Journal of Climate Research

Journal of Climate Research

Performance Analysis of SDSM in downscaling temperature in Khuzestan province

Document Type : Original Article

Authors
1 Department of Geography, Ahvaz Branch, Islamic Azad University, Ahvaz, Iran
2 Department of Geography, Science and Research Branch, Islamic Azad University, Tehran. Iran
3 Department of Climatology, Ahwaz Islamic Azad University, Ahvaz, Iran.
4 Assistant Professor, Department of Geography, Ahvaz Branch, Islamic Azad University, Ahvaz, Iran
Abstract
Introduction: By examining the trend of air temperature changes, it is possible to search for traces of climatic changes in the area of Iran. Temperature is one of the most important meteorological parameters that is used in many studies. This parameter is of special importance in climate change studies, as the increase in temperature is considered one of the most important human environmental issues. In this research, the purpose of the research is to look at the average temperature changes in the base and future period of Khuzestan province. The evaluation of the model and the reproduction of climatic variables and the perspective of the future climatic conditions are examined, and this question is raised: Is the Sdsm model in Khuzestan province highly accurate?

Materials and methods:The area studied in the current research is the synoptic stations of Khuzestan province. In this study, meteorological data including the values of minimum temperature, maximum temperature and average temperature for the studied period have been used. In this research, we used SDSM statistical micro-scale exponential model for temperature prediction and 6 synoptic stations of Khuzestan province, which had 45-year (1961-2005) and 40-year (1966-2005) climatic statistics, were selected. The outputs of the CanESM2 climate model have been used under RCP2.6 and RCP8.5 scenarios. The data of the base period (1961-2005) were used for the first 30 years of data (1961-1990) for calibration and the second 15 years (1991-2005) for the syntactic evaluation of the model performance. Error and accuracy measures are evaluated.

Results and discussion: MAE, NRMSE, RMSE, MSE and R2 were calculated based on the average values of the variables in each month. These values were obtained according to the daily temperature produced by the model and the observed values for calibration and validation data. The results showed that according to the NRMSE, the error rate in temperature estimation is acceptable (less than 10%) and is almost the same in all stations. The results showed that according to the high correlation coefficient of 87%, the performance of the model is confirmed. Finally, it indicates that the model has relatively good accuracy in estimating the climatic variable of temperature. In most stations, they overlap the most in the first months of the year, which is the reason for the accuracy of the model in the first months of the year. In the stations of Ahvaz, Bandar Mahshahr, Omidiye Aghajari and Bagh Malek in the first seven months of the year, the highest overlap and accuracy are included, and in the last five months of the year, the average retrospective temperature in these stations is 2.4, 2.4, 2.6 respectively. and 2.7 degrees Celsius shows the difference with the observational data. Dezful, Abadan and Shushtar stations have the highest overlap and accuracy in the first three months of the year and July. In the rest of the months, the average retrospective temperature in these stations is 2.6, 2 and 2 degrees Celsius, respectively, the difference with the data Shows observations. The temperature has increased in all periods and for the RCP2.6 scenario, it increases more than the RCP8.5 scenario. The highest RCP2.6 average temperature increase in Ahvaz is predicted to be 1.9 degrees and the lowest RCP8.5 increase is 0.2 degrees in Dezful and Shushtar stations. The average temperature in the forecast period with RCP2.6 and RCP8.5 scenarios is 26 and 25.7 degrees Celsius respectively, which shows an increase of 0.7 and 0.4 degrees compared to the previous period, and also the highest average temperature in the period Predicted with RCP2.6 and RCP8.5 scenarios and the observation period is approximately 28.2, 27.5 and 27.3 degrees Celsius corresponding to Shushtar station and the lowest average temperature is approximately 22.7, 22.6 and 22.2 degrees Celsius corresponding to Bagh Malek station respectively. In most of the studied stations, the increasing and decreasing trends of the observation and forecast period are similar. Aghajari station shows the most overlap. Shushtar, Abadan and Omidiye Aghajari stations have the highest temperature with an average temperature of 27.3, 26.5 and 26.4 degrees Celsius, respectively, and Bagh Malek station, which is located in the east of the province, has the lowest temperature with 20.9 degrees Celsius.

