基于SEBAL模型遥感反演的蒸散量时空分布特征研究
Spatiotemporal Distribution Characteristics of Evapotranspiration Based on SEBAL Model and Remote Sensing
DOI: 10.12677/JWRR.2020.94043, PDF,    科研立项经费支持
作者: 乔 鹏, 王 岚:吐鲁番市水资源管理中心,新疆 吐鲁番
关键词: 遥感蒸散发SEBAL模型吐鲁番市Remote Sensing Evapotranspiration SEBAL Model Turpan City
摘要: 应用2014~2018年MODIS产品、气象观测数据、DEM等数据资料,采用SEBAL模型估算分析吐鲁番市的蒸散特征。结果表明:2014~2018年吐鲁番市平均年总蒸散量为3.25 × 109 m3,且蒸散量时空差异显著,97%的蒸散量集中在4~10月份,年际间呈波动下降趋势;对于不同土地利用类型,单位面积年蒸散量耕地 > 城乡、工矿及居民用地 > 林地 > 草地 > 水域 > 其他用地,其中草地及其他用地所占面积较大,年总蒸散量最高,草地、耕地及其他用地三者蒸散量占总蒸散90%以上,水域多为积雪区、季节性水域且面积较小,年总蒸散量及单位面积年均蒸散量均不高。
Abstract: The evapotranspiration characteristics in Turpan city were estimated and analyzed based on SEBAL mod-el using MODIS, DEM and meteorological observation data during 2014-2018. The results show that the average total evapotranspiration is 3.25 × 109 m3 with significant spatiotemporal difference. 97% of the total evapotranspiration is concentrated in April-October which shows a fluctuating downward trend. For different types of land use, the average annual evapotranspiration per unit area is decreased in following order: cultivated land is greater than urban, industrial, mining lands, and residential land is greater than forestland, grassland, waters area, and other land. Grassland and other land annual total evapotranspiration are the highest due to they occupy larger area. Grassland, cultivated land and other land account for more than 90% of annual total evapotranspiration. Most of the water areas are snow-covered, seasonal, or small area, so the annual total and average evapotranspiration per unit area are not too large.
文章引用:乔鹏, 王岚. 基于SEBAL模型遥感反演的蒸散量时空分布特征研究[J]. 水资源研究, 2020, 9(4): 411-420. https://doi.org/10.12677/JWRR.2020.94043

参考文献

[1] XU, C. Y., SINGH, V. P. Evaluation of three complementary relationship evapotranspiration models by water balance approach to estimate actual regional evapotranspiration in different climatic region. Journal of Hydrology, 2005, 308: 105-121.[CrossRef
[2] 邱国玉, 熊育久. 水与能: 蒸散发、热环境及其能量收支[M]. 北京: 科学出版社, 2014. QIU Guoyu, XIONG Yujiu. Water versus energy: Evapotranspiration, thermal environment, energy budget. Beijing: Science Press, 2014. (in Chinese)
[3] MENENTI, M., CHOUDHURY, B. J. Parameterization of land surface evaporation by means of location dependent potential evaporation and surface temperature range. In BOLLE H. J., FEDDES, R. A. and KALMA, J. D. Exchange processes at the land surface for a range of space and time scales (Vol. 212). Wallingford: IAHS Publ., 1993: 561-568.
