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DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 謝正義(Cheng-I Hsieh) | |
dc.contributor.author | Cheng-Wei Huang | en |
dc.contributor.author | 黃丞瑋 | zh_TW |
dc.date.accessioned | 2021-06-14T17:16:32Z | - |
dc.date.available | 2008-08-06 | |
dc.date.copyright | 2008-08-06 | |
dc.date.issued | 2008 | |
dc.date.submitted | 2008-07-25 | |
dc.identifier.citation | References (Chapter2)
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Malek,E., 1993, Rapid changes of the surface soil heat flux and its effects on the estimation of evapo-transpiration, J. Hydrol., 142, 89-97. Miller, K. S. and Ross, B., 1993, An Introduction to the Fractional Calculus and Fractional Differential Equations, Wiley, New York. Ogee, J., E. Lamaud, Y. Brunet, P. Berbigier, J.M. Bonnefond, 2001, A long-term study of soil heat flux under a forest canopy, Agric. Forest Meteo., 106, 173-186. Stull, R. B., 1988, An introduction to Boundary Layer Meteorology, 666 pp., Kluwer Academic Publishers, Dordrecht, the Netherland. Wang, J. and R. L. Bras, 1999, Ground heat flux estimated from surface soil temperature, J. Hydrol., 216, 214-226. Zhang, H. F., X. S. Ge, H. Ye, and D. S. Jiao, 2007, Heat conduction and heat storage characteristics of soils, Applied Thermal Engineering, 27,369-373. Reference (Chapter 3) Andreas, E. L., R. J. Hill, J. R. Gosz, D. I. Moore, W. D. Otto, and A. D. 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Rosenberg, 1978, Local and regional components of sensible heat advection. J. Appl. Meteorol., 17, 955-963. Brunet, Y., B. Itier, J. Mcaneney, and P. J. Lagouarde, 1994, Downwind evolution of scalar fluxes and surface resistance under conditions of local advection. PartⅠ: a reappraisal of boundary conditions. Agric. For. Meteorol., 71, 211-225. Brunet, Y., B. Itier, J. Mcaneney, and P. J. Lagouarde, 1994, Downwind evolution of scalar fluxes and surface resistance under conditions of local advection. PartⅡ: measurements over barely. Agric. For. Meteorol., 71, 227-245. de Bruin, H. A. R., W. Kohisek, and B. J. J. M. Van Den Hurk, 1993, 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 Meteorol., 63, 231-257. Du, D.-Z., and Panos M. Pardalos, 1998, Handbook of Combinatorial Optimization Volume 3. Glover, F., 1993, A user’s guide to tuba search. Annals of Operations Research, 41, 3-28. Hipps, L. E. and D. F. Zehr, 1995, Determination of evaporation from integrated profiles of humidity and temperature over an inhomogeneous surface. Boundary-Layer Meteorol., 75, 287-299. Hunt, J. C. R. and A. H. Weber, 1979, A Lagrangian statistical analysis of diffusion from a ground-level source in a turbulent boundary layer. Quart. J. R. Met. Soc.,105, 423-443. Kroon, L. J. M., 1985, Profile derived fluxes over inhomogeneous terrain: a numerical approach . PhD. Thesis. Wageningen Agricultural University, 159 pp. Kroon, L. J. M. and H. A. R. de Bruin, 1993, Atmosphere-vegetation interaction in local advection conditions: effect of lower boundary conditions. Agric. For. Meteorol., 64, 1-28. Kroon, L. J. M. and H. A. R. de Bruin, 1995, The crau field experiment: turbulent exchange in the surface layer under conditions of strong local advection. Journal of hydrology, 166, 327-351. McAneney, K. J., Y. Brunet, and B. Itier, 1994, Downwind evolution of transpiration by two irrigated crops under conditions of local advection. Journal of hydrology, 161, 375-388. McNaughton, K. G., 1976, Evaporation and advection Ⅱ: evaporation downwind of a boundary separating regions having different surface resistances and available energies. Quart. J. R. Met. Soc., 102, 193-202. Philip, J. R., 1959, The theory of local advection. J. Meteorol., 16, 535-547. Philip, J. R., 1987, Advection, evaporation and surface resistance. Irrig. Sci., 8, 101-114. Rao, K. S., J. C. Wyngaard, and O. R. Cot , 1974, Local advection of momentum, heat, and moisture in micrometeorology. Boundary-Layer Meteorol., 7, 331-348. Rider, N. E., J. R. Philip, E. F. Bradley, 1963, The horizontal transport of heat and moisture- a micrometeorological study. Quart. J. R. Met. Soc., 89, 507-531. Tillman, J. E., 1972, The indirect determination of stability, heat and momentum fluxes in the atmosphere boundary layer from simple scalar variables during dry unstable conditions. J. App. Meteorol., 11, 783-792. Weaver, H. L., 1990, Temperature and humidity flux-variance relations determined by one-dimensional eddy correlation. Boundary-Layer Meteorol., 53, 77-91. Wilson, J. D., T. K. Flesch, and L. A. Harper, 2001, Micro-meteorological methods for estimating surface exchange with a disturbed windflow. Agric. For. Meteorol., 107, 207-225. Zerme ñ o, A., 1994, The effect of advection of heat and saturation deficit on the energy balance of a vegetated surface. PhD. Dissertation, Utah State Univ., Logan, UT. Zerme ñ o, A. and L. E. Hipps, 1997, Downwind evolution of surface fluxes over vegetated surface during local advection of heat and saturation deficit. Journal of hydrology, 192, 189-210. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/41094 | - |
