首页> 外文期刊>Exchanges : Newsletter of the Climate Variability and Predictability Programme (CLIVAR) >Progress on Understanding Land-Atmosphere Interactions and Surface Hydrology during the North American Monsoon Avances en el conocimiento de las interacciones tierra-atmósfera y la hidrología en superfcie durante el Monzón de Norteamérica
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Progress on Understanding Land-Atmosphere Interactions and Surface Hydrology during the North American Monsoon Avances en el conocimiento de las interacciones tierra-atmósfera y la hidrología en superfcie durante el Monzón de Norteamérica

机译:北美季风期间对陆地-大气相互作用和地表水文学的理解进展北美季风期间对陆地-大气相互作用和地表水文学的理解进展

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Land surface processes have been considered to play animportant, yet poorly understood, role on the evolutionof the North American Monsoon System (NAMS). Insummarizing the results of the NAME Process Study,Higgins and Gochis (2007) indicated that surface flux,vegetation and soil moisture measurements taken duringNAME could potentially help constrain estimates ofland-atmosphere interactions and moisture recycling.To understand these land surface-atmosphere feedbacksinvolves observations and modeling of the land phase ofthe hydrological cycle. As indicated by Vera et al. (2006),only the major hydrologic features of the NAMS, suchas the seasonal march of precipitation and stream?ow atcoarse spatial scales, have been quantifed. Motivated bythese studies, several efforts by a team of U.S. and Mexicoscientists were carried out during 2006-2009 in the NAMSregion.
机译:人们已经认为,地表过程在北美季风系统(NAMS)的演变中起着重要的作用,但人们对此知之甚少。 Higgins和Gochis(2007)总结了NAME过程研究的结果,指出在NAME期间进行的表面通量,植被和土壤湿度测量可能有助于限制对土地-大气相互作用和水分循环的估计。水文循环陆地阶段的建模。如Vera等人所述。 (2006),只有NAMS的主要水文特征,如降水和流量的季节性行进,在粗略的空间尺度,已被量化。受这些研究的激励,美国和墨西哥科学家团队在2006年至2009年期间在NAMS地区进行了数项努力。

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