基于TSEB模型的黄河三角洲蒸散量估算

doi:10.11873/j.issn.1004-0323.2012.1.58

遥感技术与应用

2012, Vol. 27

Issue (1): 58-67 DOI: 10.11873/j.issn.1004-0323.2012.1.58

模型与反演

基于TSEB模型的黄河三角洲蒸散量估算

李贺,王红,孔岩,李玲

(河海大学地球科学与工程学院,江苏南京 210098)

Estimation of Evapotranspiration in Yellow River Delta Wetland based on Two=Source Energy Balance (TSEB) Model

Li He,Wang Hong,Kong Yan,Li Ling

(School of Earth Sciences and Engineering Hohai University,Nanjing 210098,China)

全文: PDF

摘要：

蒸散发作为湿地生态系统中地—气间水热交换的主要方式,很大程度上影响着湿地的水热平衡,合理准确地估算蒸散发量,对湿地生态系统的水分循环、能量平衡以及科学管理具有重要意义。黄河三角洲湿地作为世界上暖温带最广阔、最完整和最年轻的河口湿地生态系统,既是气候变化的敏感区,也是生态环境的脆弱区。针对其地理位置特殊、水资源供需矛盾尖锐等特点,利用SEBAL(Surface Energy Balance Algorithm for Land)和TSEB(Two-Source Energy Balance)模型,对黄河三角洲湿地蒸散发量进行估算:首先利用SEBAL模型计算地表的特征参数和各地表通量,然后利用TSEB模型分离土壤和植被,分别计算黄河三角洲湿地瞬时的土壤蒸发、植被蒸腾和土壤植被总蒸散发量,利用积分关系法进行时间尺度转换,得到日蒸散量。利用气象站实测蒸发值和FAO Penman\|Monteith公式计算的作物系数,对遥感估算结果进行直接和间接精度评价。结果表明反演的蒸散发结果合理,精高较高。分析蒸散的空间分布及不同地表类型的蒸散特性,对比分析芦苇沼泽和芦苇草甸的不同蒸散特点,结果表明基于两模型耦合的方法可用于黄河三角洲湿地蒸散量估算。

关键词： 蒸散发; SEBAL; TSEB; FAO Penman-Monteith

Abstract:

Evapotranspiration(ET)as the main form of exchanges between the water and heat to the soil—atmosphere of the wetland ecosystem greatly affects the water thermal equilibrium.Estimation of the evaporation quantity reasonably and accurately is one of great significance to study hydrologic recycle,energy balance and scientific management of the wetland ecosystem.Wetland in Yellow River Delta(YRD),which is the most integrated,broadest,youngest wetland ecological system in warm temperate zone of the earth,is not only sensitive to climate change,but also fragile to the environment change.Remote sensing technique was used to estimate ET in YRD in our case study.Coupling the model of Surface Energy Balance Algorithm for Land(SEBAL)and Two=Source Energy Balance(TSEB),SEBAL was used to calculate land surface characteristic parameters and flux,and TSEB was used to calculate vegetation transpiration,soil evaporation and total ET separately of YRD by Considering the inner structure of the surface layer which could be divided into two sub layers representing soil and vegetation.Actual evapotranspiration of the study area was meatured from stations and calculated with Penman=Monteith equation to compare with results from remote sensing,which showed that the result is reasonable.Then the spatial distribution of the daily ET was analyzed and the characteristics of ET with different features,especially with the typical vegetation of reed marshes and meadows,were also analyzed to help realize the wetland conditions.The results illuminates that daily ET estimated is reasonable.The method can be used for the accurate estimation of ET in YRD.

Key words: Evapotranspiration SEBAL TSEB FAO Penman=Monteith

收稿日期: 2011-04-18 出版日期: 2012-03-22

P 332.2

基金资助:

国家自然科学基金项目(40871230),国家水体污染控制与治理科技重大专项(2008ZX07526-007)。

通讯作者: 王红(1968-),女,江苏南通人,博士,副教授,主要从事湿地生态系统健康检测的研究。Email:hongwang@hhu.edu.cn。

作者简介: 李贺(1987-),男,江苏徐州人,硕士研究生,主要从事湿地生态水文方面的研究。Email:76044708@qq.com。

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引用本文:

李贺,王红,孔岩,李玲. 基于TSEB模型的黄河三角洲蒸散量估算[J]. 遥感技术与应用, 2012, 27(1): 58-67.

