Vilsandi Rahvuspark Sai Alguse 1910
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Rein Einasto
Rein Einasto Nähtust ja tehtust RAAMATU VÄLJAANDMIST ON TOETANUD Tõrva Kirik-Kammersaal, juhataja Ilmar Kõverik Pärtli Paas OÜ, juhataja Hillar Müür Lossikivi OÜ, juhataja Aivar Allikmaa Paekivitoodete Tehase OÜ, juhatuse esimees Vladimir Libman Väo Paas OÜ, juhataja Veljo Haube Reval Stone OÜ, juhataja Hindrek Auväärt Gildemann Dolomite Designs, Madis ja Mihkel Villand J. Viru Markšeideribüroo OÜ, IT-tugiisik, Priit Tammik Steiger Inseneribüroo OÜ, juhataja Erki Niitlaan Talter AS, mäetöödejuht Heini Viilup Redoil OÜ, juhataja Raivo Reinu Tunne Kelam, aatesõber Ülo Vooglaid, aatesõber Toimetanud Mari-Leen Toome Kujundanud Henry Vürst / Kujunduskuur Raamatus kasutatud fotod pärinevad autori erakogust Tallinna Tehnikakõrgkool, 2009 Pärnu mnt 62, 10135 Tallinn ISBN 978-9985-9906-8-1 KIVIS ON ELU JA MÕTISKELU Küllap Sa isegi tead, palju kivis on head. Palju kultuuri on kivis pikkade ajastute rivis. palju kivi – kultuuris ajaloosündmusis suuris. Kivis peidus on aegadetagune elu ja juurdleva vaimu mõtiskelu; kivi peidab inimelu võlu ja valu – hingetuid kivi kuuldavasti ei talu. Kivisse kantuna olevik põlistub, üleisikuline inimeses õilistub, kivis on paljude põlvkondade vaev, allaheidetute põlgus ja raev. Rahva elupõline maa-ootus ja kustumatu priiuse lootus. Vaadates kivile kestvamalt silma, tajume tagamaid, igavikulist ilma; püsiväärtused saavad puhtama värvi, argipäev ei ulatu rikkuma närvi... Rein Einasto Paevana SISUKORD EESSÕNA ....................................................................................................... 6 REIN -
Currents and Waves in the Northern Gulf of Riga
doi:10.5697/oc.54-3.421 Currents and waves OCEANOLOGIA, 54 (3), 2012. in the northern Gulf of pp. 421–447. C Copyright by Riga: measurement and Polish Academy of Sciences, * Institute of Oceanology, long-term hindcast 2012. KEYWORDS Hydrodynamic modelling Water exchange Wave hindcast Wind climate RDCP Baltic Sea Ulo¨ Suursaar⋆ Tiit Kullas Robert Aps Estonian Marine Institute, University of Tartu, M¨aealuse 14, EE–12618 Tallinn, Estonia; e-mail: [email protected] ⋆corresponding author Received 27 February 2012, revised 19 April 2012, accepted 30 April 2012. Abstract Based on measurements of waves and currents obtained for a period of 302 days with a bottom-mounted RDCP (Recording Doppler Current Profiler) at two differently exposed locations, a model for significant wave height was calibrated separately for those locations; in addition, the Gulf of Riga-V¨ainameri 2D model was validated, and the hydrodynamic conditions were studied. Using wind forcing data from the Kihnu meteorological station, a set of current, water exchange and wave hindcasts were obtained for the period 1966–2011. Current patterns in the Gulf and in the straits were wind-dependent with characteristic wind switch directions. The Matsi coast was prone to upwelling in persistent northerly wind conditions. During the * The study was supported by the Estonian target financed project 0104s08, the Estonian Science Foundation grant No 8980 and by the EstKliima project of the European Regional Fund programme No 3.2.0802.11-0043. The complete text of the paper is available at http://www.iopan.gda.pl/oceanologia/ 422 U.¨ Suursaar, T. Kullas, R. -
Viron Lintuseuran Ja Tringan Saarenmaan Talviretki 3-6.1.2003 07.03.2017 Lajit 04.01.2003 05.01.2003 06.01.2003
