<?xml version="1.0" encoding="utf-8"?>
<journal>
<title>Geographical Space</title>
<title_fa>فضای جغرافیایی</title_fa>
<short_title>جغرافیایی</short_title>
<subject>Literature &amp; Humanities</subject>
<web_url>http://geographical-space.iau-ahar.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>1735322X</journal_id_issn>
<journal_id_issn_online>1735-322X</journal_id_issn_online>
<journal_id_pii></journal_id_pii>
<journal_id_doi></journal_id_doi>
<journal_id_iranmedex></journal_id_iranmedex>
<journal_id_magiran></journal_id_magiran>
<journal_id_sid></journal_id_sid>
<journal_id_nlai></journal_id_nlai>
<journal_id_science></journal_id_science>
<language>fa</language>
<pubdate>
	<type>jalali</type>
	<year>1404</year>
	<month>9</month>
	<day>1</day>
</pubdate>
<pubdate>
	<type>gregorian</type>
	<year>2025</year>
	<month>12</month>
	<day>1</day>
</pubdate>
<volume>25</volume>
<number>91</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>بررسی وضعیت خشکسالی در استان خراسان رضوی با استفاده از شاخص‌های SPEI و VCI</title_fa>
	<title>Investigating the drought situation in Razavi Khorasan province using SPEI and VCI indices</title>
	<subject_fa>تخصصي</subject_fa>
	<subject>Special</subject>
	<content_type_fa>پژوهشي</content_type_fa>
	<content_type>Research</content_type>
	<abstract_fa>&lt;span style=&quot;font-size:11pt&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 calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;خشکسالی یک خطر طبیعی است که می تواند اثرات شدید و طولانی مدتی بر سیستم&amp;shy;های طبیعی و انسانی داشته باشد. انتظار می&#8204;رود افزایش گازهای گلخانه&#8204;ای ویژگی&#8204;های خشکسالی را تغییر دهد. لذا برای بررسی خشکسالی استان خراسان رضوی طی دوره 40 ساله از داده&amp;shy;های ایستگاه&amp;shy;های هواشناسی سینوپتیک با یک دوره 40 ساله (1980-2020) و یک دوره زمانی 20 ساله (2020-2001) از داده&amp;shy;های سنجنده &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;MODIS&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt; ماهواره &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Terra&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt; با تفکیک افقی 1000 متر انجام شد. شاخص&amp;shy;های خشکسالی مورد استفاده شاخص بارش تبخیر-تعرّق استانداردشده (&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;SPEI&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;) و شاخص وضعیت پوشش گیاهی (&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;VCI&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;) است. &lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;AR-SA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;نتایج نشان داد که &lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;خشکسالی استان خرسان رضوی در 40 سال گذشته با شدت و فراوانی بالایی رخ داده است. بالاترین فروانی و شدت خشکسالی در دهه سوم (2010-2001) با بیشینه شدت خشکسالی 69/1- و فراوانی 24/34 درصد به دست آمده است. بررسی شاخص خشکسالی ماهواره&amp;shy;ای نشان داد که الگوهای خشکسالی نشان داده شده توسط &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;SPEI&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt; و &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;VCI&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt; تا حد زیادی موافق هستند. بررسی دهه&amp;shy;&amp;shy;ای شدت و فراوانی خشکسالی نشان داد که ویژگی اصلی اقلیمی استان پس از دهه 2000 حرکت به سمت یک اقلیم خشک&amp;shy;تر است. مقایسه همزمان این دو شاخص نشان داد که رویدادهای خشکسالی ناشی از بارش (شاخص &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;SPEI&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;) منجر به خشکسالی مبتنی بر پوشش گیاهی در سطح استان نمی&#8204;شوند. همچنین رویدادهای خشکسالی پوشش&amp;shy;گیاهی (شاخص &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;VCI&lt;/span&gt;&lt;/span&gt;&lt;span lang=&quot;FA&quot; style=&quot;font-size:13.0pt&quot;&gt;&lt;span b=&quot;&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;) به عنوان یک نتیجه از کمبود بارش رخ نمی&#8204;دهند.&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:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Introduction&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Drought is a natural hazard that can have severe and long-term effects on natural and human systems. An increase in greenhouse gases is expected to change the characteristics of drought. Therefore, it is necessary to have a detailed understanding of drought and its changes at the regional scale. Droughts regularly led to major socio-economic and environmental impacts. Drought is one of the most severe natural hazards, and climate change causes droughts to occur in many regions of the world in the 21&lt;sup&gt;st&lt;/sup&gt; century with a longer period. It is very important to monitor the drought in Razavi Khorasan province and understand its characteristics in the long term. The research results will have many applications in different sectors such as agriculture, water resources, environment, and agriculture.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Methods&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;To investigate the drought of the Khorasan Razavi province during a period of 40 years, the data of synoptic meteorological stations with a period of 40 years (1981-2020) have been used. The Spatio-temporal changes of drought the in Khorasan-Razavi province have been done based on the Standardized Precipitation Evapotranspiration Index (SPEI). The Penman-Monteith method has been used to calculate the potential evapotranspiration to calculate the drought. Finally, the frequency and intensity of the drought for the last four decades have been analyzed separately. Also, the VCI drought index, which is a remote-sensing drought index, has been used. This index is calculated using NDVI data from the MODIS sensor.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Discussion of Results &lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;The results showed that the drought in Khorasan Razavi province has occurred with high intensity and frequency in the last 40 years. The highest frequency and intensity of drought was obtained in the third decade (2001-2010) with the maximum intensity of drought of -1.69 and frequency of 34.24%. A decades-long study of drought severity and frequency showed that the main climate feature of the province after the 2000s was moving towards a drier climate.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;In general, the potential &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;evapotranspiration &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;in Razavi Khorasan province has an increasing slope from north to south and west to east. The frequency of drought also shows a behavior similar to potential &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;evapotranspiration &lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;in Razavi Khorasan province. The highest frequency of drought is seen in the southern and southeastern regions of the province with 26.51%. In other words, more than a quarter of the months of the year in these areas of the province are affected by drought.&lt;/span&gt;&lt;/span&gt; &lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;The simultaneous comparison of SPEI and VCI indices showed that precipitation-induced drought events (SPEI index) do not lead to vegetation-based drought in the province. Also, vegetation drought events (VCI index) do not occur as a result of a lack of precipitation.&lt;/span&gt;&lt;/span&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span style=&quot;font-family:&quot;Times New Roman&quot;,serif&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Conclusions&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;line-height:normal&quot;&gt;&lt;span calibri=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;font-size:12.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;Changes in the characteristics of drought based on the data of the last 40 years, including the frequency, intensity, and areas affected by drought, showed that the droughts of Razavi Khorasan province during the last 40 years show clear decadal changes. Based on the regional changes of drought, several regional differences of drought have been identified. The maximum frequency of drought in the first decade (1981-1990) compared to the fourth decade (2011-2020) has experienced an increase of 11.69%. Analysis of the satellite drought index showed that the drought patterns shown by SPEI and VCI agree to a large extent. the increase in drought in recent years shows that if the concentration of greenhouse gases continues along its current path, the risk of increasing drought-related tensions for natural and human systems in Razavi Khorasan province will increase greatly. Therefore, it is necessary to include programs such as water resources management and cultivation and irrigation calendar in the province-related programs.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&amp;nbsp;</abstract>
	<keyword_fa>خشکسالی, شاخص SPEI, شاخص VCI, سنجنده MODIS, خراسان رضوی.</keyword_fa>
	<keyword>Drought, SPEI index, VCI index, MODIS sensor, Razavi Khorasan.</keyword>
	<start_page>147</start_page>
	<end_page>168</end_page>
	<web_url>http://geographical-space.iau-ahar.ac.ir/browse.php?a_code=A-10-3851-2&amp;slc_lang=fa&amp;sid=1</web_url>