Li He,Wang Hong,Kong Yan,Li Ling . Estimation of Evapotranspiration in Yellow River Delta Wetland based on Two=Source Energy Balance (TSEB) Model. Remote Sensing Technology and Application, 2012, 27(1): 58-67.

链接本文:

http://www.rsta.ac.cn/CN/10.11873/j.issn.1004-0323.2012.1.58 或 http://www.rsta.ac.cn/CN/Y2012/V27/I1/58

［1］Lin Wantao.Adjustment Action of Ecosystem in Global Ch=ange Climatic and Environmental Research(in Chinese)［J］.2005,10(2):275=280.［林万涛.生态系统在全球变化中的调节作用［J］.气候与环境研究,2005,10(2):275=280.］
［2］Winter T C.A Physiographic and Climatic Framework for Hydrological Studies of Wetlands［C］//Robarts R D,Bothwell M L.Aquatic Ecosystems in Semi=arid Regions:Implications for Resource Management.Enviroment Canada:NHRI Symposium Series,1992:127=148.
［3］Mitsch W J,Gosselink J G.Wetlands［M］.New York:Van Nostrand Reinhold Company,1986.
［4］Wessel D A,Rouse W R.Modelling Evaporation from Wetland Tundra［J］.Boundary=layer Meteorology,1993,68(1):109=130.
［5］Sánchez=Carrillo S,Angeler D G,Sanchez=Andres R,et al.Evapotranspiration in Semi=arid Wetlands:Relationships between Inundation and the Macrophyte=cover:Open=water Ratio［J］.Advances in Water Resources,2004,27(6):643=655.
［6］Kellner E.Surface Energy Fluxes and Controls of Evapotranspiration from a Swedish Sphagnum Mire［J］.Agricultural and Forest Meteorology,2001,110(2):101=123.
［7］Judy Z D,Richard L S,Donatella S,et al.A Review of Models and Micrometeorological Methods Used to Estimate Wetland Evapotranspiration［J］.Hydrological Process,2004,18:2071=2101.
［8］Jia Zhijun,Song Changchun,Wang Yuesi,et al.The Evapotranspiration Research of Typical Marshes in Sanjiang Plain［J］.Climate and Environmental Research,2007,12(4):496=502.［贾志军,宋长春,王跃思,等.三江平原典型沼泽湿地蒸散量研究［J］.气候与环境研究,2007,12(4):496=502.］
［9］Tian Guoliang.Thermal Infrared Remote Sensing［M］.Beijing:Publishing House of Electronics Industry,2006.［田国良.热红外遥感［M］.北京:电子工业出版社,2006.］
［10］Jackson R D,Idso S B,Reginato R J,et al.Canopy Temperature as a Cropwater Stress Indication［J］.Water Resources,1981,17(4):1133=1138.
［11］Liu Sanchao,Zhang Wanchang,Gao Maofang,et al.Research of Surface Evapotranspiration based on the Distributed Hydrological Model and Remote Sensing［J］.Geographical Science,2007,27(3):354=358.［刘三超,张万昌,高懋芳,等.分布式水文模型结合遥感研究地表蒸散发［J］.地理科学,2007,27(3):354=358.］
［12］Liu Yani,Wu Jianjun,Xia Hong,et al.Summarizing the Me=thods of Double Model by Remote Sensing to Research the Surface Evapotranspiration［J］.Arid Land Geography,2005,28(1):65=71.［刘雅妮,武建军,夏虹,等.地表蒸散遥感反演双层模型的研究方法综述［J］.干旱区地理,2005,28(1):65=71.］
［13］Jackson R D,Reginato R J,Idso S B.Wheat Canopy Temperature:A Practical Tool for Evaluating Water Requirements［J］.Water Resources,1977,13(3):651=656.［14］Bastiaanssen W G M,Menenti M,Feddes R A,et al.A Remote Sensing Surface Energy Balance Algorithm for Land(SEBAL)1 Formulation［J］.Journal of Hydrology,1998:198=213.
［15］Bastiaanssen W G M,Pelgrum H,Wang J,et al.A Remote Sensing Surface Energy Balance Algorithm for Land(SEBAL)2 Validation［J］.Journal of Hydrology,1998:212=229.
