DOCSLIB.ORG

BR IFIC N° 2606 Index/Indice

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
BR IFIC N° 2606 Index/Indice BR IFIC N° 2606 Index/Indice International Frequency Information Circular (Terrestrial Services) ITU - Radiocommunication Bureau Circular Internacional de Información sobre Frecuencias (Servicios Terrenales) UIT - Oficina de Radiocomunicaciones Circulaire Internationale d'Information sur les Fréquences (Services de Terre) UIT - Bureau des Radiocommunications Part 1 / Partie 1 / Parte 1 Date/Fecha 30.10.2007 Description of Columns Description des colonnes Descripción de columnas No. Sequential number Numéro séquenciel Número sequencial BR Id. BR identification number Numéro d'identification du BR Número de identificación de la BR Adm Notifying Administration Administration notificatrice Administración notificante 1A [MHz] Assigned frequency [MHz] Fréquence assignée [MHz] Frecuencia asignada [MHz] Name of the location of Nom de l'emplacement de Nombre del emplazamiento de 4A/5A transmitting / receiving station la station d'émission / réception estación transmisora / receptora 4B/5B Geographical area Zone géographique Zona geográfica 4C/5C Geographical coordinates Coordonnées géographiques Coordenadas geográficas 6A Class of station Classe de station Clase de estación Purpose of the notification: Objet de la notification: Propósito de la notificación: Intent ADD-addition MOD-modify ADD-ajouter MOD-modifier ADD-añadir MOD-modificar SUP-suppress W/D-withdraw SUP-supprimer W/D-retirer SUP-suprimir W/D-retirar No. BR Id Adm 1A [MHz] 4A/5A 4B/5B 4C/5C 6A Part Intent 1 107104249 ARG 7895.9500 CAMPO VIERA MS ARG 55W03'05'' 27S20'04'' FX 1 ADD 2 107104248 ARG 8207.2700 CAMPO GRANDE MS ARG 54W58'43'' 27S12'32'' FX 1 ADD 3 107104632 BEL 1437.5500 SINT KATELIJNE WAVER BERLAARBA BEL 4E35'22'' 51N04'44'' FX 1 MOD 4 107104435 BEL 17823.7500 HAMME OV5157A BEL 4E08'19'' 51N05'49'' FX 1 ADD 5 107104436 BEL 18833.7500 DENDERMONDE OV5249A BEL 4E04'48'' 51N01'04'' FX 1 ADD 6 107104945 BLR 17726.0000 GRODNO MARKSA BLR 23E50'26'' 53N40'34'' FX 1 ADD 7 107104947 BLR 17754.0000 GRODNO MARKSA BLR 23E50'26'' 53N40'34'' FX 1 ADD 8 107104949 BLR 17754.0000 LIDA CHAPAEVA BLR 25E17'44'' 53N53'07'' FX 1 ADD 9 107104952 BLR 17999.0000 TELYAKI BLR 26E48'21'' 54N53'32'' FX 1 ADD 10 107104944 BLR 18720.0000 GRODNO TOMINA BLR 23E50'07'' 53N38'54'' FX 1 ADD 11 107104946 BLR 18736.0000 GRODNO POPOVICHA BLR 23E47'44'' 53N40'24'' FX 1 ADD 12 107104948 BLR 18764.0000 GRODNO GORKOGO BLR 23E49'13'' 53N42'13'' FX 1 ADD 13 107104950 BLR 18764.0000 LIDA SOVET BLR 25E17'29'' 53N54'05'' FX 1 ADD BR IFIC N° 2606 30.10.2007 No. BR Id Adm 1A [MHz] 4A/5A 4B/5B 4C/5C 6A Part Intent 14 107104951 BLR 19009.0000 NAROCH BLR 26E42'25'' 54N54'32'' FX 1 ADD 15 107100630 F 5.4400 CAYENNE QQ GUF 52W22'00'' 4N49'00'' FX 1 SUP 16 107099584 F 5.4400 S GEORGES QQ GUF 51W48'00'' 3N54'00'' FX 1 SUP 17 107099968 F 5.4400 S LAURENT QQ GUF 54W02'00'' 5N29'00'' FX 1 SUP 18 107102506 F 123.1500 CHAMPNIERS6 F 0E13'08'' 45N43'42'' FD 1 ADD 19 107101446 F 156.8500 CALAIS36 F 1E51'12'' 50N57'40'' MS 1 ADD 20 107101613 F 156.8500 CALAIS37 F 1E51'44'' 50N57'57'' MS 1 ADD 21 107102427 F 3453.7500 ARTIGUES PRES BORDEAUX7 F 0W29'56'' 44N51'10'' FX 1 ADD 22 107103852 F 3553.7500 REIGNAC3 F 0W30'39'' 45N14'21'' FX 1 ADD 23 107103136 F 3562.5000 LE BOURG1 F 1E55'31'' 44N42'39'' FX 1 ADD 24 107103976 F 8036.7500 LA TESTE DE BUCH17 F 1W09'49'' 44N38'49'' FX 1 ADD 25 107102491 F 8036.7500 PAULE3 F 3W27'38'' 48N12'56'' FX 1 ADD 26 107103681 F 8040.2500 CREON1 F 0W20'10'' 44N46'10'' FX 1 ADD 27 107100755 F 8040.2500 ORDONNAC3 F 0W52'41'' 45N18'18'' FX 1 ADD 28 107101463 F 8043.7500 LA TESTE DE BUCH17 F 1W09'49'' 44N38'49'' FX 1 ADD 29 107103097 F 8232.0000 PARIS 7E ARRONDISSEMENT3 F 2E17'40'' 48N51'30'' FX 1 ADD 30 107102256 F 8250.2500 LE BARP3 F 0W48'16'' 44N39'14'' FX 1 ADD 31 107102895 F 8250.2500 PLOUNEOUR MENEZ3 F 3W53'22'' 48N24'48'' FX 1 ADD 32 107103530 F 8253.7500 PORT SAINTE FOY ET PONCHA2 F 0E13'15'' 44N52'29'' FX 1 ADD 33 107101405 F 8253.7500 VENDAYS MONTALIVET4 F 1W03'33'' 45N21'15'' FX 1 ADD 34 107102381 F 8257.2500 LANTON5 F 0W54'41'' 44N47'09'' FX 1 ADD 35 107103715 F 8278.1000 FONTAINE LE PUITS7 F 6E30'35'' 45N28'46'' FX 1 ADD 36 107103071 F 8310.6000 THUILLIERES3 F 6E00'39'' 48N09'48'' FX 1 ADD 37 107104172 F 8343.1000 LES LILAS5 F 2E25'20'' 48N53'07'' FX 1 ADD 38 107102631 F 8343.1000 THUILLIERES3 F 6E00'39'' 48N09'48'' FX 1 ADD 39 107100791 F 8375.6000 DOIZIEUX8 F 4E36'40'' 45N23'33'' FX 1 ADD 40 107103513 F 8375.6000 PERROGNEY LES FONTAINES6 F 5E11'37'' 47N47'49'' FX 1 ADD 41 107102675 F 8375.6000 THUILLIERES3 F 6E00'39'' 48N09'48'' FX 1 ADD 42 107101488 F 12752.7500 BREST60 F 4W28'06'' 48N24'14'' FX 1 ADD 43 107101634 F 12752.7500 COUERON5 F 1W43'26'' 47N13'01'' FX 1 ADD 44 107103090 F 12754.5000 ARTIGUES PRES BORDEAUX7 F 0W29'56'' 44N51'10'' FX 1 ADD 45 107102511 F 12754.5000 LACANAU5 F 1W10'07'' 45N00'54'' FX 1 ADD 46 107103285 F 12754.5000 LAMAGDELAINE3 F 1E29'08'' 44N29'05'' FX 1 ADD 47 107101459 F 12754.5000 LANTON5 F 0W54'41'' 44N47'09'' FX 1 ADD 48 107101200 F 12754.5000 ORDONNAC3 F 0W52'41'' 45N18'18'' FX 1 ADD 49 107103422 F 12754.5000 PLOUNEOUR MENEZ3 F 3W53'22'' 48N24'48'' FX 1 ADD 50 107102215 F 12761.5000 LANTON5 F 0W54'41'' 44N47'09'' FX 1 ADD 51 107102642 F 12761.5000 ORDONNAC3 F 0W52'41'' 45N18'18'' FX 1 ADD 52 107103484 F 12768.5000 ARTIGUES PRES BORDEAUX7 F 0W29'56'' 44N51'10'' FX 1 ADD 53 107100857 F 12768.5000 LAMAGDELAINE3 F 1E29'08'' 44N29'05'' FX 1 ADD BR IFIC N° 2606 30.10.2007 No. BR Id Adm 1A [MHz] 4A/5A 4B/5B 4C/5C 6A Part Intent 54 107104067 F 12768.5000 SAINT LAURENT MEDOC2 F 