VIRON LINTUSEURAN JA TRINGAN SAARENMAAN TALVIRETKI 3-6.1.2003 07.03.2017 LAJIT 04.01.2003 05.01.2003 06.01.2003 1 PHACAR Merimetso kormoran x 1 Vilsandi (Ab07) 1 2 CYGOLO Kyhmyjoutsen kühmnokk-luik x 522: Undva 350 (Ab15),103 (Ab17), 26 (Ab16), 43 Panga (Ab23) x 1 Sõrve (Aa17), 23 Loode (a10/15) 540 3 CYGCYG Joutsen laululuik x 17 Undva (Ad16) x 2"3' Loode (Aa10/17) 22 4 ANACRE Tavi piilpart x 3 Roomassaare (Ad01) 3 117: 1 Panga(Ab23), 23 Kudema(Ab22), 33 Uudepanga(Ab15), 6 5 ANAPLA Sinisorsa sinikael-part x Undva(Ab16), 80 Roomassaare(Ad01), 4 Pidula x 4: Vilsandi 1 (ab05), 3 (Ab07) 120 6 AYTFUL Tukkasotka tuttvart x 5 Vilsandi (Ab07) 5 7 AYTMAR Lapasotka merivart x /1 Vilsandi (Ab05) 1 8 POLSTE Allihaahka kirjuhahk x 15 Undva (Ad16) x 250 Vilsandi (Ab07) 265 9 CLAHYE Alli aul x 280 Undva (Ab16), 2 Panga(Ab23) x 9 Vilsandi 7(Ab07) x 1300 Loode (Aa10/15) 1600 10 MELFUS Pilkkasiipi tõmmuvaeras x 2 Vilsandi (Ab07) 2 11 BUCCLA Telkkä sotkas x 159 Panga 9 (Ab23), Undva 150 (Ab16) x 200, 170, 250 Visandi (Ab07) x 500 Loode (Aa10/15) 1280 VL Vesilintu 1000+ Loode(Aa10/15), 19 Sõrve (Aa17), 5 Rõude 1000 12 MERALB Uivelo väikekoskel x 30 Undva (Ab16) x 20 Vilsandi (Ab05/07/08) x 10 Loode (Aa10/15) 60 13 MERSER Tukkakoskelo rohukoskel x 1/ Vilsandi (Ab08) 1 14 MERMER Isokoskelo jääkoskel x 64 Veere 8 (Ab19), Undva 6 (Ab15), 50 (Ab16) x 110 Vilsandi (Ab05/07/08) x 115 Lõu 15 (Aa13), 100 Loode (Aa10/15) 290 15 HALALB Merikotka merikotkas x 9: 3 Panga, 1 Veere, 5 Undva x 4 Vilsandi (Ab05) x 6 Loode 3, Sõrve 3 19 16 CIRCYA Sinisuohaukka välja-loorkull -
A Study of Hydrodynamic and Coastal Geomorphic Processes in Küdema Bay, the Baltic Sea
Coastal Engineering 187 A study of hydrodynamic and coastal geomorphic processes in Küdema Bay, the Baltic Sea Ü. Suursaar1, H. Tõnisson2, T. Kullas1, K. Orviku3, A. Kont2, R. Rivis2 & M. Otsmann1 1Estonian Marine Institute, University of Tartu, Estonia 2Instititute of Ecology, Tallinn Pedagogical University, Estonia 3Merin Ltd., Estonia Abstract The aim of the paper is to analyze relationships between hydrodynamic and geomorphic processes in a small bay in the West-Estonian Archipelago. The area consists of a Silurian limestone cliff exposed to storm activity, and a dependent accumulative distal spit consisting of gravel and pebble. Changes in shoreline position have been investigated on the basis of large-scale maps, aerial photographs, topographic surveys and field measurements using GPS. Waves and currents were investigated using a Recording Doppler Current Profiler RDCP-600 deployed into Küdema Bay in June 2004 and the rough hydrodynamic situation was simulated using hydrodynamic and wave models. The main hydrodynamic patterns were revealed and their dependences on different meteorological scenarios were analyzed. It was found that due to exposure to prevailing winds (and waves induced by the longest possible fetch for the location), the spit elongates with an average rate of 14 m/year. Major changes take place during storms. Vitalization of shore processes is anticipated due to ongoing changes in the regional wind climate above the Baltic Sea. Keywords: shoreline changes, currents, waves, sea level, hydrodynamic models. 1 Introduction Estonia has a relatively long and strongly indented shoreline (3794 km; Fig. 1), therefore the knowledge of coastal processes is of large importance for WIT Transactions on The Built Environment, Vol 78, © 2005 WIT Press www.witpress.com, ISSN 1743-3509 (on-line) 188 Coastal Engineering sustainable development and management of the coastal zone. -