［16］Jia Yangwen,Wang Hao,Ni Guangheng,et al.Theory and Practice of Distributed Hydrologic Model［M］.Beijing:China Water Conservancy and Hydropower Press,2005.［贾仰文,王浩,倪广恒,等.分布式流域水文模型原理与实践［M］.北京:中国水利水电出版社,2005.］
［17］Zhang Renhua,Sun Xiaomin,Zhu Zhilin,et al.Surface Evapotranspiration of Remote Sensing Information Model based on Differential Thermal Inertia and the Validation of Sand Areas in Gansu Province［J］.China Science D Series,2002,32(12):1041=1051.［张仁华,孙晓敏,朱治林,等.以微分热惯量为基础的地表蒸发全遥感信息模型及在甘肃沙坡头地区的验证［J］.中国科学(D辑),2002,32(12):1041=1051.］
［18］Liu Jingtao,Liu Shirong.Advances and Perspective in Evapotranspiration Studies［J］.Scientla Silvae Sinicae,2006,42(6):108=113.［刘京涛,刘世荣.植被蒸散研究方法的进展与展望［J］.林业科学,2006,42(6):108=113.］
［19］Wu Xianing,Hu Tiesong,Wang Xiugui,et al.Review of Estimatingand Measuring Regional Evapotranspiration［J］.Transactions of the CSAE,2006,22(10):257=262.［武夏宁,胡铁松,王修贵,等.区域蒸散发估算测定方法综述［J］.农业工程学报,2006,22(10):257=262.］
［20］Su Z.The Surface Energy Balance System (SEBS) for Estimation of Turbulent Heat Fluxes［J］.Hydrology and Earth System Sciences,2002,(6):85=89.
［21］Su Z.Remote Sensing of Land Use and Vegetation for Mesoscale Hydrological Studies［J］.International Journal of Remote Sensing,2000,(2):213=233.
［22］Akbari M,Toomanian N,Droogers P,et al.Monitoring Irrigation Performance in Esfahan,Iran,Using NOAA Satellite Imagery［J］.Agricultural Water Management,2007,88:99=109.
［23］Allen R G,Morse A,Tasumi M,et al.Evapotranspiration from Landsat(SEBAL)for Water Rights Management and Compliance with Multi=state Water Compacts［C］//IEEE Geoscience and Remote Sensing Symposium.IGARSS 01,Sydney,2001:830=833.
［24］Quattrochi D A,Luvall J C.Thermal Remote Sensing in Land Surface Processes［C］//Kustas W P,Norman J M,Schmugge T J.Mapping Surface Energy Fluxes with Radiometric Temperature.Boca Raton:Taylor and Francis CRC Press,2004.
［25］Zhang Wanchang,Gao Yongnian.Estimation of Regional Evapotranspiration of Soil=vegetation System based on Two=Source Energy Balance［J］.Geographical Science,2009,29(4):523=528.［张万昌,高永年.区域土壤植被系统蒸散发二源遥感估算［J］.地理科学,2009,29(4):523=528.］
［26］Pan Jinghu,Liu Chunyu.Retrieving Evapotranspiation of Loess Hilly=gully Region Using TSEB Parallel Model based on Remote Sensing Image［J］.Remote Sensing Technology and Application,2010,25(2):183=188.［潘竟虎,刘春雨.基于TSEB 平行模型的黄土丘陵沟壑区蒸散发遥感估算［J］.遥感技术与应用,2010,25(2):183=188.］
［27］Shuttleworth W J,Wallace J S.Evaporation from Sparse Crops—An Energy Combination Theory［J］.Quarterly Journal of the Royal Meteorological Society,1985,111:839=855.
［28］Norman J M ,Kustas W P.A Two=source Approach for Estimating Soil and Vegetation Energy Fluxes from Observations of Directional Radiometric Surface Temperature［J］.Agricultural and Forest Meteorology,1995,(77):263=293.
［29］Lhomme J P,Chehbouni A.Comments on Dual=source Vegetation=atmosphere Transfer Models［J］.Agricultural and Forest Meteorology,2004,94:269=273.