dc.description.abstract | 在生物圈與大氣之間的交互作用中,地表的動量通量、熱通量、水汽通量以及二氧化碳通量為相當重要的參數。本論文分別討論了推估土壤熱通量與蒸發散量的方法。第一部份,利用只需要單一層土壤溫度即可推估土壤熱通量的兩種方法(the traditional sinusoidally analytical method and the half-order time derivative method ,Wang and Bras, 1999)進行長期的土壤熱通量推估。研究結果發現,由於傳統解析解方法的假設使得土壤熱通量呈正弦函數變化,所以利用傳統解析解方法推估土壤熱通量的結果不太良好﹔然而,利用實際量測到的土壤熱通量與half-order method推估結果比較,顯示出此方法用於長期土壤熱通量推估可得到非常良好的結果。第二部份,本研究提出一個二維的Lagrangian analytical dispersion模式,利用此模式以及下風處某個位置量測到的水汽濃度剖面可以推求得地表的蒸發散量。研究的結果顯示出此模式可以在local advection的狀況下,推求得地表蒸發散量隨下風處距離增加的變化情形。 | zh_TW |
dc.description.abstract | Surface fluxes of momentum, heat, water vapor, carbon dioxide and other scalars (e.g., CH4) are important parameters for understanding of the biosphere-atmosphere interactions. This study focuses on quantifying two of these important parameters: the soil heat flux and water vapor flux. In the first part of this study, long-term estimation of soil heat flux from single layer soil temperature was carried out by the traditional sinusoidally analytical method and the half-order time derivative method of Wang and Bras (1999). Our results pointed that the analytical method did not predict the soil heat flux well due to the sinusoidal assumption for soil heat flux’s temporal variation was not valid. While good agreement between soil heat flux measurements and predictions by the half-order time derivative method was found. In the second part of this study, a two-dimensional Lagrangian analytical dispersion model in conjunction with an inverse approach was proposed for inferring surface evapotranspiration rate from the mean humidity profile under local advection conditions. Our results showed that this approach was able to reproduce the measured downwind evolution of surface evapotranspiration rate (water vapor flux) under local advection conditions. | en |
dc.description.provenance | Made available in DSpace on 2021-06-14T17:16:32Z (GMT). No. of bitstreams: 1 ntu-97-R95622004-1.pdf: 12379065 bytes, checksum: 8ab12fb94f37fca5092a7bd86969a348 (MD5) Previous issue date: 2008 | en |
dc.description.tableofcontents | Table of Contents
Acknowledgement …………………………………………… i Abstract ………………………………………………………… ii Chinese Abstract ………………………………………………… iii List of Figures …………………………………………………vi List of Tables ………………………………………………… ix Chapter 1 Preliminaries …………………………………… 1 Chapter 2 Long-Term Estimation of Soil Heat Flux by Single Layer Soil Temperature 3 2.1 Introduction …………………………………………………… 3 2.2 Methods ………………………………………………………… 5 2.2.1 Traditional sinusoidally analytical method ……………… 5 2.2.2 Half-order time derivative method ………………………… 6 2.3 Experiment …………………………………………………… 9 2.4 Results and discussion …………………………………… 11 2.4.1 Surface energy flux characteristics ………………………… 11 2.4.2 Traditional sinusoidally analytical method estimation ……… 12 2.4.3 half-order time derivative method estimation ……………… 13 2.5 Conclusions ……………………………………………………… 17 Appendixes ……………………………………………………………… 18 References ……………………………………………………………… 21 Table ……………………………………………………………………… 23 Figures …………………………………………………………………… 26 Chapter 3 Estimation of Evapotranspiration Rate under Local Advection Condition … 36 3.1 Introduction ……………………………………………………… 36 3.2 Theory and methods …………………………………………… 39 3.2.1 Lagrangian statistical dispersion model …………………… 39 3.2.2 Solve the‘inverse problem’ ……………………………… 42 3.3 Material …………………………………………………………… 44 3.4 Results and discussion ………………………………………… 46 3.5 Conclusions ……………………………………………………… 50 Appendixes ……………………………………………………………… 51 References ……………………………………………………………… 53 Figures …………………………………………………………………… 56 | |
dc.language.iso | en | |
dc.title | 地表土壤熱通量及蒸發散量之研究 | zh_TW |
dc.title | The Study of Soil Heat Flux and Evapotranspiration at The Surface | en |
dc.type | Thesis | |
dc.date.schoolyear | 96-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 朱佳仁(Chia-Ren Chu),張倉榮(Tsang-Jong Chang),陳明志(Ming-Jyh Chern) | |
dc.subject.keyword | 土壤熱通量,half-order method,土壤溫度,Lagrangian analytical dispersion model,蒸發散, | zh_TW |
dc.subject.keyword | soil heat flux,half-order method,soil temperature,Lagrangian analytical dispersion model,evapotranspiration, | en |
dc.relation.page | 54 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2008-07-28 | |
dc.contributor.author-college | 生物資源暨農學院 | zh_TW |
dc.contributor.author-dept | 生物環境系統工程學研究所 | zh_TW |
顯示於系所單位: | 生物環境系統工程學系 |
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