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Raport Z Wykonania Map Zagrożenia Powodziowego I Map Ryzyka
Projekt: Informatyczny system osłony kraju przed nadzwyczajnymi zagrożeniami Nr Projektu: POIG.07.01.00–00–025/09 RAPORT Z WYKONANIA MAP ZAGROZ ENIA POWODZIOWEGO I MAP RYZYKA POWODZIOWEGO Projekt: Informatyczny system osłony kraju przed nadzwyczajnymi zagrożeniami Nr Projektu: POIG.07.01.00–00–025/09 SPIS TREŚCI: WYKAZ SKRÓTÓW STOSOWANYCH W DOKUMENCIE 4 DEFINICJE 5 I. WPROWADZENIE 7 II. PODSTAWA OPRACOWANIA MZP I MRP 9 III. ZAKRES OPRACOWANIA MZP I MRP 13 IV. DANE WYKORZYSTANE DO MZP I MRP 37 IV.1. NUMERYCZNY MODEL TERENU 41 IV.2. PRZEKROJE KORYTOWE RZEK 41 V. OPIS METODYKI OPRACOWANIA MZP 43 V.1. MODELOWANIE HYDRAULICZNE 43 V.2. SCENARIUSZE POWODZIOWE 70 V.3. WYZNACZANIE OBSZARÓW ZAGROŻENIA POWODZIOWEGO 73 VI. OPIS METODYKI OPRACOWANIA MRP 83 VI.1. NEGATYWNE KONSEKWENCJE DLA LUDNOŚCI 83 VI.2. RODZAJ DZIAŁALNOŚCI GOSPODARCZEJ 84 VI.3. OBIEKTY ZAGRAŻAJĄCE ŚRODOWISKU W PRZYPADKU WYSTĄPIENIA POWODZI 86 VI.4. OBSZARY CHRONIONE 87 VI.5. OBSZARY I OBIEKTY DZIEDZICTWA KULTUROWEGO 87 VI.6. OBLICZENIE WARTOŚCI POTENCJALNYCH STRAT POWODZIOWYCH 88 VII. FORMA SPORZĄDZENIA MZP i MRP 91 VII.1. BAZA DANYCH PRZESTRZENNYCH MZP I MRP 91 VII.2. WIZUALIZACJA KARTOGRAFICZNA MZP i MRP 92 VIII. PUBLIKACJA I PRZEKAZANIE ORGANOM ADMINISTRACJI MZP I MRP 101 VIII.1. PRZEKAZANIE MZP i MRP ORGANOM ADMINISTRACJI 101 VIII.2. PUBLIKACJA MZP i MRP 101 VIII.3. ZASADY UDOSTĘPNIANIA MZP i MRP 105 2 Projekt: Informatyczny system osłony kraju przed nadzwyczajnymi zagrożeniami Nr Projektu: POIG.07.01.00–00–025/09 IX. MZP i MRP W PLANOWANIU I ZAGOSPODAROWANIU PRZESTRZENNYM 107 X. PRZEGLĄD I AKTUALIZACJA MZP I MRP 114 XI. -
The Case of the Vistula River in Warsaw
Vol. 14/2010 pp. 203-212 Joanna Angiel University of Warsaw Faculty of Geography and Regional Studies Department of Geographical Education e-mail: [email protected] RESTORING THE SOCIAL VALUE OF RIVERS THROUGH EDUCATION: THE CASE OF THE VISTULA RIVER IN WARSAW Abstract: The article discusses the values of the Vistula River in Poland’s capital city, Warsaw. The author presents the results of studies identifying residents’ perceptions of the river and outlines local community processes that aim to restore the river’s social value, notably through education. Key words: public awareness, Vistula River, river value, perception, geography education. INTRODUCTION People’s relationship with rivers, and more broadly speaking with nature, has changed over time. That relationship is dependent on attitudes towards the natural environment, the cultural sphere in which an individual grows up and develops, as well as individuals’ worldviews, social awareness, and the system of received values, among other factors. (Ostrowska, 1994; Pulinowa, 1996). For many pre-agrarian societies rivers held religious, or spiritual values. They provided water, food, and protection. With the rise of agrarian societies, people remained closely tied to rivers, but the relation began to include the intensified use of waterways, chiefly for agriculture. The industrial period saw the beginnings of large-scale “industrial transfor- mations of nature,” including rivers. Deprived of their sacred status and, even, of common respect, rivers often served as channels of industrial waste disposal and recipients of urban sewage. In the present period of socio-eco- nomic development, increasingly more attention is given to the state of the environment, including rivers. -
