Probabilistic Approach of the Upper and Middle Odra Basin Daily Rainfall Modeling
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The Oder-Neisse Line As Poland's Western Border
Piotr Eberhardt Piotr Eberhardt 2015 88 1 77 http://dx.doi.org/10.7163/ GPol.0007 April 2014 September 2014 Geographia Polonica 2015, Volume 88, Issue 1, pp. 77-105 http://dx.doi.org/10.7163/GPol.0007 INSTITUTE OF GEOGRAPHY AND SPATIAL ORGANIZATION POLISH ACADEMY OF SCIENCES www.igipz.pan.pl www.geographiapolonica.pl THE ODER-NEISSE LINE AS POLAND’S WESTERN BORDER: AS POSTULATED AND MADE A REALITY Piotr Eberhardt Institute of Geography and Spatial Organization Polish Academy of Sciences Twarda 51/55, 00-818 Warsaw: Poland e-mail: [email protected] Abstract This article presents the historical and political conditioning leading to the establishment of the contemporary Polish-German border along the ‘Oder-Neisse Line’ (formed by the rivers known in Poland as the Odra and Nysa Łużycka). It is recalled how – at the moment a Polish state first came into being in the 10th century – its western border also followed a course more or less coinciding with these same two rivers. In subsequent cen- turies, the political limits of the Polish and German spheres of influence shifted markedly to the east. However, as a result of the drastic reverse suffered by Nazi Germany, the western border of Poland was re-set at the Oder-Neisse Line. Consideration is given to both the causes and consequences of this far-reaching geopolitical decision taken at the Potsdam Conference by the victorious Three Powers of the USSR, UK and USA. Key words Oder-Neisse Line • western border of Poland • Potsdam Conference • international boundaries Introduction districts – one for each successor – brought the loss, at first periodically and then irrevo- At the end of the 10th century, the Western cably, of the whole of Silesia and of Western border of Poland coincided approximately Pomerania. -
SPACE RESEARCH in POLAND Report to COMMITTEE
SPACE RESEARCH IN POLAND Report to COMMITTEE ON SPACE RESEARCH (COSPAR) 2020 Space Research Centre Polish Academy of Sciences and The Committee on Space and Satellite Research PAS Report to COMMITTEE ON SPACE RESEARCH (COSPAR) ISBN 978-83-89439-04-8 First edition © Copyright by Space Research Centre Polish Academy of Sciences and The Committee on Space and Satellite Research PAS Warsaw, 2020 Editor: Iwona Stanisławska, Aneta Popowska Report to COSPAR 2020 1 SATELLITE GEODESY Space Research in Poland 3 1. SATELLITE GEODESY Compiled by Mariusz Figurski, Grzegorz Nykiel, Paweł Wielgosz, and Anna Krypiak-Gregorczyk Introduction This part of the Polish National Report concerns research on Satellite Geodesy performed in Poland from 2018 to 2020. The activity of the Polish institutions in the field of satellite geodesy and navigation are focused on the several main fields: • global and regional GPS and SLR measurements in the frame of International GNSS Service (IGS), International Laser Ranging Service (ILRS), International Earth Rotation and Reference Systems Service (IERS), European Reference Frame Permanent Network (EPN), • Polish geodetic permanent network – ASG-EUPOS, • modeling of ionosphere and troposphere, • practical utilization of satellite methods in local geodetic applications, • geodynamic study, • metrological control of Global Navigation Satellite System (GNSS) equipment, • use of gravimetric satellite missions, • application of GNSS in overland, maritime and air navigation, • multi-GNSS application in geodetic studies. Report -
The Historical Cultural Landscape of the Western Sudetes. an Introduction to the Research
Summary The historical cultural landscape of the western Sudetes. An introduction to the research I. Introduction The authors of the book attempted to describe the cultural landscape created over the course of several hundred years in the specific mountain and foothills conditions in the southwest of Lower Silesia in Poland. The pressure of environmental features had an overwhelming effect on the nature of settlements. In conditions of the widespread predominance of the agrarian economy over other categories of production, the foot- hills and mountains were settled later and less intensively than those well-suited for lowland agriculture. This tendency is confirmed by the relatively rare settlement of the Sudetes in the early Middle Ages. The planned