0W48'47'' 45N09'19'' FX 1 ADD 55 107101689 F 12864.7500 EPIAIS LES LOUVRES1 F 2E31'46'' 49N01'41'' FX 1 ADD 56 107104156 F 12864.7500 LOPERHET8 F 4W19'20'' 48N23'49'' FX 1 ADD 57 107103675 F 12864.7500 ROISSY EN FRANCE9 F 2E32'52'' 49N00'35'' FX 1 ADD 58 107101917 F 12866.5000 PARAY VIEILLE POSTE7 F 2E21'57'' 48N43'39'' FX 1 ADD 59 107101882 F 12871.7500 EPIAIS LES LOUVRES1 F 2E31'46'' 49N01'41'' FX 1 ADD 60 107102573 F 12871.7500 LOPERHET8 F 4W19'20'' 48N23'49'' FX 1 ADD 61 107101590 F 12871.7500 ROISSY EN FRANCE9 F 2E32'52'' 49N00'35'' FX 1 ADD 62 107101704 F 12873.5000 ROISSY EN FRANCE9 F 2E32'52'' 49N00'35'' FX 1 ADD 63 107101196 F 12905.0000 MONTFAUCON6 F 6E05'00'' 47N14'31'' FX 1 ADD 64 107102012 F 12933.0000 ESTEZARGUES3 F 4E38'43'' 43N57'31'' FX 1 ADD 65 107103561 F 12961.0000 ALBON1 F 4E52'27'' 45N15'04'' FX 1 ADD 66 107103563 F 12961.0000 GIVORS7 F 4E46'09'' 45N33'57'' FX 1 ADD 67 107101632 F 12971.5000 HERSERANGE1 F 5E47'05'' 49N31'21'' FX 1 ADD 68 107102662 F 13018.7500 MILIZAC4 F 4W36'50'' 48N26'42'' FX 1 ADD 69 107102944 F 13018.7500 SAINT HERBLAIN28 F 1W36'30'' 47N14'41'' FX 1 ADD 70 107102628 F 13020.5000 HOURTIN11 F 1W07'54'' 45N12'50'' FX 1 ADD 71 107102725 F 13020.5000 LAMOTHE CASSEL3 F 1E29'33'' 44N36'54'' FX 1 ADD 72 107102679 F 13020.5000 LE TEMPLE2 F 0W58'46'' 44N52'44'' FX 1 ADD 73 107100942 F 13020.5000 LIBOURNE4 F 0W13'40'' 44N55'07'' FX 1 ADD 74 107101486 F 13020.5000 MONTPEZAT DE QUERCY5 F 1E28'39'' 44N14'41'' FX 1 ADD 75 107102176 F 13020.5000 PESSAC13 F 0W37'50'' 44N47'30'' FX 1 ADD 76 107101735 F 13020.5000 REIGNAC3 F 0W30'39'' 45N14'21'' FX 1 ADD 77 107103033 F 13027.5000 LE TEMPLE2 F 0W58'46'' 44N52'44'' FX 1 ADD 78 107103938 F 13027.5000 LE VERDON SUR MER2 F 1W03'45'' 45N33'46'' FX 1 ADD 79 107101289 F 13034.5000 CAHORS21 F 1E26'53'' 44N26'01'' FX 1 ADD 80 107102356 F 13034.5000 CREON1 F 0W20'10'' 44N46'10'' FX 1 ADD 81 107101747 F 13034.5000 REIGNAC3 F 0W30'39'' 45N14'21'' FX 1 ADD 82 107101826 F 13130.7500 DAMMARTIN EN GOELE4 F 2E38'58'' 49N03'54'' FX 1 ADD 83 107102297 F 13130.7500 HANVEC3 F 4W03'57'' 48N19'27'' FX 1 ADD 84 107101215 F 13130.7500 LE MESNIL AMELOT6 F 2E36'54'' 49N00'57'' FX 1 ADD 85 107100939 F 13132.5000 LES LILAS6 F 2E25'23'' 48N53'07'' FX 1 ADD 86 107104149 F 13137.7500 DAMMARTIN EN GOELE4 F 2E38'58'' 49N03'54'' FX 1 ADD 87 107102038 F 13137.7500 HANVEC3 F 4W03'57'' 48N19'27'' FX 1 ADD 88 107102605 F 13137.7500 LE MESNIL AMELOT6 F 2E36'54'' 49N00'57'' FX 1 ADD 89 107101924 F 13139.5000 LES LILAS6 F 2E25'23'' 48N53'07'' FX 1 ADD 90 107102484 F 13227.0000 BONS EN CHABLAIS1 F 6E20'18'' 46N15'54'' FX 1 MOD 91 107103462 F 13237.5000 LONGUYON1 F 5E36'34'' 49N26'33'' FX 1 ADD 92 107103645 F 17741.2500 BEDARIEUX3 F 3E09'51'' 43N35'45'' FX 1 ADD 93 107103272 F 17741.2500 CADOLIVE1 F 5E32'40'' 43N23'49'' FX 1 ADD BR IFIC N° 2606 30.10.2007 No.