Conclusion: The most important results obtained from the performance evaluation of the SDSM model using statistical tests and various error measurement indicators showed that this model has been investigated in Khuzestan province and has the appropriate accuracy to simulate climate variables at the level of the studied region. It is absolutely necessary to evaluate the effects of global warming on the occurrence of climatic extremes. An increase in temperature has occurred in all studied stations in the coming period. In two scenarios, RCP2.6 (commitment of countries to reduce greenhouse gases) and RCP8.5 (in case of non-compliance to reduce greenhouse gases) were measured in the studied periods. Meanwhile, during the annual study period, the areas adjacent to the southern coasts of Iran will have the lowest temperature increase, so that the temperature increase in the stations located in the land is more than the stations in the coastal areas. The highest RCP2.6 average temperature increase in Ahvaz is predicted to be 1.9 degrees and the lowest RCP8.5 increase is 0.2 degrees in Dezful and Shushtar stations. In this research, the trends and types of seasonal changes have been investigated. The results obtained from the data analysis show that in all stations, in Khuzestan province in general, the average temperature parameter shows an increasing trend. Research has shown that the maximum temperature trend is an increasing trend in the base period of 1961-2005 and this trend will continue in the future periods. In the future periods, the temperature trend in the last few decades, the increase in the earth's temperature has upset the climate balance of the earth and has caused extensive climate changes in most areas of the earth, which is referred to as climate change. The minimum temperature is increasing, and as a result, it reduces the coldness of the air and moderates it.
Keywords

1.    Sabzegbaei, Gholamreza, Eslami, Masoud, Makroni, Sarwar. Consequences of climate change and its impact on people's livelihood. The third national conference on environment, energy and biodefense, Tehran. 2015.
2.    Amin, Maryam, Simulating the effect of climate change on the growth and yield of wheat and barley in Tehran province and providing crop adaptation solutions, Master's thesis, Shahid Beheshti University, Environmental Sciences Research Institute, 2019.
3.    Tavakoli, Mohsen, Mohammadi, Samira, Zarafshani, Kiyomarth, Mehdizadeh, Hossein, Amiri, Farzad. (2022). Forecasting the effects of climate change on temperature and precipitation using atmospheric general circulation models, a solution for sustainable agriculture (case study: Kermanshah city). Environmental Science and Technology Quarterly, 23(6), 15-31.
4.    Tabari, Hossein and Ayini, Ali and Aghajanlou, Mohammad Baqer, 2007, a review on the effects of climate change on the water resources of the planet, technical workshop on the effects of climate change in water resources management, Tehran.
5.    Kabaat. p، coping with impacts of climate variability and climate change in water management، A Scoping paper Wageningen p3,2000.
6.    Rasool Pournalkiashri, Samia, 2017, climate changes and its impact on water resources in the Middle East, the 4th International Conference on Environmental Planning and Management, Tehran.
7.    Hamidianpour, Mohsen and Nazaripour, Hamid and Khazai Faizabad, Elnaz and Farzaneh, Mahsa and Firuzeh, Siddiqa, 2023, Determination of the change point of temperature thresholds of heat and cold waves in Iran during the statistical period of 1966-2018, Quarterly Journal of Natural Environment Hazards, period: 12, number 37.
8.    Jamali, Farimah Sadat and Khalidi, Shahriar, 2021, The role of temperature changes in the environmental sustainability of Tehran. Earth Science Research Quarterly, Volume: 12, Number: 1.
9.    Zarei, Abdol Rasul, Moghimi, Mohammad Mahdi. 2016. Forecasting and checking the average monthly temperature using time series models. Scientific Journal of Irrigation and Water Engineering of Iran, 7(1), 142-151.
10.    Mir Tahari, Fereshte Al-Sadat and Samai, Zahra and Kasmai, Zahra and Malek Siah Chesh, Zahra, 2014, Effects of temperature increase on the planet, 7th National Conference and Specialized Exhibition of Environmental Engineering, Tehran.
11.    Ataiee, Hooshmand and Koohi, Mansooreh, 2022, Predicted changes in temperature and precipitation of Kashf Rood Basin based on dynamic and statistical straw-scale methods, Journal of Natural Environmental Hazards, Vol.10, Issue 30, Winter 2022.
12.    Wilby, R.L., and Dawson, C.W., Using SDSM Version 4.1 SDSM 4.2. 2—a decision support tool for the assessment of regional climate change impacts. User Manual, Leicestershire, UK. (2007).
13.    Khan, M. S., Coulibaly, P., Dibike, Y. (2006). Uncertainty analysis of statistical downscaling methods. Journal of Hydrology, 319, pp 357-382.
14.    Barzegari, Fatima. Maliknejad, Hossein. (2018). Investigating the effects of climate change on water demand and sustainability of water consumption in the agricultural sector of the Yazd-Ardakan Plain. Journal of Agricultural Ecology, Volume 10, Number 4: 1161-1176.
15.    Alizadefard, Elham, Mirmusavi, Seyed Hossein, Yarahamdi, Jamshid, Faraji, Abdullah 2020. Evaluation of the effect of climate change on precipitation in areas without observational statistics using CCT software package, case study: Daryan Basin. Journal of Geography and Planning, No. 73:305-323.
16.    Chobeh, Sepideh and Kake Memi, Azad, 2015, investigation of the effectiveness of statistical exponential microscale model (SDSM) in predicting temperature and precipitation parameters (case study: Ardabil Baliqlochai watershed), the second national conference on protection of natural resources and environment, Ardabil.
17.    Hajari, Zainab and Zand, Mehran and Karampour, Mostafa and Tagvi Guderzi, Saeed and Fakhrabadi, Amir, 2019, Prediction of monthly and seasonal temperature and precipitation parameters using the SDSM model (case study: Khorramabad), 2nd international conference new horizons in basic and technical sciences and engineering, Tehran.
18.    Destranj, Ali and Rostami, Mohammad, 2020, evaluation and prediction of climate changes in the coming decades using micro-scale exponential atmospheric general circulation models.
19.    Khan, M.S., Coulibaly, P. and Dibike, Y. 2006. Uncertainty analysis of statistical downscaling methods. J. Hydrol, 1-4: 357-382.
20.    Dibike, Y.B. and Coulibaly, P. 2018. Temporal neural networks for downscaling climate variability and extremes. Neural Networks, 2: 135-144.
21.    Rahimi Moghadam, Sajjad, Kambozia, Jafar, Dihim Fard, Reza. 2017, Risk assessment due to heat stress in grain corn of Khuzestan province under climate change conditions., Environmental Stresses in Agricultural Sciences, Volume 11, Number 3, pp 749-764.
22.    Hamidianpour, Mohsen, Fallah Qalhari, Gholam Abbas, Alimoradi, Mohammadreza. 2021. Evaluating the effectiveness of the SDSM model in investigating the consequences of climate change for different climatic zones of Iran. Climate change researches 2(5), 1-14.
23.    Asakareh, Hossein and Shadman, Hassan, 2017, evaluation of the power of SDSM model in simulating the average temperature of Urmia city, Journal of Geography and Environmental Planning, Volume: 29, Number: 4.
24.    Arab Salghar, Ali Akbar, Parhamt, Jahangir, Godarzi, Massoud. 2022. Forecasting climate changes using atmospheric general circulation models and straw-scale SDSM and LARS-WG models under radiative forcing scenarios in the Dez catchment. Natural Geography 15(55), 129-149.
25.    Shamsipour, Ali Akbar. 2012. Climate modeling, theory and method. Tehran: University of Tehran.
26.    McGuffey, KA and Henderson, Sellers. 2001. The first step in climate modeling. Translated by Seyedaboulfazl Masoudian and Hasan Ali Ghayor 2000. Isfahan University Publications.
27.    Semenov, M.A, Stratonovitch, P, 2010, Use of Multi-Model Ensembles from Global Climate Models for Assessment of Climate Change Impacts, Climate Research, No. 4, PP. 1–14. 
28.    Xu, C.H, Xu, Y, 2012, The projection of temperature and precipitation over china under RCP scenarios using a CMIP5 multi-model ensemble, Atmospheric and Oceanic Science Letters, Vol. 5, No. 6, PP. 527-533.
 