colonisation, conducted in Silesia in the 13th century, did not have such an intensive course in mountainous areas as in the lowland zone. The western part of Lower Silesia and the neighbouring areas of Lusatia were colonised by in a planned programme, bringing settlers from the German lan- guage area and using German legal models. The success of this programme is consid- ered one of the significant economic and organisational achievements of Prince Henry I the Bearded. The testimony to the implementation of his plan was the creation of the foundations of mining and the first locations in Silesia of the cities of Złotoryja (probably 1211) and Lwówek (1217), perhaps also Wleń (1214?). The mountain areas further south remained outside the zone of intensive colonisation. This was undertak- en several dozen years later, at the turn of the 13th and 14th centuries, and mainly in the 14th century, adapting settlement and economy to the special conditions of the natural environment. -
The Late Holocene Decline of Trapa Natans L. in Northern Poland in the Light of New Palaeobotanical and Geochemical Data
Limnol. Rev. (2019) 19, 2: 77–91 DOI 10.2478/limre-2019-0007 The late Holocene decline of Trapa natans L. in Northern Poland in the light of new palaeobotanical and geochemical data Agnieszka Lewandowska1*, Przemysław Niedzielski2, Mariusz Gałka3 1Department of Biogeography and Palaeoecology, Adam Mickiewicz University in Poznan, Krygowskiego 10, 61-680 Poznań, Poland, e-mail: [email protected] (* corresponding author) 2Department of Analytical Chemistry, Adam Mickiewicz University in Poznan, Umultowska 89, 61-614 Poznań, Poland, e-mail: [email protected] 3Department of Geobotany and Plant Ecology, University of Lodz, Banacha 12/16, 90-237 Łódź, Poland, e-mail: [email protected] Abstract: Trapa natans (water chestnut) is an aquatic, thermophilic plant whose decline has been observed in many localities in central Europe during the last decades. In this paper, we present a description of two new T. natans subfossil sites located outside its present northern distribution in Poland. High-resolution analysis of plant macrofossils supported by geochemical analysis were undertaken to reconstruct the palaeoecological habitat and examine the cause of the late Holocene decline of T. natans that took place ca. 4000 calibrated years before AD 1950 (cal. yr BP) in a paleolake, presently the Bagno Kusowo bog. Its disappearance was a consequence of terrestrialisation and the development of peatland. In paleolake sediments covered by the peat layer in the Mechacz Wielki bog, T. natans macrofossils were found from before ca. 3300 cal. yr BP. The decline ofT. natans could have resulted from the changes and development of other plant communities where the dominant role was played by Stratiotes aloides and Nymphaea sp. -
Action Plan Lower Silesia, Poland
Smart and Green Mining Regions of EU Action Plan Lower Silesia, Poland Leading the European policies Research innovation towards more sustainable mining www.interregeurope.eu/remix Action Plan Lower Silesia, Poland Contents Go to the content by clicking the section title 1. General information 3 2. Policy context 4 3. Action 1: Impact on the changes in the Regional 7 Innovation Strategy of the Lower Silesian Voivodeship for 2011–2020 in the area of mining and raw materials 3.1. Relevance to the REMIX project 7 3.2. Nature of the action 9 3.3. Stakeholders involved 12 3.4. Timeframe 14 3.5. Costs 15 3.6. Funding sources 15 4. Action 2: Improving the governance of the RIS3 16 and raising public awareness of the importance of innovative mining in regional economic development 4.1. Relevance to the REMIX project 16 4.2. Nature of the action 18 4.3. Stakeholders involved 19 4.4. Timeframe 20 4.5. Costs 21 4.6. Funding sources 21 Back to Contents 1. General information Project: REMIX – Smart and Green Mining Regions of EU Partner organisation: The Marshal’s Office of Lower Silesian Voivodeship Country: Poland NUTS2 region: PL51 Lower Silesia Contact person: Ewa Król Email address: [email protected] Phone number: +48 71 776 9396 REMIX Interreg Europe . Action plan 3 Back to Contents 2. Policy context The Action Plan aims to impact: Investment for Growth and Jobs programme European Territorial Cooperation programme Other regional development policy instrument Name of the policy instrument addressed: Regional Innovation Strategy of Lower Silesian Voivodeship The Marshal’s Office of Lower Silesian Voivodeship is the regional authority responsible for the management of regional development policy on the territory of Lower Silesia pursuant to Article 3 of the Act of 6 December 2006 (Dziennik Ustaw [Journal of Laws] 2006, No. -