Load more

Recommended publications
  • Sand Dune Systems in Iran - Distribution and Activity
    Sand Dune Systems in Iran - Distribution and Activity. Wind Regimes, Spatial and Temporal Variations of the Aeolian Sediment Transport in Sistan Plain (East Iran) Dissertation Thesis Submitted for obtaining the degree of Doctor of Natural Science (Dr. rer. nat.) i to the Fachbereich Geographie Philipps-Universität Marburg by M.Sc. Hamidreza Abbasi Marburg, December 2019 Supervisor: Prof. Dr. Christian Opp Physical Geography Faculty of Geography Phillipps-Universität Marburg ii To my wife and my son (Hamoun) iii A picture of the rock painting in the Golpayegan Mountains, my city in Isfahan province of Iran, it is written in the Sassanid Pahlavi line about 2000 years ago: “Preserve three things; water, fire, and soil” Translated by: Prof. Dr. Rasoul Bashash, Photo: Mohammad Naserifard, winter 2004. Declaration by the Author I declared that this thesis is composed of my original work, and contains no material previously published or written by another person except where due reference has been made in the text. I have clearly stated the contribution by others to jointly-authored works that I have included in my thesis. Hamidreza Abbasi iv List of Contents Abstract ................................................................................................................................................. 1 1. General Introduction ........................................................................................................................ 7 1.1 Introduction and justification ........................................................................................................
    [Show full text]
  • Iran Map, the Middle East
    THE REGIONAL GUIDE AND MAP OF Bandar-e Anzali Astaneh Lahijan Rasht Rud Sar GILAN Ramsar Manjil Tonekabon ChalusNow Shahr Qareh Tekan Amol Marshun Kojur Kuhin Qazvin MAZANDARAN Gach Sur Baladeh QAZVIN Ziaran Kahak IranHashtjerd Takestan Tairsh Karaj Tehran Nehavand Damavand Eslamshahr ReyEyvanki Robatkarim Zarand Varamin Saveh Manzariyeh Tafresh QOM Qom Weller 09103 WELLER CARTOGRAPHIC SERVICES LTD. is pleased to continue its efforts to provide map information on the internet for free but we are asking you for your support if you have the financial means to do so? With the introduction of Apple's iPhone and iPad using GoodReader you can now make our pdf maps mobile. If enough users can help us, we can update our existing material and create new maps. We have joined PayPal to provide the means for you to make a donation for these maps. We are asking for $5.00 per map used but would be happy with any support. Weller Cartographic is adding this page to all our map products. If you want this file without this request please return to our catalogue and use the html page to purchase the file for the amount requested. click here to return to the html page If you want a file that is print enabled return to the html page and purchase the file for the amount requested. click here to return to the html page We can sell you Adobe Illustrator files as well, on a map by map basis please contact us for details. click here to reach [email protected] Weller Cartographic Services Ltd.