Improved Tools for River Flood Preparedness Under Changing Risk - Poland
7th Study Conference on BALTEX, Borgholm, Sweden, 10-14 June 2013 Improved tools for river flood preparedness under changing risk - Poland Zbigniew W. Kundzewicz Institute of Agricultural and Forest Environment, Polish Academy of Sciences, Poznań, Poland and Potsdam Institute for Climate Impact Research, Potsdam, Germany - Changing flood risk in Poland - Improved tools for river flood preparedness - Changing flood risk in Poland - Improved tools for river flood preparedness River flooding in Poland River flooding is the most destructive natural peril in the Baltic Sea Basin in general and in Poland in particular. Flood risk and preparedness became matters of broad concern, following the dramatic floods in Poland in 1997 and 2010, when dozens of people were killed, national flood losses reached the level of billions of Euros and the topic made it to cover stories. Floods in PL, May-June 2013 IAHS Special Publication 10 (April 2012) ISBN ISBN 978-1- 907161-28-5 (Paperback); 516 + xvi pages 10 12 14 0 2 4 6 8 Dartmouth Flood Observatory. Source: et al. (2012) Kundzewicz Dartmouth Flood Observatory. Increasing number of large floods, according tothedata in 1985 1986 1987 1988 1989 1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 y = 0.3123x + 2.46 y = 0.2608x + 0.33 R R 2 2 = 0.4339 = 0.6012 Magnitude=>5 Severity=>1.5 Trend in number of days with precipitation in excess of 30 mm, and (b) trend in maximum 5-day precipitation, 1971–2002 (after Lorenc & Olecka, 2006). Catastrophic floods of regional extent in Poland: from 1946 to 1970; from 1971 to 1990; from 1991 to 2010; from 1946 to 2010. -
Forestry in Poland with Special Attention to the Region of the Pomeranian Young Moraine
AFSV Forstwirtschaft und Standortkartierung Waldoekologie online Heft 2 Seite 49 - 58 9 Fig., 2 Tab. Freising, Oktober 2005 Forestry in Poland with special attention to the region of the Pomeranian Young Moraine Marcin S z y d l a r s k i Abstract In the year 2004 the ASFV celebrated its 50th anniversary holding a conference in Sulęczyno, Kartuzy. This event offered the possibility to give an actual overview of forest resources and forest functions in Poland. The excursions of the meeting focused on the fascinating, diversified forest landscape formed by the Pomeranian phase of the Baltic glaciation. The Kartuzy Forest District is situated in the heart of the Kashubian Lakeland and the moraine hills. The landscape is not only characterized by the natural occurrence of Baltic beech forests but also by high diversity of soils and meso- and microclimatic de- viations providing habitats for rare plant species, including some plants typical of mountain regions. The tree species combination of the District is formed by pine, spruce, and beech. The oldest parts of the forests are legally protected as nature reserves. I. POLISH FOREST RESOURCES At the end of the 18th century the Polish forest area comprised about 40%, nowadays forests in Po- land cover approximately 8,942,000 hectares, which is 28.6% of an overall country area. According to international standards (FAO Forestry Department) and tests on economic forestry areas, the wooded area in Poland comprises more than 9,040,000 hectares, which is as many as 30% forest cover and is close to Central European average (www.fao.org/forestry/site/18308/en/pol). -