Estuarine, Coastal and Shelf Science 80 (2008) 31–41
Estuarine, Coastal and Shelf Science 80 (2008) 31–41 Contents lists available at ScienceDirect Estuarine, Coastal and Shelf Science journal homepage: www.elsevier.com/locate/ecss Field observations on hydrodynamic and coastal geomorphic processes off Harilaid Peninsula (Baltic Sea) in winter and spring 2006–2007 U¨ . Suursaar a,*, J. Jaagus b,A.Kontc, R. Rivis c,H.To˜nisson c a Estonian Marine Institute, University of Tartu, Ma¨ealuse 10a, Tallinn 12618, Estonia b Institute of Geography, University of Tartu, Vanemuise 46, Tartu 51014, Estonia c Institute of Ecology, Tallinn University, Narva 25, Tallinn 10120, Estonia article info abstract Article history: Investigations of multi-layer current regime, variations in sea level and wave parameters using a bottom- Received 30 April 2008 mounted RDCP (Recording Doppler Current Profiler) during 20 December 2006–23 May 2007 were Accepted 5 July 2008 integrated with surveys on changes of shorelines and contours of beach ridges at nearby Harilaid Available online 18 July 2008 Peninsula (Saaremaa Island). A W-storm with a maximum average wind speed of 23 m sÀ1 occurred on 14–15 January with an accompanying sea level rise of at least 100 cm and a significant wave height of Keywords: 3.2 m at the 14 m deep RDCP mooring site. It appeared that in practically tideless Estonian coastal waters, sea level Doppler-based ‘‘vertical velocity’’ measurements reflect mainly site-dependent equilibrium between currents waves resuspension and sedimentation. The mooring site, 1.5 km off the Kelba Spit of Harilaid, was located in vertical fluxes the accumulation zone, where downward fluxes dominated and fine sand settled. -
Vabariigi Valitsuse Määruse „Vilsandi Rahvuspargi Kaitse-Eeskiri“ Eelnõu SELETUSKIRI
Vabariigi Valitsuse määruse „Vilsandi rahvuspargi kaitse-eeskiri“ eelnõu SELETUSKIRI 1. Sissejuhatus „Looduskaitseseaduse“ § 10 lõike 1 kohaselt on Vabariigi Valitsusel õigus võtta määrusega ala kaitse alla ning kehtestada ala kaitsekord. Väiksemad osad praegusest Vilsandi rahvuspargist olid kaitse alla võetud juba 1910. a. (Vaika saared) ja 1939. a. (Harilaid). Rahvuspargi territooriumi põhiosa on olnud Vilsandi Riikliku Looduskaitsealana kaitse all alates 21. septembrist 1971. a., mil ENSV Ministrite Nõukogu kinnitas oma määruse nr. 457 „Vaika Riikliku Looduskaitseala territooriumi laiendamise ja Vilsandi Riiklikuks Looduskaitsealaks ümbernimetamise kohta“. Vabariigi Valitsuse 1993. a. 8. detsembri määrusega nr 387 “Soomaa, Vilsandi ja Karula rahvuspargi moodustamine” reorganiseeriti looduskaitseala Vilsandi rahvuspargiks. Vastavalt “Looduskaitseseaduse” § 91 lõikele 1 kehtivad enne käesoleva seaduse jõustumist moodustatud kaitsealade ja looduse üksikobjektide kaitseks kehtestatud kaitse-eeskirjad ja kaitsekord seni kuni käesoleva seaduse alusel kehtestatud kaitse-eeskirjade jõustumiseni või kaitse kehtetuks tunnistamiseni, kuid mitte kauemaks kui 2016. aasta 1. maini. Seega ei võeta määrusega kaitse alla uut ala, vaid laiendatakse olemasolevat kaitstavat loodusobjekti, muudetakse selle tsoneeringut ning kehtestatakse uus kaitse-eeskiri. Vilsandi rahvuspark paikneb Saare maakonna lääneosas Kihelkonna kihekonnas, praeguse haldusjaotuse järgi jaguneb ta Kihelkonna ja Lümanda valla maa-ala vahel. Kaitseala kogupindala on ca 29 530ha, millest -