LCSH Section W
W., D. (Fictitious character) William Kerr Scott Lake (N.C.) Waaddah Island (Wash.) USE D. W. (Fictitious character) William Kerr Scott Reservoir (N.C.) BT Islands—Washington (State) W.12 (Military aircraft) BT Reservoirs—North Carolina Waaddah Island (Wash.) USE Hansa Brandenburg W.12 (Military aircraft) W particles USE Waadah Island (Wash.) W.13 (Seaplane) USE W bosons Waag family USE Hansa Brandenburg W.13 (Seaplane) W-platform cars USE Waaga family W.29 (Military aircraft) USE General Motors W-cars Waag River (Slovakia) USE Hansa Brandenburg W.29 (Military aircraft) W. R. Holway Reservoir (Okla.) USE Váh River (Slovakia) W.A. Blount Building (Pensacola, Fla.) UF Chimney Rock Reservoir (Okla.) Waaga family (Not Subd Geog) UF Blount Building (Pensacola, Fla.) Holway Reservoir (Okla.) UF Vaaga family BT Office buildings—Florida BT Lakes—Oklahoma Waag family W Award Reservoirs—Oklahoma Waage family USE Prix W W. R. Motherwell Farmstead National Historic Park Waage family W.B. Umstead State Park (N.C.) (Sask.) USE Waaga family USE William B. Umstead State Park (N.C.) USE Motherwell Homestead National Historic Site Waahi, Lake (N.Z.) W bosons (Sask.) UF Lake Rotongaru (N.Z.) [QC793.5.B62-QC793.5.B629] W. R. Motherwell Stone House (Sask.) Lake Waahi (N.Z.) UF W particles UF Motherwell House (Sask.) Lake Wahi (N.Z.) BT Bosons Motherwell Stone House (Sask.) Rotongaru, Lake (N.Z.) W. Burling Cocks Memorial Race Course at Radnor BT Dwellings—Saskatchewan Wahi, Lake (N.Z.) Hunt (Malvern, Pa.) W.S. Payne Medical Arts Building (Pensacola, Fla.) BT Lakes—New Zealand UF Cocks Memorial Race Course at Radnor Hunt UF Medical Arts Building (Pensacola, Fla.) Waʻahila Ridge (Hawaii) (Malvern, Pa.) Payne Medical Arts Building (Pensacola, Fla.) BT Mountains—Hawaii BT Racetracks (Horse racing)—Pennsylvania BT Office buildings—Florida Waaihoek (KwaZulu-Natal, South Africa) W-cars W star algebras USE Waay Hoek (KwaZulu-Natal, South Africa : USE General Motors W-cars USE C*-algebras Farm) W. -
Silesia, Poland - Regional Profile 1
SILESIA, POLAND - REGIONAL PROFILE 1 REGIONAL PROFILE Silesia GENERAL INFORMATION Country: Poland Region Name: Silesia Region NUTS2 code*: PL22 - Silesia Region NUTS3 code PL22A - Katowicki / PL228 Bytomski PL229 - Gliwicki / PL227 - Rybnicki PL22B - Sosnowiecki / PL22C - Tyski Main urban centres in the region (by population): Katowice - 294,510 / Częstochowa - 222,292 Sosnowiec - 202,036 / Gliwice - 179,806 Zabrze - 173,374 / Bielsko-Biała - 171,259 Bytom - 166,795 / Rybnik - 138,696 Ruda Śląska - 138,000 / Tychy - 127,831 *NUTS: Nomenclature of Territorial Units for Statistics NOTICE ON COVID-19 The data contained within this regional profile was primarily gathered prior to the COVID-19 pandemic. It is recognised that the pandemic has had an adverse impact on energy demand. Although the consequences and implications are significant, they remain emergent and dynamic. An update to this document should be considered, once these consequences and implications are clearer and more quantifiable. INITIATIVE FOR COAL REGIONS IN TRANSITION SILESIA, POLAND - REGIONAL PROFILE 2 Overview Silesia is the most populated and urbanised region in Poland with over 4.5 million inhabitants. 78% of its population live in cities and its population density is 370 people/km2. The region comprises of eight NUTS-3 subregions, out of which six are notably affected by coal mining and related industries. The communities where the majority of the miners live are located in central and western subregions - namely Katowicki subregion, Bytomski subregion, Gliwicki subregion, Rybnicki subregion, Sosnowiecki subregion, and Tyski subregion. Silesia is the most coal-dependent region in Poland with mining playing an important role in the regional economy. However, its gradual decline in recent years is also apparent as production is declining in view of falling productivity and low profitability. -
Changes in the Spatial Development of Flood Hazard Areas in Poland Between 1990 and 2018 in the Light of Legal Conditions