<author_list>
	<author>
	<first_name>Mahsan</first_name>
	<middle_name></middle_name>
	<last_name>Koroozhdeh</last_name>
	<suffix></suffix>
	<first_name_fa>مهسان</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>کروژده</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>mahsankoroozhdeh@gmail.com</email>
	<code>100319475328460023390</code>
	<orcid>100319475328460023390</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Doctoral student of Climatology, Department of Geography, Ahar Branch, Islamic Azad University - Ahar-Iran.</affiliation>
	<affiliation_fa>دانشجوی دکتری رشته آب و هواشناسی، واحد اهر، دانشگاه آزاد اسلامی، اهر، ایران</affiliation_fa>
	 </author>


	<author>
	<first_name>karim</first_name>
	<middle_name></middle_name>
	<last_name>Amininia</last_name>
	<suffix></suffix>
	<first_name_fa>کریم</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>امینی نیا</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>karimaminini@gmail.com</email>
	<code>100319475328460023391</code>
	<orcid>100319475328460023391</orcid>
	<coreauthor>Yes
</coreauthor>
	<affiliation>Department of Geography, Ahar Branch, Islamic Azad University - Ahar-Iran.</affiliation>
	<affiliation_fa>گروه جغرافیا، واحد اهر، دانشگاه آزاد اسلامی، اهر - ایران</affiliation_fa>
	 </author>


	<author>
	<first_name>Mehdi</first_name>
	<middle_name></middle_name>
	<last_name>Saghebian</last_name>
	<suffix></suffix>
	<first_name_fa>سیدمهدی</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>ثاقبیان</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>smsaghebian@gmail.com</email>
	<code>100319475328460023392</code>
	<orcid>100319475328460023392</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Civil Engineerin, Ahar Branch, Islamic Azad University - Ahar - Iran</affiliation>
	<affiliation_fa>گروه عمران، دانشکده فنی و مهندسی، واحد اهر، دانشگاه آزاد اسلامی، اهر - ایران</affiliation_fa>
	 </author>


</author_list>


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