Total Mercury in Floodplain Soils of the Warta River, Poland
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Instytut Meteorologii I Gospodarki Wodnej Projekt PBZ-KBN-061/T07/2001
PROJEKT PBZ-KBN-061/T07/2001 ZADANIE 13. OPRACOWANIE PROGRAMU NARODOWEGO PLANU ZINTEGROWANEGO ROZWOJU GOSPODARKI WODNEJ W POLSCE STUDIUM DLA ZLEWNI PROSNY Instytut Meteorologii i Gospodarki Wodnej Projekt PBZ-KBN-061/T07/2001 METODYCZNE PODSTAWY NARODOWEGO PLANU ZINTEGROWANEGO ROZWOJU GOSPODARKI WODNEJ W POLSCE ZADANIE 13. OPRACOWANIE PROGRAMU NARODOWEGO PLANU ZINTEGROWANEGO ROZWOJU GOSPODARKI WODNEJ W POLSCE STUDIUM DLA ZLEWNI PROSNYT Kierownik projektu: Elżbieta Nachlik Zespół autorski : Tomasz Walczykiewicz – kierownik zadania Katarzyna Czoch Urszula Opial – Gałuszka Celina Rataj Tadeusz Stochliński Barbara Zientarska Kierownik Zakładu Dyrektor Oddziału Tomasz Walczykiewicz Jan Sadoń Kraków, grudzień 2004 IMGW ODDZIAŁ W KRAKOWIE - STRONA - 1 - PROJEKT PBZ-KBN-061/T07/2001 ZADANIE 13. OPRACOWANIE PROGRAMU NARODOWEGO PLANU ZINTEGROWANEGO ROZWOJU GOSPODARKI WODNEJ W POLSCE STUDIUM DLA ZLEWNI PROSNY Spis Treści 1 DOKUMENTY WYJŚCIOWE ................................................................................................................................ 3 2 OGÓLNA CHARAKTERYSTYKA ZLEWNI ...................................................................................................... 5 3 DELIMITACJA WÓD POWIERZCHNIOWYCH I PODZIEMNYCH UMOŻLIWIAJĄCA PROWADZENIE OCEN I ANALIZ W ZLEWNI PROSNY ................................................................................ 10 3.1 Delimitacja wód powierzchniowych .................................................................................................................. 10 3.2 -
Grubość Pokrywy Śnieżnej I Zapas Wody W Śniegu Na Stacjach 21.11.2020 Meteorologicznych IMGW-PIB
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 fax.: (22) 83-45-097 e-mail: [email protected] www..imgw.pl www.meteo.imgw.pl www.stopsuszy.imgw.pll Grubość pokrywy śnieżnej i zapas wody w śniegu na stacjach 21.11.2020 meteorologicznych IMGW-PIB Grubość Zapas Norma Grubość świeżo Gatunek Obciążenie Lp. Nazwa stacji Rzeka Zlewnia Województwo Wysokość wody obciążenia pokrywy spadłego śniegu śniegiem w śniegu śniegiem śniegu m n.p.m. cm cm kod mm kN/m 2 kN/m 2 A B C D E F G H I J K L 1. BOGATYNIA Miedzianka (17416) Nysa Łużycka (174) dolnośląskie 295 0,665 2. BOLESŁAWÓW Morawka (12162) Nysa Kłodzka (12) dolnośląskie 600 2,800 3. BUKÓWKA Bóbr (16) Bóbr (16) dolnośląskie 510 2,170 4. GRYFÓW ŚLĄSKI Kwisa (166) Kwisa (166) dolnośląskie 325 0,875 5. JAKUSZYCE Kamienna (162) Bóbr (16) dolnośląskie 860 1,0 1 1 4,620 6. JELCZ-LASKOWICE Widawa (136) Widawa (136) dolnośląskie 135 0,700 7. JELENIA GÓRA Bóbr (16) Bóbr (16) dolnośląskie 342 1,0 0 1 0,994 8. KAMIENICA Kamienica (121624) Nysa Kłodzka (12) dolnośląskie 680 3,360 9. KAMIENNA GÓRA Bóbr (16) Bóbr (16) dolnośląskie 360 1,120 10. KARPACZ Skałka (161844) Bóbr (16) dolnośląskie 575 1,0 0 2 2,625 11. KŁODZKO Nysa Kłodzka (12) Nysa Kłodzka (12) dolnośląskie 356 1,092 12. LĄDEK-ZDRÓJ Biała Lądecka (1216) Nysa Kłodzka (12) dolnośląskie 460 1,820 13. LEGNICA Kaczawa (138) Kaczawa (138) dolnośląskie 122 0,700 14. -
EFAS Upgrade for the Extended Model Domain
EFAS upgrade for the extended model domain Technical documentation 2019 This publication is a Technical report by the Joint Research Centre (JRC), the European Commission’s science and knowledge service. It aims to provide evidence-based scientific support to the European policymaking process. The scientific output expressed does not imply a policy position of the European Commission. Neither the European Commission nor any person acting on behalf of the Commission is responsible for the use that might be made of this publication. JRC Science Hub https://ec.europa.eu/jrc JRC Ispra: European Commission, 2019 © European Union, 2019 Reuse is authorised provided the source is acknowledged. The reuse policy of European Commission documents is regulated by Decision 2011/833/EU (OJ L 330, 14.12.2011, p. 39). For any use or reproduction of photos or other material that is not under the EU copyright, permission must be sought directly from the copyright holders. How to cite this report: L. Arnal, S.-S. Asp, C. Baugh, A. de Roo, J. Disperati, F. Dottori, R. Garcia, M. Garcia- Padilla, E. Gelati, G. Gomes, M. Kalas, B. Krzeminski, M. Latini, V. Lorini, C. Mazzetti, M. Mikulickova, D. Muraro, C. Prudhomme, A. Rauthe-Schöch, K. Rehfeldt, P. Salamon, C. Schweim, J.O. Skoien, P. Smith, E. Sprokkereef, V. Thiemig, F. Wetterhall, M. Ziese, EFAS upgrade for the extended model domain – technical documentation, EUR 29323 EN, Publications Office of the European Union, Luxembourg, 2019, ISBN 978-92- 79-92881-9, doi: 10.2760/806324, JRC111610. All images © European Union 2019 Contents Acknowledgements ................................................................................................ 2 1 Introduction ..................................................................................................... -
Zmiany I Wieloletnia Zmienność Sezonowości Przepływu Wybranych Rzek Polski
