设为首页
加入收藏
大口径闪烁仪及其在地表能量平衡监测中的应用
LARGE APERTURE SCINTILLOMETER AND ITS APPLICATION TO SURFACE ENERGY BALANCE MONITORING
-
摘要: 介绍了LAS仪器的测量原理及数据处理方法, 并利用中荷合作项目CEWBMS中获得的河南郑州LAS测站2000年的观测资料, 同时结合其它辅助资料, 对观测点附近地区的能量平衡状况进行了分析。分析结果表明, 由LAS测值得到的显热通量值, 以及结合净辐射资料间接得到的潜热通量值, 合理地反映出了当地能量平衡状况的季节变化, 显示出一年之中当地大部分的净辐射能用于潜热通量的释放。其数据结果所表征的当地下垫面干湿程度的变化与同期的降水及土壤相对湿度相比, 表现出了相当好的一致性, 这为拓展LAS在局地地表能量平衡监测中的应用提供了物理依据。Abstract: The large aperture scintillometer (LAS) is a device that measures the turbulent intensity of the refraction index of air.The instrument consists of a transmitter and a receiver, which are placed at a given distance apart with the path length being to 5 km.Therefore, the measurement of LAS is an area-averaged result between the transmitter and the receiver.At the receiver the spatial turbulent intensity is expressed in the refractive structure index Cn2. With some additional data users are able to derive the sensible heat fluxes between surface and atmosphere.As part of the Chinese-Dutch CEWBMS (China Energy and Water Balance Monitoring System) project, five LASs were installed in China.As one site representing the agricultural area in North China, a LAS was set up over a crop field at Zhengzhou in Henan Province with a path length of 1350 m.Using the LAS measurements and some additional data collected in the Zhengzhou site in 2000, daily average sensible heat fluxes are deduced, and the basic characteristics of surface energy balance components during the w hole year are analyzed.The results show a good consistence with the features of the rainfall and the soil relative humidity in the same period.This work improved the understanding of the seasonal variation of the energy balance in the LAS site area; furthermore, provided the phy sical foundation for the LAS application in local surface energy balance monitoring.
-
[1] 朱治林, 孙晓敏, 张仁华.淮河流域典型地面水热通量的观测分析.气候与环境研究, 2001, 6(2):214-220. http://www.cnki.com.cn/Article/CJFDTOTAL-QHYH200102012.htm [2] de Bruin H A R, Van Den Hurk B J J M, Koh siek W.The scintillation method tested over a dry vineyard area.Boundary Layer Meteorology, 1995, 76 :25-40. doi: 10.1007/BF00710889 [3] de Bruin H A R, Nieveen J P, de Wekker S F J, et al.Large aperture scintillometry over a 4.8 km path for measuringareally-average sensible heat flux :A case study.The Volume on the 22nd AMS Symposiumon Agricultural and ForestMeteorology, 28 January 1996, At lanta, USA. [4] Meijninger W M L, Moene A, Hartogensis O, et al.The large aperture scintillometeruser manual and technicalin formation, Version 1.5, Wageningen :Wageningen University Research Center, 2000. [5] 吴蓉璋, 胡丽琴, 游然, 等. 用于测量显热通量的"大口径闪烁仪"(LAS). 首届气象仪器与观测技术交流和研讨会学术论文集, 海南海口, 2001年11月, 中国气象局监测网络司及中国气象学会秘书处. [6] Hill R J, Clifford S F, Lawrence R S.Refractive-index and absorption fluctuations in the infrared caused by temperature, humidity and pressure fluctuations, J.Opt.Soc.Amer, 1980, 70 :1192-1205. doi: 10.1364/JOSA.70.001192 [7] Andreas E L.Two-wavelength method of measuring path-averaged turbulent surface heat fluxes.J.A tmos.Ocean.Tech., 1989, 6 :280-292. doi: 10.1175/1520-0426(1989)006 & lt; 0280:TWMOMP & gt; 2.0.CO; 2 [8] Wang T I, Ochs G R, Clifford S F.A saturation resistant optical scintillometer to measure Cn2.J.Op t.Soc.Amer, 1978, 68 :334-338. [9] Wesely M L.The combined effect of temperature and humidity on the refractive index.J.Appl.Meteor., 1976, 15 :43-49. doi: 10.1175/1520-0450(1976)015 & lt; 0043:TCEOTA & gt; 2.0.CO; 2 [10] Kohsiek W.Measuring CT2, Cq2 and CTq in the unstable surface layer, and relations to the vertical fluxes of heat andmoisture.Boundary-Layer Meteor., 1982, 24 :89-107. doi: 10.1007/BF00121802 [11] Wyngaard J C, Izumi Y, Collins S A Jr.Behavior of the refractive index structure parameter near the ground.J.Opt.Soc.Amer., 1971, 61 :1646-1650. doi: 10.1364/JOSA.61.001646 [12] de Bruin H A R, Kohsiek W, Van den Hurk B J J M.A verification of some methods to determine the fluxes of momentum, sensible heat, and water vapor using standard deviation and structure parameter of scalar meteorological quantities.Boundary-Layer Meteor., 1993, 63 :231-257. doi: 10.1007/BF00710461 [13] Panofsky H A, Dutt on J A.Atmospheric turbulence :Models and methods for engineering applications.New York :John Wiley & Sons, 1984.397. [14] Meijninger W M L, de Bruin H A R.The sensible heat fluxes over irrigated areas in western Turkey determined with a large aperture scintillometer.Journal of Hydrology, 2000, 229 :42-49. doi: 10.1016/S0022-1694(99)00197-3 [15] McAneney K J, Green A E.Ast ill M S.Large-aperture scintillometry :the homogeneous case.Agricultural and ForestMeteorology, 1995, 76 :149-162. -
下载:
图(5)
计量
- 摘要浏览量: 2656
- HTML全文浏览量: 543
- PDF下载量: 1997
- 被引次数: 0
