<?xml version="1.0" encoding="utf-8"?>
<journal>
<title>Environmental Erosion Research</title>
<title_fa>پژوهش هاي فرسايش محيطي</title_fa>
<short_title>E.E.R.</short_title>
<subject>Literature &amp; Humanities</subject>
<web_url>http://magazine.hormozgan.ac.ir</web_url>
<journal_hbi_system_id>1</journal_hbi_system_id>
<journal_hbi_system_user>admin</journal_hbi_system_user>
<journal_id_issn>2251-7812</journal_id_issn>
<journal_id_issn_online>2717-3968</journal_id_issn_online>
<journal_id_pii></journal_id_pii>
<journal_id_doi>10.61882/jeer</journal_id_doi>
<journal_id_iranmedex></journal_id_iranmedex>
<journal_id_magiran></journal_id_magiran>
<journal_id_sid>6561</journal_id_sid>
<journal_id_nlai>8888</journal_id_nlai>
<journal_id_science>45855/11/3/90</journal_id_science>
<language>fa</language>
<pubdate>
	<type>jalali</type>
	<year>1401</year>
	<month>6</month>
	<day>1</day>
</pubdate>
<pubdate>
	<type>gregorian</type>
	<year>2022</year>
	<month>9</month>
	<day>1</day>
</pubdate>
<volume>12</volume>
<number>3</number>
<publish_type>online</publish_type>
<publish_edition>1</publish_edition>
<article_type>fulltext</article_type>
<articleset>
	<article>