29.    Yousefi, Abdul Hossein, 2019, Investigating the impact of climate change on the desertification risk potential of land based on climate and groundwater criteria (case study: Bagh Fars Desert), PhD Thesis, Lorestan University, Faculty of Literature and Human Sciences.
30.    Hajivandpaydari, Samia, Yazdan Panah, Hojat Elah, Andarzian, Seyyed Bahram. 2022. Investigating the regional effects of the climate change phenomenon in the north of Khuzestan province using the HadCM3 model under the LARS-WG micro-exponential comparison in the statistical period of 2010-2030 and 2030-2050. Geography and Human Relations 299-31
31.    Ghasemi, Mahbobeh, Soltani, Amir, Naseri, Abdul Ali, Moazed, Hadi. 2018. Investigating future climate change trends under radiative forcing scenarios using non-parametric Mann-Kendall test (case study: south of Ahvaz). Newar 43(106-107), 79-88.
32.    Intergovernmental Panel on Climate Change. 2013. Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge Univ. Press, Cambridge.
33.    Taylor, K.E., Stouffer, R.J., Meehl, G.A. 2012. An overview of CMIP5 and the experiment design. Bulletin of the American Meteorological Society. 93: 485–498.
34.    Mohammadi, Mohammad Reza and Borna, Reza, 2015, the increase in temperature in Khuzestan province during the last two decades and the investigation of its factors, environmental consequences and the mutual effect that this increase in temperature has on energy consumption and also energy consumption on temperature increase, the third national environmental conference, energy and biological defense, Tehran, https://civilica.com/doc/402151