Saare MAAKONNA Loodusväärtused Saare MAAKONNA Loodusväärtused 2 3
SAARE MAAKONNA loodusväärtused SAARE MAAKONNA loodusväärtused 2 3 SISUKORD KAITSEALAD ................... 8 Odalätsi maastikukaitseala ....... 27 Vilsandi rahvuspark ............. 9 Panga maastikukaitseala ......... 27 Abruka looduskaitseala .......... 10 Üügu maastikukaitseala ......... 28 Laidevahe looduskaitseala ........ 11 HOIUALAD .................... 30 Liiva-Putla looduskaitseala ....... 12 Karala-Pilguse hoiuala ........... 31 Linnulaht .................... 13 Karujärve hoiuala .............. 31 Loode tammik ................ 14 Väikese väina hoiuala ........... 33 Rahuste looduskaitseala ......... 15 Viidumäe looduskaitseala ........ 16 KAITSEALUSED PARGID ........... 34 Viieristi looduskaitseala. 17 Kuressaare lossipark ............ 34 Järve luidete maastikukaitseala .... 20 Mihkel Ranna dendraarium ....... 34 Kaali maastikukaitseala .......... 20 Mõntu park .................. 35 Kaugatoma-Lõo maastikukaitseala .. 21 Pädaste park ................. 35 Kaart ....................... 22 ÜksikobjEKTID ................ 36 Kesselaiu maastikukaitseala ...... 25 Põlispuud ................... 36 Koigi maastikukaitseala .......... 25 Rändrahnud .................. 40 KAITSTAVATE LOODUSOBJEKTIDE VALITSEJA Keskkonnaamet Hiiu-Lääne-Saare regioon Tallinna 22, 93819 Kuressaare tel 452 7777 [email protected] www.keskkonnaamet.ee KAITSTAVATE LOODUSOBJEKTIDE KÜLASTUSE KORRALDAJA RMK loodushoiuosakond Viljandi mnt. 18b, 11216 Tallinn [email protected] www.rmk.ee Koostaja: Maris Sepp Trükise valmimisele aitasid kaasa: Kadri Paomees, Rein Nellis, Veljo -
Lääne-Saare Valla Arengukava 2015–2023 (2030)
Lisa 1 Lääne-Saare vallavolikogu 21.08.2017 määruse nr 10 juurde LÄÄNE-SAARE VALLA ARENGUKAVA 2015–2023 (2030) Lääne-Saare valla arengukava aastateks 2015-2023(2030) Sisukord 1. LÄÄNE-SAARE VALLA PRAEGUNE OLUKORD JA ARENGUSUUNDUMUSED ......................... 4 1.1 ASUKOHT JA TERRITOORIUM ................................................................................................. 4 1.2 ASUSTUS JA RAHVASTIK ........................................................................................................... 6 1.3 TÖÖHÕIVE ................................................................................................................................... 9 2. KOHALIKU OMAVALITSUSE JUHTIMINE JA HALDAMINE ........................................................... 11 2.1. VALLA JUHTIMINE .............................................................................................................. 11 2.2. KOHALIK EELARVE ............................................................................................................. 11 2.3 KOONDHINNANG PRAEGUSELE OLUKORRALE ......................................................... 12 2.4 VALITSEMISEKS VAJALIKUD HOONED JA RAJATISED ...................................................... 13 3. LÄÄNE-SAARE VALLA ARENGUNÄGEMUS ....................................................................................... 14 3.1. VISIOON AASTAKS 2023 ........................................................................................................ 14 3.2. STRATEEGILISED EESMÄRGID ............................................................................................ -
