in north Tibetan Plateau[J]. Atmospheric Re‐  ness length schemes implemented within the Noah land surface
                 search,176:231-239. DOI:10. 1016/j. atmosres. 2016. 02. 025.  model for high-altitude regions[J]. Journal of Hydrometeorolo‐
             Sun J,1999. Diurnal variations of thermal roughness height over a  gy,15(3):921-937. DOI:10. 1175/JHM-D-13-0102. 1
                 grassland[J]. Boundary-Layer Meteorology,92(3):407-427.  Zilitinkevich S,1995. Scaling for convective boundary layers[M]//
                 DOI:10. 1023/A:1002071421362.                     Wind Climate in Cities. Springer,Dordrecht,67-79. DOI:10.
             Su Z,2002. The Surface Energy Balance System(SEBS)for estima‐  1007/978-94-017-3686-2_4
                 tion of turbulent heat fluxes[J]. Hydrology and Earth System Sci‐  陈海山,孙照渤,等,2005. 青藏高原单点地气交换过程的模拟试
                 ences,6(1):85-99.                                 验[J]. 高原气象,24(1):9-15.
             Tanaka K,Ishikawa H,Hayashi T,et al,2001. Surface energy bud‐  陈家宜,王介民,光田宁,1993. 一种确定地表粗糙度的独立方法
                 get at Amdo on the Tibetan Plateau using GAME/Tibet IOP98 data  [J]. 大气科学,17(1):21-26. doi:10. 3878/j. issn. 1006-9895.
                [J]. Journal of the Meteorological Society of Japan. Ser. II,79  1993. 01. 03.
                (1B):505-517. DOI:10. 2151/jmsj. 79. 505.       郭东林,杨梅学,屈鹏,等,2009. 能量和水分循环过程研究:回顾
             Wang S,Ma Y,2019. On the simulation of sensible heat flux over the  与探讨[J]. 冰川冻土,31(6):1116-1126. DOI:10. 11928/j.
                 Tibetan Plateau using different thermal roughness length parame‐  issn. 1001-7410. 2017. 05. 17.
                 terization schemes[J]. Theoretical and Applied Climatology,137  季国良,时兴和,高务祥,2001. 藏北高原地面加热场的变化及其
                (3-4):1883-1893. DOI:10. 1007/s00704-018-2704-1.   对气候的影响[J]. 高原气象,20(3):239-244.
             Wu G,Duan A,Liu Y,et al,2015. Tibetan Plateau climate dynam‐  贾东于,文军,马耀明,等,2017. 植被对黄河源区水热交换影响的
                 ics:recent research progress and outlook[J]. National Science  研究[J]. 高原气象,36(2):424-435. DOI:10. 7522/j. issn.
                 Review,2(1):100-116. DOIi:10. 1093/nsr/nwu045.    1000-0534. 2016. 00044.
             Yao T,Xue Y,Chen D,et al,2019. Recent third pole’s rapid warm‐  李锁锁,吕世华,柳媛普,等,2010. 黄河上游玛曲地区空气动力学
                 ing accompanies cryospheric melt and water cycle intensification  参数的确定及其在陆面过程模式中的应用[J]. 高原气象,29
                 and interactions between monsoon and environment:Multidisci‐  (6):1408-1413.
                 plinary approach with observations,modeling,and analysis[J].  李英,胡泽勇,2006. 藏北高原地表反照率的初步研究[J]. 高原气
                 Bulletin of the American Meteorological Society,100(3):423-  象,25(6):1034-1041.
                 444. DOI:10. 1175/BAMS-D-17-0057. 1.           刘少锋,林朝晖,2005. 通用陆面模式 CLM 在东亚不同典型下垫面
             Yang K,Koike T,Yang D,2003. Surface flux parameterization in the  的验证试验[J]. 气候与环境研究,2005(3):406-421. DOI:
                 Tibetan Plateau[J]. Boundary-layer meteorology,106(2):245-  10. 3878/j. issn. 1006-9585. 2005. 03. 34.
                 262. DOI:10. 1023/A:1021152407334.             刘啸然,李茂善,胡文斌,2019. 藏北高原那曲地区不同下垫面地
             Yang K,Koike T,Ishikawa H,et al,2008. Turbulent flux transfer  表粗糙度的变化特征研究[J]. 高原气象,38(2):428-438.
                 over bare-soil surfaces:Characteristics and parameterization[J].  DOI:10. 7522/j. issn. 1000-0534. 2018. 00083.
                 Journal of Applied Meteorology and Climatology,47(1):276-  刘新,吴国雄,刘屹岷,等,2002. 青藏高原加热与亚洲环流季节变
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