［30］Timmermans W J,Kustas W P,Anderson M C,et al.An Intercomparison of the Surface Energy Balance Algorithm for Land (SEBAL) and the Two=Source Energy Balance (TSEB) Modeling Schemes［J］.Remote Sensing of Environment,2007,108:369=384.
［31］Yao W,Han M,Xu S G.Estimating the Regional Evapotranspiration in Zhalong Wetland with the Two=Source Energy Balance (TSEB) Model and Landsat7/ETM+ Images［J］.Ecological Informatics,2010,5:348=358.
［32］Zhang Changchun,Wang Xiaoyan,Shao Jingli.Estimated Evapotranspiration based on NOAA Data in the Yellow River Delta［J］.Resources Science,2005,27(1):86=91.［张长春,王晓燕,邵景力.利用NOAA 数据估算黄河三角洲区域蒸散量［J］.资源科学,2005,27(1):86=91.］
［33］Pan Zhiqiang,Liu Gaohuan.Evapotranspiration Research of Yellow River Delta Using Remote Sensing Method［J］.Geo=information Science,2003,(3):91=96.［潘志强,刘高焕.黄河三角洲蒸散的遥感研究［J］.地球信息科学,2003,(3):91=96.］
［34］Xi Ge,Liu Shaomin,Jia Li.Estimation of Regional Evapotranspiration and Ecological Water Reqirement of Vegetation by Remote Sensing in the Yellow River Delta Wetland［J］.Acta Ecoologica Sinica,2008,28(11):5356=5369.［奚歌,刘绍民,贾立.黄河三角洲湿地蒸散量与典型植被的生态需水量［J］.生态学报,2008,28(11):5356=5369.］
［35］Li Fapeng,Xu Zongxue,Li Jingyu.Characteristics of the Spatial and Temporal Distribution for Regional Evapotranspiration in the Yellow River Delta based on MODIS Data［J］.Agriculture and Engineering,2009,25(2):113=120.［李发鹏,徐宗学,李景玉.基于MODIS 数据的黄河三角洲区域蒸散发量时空分布特征［J］.农业工程学报,2009,25(2):113=120.］
［36］Liu Gaohuan,Hans D E R.Atlas of Sustainable Development in Yellow River Delta［M］.Beijing:Surveying and Mapping Press,1997.［刘高焕,汉斯·德罗斯特.黄河三角洲可持续发展图集［M］.北京:测绘出版社,1997.］
［37］Anderson M C,Norman J M,Diak G R,et al.A Two=source Time=integrated Model for Estimating Surface Fluxes from Thermal Infrared Satellite Observations［J］.Remote Sensing of Environment,1997,60(2):195=216.
［38］Priestly C H B,Taylor R J.On the Assessment of Surface Heat Flux and Evaporation Using Large=scale Parameters［J］.Monthly Weather Review,1972,100:81=92.
［39］Xie Xianqun.Estimation of the Crop Daily Evapotranspiration Using Instantaneous Surface Temperature［J］.Environment Remote Sensing,1991,6(4):253=259.［谢贤群.遥感瞬时作物表面温度估算农田全日蒸散总量［J］.环境遥感,1991,6(4):253=259.］
［40］Hong J L,Fu G B,Guo Z N,et al.Experimental Research on the Water=surface Evaporation of Nansi Lake in Shandong Province［J］.Geographical Research,1996,15(3):42=49.
［41］Allen R G,Pereira L S,Raes D,et al.Crop Evapotranspiration:Guideline for Computing Crop Requirement［M］.Italy:FAO Irrigation and Drainage Paper No.56,FAO of UN Rome,1998:51=202.
［42］Evans R G.National Irrigation Symposium,ASAE Phoenix,ASCE［C］//Walter I A,Allen R G,Elliott R,et al.ASCE Standardized Reference Evapotranspiration Equation,2000:1=6.
［43］Wes=warren D E,Tang=lindsey G.The Ministry of Water Resources International Cooperation Department,eds.Handbook of National Irrigation Engineering［M］.Beijing:China WaterPower Press,1998.［韦斯·沃伦德,唐·格兰姆斯.水利部国际合作司等编译.美国国家灌溉工程手册［M］.北京:中国水利水电出版社,1998.］

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