Land Use Policy 102 (2021) 105274 Contents lists available at ScienceDirect Land Use Policy journal homepage: www.elsevier.com/locate/landusepol Changes in the spatial development of flood hazard areas in Poland between 1990 and 2018 in the light of legal conditions Marta Borowska-Stefanska´ a,*, Sławomir Kobojek a, Michał Kowalski a, Marek Lewicki b, Przemysław Tomalski a, Szymon Wi´sniewski a a University of Lodz, Faculty of Geographical Sciences, Poland b University of Lodz, Faculty of Law and Administration, Poland ARTICLE INFO ABSTRACT Keywords: The study presented herein focuses on determining the relationship between changes in the scale of economic Flood hazard areas losses between 1990–2018 which occurred in areas of high (10 %) and medium (1%) probability of flood Floods occurrence as well as floodhazard areas due to the destruction of a stopbank, and changes in legislation affecting Flood plain legislation the spatial development of such areas within the said period. The analysis of changes in the development of flood Spatial development hazard areas was conducted by means of the Corine Land Cover database. The results of the analysis were later Poland used to evaluate potential economic losses on flood plains, and then spatiotemporal analysis was applied to identify areas with clusters of high and low loss values and the trends regarding their transformations. In consequence, the identification of municipality (Polish: gmina) clusters allowed us to verify the dependence of such transformations on those factors that could impact their intensity. For that purpose, we analysed the coverage of local spatial development plans for individual clusters. On the basis of the conducted studies, we concluded that the implemented legal solutions are not entirely effective, which has also been stated by the legislator. -
Wykaz Identyfikatorów I Nazw Jednostek Podziału Terytorialnego Kraju” Zawiera Jednostki Tego Podziału Określone W: − Ustawie Z Dnia 24 Lipca 1998 R
ZAK£AD WYDAWNICTW STATYSTYCZNYCH, 00-925 WARSZAWA, AL. NIEPODLEG£0ŒCI 208 Informacje w sprawach sprzeda¿y publikacji – tel.: (0 22) 608 32 10, 608 38 10 PRZEDMOWA Niniejsza publikacja „Wykaz identyfikatorów i nazw jednostek podziału terytorialnego kraju” zawiera jednostki tego podziału określone w: − ustawie z dnia 24 lipca 1998 r. o wprowadzeniu zasadniczego trójstopniowego podziału terytorialnego państwa (Dz. U. Nr 96, poz. 603 i Nr 104, poz. 656), − rozporządzeniu Rady Ministrów z dnia 7 sierpnia 1998 r. w sprawie utworzenia powiatów (Dz. U. Nr 103, poz. 652) zaktualizowane na dzień 1 stycznia 2010 r. Aktualizacja ta uwzględnia zmiany w podziale teryto- rialnym kraju dokonane na podstawie rozporządzeń Rady Ministrów w okresie od 02.01.1999 r. do 01.01.2010 r. W „Wykazie...”, jako odrębne pozycje wchodzące w skład jednostek zasadniczego podziału terytorialnego kraju ujęto dzielnice m. st. Warszawy oraz delegatury (dawne dzielnice) miast: Kraków, Łódź, Poznań i Wrocław a także miasta i obszary wiejskie wchodzące w skład gmin miejsko-wiejskich. Zamieszczone w wykazie identyfikatory jednostek podziału terytorialnego zostały okre- ślone w: − załączniku nr 1 do rozporządzenia Rady Ministrów z dnia 15 grudnia 1998 r. w sprawie szczegółowych zasad prowadzenia, stosowania i udostępniania krajowego rejestru urzędo- wego podziału terytorialnego kraju oraz związanych z tym obowiązków organów admini- stracji rządowej i jednostek samorządu terytorialnego, obowiązującego od dnia 1 stycz- nia 1999 r. (Dz. U. z 1998 r. Nr 157, poz. 1031), − kolejnych rozporządzeniach Rady Ministrów zmieniających powyższe rozporządzenie w zakresie załącznika nr 1 (Dz. U. z 2000 Nr 13, poz. 161, z 2001 r. Nr 12, poz. 100 i Nr 157, poz. -
Geological Map Lausitz-Jizera-Karkonosze And
Przegl¹d Geologiczny, vol. 52, no. 8/2, 2004 Geological Map Lausitz-Jizera-Karkonosze and Muskau Arch Geopark as examples of cross-border cooperation of the national geological surveys of Poland, the Czech Republic and Germany Jacek Robert Kasiñski1, Wies³aw Kozdrój2, Jacek KoŸma2, Ottomar Krentz3, Mojmir Opletal4, Andrzej Stachowiak2 A b s t r a c t . The article presents the cross-border cooperation of geologists from the Lower Silesian Branch of Polish Geological Institute and the national geological surveys of the Czech Republic and Germany. The current cooperation is discussed on the basis of Geological Map Lausitz–Jizera–Karkonosze as well as on geological research of the Muskau Arch. The Geological Map