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Institute of National Remembrance https://ipn.gov.pl/en/digital-resources/articles/7371,Under-the-red-boot.html 2021-09-29, 04:21 10.02.2021 Under the red boot It wasn’t an “ordinary” attack, because even assuming that every aggression is unique on its own, it’s hard not to notice some unprecedented aspects of the soviet invasion of Poland on September 17th, 1939. For the first time ever, one country invaded another claiming that the invaded one… didn’t exist. Narrative: abolishing of a country This was the Soviet stance on Poland on the 17th day of the German occupation, in an infamous note handed to Wacław Grzybowski, the Polish ambassador in the Soviet Union, on September 17th 1939. The note said, that Warsaw was no longer the capital of Poland and that the Polish government was disbanded. All this was supposed to mean that the Polish state “factually” ceased to exist. The Soviets went even further in creating an excuse for their aggression, claiming in a shocking document, that Poland left for itself was a place where different kinds of initiatives that could be a threat to the Soviet Union could sprout from. The “final nail in the coffin” were the note’s closing words stating that the Soviet government, unable to remain indifferent to the situation of the defenceless, “brotherly” Ukrainian and Belarusian people, ordered the Red Army to cross the Polish border and take these people under its protection. Why did Kremlin portray itself in the document as a party which wasn’t involved in the war? After all, it didn’t make a pact with Germany on the 23rd of August, 1939 to then remain neutral in the face of the German occupation of Poland. -
Floods in Poland from 1946 to 2001 — Origin, Territorial Extent and Frequency
Polish Geological Institute Special Papers, 15 (2004): 69–76 Proceedings of the Conference “Risks caused by the geodynamic phenomena in Europe” FLOODS IN POLAND FROM 1946 TO 2001 — ORIGIN, TERRITORIAL EXTENT AND FREQUENCY Andrzej DOBROWOLSKI1, Halina CZARNECKA1, Janusz OSTROWSKI1, Monika ZANIEWSKA1 Abstract. Based on the data concerning floods on the territory of Poland during the period 1946–2001, the reasons generating floods, the number of regional floods in the rivers catchment systems, and sites of local floods occurrence, were defined. Both types of floods: caused by riverbank overflows, and land flooding by rain or snow-melt water, were considered. In the most cases, the floods were caused by rainfall. They were connected with changes in the rainfall structure within Po- land. In each season of the year floods of various origin were observed. When the flood initiating factors appeared simulta- neously, the flood grew into a catastrophic size. In present analysis, for the first time in Poland, a large group of local floods has been distinguished. A special attention has been paid to floods caused by sudden flooding of the land (flash flood), including floods in the urban areas — more and more frequent during the recent years. The results of the analyses have provided important data for the assessment of the flood hazard in Poland, and for the creation of a complex flood control strategy for the whole country and/or for selected regions. Key words: flood, classification of floods, floods territorial extent, frequency of floods occurrence, torrential and rapid rain- fall, threat of life, material losses. Abstrakt. Na podstawie zbioru danych z lat 1946–2001 okreœlono przyczyny wystêpowania powodzi w Polsce, liczbê powodzi re- gionalnych w uk³adzie zlewni rzecznych oraz miejsca wyst¹pieñ powodzi lokalnych. -
