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بهبود تخمین سیلاب مدل HEC-HMS با روندیابی مکانی تبخیر-تعرق به‌وسیله الگوریتم سبس

نوع مقاله : مقاله پژوهشی

نویسندگان

1 دانشگاه هرمزگان

2 عضو هیأت علمی مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی فارس

3 معاون بخش تحقیقات حفاظت خاک و آبخیزداری، مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان فارس، سازمان تحقیقات، آموزش و ترویج کشاورزی،

چکیده

محدودیت‌های روش‌های فیزیکی و تجربی برآورد تبخیر-تعرق، کاربرد فن‌آوری سنجش از دور را برای حل معادله بیلان انرژی در سال‌های اخیر رایج ساخته است. در این پژوهش به‌منظور تدقیق عامل تبخیر-تعرق در مدل HEC-HMS و بهبود تخمین سیلاب، تعداد نه تصویر لندست هشت، داده‌های هواشناسی مربوط به ایستگاه محلی و مدل سبس، تبخیر-تعرق مربوط به پنج واقعه در دوره زمانی 1393 تا 1396 در حوزه‌آبخیز کلستان واقع در شمال‌غربی شیراز محاسبه و به کمک داده‌های فائو پنمن-مانتیس در یک پیکره‌ی آبی اعتبار‌سنجی شد. تبخیر در HEC-HMS شامل تبخیر مستقیم از آب و از سطح خاک و تعرق گیاهی به‌صورت یک ارتفاع متوسط تخمین زده می‌شود. در این پژوهش سعی شد با جایگزین کردن تبخیر-تعرق واقعی در مدل HEC-HMS، میزان رواناب حاصـل از بـارش با دقت بیشتری محاسبه شود. نتایج نشان داد پس از تدقیق تبخیر-تعرق، همبستگی سیلاب مدل با سیلاب اندازه‌گیری شده افزایش مشهودی داشته به طوری که R2 از 92 به 99 درصد و RMSE از 14/0 به 01/0 رسیده است. نتایج همچنین نشانگر آن است که استفاده از تصاویر ماهوارهای و الگوریتم سبس ابزار مناسبی برای برآورد تبخیر-تعرق واقعی می‌باشد. این تحقیق با در نظر گرفتن تشخیص کارایی SEBS در تعیین پراکنش مکانی و زمانی تبخیر-تعرق در یک منطقه کوهستانی و با هدف هیدرولوژیک، انجام شده است. چراکه محاسبه‌ی ET در مدل‌های هیدرلوژیک می‌تواند سبب بهبود نتایج و افزایش دقت مدل‌های مذکور شود.

کلیدواژه‌ها

عنوان مقاله [English]

Optimizing the Assessment of Runoff with HEC-HMS Model Using Spatial Evapotranspiration by SEBS model

نویسندگان [English]

  • maryam zare 1
  • Ommolbanin bazrafshan 1
  • Mojtaba Pakparvar 2
  • gholamreza Ghahari 3

1 hormozgan university

2 Researcher, Fars Agricultural & Natural Resources Research & Education Center

3 Soil Conservation and Watershed Management Research Department, Fars Agricultural and Natural Resources Research and Education Center, Agricultural Research, Education and Extension Organization (AREEO), Shiraz, Iran

چکیده [English]

Limitations of physical and experimental methods for estimating the evapotranspiration have been rationalized the employment of remote sensing technology to solve the energy balance equation in recent years. In this study, in order to investigate the evapotranspiration factor in the application of the HEC-HMS model and to optimize the flood estimation, using Landsat 8 Satellite Images (nine images) and the meteorological data related to the Kelestan Station and the SEBS Evapotranspiration Model for the period 2015-2017, ET values were calculated in the region of Kelestan Located in the Northwest of Shiraz, and the results were compared to the FAO Penman-Monteith equation to verify the accuracy of this model in the region of Kolding with water body. Evaporation in HEC-HMS including the direct evaporation of water, evaporation from soil surface, and transpiration of plants was estimated as an average elevation. In this study, we attempted to replace the actual evapotranspiration in the HEC-HMS model, The amount of runoff from the precipitation is calculated more accurately. The results showed that after scrutinizing the ET input, the simulated flood correlation with the measured flood was increased with R2 from 92 to 99%, and RMSE from 0.14 to 0.01, respectively. The results also indicated that the use of Landsat 8 Satellite Images and SEBS model is a suitable tool for estimating actual evapotranspiration in mountainous and field areas in hydrological studies. This research is for the performance of SEBS in determining the spatial and temporal distribution of evapotranspiration in a mountainous and hydrological area. Because the calculation of ET in hydrological models can improve the results and increase the accuracy of these models.

کلیدواژه‌ها [English]

  • Runoff
  • Evapotranspiration
  • Remote Sensing
  • FAO Penman-Monteith
  • Energy Balance
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مهندسی و مدیریت آبخیز
دوره 13، شماره 1
فروردین 1400
صفحه 81-97
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