Instytut Meteorologii I Gospodarki Wodnej

Total Page:16

File Type:pdf, Size:1020Kb

Instytut Meteorologii I Gospodarki Wodnej INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY Biuro Prognoz Hydrologicznych w Krakowie Wydział Prognoz i Opracowań Hydrologicznych w Warszawie 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 Wydział Prognoz i Opracowań Hydrologicznych w Warszawie podaje KOMUNIKAT HYDROLOGICZNY z dnia 03.10.2019 godz. 12 UTC UTC - ang. Universal Time Coordinated - czas uniwersalny; w okresie letnim czas urzedowy w Polsce UTC+2h, a w okresie zimowym UTC+1h. Stan wody Stan wody Stan wody Stan wody Stan wody Stan Stan 6 UTC 9 UTC 12 UTC 15 UTC 18 UTC Stacja ostrze- alar- Rzeka gawczy mowy obser- obser- obser- obser- obser- wodowskazowa wator czujnik wator czujnik wator czujnik wator czujnik wator czujnik [cm] A B C D E F G H I J K L M N województwo śląskie W ĄSOSZ Pilica 250 300 167 168 168 województwo świętokrzyskie Czarna JANUSZEW ICE (W łoszczowska) 320 400 274 273 274 274 województwo podlaskie SIEMIANÓW KA Narew 148 148 148 BONDARY Narew 177 177 177 NAREW Narew 170 200 46 46 46 46 PLOSKI Narew 330 370 214 213 213 SURAŻ Narew 320 340 125 125 124 124 BABINO Narew 540 570 324 324 324 STRĘKOW A GÓRA Narew 420 440 156 156 156 156 W IZNA Narew 440 470 176 176 177 177 PIĄTNICA-ŁOMŻA Narew 410 460 98 98 98 99 NOW OGRÓD Narew 360 400 48 48 49 49 BIAŁOW IEŻA - PARK Narewka 180 200 69 69 69 NAREW KA Narewka 260 290 98 98 98 CHRABOŁY Orlanka 310 350 113 114 114 NOW OSIÓŁKI Supraśl 200 240 151 151 151 SUPRAŚL Supraśl 220 260 153 153 153 FASTY Supraśl 220 250 152 152 145 146 SOKOŁDA Sokołda 250 300 192 191 192 192 SOCHONIE Czarna 100 120 100 100 100 ZAW ADY Biała 239 237 235 KULESZE CHOBOTKI Nereśl 330 360 259 259 260 ZAW ADY Ślina 380 400 270 271 271 SZTABIN Biebrza 170 190 22 23 DĘBOW O Biebrza 270 300 115 102 90 OSOW IEC Biebrza 400 430 224 225 226 227 BURZYN Biebrza 380 400 144 145 146 146 HARASIMOW ICZE Sidra 590 620 498 498 497 BIAŁOBRZEGI Netta 200 240 136 136 136 KARPOW ICZE Brzozówka 290 330 165 165 166 RAJGRÓD Jez. 225 240 120 120 120 Rajgrodzkie RAJGRÓD Jegrznia 140 160 84 84 84 Ełk (Kanał PRZECHODY Rudzki) 330 360 208 208 208 Ełk (Kanał OSOW IEC Rudzki) 460 490 362 362 362 A B C D E F G H I J K L M N CZACHY W issa 320 360 243 244 244 PTAKI Pisa 210 240 60 59 59 59 DOBRYLAS Pisa 250 290 80 80 80 80 ZARUZIE Ruż 220 260 111 111 111 FRANKOPOL Bug 250 350 58 58 58 BRAŃSK Nurzec 250 300 99 98 98 województwo łódzkie PRZEDBÓRZ Pilica 360 400 208 208 207 206 SULEJÓW (KOPALNIA) Pilica 230 260 158 161 161 SPAŁA Pilica 220 280 27 27 27 Czarna DĄBROW A (Maleniecka) 370 400 248 250 254 KŁUDZICE Luciąża 350 380 254 254 255 KW IATKÓW EK Bzura 200 250 107 105 104 ŁOW ICZ Bzura 350 400 180 BIELAW Y Mroga 310 360 292 297 300 KĘSZYCE Rawka 350 400 258 262 260 województwo mazowieckie GUSIN W isła 370 420 24 23 24 W ARSZAW A- NADW ILANÓW KA W isła 750 800 113 112 112 W ARSZAW A- BULW ARY W isła 600 650 39 38 38 38 MODLIN W isła 650 700 244 244 244 W YCHÓDŹC W isła 256 256 256 W YSZOGRÓD W isła 500 550 254 253 253 254 KĘPA POLSKA W isła 450 500 168 169 170 172 KAZANÓW Iłżanka 195 270 164 165 166 166 ROGOŻEK Radomka 330 380 137 136 136 NOW E MIASTO Pilica 160 200 45 44 46 BIAŁOBRZEGI Pilica 200 250 138 138 138 138 ODRZYW ÓŁ Drzewiczka 220 260 130 131 131 W ÓLKA Świder 210 300 68 69 69 MLĄDZKA PIASECZNO 2 Jeziorka 300 350 182 181 181 OSTROŁĘKA Narew 360 380 62 62 63 63 ZAMBSKI Narew 420 480 138 137 138 138 KOŚCIELNE ORZECHOW O Narew 320 400 55 50 53 SZKW A Szkwa 460 500 370 370 370 W ALERY Rozoga 300 340 161 160 160 BIAŁOBRZEG BLIŻSZY Omulew 180 220 79 77 77 77 CZARNOW O Orz 270 320 122 122 122 MAKÓW Orzyc 370 390 146 146 146 146 MAZOW IECKI ZABUŻE Bug 216 215 215 MAŁKINIA Bug 350 430 110 110 111 W YSZKÓW Bug 400 450 166 167 167 168 POPOW O Bug 213 212 212 ZALIW IE- Liwiec 220 270 157 156 157 PIEGAW KI ŁOCHÓW Liwiec 300 350 117 117 117 TRZCINIEC W kra 280 330 179 179 179 BORKOW O W kra 280 300 131 131 131 129 SZREŃSK Mławka 130 180 64 64 64 ŻUKÓW Bzura 300 350 108 108 108 KRUBICE Utrata 220 280 188 186 186 województwo kujawsko-pomorskie W ŁOCŁAW EK W isła 600 650 107 106 106 A B C D E F G H I J K L M N TORUŃ W isła 530 650 127 127 127 126 FORDON W isła 530 650 127 126 126 126 CHEŁMNO W isła 510 630 167 167 168 169 GRUDZIĄDZ W isła 540 650 160 162 163 164 BRODNICA Drwęca 230 260 108 109 109 109 ELGISZEW O Drwęca 200 230 79 79 80 ROGÓŹNO 2 Osa 230 260 37 39 38 38 TUCHOLA Brda 140 190 114 113 113 SMUKAŁA Brda 230 260 184 182 183 KRĄPLEW ICE W da 220 280 88 154 155 województwo warmińsko-mazurskie EŁK Ełk 200 230 102 102 102 EŁK Jez. Ełckie 220 235 128 128 128 PROSTKI Ełk 190 220 78 78 77 Pisa (Kanał GIŻYCKO Giżycki) 130 150 105 105 105 MIKOŁAJKI Jez. Mikołajskie 110 120 52 MALDANIN Jez. Roś 140 160 42 42 43 PISZ Pisa 270 290 124 125 125 125 OSTRÓDA Jez. Drwęckie 500 510 466 463 463 RODZONE Drwęca 280 320 163 162 165 NOW E MIASTO LUBAW SKIE Drwęca 330 340 167 166 166 166 IŁAW A Jez. Jeziorak 930 940 900 DZIARNY Iławka 130 140 24 LIDZBARK W el 110 120 56 55 55 KULIGI W el 150 180 83 82 81 80 PRZYSTAŃ Jez. Mamry 160 180 125 125 125 W ĘGORZEW O W ęgorapa 250 280 201 200 199 PRYNOW O W ęgorapa 250 280 188 188 187 MIEDUNISZKI W ęgorapa 400 450 180 179 173 168 JURKISZKI Gołdapa (Jarka) 180 210 49 48 48 GOŁDAP 2 Gołdapa 180 210 85 84 84 BANIE MAZURSKIE Gołdapa 260 290 132 133 132 136 OLSZTYN- Łyna 140 160 104 104 104 KORTOW O SMOLAJNY Łyna 280 300 138 139 138 SĘPOPOL Łyna 420 450 139 140 133 137 SZYPRY Jez. W adąg 212 211 211 PROSNA Guber 300 330 168 170 174 województwo pomorskie TCZEW W isła 700 820 260 259 259 CIECHOLEW Y Brda 210 240 224 CZARNA W ODA W da 130 150 72 69 73 72 BOŻEPOLE SZLACHECKIE W ierzyca 150 180 91 90 90 BRODY W ierzyca 320 350 200 202 207 POMORSKIE Dyżurny hydrolog: Michał Ceran Opracowanie niniejsze jako przedmiot prawa autorskiego podlega ochronie prawnej, zgodnie z przepisami ustawy z dnia 4 lutego 1994 r o prawie autorskim i prawach pokrewnych (Dz. U. z 2017 r. poz. 880, 1089, z 2018 r. poz. 650). Wszelkie dalsze udostępnianie, rozpowszechnianie (przedruk, kopiowanie) jest dozwolone wyłącznie w formie dosłownej, z bezwzględnym wskazaniem źródła informacji, tj. IMGW-PIB. Przytoczone wartości pochodzą z operacyjnej bazy danych i mogą ulec zmianie po weryfikacji. Odbiorcy przysługuje prawo do reklamacji. Składanie reklamacji: [email protected].
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • Generate PDF of This Page
    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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]