    [Show full text]
  • Poll Res-16.Pmd
    Poll Res. 36 (3) : 481-488 (2017) Copyright © EM International ISSN 0257–8050 AN INDIRECT ESTIMATION OF SOIL QUALITY CHANGES RESULTING FROM GROUNDWATER USE IN SISTAN AND BALUCHISTAN MOHAMMAD MOBINI1, HAMED BIGLARI2,*, AMIN ZAREI3, GHOLAMREZA EBRAHIMZADEH4, ALI BIGLARI5, MOHAMMAD REZA NAROOIE6, EHSAN ABOUEE MEHRIZI7 AND MOHAMMAD MEHDI BANESHI8 1 Department of Environmental Health Engineering, School of Health, Rafsanjan University of Medical Sciences, Rafsanjan, Iran. 2 Department of Environmental Health Engineering, School of Public Health, Gonabad University of Medical Sciences, Gonabad, Iran. 3 Department of Environmental Health Engineering, School of Health, Torbat Heydariyeh University of Medical Sciences, Torbat Heydariyeh, Iran. 4 Department of Environmental Health Engineering, School of Public Health, Zabol University of Medical Sciences, Zabol, Iran. 5 Research Center for Environmental Determinants of Health (RCEDH), Kermanshah University of Medical Sciences, Kermanshah, Iran. 6 Department of Environmental Health Engineering, School of Public Health, Iranshahr University of Medical Sciences, Iranshahr, Iran. 7 Department of Environmental Health Engineering, Faculty of Public Health, North Khorasan University of Medical sciences, Bojnurd, Iran. 8 Social Determinants of Health Research Center, Yasuj University of Medical Sciences, Yasuj, Iran. (Received 1 February, 2017; accepted 30 July, 2017) ABSTRACT Soil salinity and its exacerbation resulting from water quality effects decrease product quality and cause specific ion toxicity in plants. The present study examined the sodium adsorption ratio (SAR) and sodium soluble percentage (SSP) indicators of groundwater resources to indirectly evaluate the water quality effects on the soil of Sistan and Baluchistan, Iran. For this purpose, 655 samples were collected during nine years from groundwater wells with agricultural land use in fixed sites of the province.
    [Show full text]
  • Sustainable Urban and Architecture Future of Iranian Islamic Cities (Strategic and Challenges) the Case Sample of Zahedan City
    J. Appl. Environ. Biol. Sci. , 4(12S )329 -338 , 2015 ISSN: 2090-4274 Journal of Applied Environmental © 2015, TextRoad Publication and Biological Sciences www.textroad.com Sustainable Urban and Architecture Future of Iranian Islamic Cities (Strategic and Challenges) The Case Sample of Zahedan City Zeynab Karkeh Abadi (PHD), Reza Mohammadi, Sasan Masoudi 1,2,3, Department of Geography, College of human science, Semnan Branch, Islamic Azad University, Semnan, Iran Received: November 21, 2014 Accepted: January 25, 2015 ABSTRACT Although the future is uncertain, but the definitions all in the fields of concepts "forecast" and "future" or providence whatever the look to tomorrow has in common points. But we can guess that it's the broad and full orientations and deal with by reasonable to it. Futurism not only profit all the tools of the future it is also seeking to optimize present the tasks and actions. Relationship of urban planning (urban) with sustainable urban architecture has directly relationship and is of a type that cannot be led distribute or in order to defined separate form for each them. the study was carried out in the past few decades, particularly since 1304 solar pahlavi era began with the arrival of modernity to country planning and architecture for large and medium-sized cities were palpably affected of it that with the study found that the documents appear on the facts between these two cities were the dominant instability rather than stability, therefore, migration and subsequent creation of uncontrolled urbanization , urban planning retardation and has suffered from unbalanced , so in this paper, a sample of case study Putting Zahedan that the so-called is mega-cities this issue will be discussed.
    [Show full text]
  • Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト
    Mayors for Peace Member Cities 2021/10/01 平和首長会議 加盟都市リスト ● Asia 4 Bangladesh 7 China アジア バングラデシュ 中国 1 Afghanistan 9 Khulna 6 Hangzhou アフガニスタン クルナ 杭州（ハンチォウ） 1 Herat 10 Kotwalipara 7 Wuhan ヘラート コタリパラ 武漢（ウハン） 2 Kabul 11 Meherpur 8 Cyprus カブール メヘルプール キプロス 3 Nili 12 Moulvibazar 1 Aglantzia ニリ モウロビバザール アグランツィア 2 Armenia 13 Narayanganj 2 Ammochostos (Famagusta) アルメニア ナラヤンガンジ アモコストス（ファマグスタ） 1 Yerevan 14 Narsingdi 3 Kyrenia エレバン ナールシンジ キレニア 3 Azerbaijan 15 Noapara 4 Kythrea アゼルバイジャン ノアパラ キシレア 1 Agdam 16 Patuakhali 5 Morphou アグダム（県） パトゥアカリ モルフー 2 Fuzuli 17 Rajshahi 9 Georgia フュズリ（県） ラージシャヒ ジョージア 3 Gubadli 18 Rangpur 1 Kutaisi クバドリ（県） ラングプール クタイシ 4 Jabrail Region 19 Swarupkati 2 Tbilisi ジャブライル（県） サルプカティ トビリシ 5 Kalbajar 20 Sylhet 10 India カルバジャル（県） シルヘット インド 6 Khocali 21 Tangail 1 Ahmedabad ホジャリ（県） タンガイル アーメダバード 7 Khojavend 22 Tongi 2 Bhopal ホジャヴェンド（県） トンギ ボパール 8 Lachin 5 Bhutan 3 Chandernagore ラチン（県） ブータン チャンダルナゴール 9 Shusha Region 1 Thimphu 4 Chandigarh シュシャ（県） ティンプー チャンディーガル 10 Zangilan Region 6 Cambodia 5 Chennai ザンギラン（県） カンボジア チェンナイ 4 Bangladesh 1 Ba Phnom 6 Cochin バングラデシュ バプノム コーチ（コーチン） 1 Bera 2 Phnom Penh 7 Delhi ベラ プノンペン デリー 2 Chapai Nawabganj 3 Siem Reap Province 8 Imphal チャパイ・ナワブガンジ シェムリアップ州 インパール 3 Chittagong 7 China 9 Kolkata チッタゴン 中国 コルカタ 4 Comilla 1 Beijing 10 Lucknow コミラ 北京（ペイチン） ラクノウ 5 Cox's Bazar 2 Chengdu 11 Mallappuzhassery コックスバザール 成都（チォントゥ） マラパザーサリー 6 Dhaka 3 Chongqing 12 Meerut ダッカ 重慶（チョンチン） メーラト 7 Gazipur 4 Dalian 13 Mumbai (Bombay) ガジプール 大連（タァリィェン） ムンバイ（旧ボンベイ） 8 Gopalpur 5 Fuzhou 14 Nagpur ゴパルプール 福州（フゥチォウ） ナーグプル 1/108 Pages
    [Show full text]
  • University Microfilms International 300 N ZEEB ROAD, ANN ARBOR, Ml 48106 18 BEDFORD ROW, LONDON WC1R 4EJ, ENGLAND / 791734*
    INFORMATION TO USERS This was produced from a copy of a document sent to us for microfilming. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the material submitted. The following explanation of techniques is provided to help you understand markings or notations which may appear on this reproduction. 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting through an image and duplicating adjacent pages to assure you of complete continuity. 2. When an image on the film is obliterated with a round black mark it is an indication that the film inspector noticed either blurred copy because of movement during exposure, or duplicate copy. Unless we meant to delete copyrighted materials that should not have been filmed, you will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., is part of the material being photo­ graphed the photographer has followed a definite method in "sectioning" the material. It is customary to begin filming at the upper left hand corner of a large sheet and to continue from left to right in equal sections with small overlaps. If necessary, sectioning is continued again—beginning below the first row and continuing on until complete. 4. For any illustrations that cannot be reproduced satisfactorily by xerography, photographic prints can be purchased at additional cost and tipped into your xerographic copy.
    [Show full text]
  • Assessment of the Distribution and Activity of Dunes in Iran Based on T Mobility Indices and Ground Data ⁎ H.R
    Aeolian Research 41 (2019) 100539 Contents lists available at ScienceDirect Aeolian Research journal homepage: www.elsevier.com/locate/aeolia Assessment of the distribution and activity of dunes in Iran based on T mobility indices and ground data ⁎ H.R. Abbasia,b, , C. Oppa, M. Grolla, H. Rohipourb, A. Gohardoustb a Faculty of Geography, University of Marburg, 35032 Marburg, Germany b Desert Division, Research Institute of Forests and Rangelands, Agricultural Research Education and Extension Organization (AREEO), 13165-116 Tehran, Iran ARTICLE INFO ABSTRACT Keywords: Sand dune movement causes severe damage to infrastructure and rural settlements in Iran every year. Iran, sand dunes Identifying active dunes and monitoring areas with migrating sand are important prerequisites for mitigating Dune mobility index these damages. With regard to this objective, the spatial variation of the wind energy environment based on the Wind energy sand drift potential (DP) was calculated from 204 meteorological stations. Three commonly used dune activity Active dune models – the Lancaster mobility index (1988), the Tsoar mobility index (2005), and the index developed by Yizhaq et al. (2009) – were used for the evaluation of Iran’s sand dune activity. The analysis of the indices showed that the dune activity was characterized by great spatial variation across Iran’s deserts. All three models identified fully active dunes in the Sistan plain, the whole of the Lut desert, as well as in the ZirkuhQaienand Deyhook regions, while the dunes in the northern part of Rig Boland, Booshroyeh and in the Neyshabor du- nefields were categorized as stabilized dunes. For other dunes, the models show a less unified activity classifi- cation, with the Lancaster and Yizhaq models having more similar results while the Tsoar model stands more apart.