	<language>fa</language>
	<article_id_doi></article_id_doi>
	<title_fa>مدل‌سازی و پیش‌بینی رواناب ماهانه در دامنه زمان (مطالعه موردی: حوضه آبریز قره‌سو)</title_fa>
	<title>Modeling and Forecasting of Monthly Runoff in the Time Domain
(Case Study: Gharasou River Basin)</title>
	<subject_fa>مدلسازی و تحلیل زمانی و مکانی رخداد انواع مختلف فرسایش محیطی</subject_fa>
	<subject></subject>
	<content_type_fa>مستخرج از پایان‌نامه / رساله / طرح پژوهشی</content_type_fa>
	<content_type></content_type>
	<abstract_fa>&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;text-justify:kashida&quot;&gt;&lt;span style=&quot;text-kashida:0%&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span style=&quot;direction:rtl&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;در &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;پژوهش حاضر&lt;/span&gt;&lt;/b&gt;&lt;b&gt; &lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;برای&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; مدل&amp;shy;سازی رواناب ماهانه&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;،&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; از داده&amp;shy;های چهار ایستگاه هیدرومتری پل توسکاستان، نهارخوران، غازمحله و سیاه&amp;shy;آب در حوضه آبریز قره&amp;shy;سو&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; در یک دوره آماری &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;36&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; ساله &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;استفاده شد. سپس بررسی همگنی سری داده&amp;shy;ها با استفاده از آزمون چاو انجام شد. &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;پس از مرتب&amp;shy;سازی&amp;shy; داده&amp;shy;ها، برای مدل&amp;shy;سازی مقادیر رواناب ماهانه از چهار روش&amp;shy; باکس و جنکینز &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;(SARIMA)&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، شبکه عصبی مصنوعی &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;(&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;ANN&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;)،&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; شبکه عصبی مصنوعی ـ فازی &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;(&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;ANFIS&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;)&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; و الگوریتم ژنتیک &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;(&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;GA&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;)&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; در ایستگاه&amp;shy;های هیدرومتری منتخب استفاده شد. پس از مدل&amp;shy;سازی مقادیر رواناب&amp;shy; ماهانه با استفاده از چهار مدل فوق، به پیش&amp;shy;بینی تغییرات رواناب ماهانه در ایستگاه&amp;shy;های هیدرومتری منتخب برای دوازده ماه آینده پرداخته شد و این امر با کمک نرم&amp;shy;افزارهای &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;Minitab&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;R&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; و &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;SPSS&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; &amp;nbsp;صورت گرفت. با توجه به نوع پراکنش مقادیر رواناب و وجود داده صفر، برای تثبیت واریانس از تبدیل&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;log(1+Y&lt;sub&gt;t&lt;/sub&gt;) &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;/span&gt;&lt;/b&gt;&lt;m:omath&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;&lt;m:rpr&gt;&lt;m:scr m:val=&quot;roman&quot;&gt;&lt;m:sty m:val=&quot;p&quot;&gt;&lt;/m:sty&gt;&lt;/m:scr&gt;&lt;/m:rpr&gt;&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;m:ssub&gt;&lt;m:ssubpr&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-weight:bold&quot;&gt;&lt;m:ctrlpr&gt;&lt;/m:ctrlpr&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/m:ssubpr&gt;&lt;m:e&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;&lt;m:rpr&gt;&lt;m:scr m:val=&quot;roman&quot;&gt;&lt;m:sty m:val=&quot;p&quot;&gt;&lt;/m:sty&gt;&lt;/m:scr&gt;&lt;/m:rpr&gt;&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;/m:e&gt;&lt;m:sub&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;&lt;m:rpr&gt;&lt;m:scr m:val=&quot;roman&quot;&gt;&lt;m:sty m:val=&quot;p&quot;&gt;&lt;/m:sty&gt;&lt;/m:scr&gt;&lt;/m:rpr&gt;&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;/m:sub&gt;&lt;/m:ssub&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span cambria=&quot;&quot; math=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;m:r&gt;&lt;m:rpr&gt;&lt;m:scr m:val=&quot;roman&quot;&gt;&lt;m:sty m:val=&quot;p&quot;&gt;&lt;/m:sty&gt;&lt;/m:scr&gt;&lt;/m:rpr&gt;&lt;/m:r&gt;&lt;/span&gt;&lt;/span&gt;&lt;/m:omath&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;position:relative&quot;&gt;&lt;span style=&quot;top:4.5pt&quot;&gt; &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;b&gt;&amp;nbsp;&lt;/b&gt;&lt;b&gt;&amp;nbsp;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;در مدل استفاده شد. در مرحله بعد، &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;اعتبارسنجی مقادیر پیش&amp;shy;بینی شده توسط مدل&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&amp;shy;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;ها&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; با استفاده از شاخص&amp;shy;های &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;MAD&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;، &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;RMSE&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt; و &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:11.0pt&quot;&gt;MAPE&lt;/span&gt;&lt;/b&gt;&lt;b&gt; &lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;ارزیابی شد. &lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;color:black&quot;&gt;نتایج نشان داد که در اکثر ایستگاه&amp;shy;های هیدرومتری منتخب، مدل شبکه عصبی مصنوعی بهترین عملکرد را در بین چهار مدل مورد استفاده داشت. بعد از شبکه عصبی مصنوعی، شبکه عصبی مصنوعی ـ فازی دارای مناسب&amp;shy;ترین عملکرد بود. روش باکس و جنکینز نیز با وجود اینکه در تشخیص روند تغییرات به صورت مناسب عمل کرده بود، در بین چهار&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span 2=&quot;&quot; compset=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;color:black&quot;&gt; مدل مورد استفاده عملکرد ضعیف&amp;shy;تری را در پیش&amp;shy;بینی مقادیر رواناب داشت.&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-family:&quot;Calibri&quot;,sans-serif&quot;&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&amp;nbsp;</abstract_fa>