Lausitz–Jizera–Karkonosze, in 1 : 100,000 scale, with Comments, presents the geology of the north-western part of the Bohemian Massif. A short geotectonic evolution of the area from Neoproterozoic to Cenozoic is presented. The results of Polish-German geo- logical research and inventory of so-called “geotopes” are the basis to establish a cross-border Muskau Arch Geopark. Key words: geological map, Bohemian Massif, Cadomian and Variscan orogenesis, epi-Variscan cover, geotectonic evolution, geotope, geopark, geodiversity conservation, goetourism, Muskau Arch, glaciotectonics The Lower Silesian Branch of the Polish Geological 1997), Geological Map for Tourists, Góry Sto³owe Mts.,in Institute operates in southwestern Poland. A cross-border 1 : 50,000 scale (Èech & Gawlikowska, 1999), and Geolo- cooperation with geological surveys of the neighbouring gical Map for Tourists Góry Bystrzyckie and Orlickie Mts., countries, the Czech Republic and Germany, has been in 1 : 50,000 scale (to be published). -
Mineralogical Society of Poland
Mineralogical Society of Poland www.ptmin.agh.edu.pl The picturesque location of the Obrzycko Palace (19th century) on the banks of the Warta River, the warm and sunny autumn days, and the colorful trees of the historic park were the background for the discus- ANNUAL MEETING OF THE PETROLOGY GROUP sions that lasted until late into the night. On the fi nal day, participants OF THE MINERALOGICAL SOCIETY OF POLAND, visited the Morasko Reserve in Poznan´ , where 8 preserved craters bear OBRZYCKO, POLAND, OCTOBER 19–21, 2012 witness to the largest iron meteorite shower in Europe. In the surround- ings of the craters, many fragments of IAB iron have been found. The 20th annual meeting of the Petrology Group of the MSP will be held in the Sudetes and will be devoted to mantle rocks and their geodynamic signifi cance. A NEW DISCOVERY: THE LARGEST MORASKO IRON Participants in the MSP Petrology Group meeting at Obrzycko, Poland The Petrology Group of the Mineralogical Society of Poland (MSP) gathered for its 19th annual meeting at Obrzycko, western Poland, and U devoted a special session to meteorites. The conference theme was a ˙ great opportunity for the organizers, the Poznan´ members of the MSP -Z ski ´ under the leadership of Prof. Andrzej Muszyn´ ski, to present the famous czyn ˛ Morasko iron meteorite, which fell to Earth in ca. 5000 BP near the present-day location of the Institute of Geology of the Adam Mickiewicz University in Poznan´ . The scientifi c program included 6 invited lectures, 21 talks, and 25 Me Maciej Photo: poster presentations. -
Flood Risk of Lower Silesia Voivodship
CIVIL AND ENVIRONMENTAL ENGINEERING REPORTS No. 10 2013 FLOOD RISK OF LOWER SILESIA VOIVODSHIP Mariusz ADYNKIEWICZ-PIRAGAS*, Iwona LEJCUŚ Institute of Meteorology and Water Mangement – National Resarch Instytute Wrocław Branch, Regional Research Department, Parkowa St. 30, 51-616 Wrocław, Poland Floods are natural events of a random nature that cause damage in property, agriculture, and industry. Floods in the upper and middle Odra basin, particularly on a large scale, are characterized by their specificity of arising and shaping. Analyses of historical material prove that the largest floods are during the summer season, especially in July and August. Those events are caused by wide and intensive precipitation lasting 2-3 days. Moreover spatial ranges in the Odra basin and runoff sequence are also the important reasons. Other important factors for the flood risk scale in a region is knowledge of the flood risk index established on the basis of observed floods or that of Maximum Probability Flood. In this paper flood risk in the territory of Lower Silesia Province was evaluated on the basis of chosen indices of flood risk. Keywords: Odra catchment, flood risk zones 1. INTRODUCTION Flood is a natural disaster that threatens the safety of people and animals, and cause damage to human property, and losses in the national economy. It is natural and random phenomenon. It can cause torrential rains, short thunderstorms, rapid melting of snow, strong winds on the coast from the sea towards the land and the freezing of rivers. Flood is a high water, during which water overflows the level of embankment crown and flood river valleys or depressed areas, thereby causing damage and financial and non-economic (social, moral, etc.) losses [Dubicki, Malinowska-Małek 1999].