    [Show full text]
  • Mapping and Analyzing the Risk of Frost and Chilling Damage on Horticultural Crops (Study Case: Taftan Border Area, Southeast of Iran)
    J. Bio. & Env. Sci. 2015 Journal of Biodiversity and Environmental Sciences (JBES) ISSN: 2220-6663 (Print) 2222-3045 (Online) Vol. 7, No. 2, p. 261-275, 2015 http://www.innspub.net RESEARCH PAPER OPEN ACCESS Mapping and analyzing the risk of frost and chilling damage on horticultural crops (study case: Taftan border area, Southeast of Iran) * Behrooz Kordi Tamandani , Dr. Mahmood Khosravi, Dr. Payman Mahmoodi Department of Climatology University of Sistan and Baluchestan, Iran Article published on August 31, 2015 Key words: Chilling, Frost, Taftan, Sistan and Baluchestan, Geographical Information System (GIS). Abstract Frosts have obvious effects on the energy, transport, and agriculture, while their greatest impact is on agriculture. Since chilling and frost cause’s lots of damage to crops in Taftan area, it is essential to examine the chilling and frost in this area. To study this phenomenon in Taftan area, the minimum temperature data of 4 synoptic stations (Zahedan, Khash, Nosratabad, Mirjaveh) and 4 climatology stations (Goharkouh, Karvandar, Cheshme ziarat, and Korin) were used. Early autumn and late spring frost dates at the desired thresholds (zero and lower) for chilling, and temperatures of 1.1, 2.2, 3.3, 4.4 ° C for frost damage were extracted, and duration, frequency of frost and chilling days and the growing season was calculated. Then, determining the appropriate probability distribution, the probability of early and late, chilling and frost was estimated. After examining the relationship between chilling and elevation, zoning maps were drawn by using the geographical information system (GIS), and finally using the Spearman correlation method, the relationship between chilling and frost and horticultural crops was analyzed.
    [Show full text]
  • Agroclimatic Zones Map of Iran Explanatory Notes
    AGROCLIMATIC ZONES MAP OF IRAN EXPLANATORY NOTES E. De Pauw1, A. Ghaffari2, V. Ghasemi3 1 Agroclimatologist/ Research Project Manager, International Center for Agricultural Research in the Dry Areas (ICARDA), Aleppo Syria 2 Director-General, Drylands Agricultural Research Institute (DARI), Maragheh, Iran 3 Head of GIS/RS Department, Soil and Water Research Institute (SWRI), Tehran, Iran INTRODUCTION The agroclimatic zones map of Iran has been produced to as one of the outputs of the joint DARI-ICARDA project “Agroecological Zoning of Iran”. The objective of this project is to develop an agroecological zones framework for targeting germplasm to specific environments, formulating land use and land management recommendations, and assisting development planning. In view of the very diverse climates in this part of Iran, an agroclimatic zones map is of vital importance to achieve this objective. METHODOLOGY Spatial interpolation A database was established of point climatic data covering monthly averages of precipitation and temperature for the main stations in Iran, covering the period 1973-1998 (Appendix 1, Tables 2-3). These quality-controlled data were obtained from the Organization of Meteorology, based in Tehran. From Iran 126 stations were accepted with a precipitation record length of at least 20 years, and 590 stations with a temperature record length of at least 5 years. The database also included some precipitation and temperature data from neighboring countries, leading to a total database of 244 precipitation stations and 627 temperature stations. The ‘thin-plate smoothing spline’ method of Hutchinson (1995), as implemented in the ANUSPLIN software (Hutchinson, 2000), was used to convert this point database into ‘climate surfaces’.