Program Ochrony Środowiska Dla Gminy Juchnowiec Kościelny Do 2022 R
GMINA JUCHNOWIEC KOŚCIELNY Program Ochrony Środowiska dla Gminy Juchnowiec Kościelny do 2022 r. z perspektywą do 2026 r. 2019 r. 1 | S t r o n a Opracowanie wykonane na zlecenie: Urząd Juchnowiec Kościelny ul. Lipowa 10 16-061 Juchnowiec Kościelny www.juchnowiec.gmina.pl Wykonawca: Idenea Consulting sp. z o.o. ul. Skłodowskiej – Curie 3 lok. 63 15-094 Białystok www.idenea.pl [email protected] 2 | S t r o n a Spis treści Wykaz skrótów i symboli ......................................................................................................................... 4 1. Wstęp .............................................................................................................................................. 6 2. Streszczenie ................................................................................................................................... 10 3. Podstawowe informacje o gminie ................................................................................................. 12 3.1. Położenie i podział administracyjny .......................................................................................... 12 3.2. Budowa geologiczna, krajobraz ................................................................................................. 12 3.3. Ludność i struktura osadnicza ................................................................................................... 13 3.4. Gospodarka i rynek pracy .......................................................................................................... 14 4. -
Mühlen-Tabelle (Nicht Im Buch Enthalten)
In der nachfolgenden Übersicht wurden alle in Pommern zu Beginn des 20. Jh. vorhandenen Ortschaften mit den Standorten ihrer Wind- (WI), Wasser- (WA), Dampf- (DA) und Motormühlen (MM) sowie ihrer Wasserkraftwerke (WKW) aufgelistet. Ortschaften der WI erh. W erh. DA erh. W erh. M u. erh. Mühlen- und WKW- Standorte WI A W u. DA K W WK Exp A MM u. W K W l. MM W ges. ges Abtshagen/AK Grimmen 1 1 Abtshagen/AK Schlawe 2 2 (Dobiesław) Adl. Boltenhgn./AK Greifwald 1 1 Adl. Freest/AK Lauenburg 2 2 (Wrześcienko) Ahlbeck/AK Ueckermünde 1 1 2 1 Ahrenshagen/AK Franzb.-B. 1 1 Ahrenshoop/AK Franzb,-Barth 1 1 1 1 Albinshof/AK Anklam 1 1 Albrechtsdorf/AK Ueckerm. 1 1 1* 3 (Karczno)* Alexandrahütte/AK Schlawe 2 2 (Nowy Zytnik) Alt Banzin/AK Köslin 1 1 (Będzino) Alt Belz/AK Köslin 2 2 (Str. Bielice) Alt Bewersdorf/AK Schlawe 1 1* 2 (Bobrowice)* Alt Bork/AK Kolberg-Körlin 1 1 (SraryBorek) Altbraa/AK Schlochau 1 1 (Stara Brda) Altdamm/AK Randow 1* 5 1 6 1 (Dąbie)* Alt Dargsow/AK Cammin 1 1 (Dargoszewo) Alt Döberitz/AK Regenw. 1* 1 (Str. Dobrzyca)* Altefähr/AK Rügen* 2* 2 Altendorf/AK Greifenberg 1 1 1 1 (Łatno) Altenfließ/AK Friedeberg 1 1 (Prrzyłęg) Altenhagen/AK Demmin 1 1 Altenhagen/AK Schlawe 2 2 (Jezyce) Altenkirchen/AK Rügen* 2* 2 Altensien/AK Rügen 2 2 Altentreptow/AK Demmin 5 2 1 7 1 Altenwalde/AK Neustettin 2 2 (Liszkowo) Altenwedel/AK Saatzig 1 1 2 (Sicko) Alt Falkenberg/AK Pyritz 2 2 (Chabowo) Alt Fanger/AK Naugard 1 1 (Węgorza) Alt Gatschow/AK Demmin 1 1 Alt Grape/AK Pyritz 1 1 (Str. -
Bydgoszcz 20-01-2006
