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<doi_batch version="4.4.2" xmlns="http://www.crossref.org/schema/4.4.2" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:jats="http://www.ncbi.nlm.nih.gov/JATS1" xsi:schemaLocation="http://www.crossref.org/schema/4.4.2 http://www.crossref.org/schema/deposit/crossref4.4.2.xsd">
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<doi_batch_id>-4d90550d17f4602e089-5267</doi_batch_id>
<timestamp>20220409162955690</timestamp>
<depositor>
  <depositor_name>hyperscienceij@gmail.com:rcrl</depositor_name> 
  <email_address>hyperscienceij@gmail.com</email_address>
</depositor>
<registrant>WEB-FORM</registrant> 
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<body>
<journal>
<journal_metadata>   <full_title>Hyperscience International Journals</full_title>   <abbrev_title>HIJ</abbrev_title>   <issn media_type='electronic'>28213300</issn> </journal_metadata> <journal_issue>  <publication_date media_type='online'>     <month>03</month>     <year>2022</year>   </publication_date>   <journal_volume>     <volume>2</volume>   </journal_volume>   <issue>1</issue> </journal_issue><!-- ============== --> <journal_article publication_type='full_text'>   <titles>     <title>Monitoring of Climatic Factors Affecting on Dust &amp; Sand Storm in Tehran Province</title>   </titles>   <contributors>      <organization sequence='first' contributor_role='author'>Soil Conservation and Watershed Management Department, Agricultural and Natural Resources Research and Education Center of Tehran Province, AREEO, Tehran Iran.</organization>    <person_name sequence='first' contributor_role='author'>      <given_name>Rahman</given_name>      <surname>Sharifi</surname>      <ORCID>https://orcid.org/0000-0002-0602-5001</ORCID>    </person_name>  </contributors>    <jats:abstract xml:lang='en'>         <jats:p>In this study, according to the objectives and implementation method, climatic factors affecting ‎the dust phenomenon in active meteorological stations in Tehran province for a period of 30 years ‎were studied and analyzed. The results showed that in Mehrabad meteorological station, ‎temperature, humidity, rainfall, evaporation factors were directly related to DSI indices, wind ‎trend and dust storm changes, Lancaster, wind and storm diagrams, SPEI and the increase of ‎drought indices in the statistical period increased with temperature, evaporation and decrease. ‎Rainfall and humidity are proportional. DSI dust storm indexes were compared to 1 and ‎Lancaster drought index was compared to 50 and SPEI index was compared positively and ‎negatively in different years of the statistical period in the region and was classified in terms of ‎drought and wet season. The results of monthly and annual changes in wind trend and dust ‎storms showed that the region has no wind in all months and seasons with a speed of more than ‎‎20 meters per second. In terms of wind speed and frequency percentage, the highest wind speed ‎was related to late May and early June, and the lowest wind speed was related to late December ‎and early January. In addition, according to the changes in the wind trend and the documents of the ‎winds and thunderstorms, the prevailing wind direction in the region was from the west.‎</jats:p>     </jats:abstract>  <publication_date media_type='online'>     <month>03</month>     <year>2022</year>   </publication_date>   <pages>     <first_page>26</first_page>     <last_page>35</last_page>   </pages>   <doi_data>     <doi>10.55672/hij2022pp26-35</doi>     <resource>https://hscience.org/index.php/hij/article/view/20</resource>   </doi_data> </journal_article>
</journal>
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