    [Show full text]
  • Factors Affecting the Qajar-Era Fort Settlements in Iran's Sistan Region Due to Hydrographic Changes in the Hirmand River
    Zarei, M, E and others ______________________ Intl. J. Humanities (2016) Vol. 23 (4): (106-132) Factors Affecting the Qajar-Era Fort Settlements in Iran's Sistan Region Due to Hydrographic Changes in the Hirmand River Mohammad Ebrahim Zarei1, Seyyed Rasool Mousavi Haji 2 Naghmeh Behboodi3 Received: 2016/12/26 Accepted: 2017/9/29 Abstract Locating fort settlements in Iran's Sistan region during different historical periods have always been associated with changes in the direction of Hirmand River which often occurred due to various natural and human factors. One of the most important determining factors in locating the aforementioned settlements is changes in hydrographic network. This study aims to identify the relation between the Iranian province of Sistan hydrographic networks and the fort settlement during the Qajar era. The research method applied, here, is descriptive-analytical, historical- comparative, documentary, library and the field study in Iran's Sistan area. The main focus of the study is on the issue of changes in the hydrographic network of the Hirmand River. The main question is to what extent have the changes in the direction of the hydrographic network of Hirmand played a role in locating fort settlements of the Qajar era in Iran's Sistan region. Records, documents, data and historical information related to the Qajar era were collected and comprehensively compared and analyzed regarding the current and the past situations in the geographic information system (GIS) using ArcGIS software. The results show that the highest number of the locating and the density of fort settlements during Qajar are related to the hydrographic basin of the Sistanriver.
    [Show full text]
  • The Spatial Analysis of Heat Waves in South East of Iran a Case Study: Sistan and Baluchestan Province
    Geographia Technica, Vol. 11, Issue 2, 2016, pp 50 to 60 THE SPATIAL ANALYSIS OF HEAT WAVES IN SOUTH EAST OF IRAN A CASE STUDY: SISTAN AND BALUCHESTAN PROVINCE Morteza ESMAILNEJAD1 DOI: 10.21163/GT_2016.112.05 ABSTRACT: This study describes the main characteristics of a heat wave that occurred over Sistan and Baluchestan. Province located in the south east of Iran. First, we analyzed daily maximum temperature (DMT) recorded at 12 stations during 1961–2015, in southern of Iran. Then geographical patterns of heat waves (HWs), including those persisting for 2–5 days and longer over this province were studied. To indicate heat waves we used the value of the 90th percentile of the annual maximum temperature distribution at a station an then heat wave (HWs) is defined as the maximum number of consecutive days where the daily maximum temperature the long-term daily 90th percentile. Our analysis showed that Two poles of high frequencies (over 2 days per year) of the HWs during April–October were found in the regions of Jazmourian plain and the northern areas of SB. HWs increased significantly during the studied period in most regions of the province, especially over the northwestern areas and the west Sistan and Baluchestan. Increasing trend of HWs occurred after the 2005s in all regions, especially in northern SB and the southeastern coastal. Key-words: Iran, Sistan and Baluchestan, Heat waves, Trend. 1. INTRODUCTION The rapid buildup of greenhouse gases is expected to increase both mean temperature and temperature variability around the world (Schar et al., 2004). Extreme weather situations produce strong impacts on humankind activities (Easterling et al., 2000).
    [Show full text]
  • Analysis of the Level of Environmental Development in the Rural Areas of Sistan with an Emphasis on Quranic Indices
    Journal of Research and Rural Planning Volume 7, No. 1, Spring 2018, Serial No.21 ISSN: 2322-2514 eISSN: 2383-2495 http://jrrp.um.ac.ir Analysis of the Level of Environmental Development in the Rural Areas of Sistan with an Emphasis on Quranic Indices 1 2 Mahamoud Reza Mirlotfi * - Maryam Nouri 1- Associate Prof. in Geography and Rural Planning, University of Zabol, Zabol, Iran 2- MSc. in Geography and Rural Planning, University of Zabol, Zabol, Iran Received: 6 June 2017 Accepted: 26 December 2017 Abstract Purpose: The environment is a divine favor whose protection can have a positive effect on lives of humans and other creatures. A look at the verses of the Quran and the life style of the Prophet�s family (PBUT) make it clear that no school like Islam has attached such a great importance to nature and the environment. Accordingly, using Quranic indices, in this study we have aimed to analyze the level of environmental development in rural areas of Sistan. Design/methodology/approach- The population of the study is the people in the rural areas of Sistan. To determine the sample population using Sharpe formula, 40 villages (with 51663 households) out of 796 villages in Sistan region were selected, and 381 heads of households were randomly selected according to Cochran formula. For data analysis, Kruskal-Wallis statistical method in SPSS was used, and then Topsis was employed to weigh and determine the degree of development of the villages. Findings: The evaluation showed that level of environmental development in rural areas is less than .01% percent significant.
    [Show full text]