Lajit 05.12.2007 06.12.2007 07.12.2007 08.12.2007 09.12.2007
VIRON LINTUSEURAN HIIDENMAA-SAARENMAA TALVIRETKI 5-9.12.2007 05.01.2016 LAJIT 05.12.2007 06.12.2007 07.12.2007 08.12.2007 09.12.2007 3 Suuresadama, 12 Tahkuna, 30 28 Undva, 2 Veere, 7 Kuressaare (Tori 1 CYGOLO Kyhmyjoutsen kühmnokk-luik x x 50 Haldi, 20 Sõru x x 25p Põõsaspea, 2 Söderby Kõrgessaare abajas), 6 Roomassaare 185 2 Hellamaa, 2 Suuresadama, 30 2 CYGCYG Joutsen laululuik x x 4 Haldi Kõrgessaare 38 CYG SP Joutsenlaji luik 310 Sõru-Triigi 3 Ookivi, 150 Kuressaare 460 3 BRALEU Valkoposkihanhi Valgepõsk-lagle x 1 Haldi 1 4 BRABER Sepelhanhi mustlagle x 2 Sõru 2 5 ANAPEN Haapana viupart x 2 Roomassaare 2 6 ANASTR Harmaasorsa rääkspart x 2 Kuressaare (P-linna), 7 Roomassaare 9 7 ANACRE Tavi piilpart x 60 Roomassaare 60 6 Suuresadama, 20 Kärdla, 30 Kõrgessaare, 14 Undva, 83 Kuressaare (P-linna), 15 8 ANAPLA Sinisorsa sinikael-part x x 35 Haldi, 70 Sõru, 5 Sõru-Triigi x x 2 Dirhami, 3 Keila-joa, 40 Tallinna 390 15 Käina Kuressaare, 50 Roomassaare 9 ANAACU Jouhisorsa soopart x /1 Kuressaare (Piispanlinna) 1 10 AYTFUL Tukkasotka tuttvart x 22 Suuresadama x 300 Roomassaare 320 11 AYTMAR Lapasotka merivart x 12 Veere x 4 Põõsaspea 16 12 SOMMOL Haahka hahk x 11 Ristna x /1 Undva, 1/ Veere 13 13 POLSTE Allihaahka kirjuhahk x 28 Undva 28 14 CLAHYE Alli aul x 6 Suuresadama, 3p11m Tahkuna x 100p500m Ristna, 10 Sõru, 500 Sõru-Triigi x 100 Undva, 40 Veere x 10000+ Põõsaspea, 40 Dirhami 11000 15 MELNIG Mustalintu mustvaeras x 2 Tahkuna x 300p300m Ristna x 5 Undva x 40 Põõsaspea 650 16 MELFUS Pilkkasiipi tõmmuvaeras x 5 Tahkuna x 2 Ristna, 2 Sõru-Triigi -
Rmk Annual Report 2014
RMK ANNUAL REPORT 2014 ANNUAL REPORT 2014 3 ADDRESS BY THE CHAIRMAN OF THE BOARD 32-39 ACTIVITIES IN NATURE AND NATURE EDUCATION GROWING FOREST BENEFITS 3 POSSIBILITIES FOR MOVING IN NATURE 34 5 TEN FACTS ABOUT RMK 5 NATURE EDUCATION 36 SAGADI FOREST CENTRE 37 6-11 ABOUT THE ORGANISATION ELISTVERE ANIMAL PARK 38 NATURE CAMERA 38 ALL OVER ESTONIA 8 CHRISTMAS TREES 39 EMPLOYEES 9 HERITAGE CULTURE 39 ACKNOWLEDGEMENTS 10 COOPERATION PROJECTS 11 40-45 RESEARCH WORK 12-23 FOREST MANAGEMENT APPLIED RESEARCH PROJECTS 42 USE OF RESEARCH RESULTS 44 FOREST LAND OVERVIEW 14 SCHOLARSHIPS 45 CUTTING WORKS 15 FOREST RENEWAL 16 AFFORESTATION OF QUARRIES 18 46-51 FINANCIAL SUMMARY TIMBER MARKETING 18 FOREST IMPROVEMENT 20 BALANCE SHEET 48 WASTE COLLECTION 22 INCOME STATEMENT 50 FOREST FIRES 22 AUDITOR’S REPORT 51 HUNTING 23 24-31 NATURE PROTECTION DIVISION OF STATE FOREST 26 PROTECTED AREAS 26 SPECIES UNDER PROTECTION 27 KEY BIOTOPES 28 BIODIVERSITY 28 NATURE PROTECTION WORKS 29 PÕLULA FISH FARM 31 2 Address by the Chairman of the Board GROWING FOREST BENEFITS Aigar Kallas Chairman of the Management Board of RMK The RMK Development Plan 2015-2020 was laid be certain that Estonia’s only renewable natural down in 2014. The overall idea of the six strategic resource would be used wisely for the benefit of goals established with the Development Plan is the society of both today and tomorrow, and that that the forest, land and diverse natural values natural diversity would be preserved, both in the entrusted to RMK must bring greater and more di- protected as well as the managed forest. -
Hydrodynamical and Geological Investigations of Possible Deep Harbour Sites in North-Western Saaremaa Island: Overview and Conclusions
