Volume 23, Issue 69 (6-2023)
jgs 2023, 23(69): 425-438 |
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Ataei H, Ravarian M, Tashakori Hashemi S A. (2023). Application of SIMETAW simulation model for prediction of climate parameters in different regions of Iran. jgs. 23(69), : 22 doi:10.61186/jgs.23.69.425
URL: http://jgs.khu.ac.ir/article-1-3224-en.html
URL: http://jgs.khu.ac.ir/article-1-3224-en.html
1- Payamenoor University, Payamenoor University-KOhandej BL- Isfahan , hoo_ataei@yahoo.com
2- 32-yassaman2-Sajad Bl-MAshhad-khorasan Razavi
3- No 6-Khodaverdi 3-End of Kashani 12-MAshhad-Khorasan Razavi
2- 32-yassaman2-Sajad Bl-MAshhad-khorasan Razavi
3- No 6-Khodaverdi 3-End of Kashani 12-MAshhad-Khorasan Razavi
Abstract: (3631 Views)
So far, several models have been proposed for estimating different climate parameters, but due to the lack of valid and long-term data in some meteorological stations, some models have been difficult to use. The SIMETAV V.1.0 model has been developed in cooperation with the University of California Davis and the Water Resources Authority of California in 2005. The SIMETAW model is a new and innovative tool for the estimation of applied water evapotranspiration (ETAW). SIMETAW simulation model is presented to estimate potential evapotranspiration and also estimate the net amount of water required for irrigation (ETaw). In addition, using this model, you can simulate daily meteorological data from meteorological data. The simulation of daily weather information where there are only monthly averages is a great tool for filling out lost data. In this research, Simetaw simulation model predicts different climate parameters such as solar radiation, minimum and maximum temperature, wind speed, dew point, precipitation and evapotranspiration potential in four different semi-arid climate zones (Mashhad). Dry (Bandar Abbas), moderate and humid (Ramsar) and Mediterranean (Sanandaj) during the years (1967-2017). The results of these studies showed that SIMETAW model has high ability to simulate climate variables and has the highest model accuracy in precipitation simulation (R2 = 0.998) and maximum temperature (R2 = 0.997) for semi-arid climate (Mashhad) , Dew point (R2 = 0.998) for temperate and humid climate (Ramsar), for radiation (R2 = 0.998) and wind speed (R2 = 0.9) for Mediterranean climate (Sanandaj) and minimum temperature (R2 = 0.998) for warm and dry climates (Bandar Abbas).
According to the sensitivity analysis of SIMETAW model, the input parameters of the model are respectively their effect on potential evapotranspiration from maximum temperature, precipitation, dew point temperature and minimum temperature, solar radiation and wind speed.
Article number: 22
Type of Study: Research |
Subject:
climatology
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