[4] BASTIAANSSEN, W. G. M., MENENTI, M., FEDDES, R. A., et al. A remote sensing surface energy balance algorithm for land (SEBAL): Part 1 formulation. Journal of Hydrology, 1998, 212: 198-213. [Google Scholar] [CrossRef
[5] SU, Z. The surface energy balance system (SEBS) for estimation of turbulent heat fluxes. Hydrology and Earth System Sciences, 2002, 6(1): 85-99. [Google Scholar] [CrossRef
[6] ALLEN, R. G., TASUMI, M. and TREZZA, R. Satellite-based energy balance for mapping evapotranspiration with internalized calibration (METRIC) model. Journal of Irrigation and Drainage Engineering, 2007, 133(4): 380-394. [Google Scholar] [CrossRef
[7] WANG, J. M., BASTIAANSSEN, W. G. M., MA, Y. M., et al. Aggregation of land surface parameters in the oasis-desert systems of north-west China. Hydrological Processes, 1998, 12(13/14): 2133-2147. [Google Scholar] [CrossRef
[8] 李宝富, 陈亚宁, 李卫红, 等. 基于遥感和SEBAL模型的塔里木河干流区蒸散发估算[J]. 地理学报, 2011, 66(9): 1230-1238. LI Baofu, CHEN Yaning, LI Wenhong, et al. Evapotranspiration estimation of the Tarim River Basin with SEBAL and remote sensing. Acta Geographica Sinica, 2011, 66(9): 1230-1238. (in Chinese)
[9] 杜嘉, 张柏, 宋开山, 等. 基于MODIS产品和SEBAL模型的三江平原日蒸散量估算[J]. 中国农业气象, 2010, 31(1): 104-110, 162. DU Jia, ZHANG Bai, SONG Kaishan, et al. Study on daily evapotranspiration estimation of Sanjiang Plain based on MODIS product and SEBAL model. Chinese Journal of Agrometeorology, 2010, 31(1): 104-110, 162. (in Chinese)
[10] 周妍妍, 郭晓娟, 郭建军, 等. 基于SEBAL模型的疏勒河流域蒸散量时空动态[J]. 水土保持研究, 2019, 26(1): 168-177. ZHOU Yanyan, GUO Xiaojuan, GUO Jianjun, et al. Spatiotemporal dynamics of evapotranspiration in Shule River Basin based on SEBAL model. Research of Soil and Water Conservation, 2019, 26(1): 168-177. (in Chinese)
[11] 李吉玫, 张毓涛. 近60年新疆吐鲁番盆地坎儿井衰败的影响因素及环境效应[J]. 水土保持通报, 2013, 33(5): 239-244. LI Jimei, ZHANG Yutao. Influence factors for Karez abandonment and its environmental effects in Turpan Basin of Xinjiang au-tonomous region over last 60 years. Bulletin of Soil and Water Conservation, 2013, 33(5): 239-244. (in Chinese)
[12] 傅小锋. 吐鲁番盆地水资源利用与绿洲经济发展探讨[J]. 地理研究, 1996(4): 74-81. FU Xiaofeng. The utilization of water resources and the oasis economic development in Turpan Basin. Geographical Research, 1996(4): 74-81. (in Chinese)
[13] 曹培武, 白云岗, 张江辉. 吐鲁番地区水资源可持续利用的对策与建议[J]. 新疆水利, 2011(5): 1-5. CAO Peiwu, BAI Yungang and ZHANG Jianghui. Countermeasure and suggestion of Turpan water resource sustainable use. Xinjiang Water Resources, 2011(5): 1-5. (in Chinese)
[14] 伏吉芮, 瓦哈甫•哈力克, 姚一平. 协调模式下的吐鲁番地区水资源合理供求模式[J]. 南水北调与水利科技, 2017, 15(1): 67-71, 144. FU Jirui, WAHAP HALIK and YAO Yiping. Analysis of rational supply and demand of water resources in Turpan area in the coordination mode. South-to-North Water Transfers and Water Science & Technology, 2017, 15(1): 67-71+144. (in Chi-nese)
[15] BASTIAANSSEN, W. G. M. SEBAL-based sensible and latent heat fluxes in the irrigated Gediz Basin, Turkey. Journal of Hydrology, 2000, 229(1-2): 87-100. [Google Scholar] [CrossRef
[16] BRUTSAERT, W. Evaporation into the atmosphere—Theory, history, and application. Dordrecht: D. Reidel Publishing Company, 1982.
[17] PAULSON, C. A. The mathematical representation of wind speed and temperature profiles in the unstable atmos-pheric surface layer. Journal of Applied Meteorology, 1970, 9: 857-861. [Google Scholar] [CrossRef
[18] WEBB, E. K. Profile relationships: The log-linear range, and extension to strong stability. Quarterly Journal of the Royal Meteorological Society, 1970, 96: 67-90.[CrossRef
[19] ALLEN, R. G., PEREIRA, L. S., RAES, D., et al. Crop evapotranspiration: Guidelines for computing crop water requirements. FAO irrigation and DRAINAGE Paper No. 56. Rome: United Nations Food and Agriculture Organization, 1998.