Proc. Estonian Acad. Sci. Eng., 2001, 7, 2, 85–98 HYDRODYNAMICAL AND GEOLOGICAL INVESTIGATIONS OF POSSIBLE DEEP HARBOUR SITES IN NORTH-WESTERN SAAREMAA ISLAND: OVERVIEW AND CONCLUSIONS Jüri ELKENa, Jüri KASKb, Tarmo KÕUTSa, Uno LIIVc, Rein PERENSb, and Tarmo SOOMEREa a Estonian Marine Institute, Paldiski mnt. 1, 10317 Tallinn, Estonia; [email protected] b Estonian Geological Survey, Kadaka tee 82, 12618 Tallinn, Estonia c Corson Consulting, Akadeemia tee 21 B413, 12618 Tallinn, Estonia Received 5 April 2001 Abstract. Saaremaa is the largest Estonian island located to the west of Estonian mainland. A new deep harbour, need for which is stated in the Saaremaa County development plan, is possible only in the north-western part of the island that is environmentally sensitive and belongs partly to the area of Vilsandi National Park. This part of the island is known as wintering area of Steller’s Eider and the sanctuary for seals. Environmental impact assessment of the harbour site selection indicated environmental risks at all the considered sites. Discussion of the assessment results led to additional hydrodynamical and geological investigations of the three harbour location alternatives on the Tagamõisa Peninsula: Undva (Uudepanga Bay), Suuriku-Kuriku (entrance of Tagalaht Bay), and Vaigu (central part of Tagalaht Bay). The investigations contained geological and hydrographic field work and modelling of currents and waves. The results revealed that due to dominating cyclonic circulation and small current speeds in the Uudepanga Bay, the risk of oil pollution from the Undva harbour to nearby Vilsandi National Park is rather low. The risk of polluting Steller’s Eider wintering area in the north from the harbour site is somewhat higher, but still small. -
Eestimaa Looduse Fond Vilsandi Rahvuspargi Kaitsekorralduskava
ELF-i poolt Keskkonnaametile üle antud kinnitamata versioon Eestimaa Looduse Fond Vilsandi rahvuspargi kaitsekorralduskava aastateks 2011-2020 Liis Kuresoo ja Kaupo Kohv Tartu-Vilsandi 2010 ELF-i poolt Keskkonnaametile üle antud kinnitamata versioon SISUKORD Sissejuhatus ..................................................................................................................................... 6 1 Vilsandi rahvuspargi iseloomustus ......................................................................................... 8 1.1 Vilsandi rahvuspargi asend .......................................................................................... 8 1.2 Vilsandi rahvuspargi geomorfoloogiline ja bioloogiline iseloomustus ....................... 8 1.3 Vilsandi rahvuspargi kaitse-eesmärk, kaitsekord ja rahvusvaheline staatus................ 8 1.4 Maakasutus ja maaomand ............................................................................................ 9 1.5 Huvigrupid ................................................................................................................. 13 1.6 Vilsandi rahvuspargi visioon ..................................................................................... 16 2 Väärtused ja kaitse-eesmärgid .............................................................................................. 17 Elustik ........................................................................................................................................... 17 2.1 Linnustik ...................................................................................................................