Physical controls on half-hourly, daily, and monthly turbulent flux and energy budget over a high-altitude small lake on the Tibetan Plateau

doi:10.1002/2016JD026109

	Physical controls on half-hourly, daily, and monthly turbulent flux and energy budget over a high-altitude small lake on the Tibetan Plateau
	Wang, BB ; Wang, BB (Wang, Binbin)1,2,3; Ma, YM (Ma, Yaoming)1,2,4; Ma, WQ (Ma, Weiqiang)1,2,4; Su, ZB (Su, Zhongbo)3
刊名	JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
	2017
卷号	122 期号:4 页码:2289-2303
关键词	GREAT SLAVE LAKE NAM CO HEAT FLUXES EVAPORATION WATER BALANCE AIR TEMPERATURE VARIABILITY WARM
DOI	10.1002/2016JD026109
文献子类	Article
英文摘要	Precise measurements of evaporation and understanding of the physical controls on turbulent heat flux over lakes have fundamental significance for catchment-scale water balance analysis and local-scale climate modeling. The observation and simulation of lake-air turbulent flux processes have been widely carried out, but studies that examine high-altitude lakes on the Tibetan Plateau are still rare, especially for small lakes. An eddy covariance (EC) system, together with a four-component radiation sensor and instruments for measuring water temperature profiles, was set up in a small lake within the Nam Co basin in April 2012 for long-term evaporation and energy budget observations. With the valuable measurements collected during the ice-free periods in 2012 and 2013, the main conclusions are summarized as follows: First, a bulk aerodynamic transfer model (B model), with parameters optimized for the specific wave pattern in the small lake, could provide reliable and consistent results with EC measurements, and B model simulations are suitable for data interpolation due to inadequate footprint or malfunction of the EC instrument. Second, the total evaporation in this small lake (812mm) is approximately 200mm larger than that from adjacent Nam Co (approximately 627mm) during their ice-free seasons. Third, wind speed shows significance at temporal scales of half hourly, whereas water vapor and temperature gradients have higher correlations over temporal scales of daily and monthly in lake-air turbulent heat exchange. Finally, energy stored during April to June is mainly released during September to November, suggesting an energy balance closure value of 0.97.
学科主题	自然地理学
WOS研究方向	Meteorology & Atmospheric Sciences
语种	英语
WOS记录号	WOS:000396121200015
内容类型	期刊论文
源URL	[http://ir.itpcas.ac.cn/handle/131C11/8330]
专题	青藏高原研究所_图书馆
通讯作者	Wang, BB
作者单位	1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China. 2.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China. 3.Univ Twente, Fac Geoinformat Sci & Earth Observat, Enschede, Netherlands. 4.Univ Chinese Acad Sci, Beijing, Peoples R China.
推荐引用方式 GB/T 7714	Wang, BB,Wang, BB ,Ma, YM ,et al. Physical controls on half-hourly, daily, and monthly turbulent flux and energy budget over a high-altitude small lake on the Tibetan Plateau[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2017,122(4):2289-2303.
APA	Wang, BB,Wang, BB ,Ma, YM ,Ma, WQ ,&Su, ZB .(2017).Physical controls on half-hourly, daily, and monthly turbulent flux and energy budget over a high-altitude small lake on the Tibetan Plateau.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,122(4),2289-2303.
MLA	Wang, BB,et al."Physical controls on half-hourly, daily, and monthly turbulent flux and energy budget over a high-altitude small lake on the Tibetan Plateau".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 122.4(2017):2289-2303.