	<abstract>&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span style=&quot;text-autospace:none&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;1- &lt;/b&gt;&lt;b&gt;Introduction&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;color:black&quot;&gt;Nowadays, demand for water is increasing especially in arid and semi-arid regions&amp;nbsp;(e.g., Iran) due to population growth, &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;economic&amp;nbsp;development,&amp;nbsp;higher standard of living, and changes in consumption patterns. Hence, optimal management of water resources in these areas is essential. Furthermore, climate change and increasingly extreme weather events have caused a surge in natural disasters (e.g., floods) over the past 50 years in arid and semi-arid regions.&amp;nbsp;Thus, forecasting and modeling of runoff data is extremely necessary for planning and managing of water resources. Water flow forecasting plays a key role in flood reduction, reservoir optimization, and reservoir management. These models are mostly developed and applied for simulation and prediction. Therefore, different types of forecasting methods have been proposed over the decades including: Box and Jenkins (SARIMA), Artificial Neural Network (ANN), Adaptive Neuro-Fuzzy Inference Systems (ANFIS), and Genetic Algorithm (GA) models. Forecasting hydrological reactions invariably involves uncertainty. So far, numerous studies have been performed to improve the reliability and accuracy of hydrological forecasts, resulting in reduced risk error. Therefore, the main objective of current research was to use artificial intelligence methods consisting of ANN, ANFIS, GA, and SARIMA models to predict monthly runoff data and also select the best model for the efficient management of water resources in the Gharasou River basin.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:-0.5pt&quot;&gt;&lt;b&gt;2- Methodology&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;Gharasou river basin with an area of 1624 square kilometers is located in the west of Golestan province and has an important role in providing water resources required in this province. In this research, to model and forecast the runoff process, the monthly runoff time series of 4 hydrometric stations of Pol-Tuskestan, Naharkhoran, Ghazmahale, and Siah-ab over Gharasou River basin were used for a period of 36 years (1982-2018). The time series homogeneity was examined using the Chow`s method. Runoff data are time dependent, so initially these data were arranged in time series. After sorting the data, four models consisting of Box and Jenkins (SARIMA), Artificial Neural Network (ANN), Adaptive Neuro-Fuzzy Inference Systems (ANFIS), and Genetic Algorithm (GA) models were used to forecast monthly runoff. To increase the&amp;nbsp;prediction accuracy of other methods, the far time series of monthly runoff were first ignored based on to neural network method and then the number of effective years for modeling was determined. Later, &lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;the monthly runoff was forecasted &lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;for the next 12 months using four models consisting of SARIMA, ANN, ANFIS, and GA. Lastly, based on the forecasted values and using MAD, RMSE and MAPE indices, the accuracy and precision of SARIMA, ANN, ANFIS and GA models were compared. Modeling and forecasting were done using Minitab, R and SPSS software packages.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:-0.5pt&quot;&gt;&lt;b&gt;3- Results &lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;Based on the type of distribution of monthly runoff and the presence of zero data, &lt;i&gt;log(1+Y&lt;sub&gt;t&lt;/sub&gt;)&lt;/i&gt; conversion was used in the models to stabilize the variance. The results according to the autocorrelation diagrams revealed that &lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;the time series in all stations &lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;have seasonal trend with a period of 12 months. Then, the monthly runoff of the next 12 months was forecasted using four models including SARIMA, ANN, ANFIS and GA. Model validation results using three indicators of MAD, RMSE and MAPE revealed that the ANN model in the three hydrometric stations of Naharkhoran, Pol-Tuskestan and Siah-ab had the best performance. In these three hydrometric stations, after ANN model, the ANFIS model has been selected as the most suitable model. However, the performance of these two models has been very similar. In the Ghazmahaleh hydrometric station, two models of ANFIS and ANN had the best performance, respectively. In this study, it was also found that in four selected hydrometric stations, the GA model had a good performance after the two models of ANN and ANFIS. Although SARIMA model performed very well in identifying the trend of monthly runoff changes, it had &lt;/span&gt;the weakest &lt;span style=&quot;font-size:11.0pt&quot;&gt;performance &lt;/span&gt;among the methods&lt;span style=&quot;font-size:11.0pt&quot;&gt;. The forecast data using SARIMA model were overestimated compared to the actual data for March and April, but in other months, the forecast data using this model were relatively appropriate.&lt;/span&gt;&lt;span dir=&quot;RTL&quot; style=&quot;font-family:&quot;B Lotus&quot;&quot; lang=&quot;FA&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:-0.5pt&quot;&gt;&lt;b&gt;4- Discussion &amp; &lt;/b&gt;&lt;b&gt;&lt;span style=&quot;letter-spacing:-.2pt&quot;&gt;Conclusions &lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:12pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;In this research, to model and predict the monthly runoff process, &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;four &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;models including SARIMA, ANN, ANFIS, and GA models were used for &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;four &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;selected hydrometric stations in Gharasou River basin. The results of model validation using three indicators of MAD, RMSE and MAPE showed that the ANN and ANFIS models had the best performance among the four models used. It was also found that time series of runoff data in hydrometric stations have undergone structural changes due to the physical and climatic alterations in the upstream of rivers. Therefore, the distant past of time series may cause deviations in modeling and forecasting results. To &lt;/span&gt;&lt;/span&gt;overcome&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt; this problem, making use of an algorithm to select the number of effective years in modeling and forecasting can be useful. Artificial neural network &lt;/span&gt;&lt;/span&gt;provides&lt;span style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt; a suitable criterion for selecting the number of effective years due to its high accuracy in modeling and forecasting. Based on the effective years identified by this model, other models can be modified and provide more appropriate input data for forecasting from other models.&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;RTL&quot; lang=&quot;FA&quot; style=&quot;font-size:11.0pt&quot;&gt;&lt;span style=&quot;line-height:115%&quot;&gt;&lt;span style=&quot;font-family:&quot;B Nazanin&quot;&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&amp;nbsp;</abstract>
	<keyword_fa>رواناب ماهانه, شبکه عصبی مصنوعی, الگوریتم ژنتیک, باکس و جنکینز, حوضه آبریز قره‌سو.</keyword_fa>
	<keyword>Monthly runoff, Artificial Neural Network, Genetic Algorithm, Box and Jenkins, Gharasou River Basin</keyword>
	<start_page>165</start_page>
	<end_page>189</end_page>
	<web_url>http://magazine.hormozgan.ac.ir/browse.php?a_code=A-10-720-3&amp;slc_lang=fa&amp;sid=1</web_url>