Bull Vet Inst Pulawy 58, 399-404, 2014 DOI: 10.2478/bvip-2014-0062 Occurrence of veterinary antibiotics and chemotherapeutics in fresh water, sediment, and fish of the rivers and lakes in Poland Małgorzata Gbylik-Sikorska, Andrzej Posyniak, Kamila Mitrowska, Anna Gajda, Tomasz Błądek, Tomasz Śniegocki, Jan Żmudzki Department of Pharmacology and Toxicology, National Veterinary Research Institute, 24-100 Pulawy, Poland [email protected] Received: January 29, 2014 Accepted: August 22, 2014 Abstract The occurrence of commonly used veterinary antimicrobial agents was investigated in 159 fresh water, 443 fish, and 150 sediment samples from Polish rivers and lakes. The agents included aminoglycosides, β-lactams, diaminopyrimidines, fluoroquinolones, lincosamides, macrolides, pleuromutilins, sulfonamides, and tetracyclines. The analysis was performed by three different sample preparation procedures for each matrix and it was performed by liquid chromatography-tandem mass spectrometry with electrospray ionisation source in positive mode, under the same conditions. All analytical methods used were validated and showed good sensitivity, accuracy, and precision. The LOQ was in the range from 5 µg/kg to 125 µg/kg for fish samples, from 0.02 µg/L to 10 µg/L for fresh water samples, and from 1 µg/kg to 8 µg/kg for sediment samples. Keywords: antibiotics, water, sediments, fish, LC-MS/MS, Poland. Introduction have a negative influence on human health (7, 8). Several publications have reported the occurrence of Antimicrobial compounds are widely used in various veterinary and human pharmaceuticals, human and veterinary medicine to protect human and including antibiotics, in surface water, groundwater, animal health, to prevent economic losses, and to help wastewater, sediments, and soil. -
BIULETYN CODZIENNY.Pdf
INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY Centralne Biuro Hydrologii Operacyjnej w Warszawie ul. Podleśna 61, 01-673 Warszawa tel.: (22) 56-94-140 e-mail: [email protected] www.imgw.pl www.meteo.imgw.pl www.stopsuszy.imgw.pl CODZIENNY BIULETYN HYDROLOGICZNY - AKTUALIZACJA* STANY WODY NA WYBRANYCH STACJACH WODOWSKAZOWYCH W DORZECZU WISŁY 27.09.2021 r. na godz. 08:00 Prognoza stanu na dzień Stan alarmowy Stan ostrzegawczy Przepływ Stan wody Dobowa zmiana Rzeka Stacja wodowskazowa Strefa stanu [cm] [cm] [cm] [m3/s] [cm] [cm] 28.09.2021 29.09.2021 30.09.2021 Wisła USTROŃ-OBŁAZIEC dolna średnich 230 180 1,83 116 -2 Wisła SKOCZÓW dolna średnich 260 210 3,26 152 -1 Wisła BIERUŃ NOWY górna średnich 330 220 25,9 109 -2 Wisła KRAKÓW-BIELANY dolna średnich 520 370 166 7 Wisła KARSY górna średnich 750 550 213 226 5 Wisła SZCZUCIN górna średnich 660 460 253 195 -2 Wisła SANDOMIERZ górna średnich 610 420 353 218 -15 Wisła ZAWICHOST dolna średnich 620 480 441 302 -16 295 280 275 Wisła PUŁAWY-AZOTY górna średnich 550 450 549 237 -14 225 220 205 Wisła WARSZAWA-NADWILANÓWKAgórna średnich 800 750 742 265 -12 Wisła WARSZAWA-BULWARY dolna średnich 650 600 740 178 -9 165 154 148 Wisła WYSZOGRÓD górna średnich 550 500 1010 376 -7 Wisła KĘPA POLSKA górna średnich 500 450 1090 311 -13 302 294 285 Wisła WŁOCŁAWEK górna średnich 650 600 1040 250 6 Wisła TORUŃ dolna średnich 650 530 1020 285 -22 Wisła FORDON dolna średnich 650 530 1060 278 -32 Wisła CHEŁMNO górna średnich 630 510 1170 331 -42 Wisła GRUDZIĄDZ górna średnich 650 540 -
INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY Biuro Prognoz Hydrologicznych W Krakowie Obszar Warszawa Ul
INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY Biuro Prognoz Hydrologicznych w Krakowie Obszar Warszawa ul. Podleśna 61, 01-673 Warszawa tel.: 22-56-94-144 fax.: 22-834-48-97 e-mail: [email protected] www.pogodynka.pl www.imgw.pl INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY BIURO PROGNOZ HYDROLOGICZNYCH W KRAKOWIE Obszar Warszawa podaje KOMUNIKAT OPADOWY z dnia 30.07.2019 godz. 6 UTC UTC - ang. Universal Time Coordinated - czas uniwersalny; w okresie letnim czas urzedowy w Polsce UTC+2h, a w okresie zimowym UTC+1h. Dobowa suma opadu 6 UTC Stacja meteorologiczna Rzeka [mm] A B C województwo śląskie PILICA Pilica 24.7 BONOW ICE Pilica 18.5 W ĄSOSZ Pilica 10.5 województwo świętokrzyskie STANOW ISKA Czarna (Maleniecka) 9.8 PILCZYCA Czarna (W łoszczowska) 1.4 JANUSZEW ICE Czarna (W łoszczowska) 8.4 województwo lubelskie JARCZEW W ilga 37.6 województwo podlaskie ZAMOSZE Narew 0.7 BONDARY Narew 1.1 NAREW Narew 0.1 TYKOCIN Narew 0.3 MARIANOW O II Narew 0.1 NOW OSADY Kołonna 1.8 BIAŁOW IEŻA Narewka 2.3 NAREW KA Narewka 0.9 CHRABOŁY Orlanka 0.0 NOW OSIÓŁKI Supraśl 2.0 SUPRAŚL Supraśl 0.0 FASTY Supraśl 0.0 DRAHLE Sokołda 0.0 JAŁÓW KA Sokołda 0.0 BIAŁYSTOK Biała 0.0 MOŃKI Nereśl 0.0 JABŁONOW O-W YPYCHY Ślina 0.1 ZAW ADY Ślina 0.0 DĘBOW O Biebrza 1.4 OSOW IEC Biebrza 0.0 BURZYN Biebrza 0.0 RÓŻANYSTOK Sidra 0.0 JANÓW Brzozówka 0.0 BIEBRZA Ełk 0.0 RADZIŁÓW W issa 0.2 PTAKI Pisa 0.1 A B C DOBRYLAS Pisa 0.0 TYSZKI-W ĄDOŁOW O Skroda 0.0 ZARUZIE Ruż 0.3 HAJNÓW KA Leśna 0.0 TONKIELE Bug 0.0 BRAŃSK Nurzec 0.0 -
Transformation of the Flow Regime of a Large Allochthonous River in Central Europe—An Example of the Vistula River in Poland
water Article Transformation of the Flow Regime of a Large Allochthonous River in Central Europe—An Example of the Vistula River in Poland Dariusz Wrzesi ´nski and Leszek Sobkowiak * Department of Hydrology and Water Management, Institute of Physical Geography and Environmental Planning, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Krygowskiego str. 10, 61-712 Pozna´n,Poland; [email protected] * Correspondence: [email protected] Received: 31 December 2019; Accepted: 10 February 2020; Published: 12 February 2020 Abstract: Identification of river flow regime and its possible changes caused by natural factors or human activity is one of major issues in modern hydrology. In such studies different approaches and different indicators can be used. The aim of this study is to determine changes in flow regime of the largest river in Poland—the Vistula, using new, more objectified coefficients and indices, based on data recorded in 22 gauges on the Vistula mainstream and 38 gauges on its tributaries in the multi-year period 1971–2010. The paper consists of three main parts: in the first part, in order to recognize changes in the flow regime characteristics along the Vistula, data from gauges located on the river mainstream were analyzed with the help of the theory of entropy. In the second part gauging stations on the Vistula mainstream and its tributaries were grouped; values of the newly introduced pentadic Pardé’s coefficient of flow (discharge) (PPC) were taken as the grouping criterion. In the third part of the study a novel method of determining river regime characteristics was applied: through the recognition of the temporal structure of hydrological phenomena and their changes in the annual cycle sequences of hydrological periods (characteristic phases of the hydrological cycle) on the Vistula River mainstream and its tributaries were identified and their occurrence in the yearly cycle was discussed.