<author_list>
	<author>
	<first_name>Hamed</first_name>
	<middle_name></middle_name>
	<last_name>Ghezelsefla</last_name>
	<suffix></suffix>
	<first_name_fa>حامد</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>قزل‌سفلی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>hamgheze@gmail.com</email>
	<code>10031947532846007318</code>
	<orcid>10031947532846007318</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Rangeland and Watershed Management Department, Faculty of Agriculture &amp; Natural Resources, University of Gonbad Kavous</affiliation>
	<affiliation_fa>گروه مرتع‌و‌آبخیزداری، دانشگاه گنبد کاووس، گنبد کاووس</affiliation_fa>
	 </author>


	<author>
	<first_name>Nader</first_name>
	<middle_name></middle_name>
	<last_name>Jandaghi</last_name>
	<suffix></suffix>
	<first_name_fa>نادر</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>جندقی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>nader.jandaghii@gmail.com</email>
	<code>10031947532846007319</code>
	<orcid>10031947532846007319</orcid>
	<coreauthor>Yes
</coreauthor>
	<affiliation>Rangeland and Watershed Management Department, Faculty of Agriculture &amp; Natural Resources, University of Gonbad Kavous</affiliation>
	<affiliation_fa>گروه مرتع و آبخیزداری، دانشگاه گنبد کاووس، گنبد کاووس</affiliation_fa>
	 </author>


	<author>
	<first_name>Mojtaba</first_name>
	<middle_name></middle_name>
	<last_name>Ghareh Mahmoodlu</last_name>
	<suffix></suffix>
	<first_name_fa>مجتبی</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>قره محمودلو</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>mmahmoodlu@yahoo.com</email>
	<code>10031947532846007320</code>
	<orcid>10031947532846007320</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Rangeland and Watershed Management Department, Faculty of Agriculture &amp; Natural Resources, University of Gonbad Kavous</affiliation>
	<affiliation_fa>گروه مرتع و آبخیزداری، دانشگاه گنبد کاووس، گنبد کاووس</affiliation_fa>
	 </author>


	<author>
	<first_name>Majid</first_name>
	<middle_name></middle_name>
	<last_name>Azimmohseni</last_name>
	<suffix></suffix>
	<first_name_fa>مجید</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>عظیم محسنی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>azim_mohseni@yahoo.com</email>
	<code>10031947532846007321</code>
	<orcid>10031947532846007321</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Statistics, Faculty of Science,  Golestan University</affiliation>
	<affiliation_fa>گروه آمار، دانشگاه گلستان، گلستان</affiliation_fa>
	 </author>


	<author>
	<first_name>Seyed Morteza </first_name>
	<middle_name></middle_name>
	<last_name>Seyedian</last_name>
	<suffix></suffix>
	<first_name_fa>مرتضی</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>سیدیان</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>s.m.seyedian@gmail.com</email>
	<code>10031947532846007322</code>
	<orcid>10031947532846007322</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Rangeland and Watershed Management Department, Faculty of Agriculture &amp; Natural Resources, University of Gonbad Kavous</affiliation>
	<affiliation_fa>گروه مرتع و آبخیزداری، دانشگاه گنبد کاووس، گنبد کاووس</affiliation_fa>
	 </author>


</author_list>


	</article>
</articleset>
</journal>