PrACe GeOGrAfiCzne, zeszyt 144 instytut Geografii i Gospodarki Przestrzennej UJ Kraków 2016, 9 – 33 doi: 10.4467/20833113PG.16.001.5126 ZMIANY I WIELOLETNIA ZMIENNOŚĆ SEZONOWOŚCI PRZEPŁYWU WYBRANYCH RZEK POLSKI Paweł Jokiel, Beata Stanisławczyk Long-term changes and variability in the seasonality of river discharge for selected Polish rivers Abstract: The aim of the paper is to carry out a multi-faceted analysis of the changes and the multiannual variability of the seasonal structure of river runoff in Poland. The research study is focused on river catchments situated in various regions of Poland. The seasonality index (Markham 1970) is employed to provide an assessment of river discharge seasonality for a multi-year period using data obtained from 40 water gauges. The collected data include the daily discharge of the analyzed rivers in the period 1951–2010. Average seasonality indices of the discharge of the investigated rivers were computed. On the basis of average seasonality indices (8%–37%) and their variability levels in the studied multiannual period, it is possible to compute small differences in the magnitude and dynamics of the changes in the seasonal structure of river runoff and precipitation in the studied multiannual period (Kożuchowski, Wibig 1988) and the total outflow from river catchments in the central Poland (Bartnik, Jokiel 2001), respectively. At the same time, the seasonal structure of river runoff, it is conjectured, continually constitutes a stable part of the river regime in Poland over the years as well as across geographic space. However, statistically significant trends (α=0.05) for the obtained seasonality indices of river discharge in the multiannual period was identified only for seven rivers. -
Mazovian Nature and Architecture Mazovia Live It and Feel It
FOR THE TRAVELLERS See the beauty of Mazovian nature and architecture Mazovia Live it and feel it The Papal Route and Routes of St. James in Mazovia Mazovia Live it and feel it etting out to a journey, you should Sthink of a good guide, also a good spiritual guide to be sure that you have taken the right way. You’ll need it to be able to follow the Mazovian Routes of S. James, learn a great deal of history and be at places gloried by the personality of St. John Paul II. Not only will this guide provide you with tourist information, but also will give you a spiritual guidance while you are travelling along the Papal Routes in Mazovia. The guide will take you thro- ugh various places related to John Paul II, old wooden churches, huge and impres- sive temples for hundreds of faithful. You will read about seemingly normal pu- blic space objects that become special when you take a closer look. Also those interested in architecture will read de- tailed description of historical buildings and churches, and also look into details of objects of worship, nature’s wonders and works of art both religious and lay. History lovers will read about the lives of saints and other historical persons and know legends and interesting anecdo- tes. However, it is the words of John Paul II that are in the centre of attention in this guide. We invite you to Mazovia to take a spiritual trip along its Routes of St. James and feel the power of the sacrum. -
River Valleys of the M Azovian Interglacial in Eastern Central Europe
acta geologlca pOlOnica Vol~ 32, No. 3-4 Warszawa 1982 LESZEK LINDNER, ZBIGNIEW LAMPARSKI & STANISl..AW D.t\BROWSKI River valleys of the M azovian Interglacial in eastern Central Europe ABSTRACT: A reconstructed pattern of main river valleys .of the Mazovian (Mindel II/Riss I; Holstein in Germany) Interglacial for eastern Central Europe is considerably different from those presented previously. This pattern comprises the pre-Vistula and pre-Neman drainage basins, both entering northwards to the Holstein Sea bay and including the Sambia region, as well as of the pre-Wartal .Odra and pre-Notec drainage basins, running westwards into the Holstein Sea bay that reached the present~day Lower Elbe area. The development of this valley system depended upon the extent of glacidynamic structures and deglaciation after the Sanian (= Mindel 11) Glaciation as well as upon the results of neotectonic movements. INTRODUCTION Floristic localities of the Mazovian Interglacial, limited by tills of the Sanian (= Mindel Il, Elstera Il, Oka Il) and the Odranian (= Riss I, Saale 1-2, Dnieper) glaciations or their residua, and corresponding alluvial series represent several successive interglacial warmings in eastern Central Europe (R6zycki 1961, 1964, 1967; Riihle 1973). The works undertaken during the last ten years proved that some loclllities represent the real interglacial whereas some of them are younger and represent the anaglacial warmings of the Odranian Glaciation (R6zycki 1972, 1978, 1980; Lindner 1981). Janczyk-Kopikowa (1980) suggested recently that -
Late Glacial and Early Holocene Development of an Oxbow Lake in Central Europe (Poland) Based on Plant Macrofossil and Geochemical Data
This is a repository copy of Late Glacial and early Holocene development of an oxbow lake in Central Europe (Poland) based on plant macrofossil and geochemical data. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/148899/ Version: Accepted Version Article: Gałka, M, Lewandowska, A, Niedzielski, P et al. (3 more authors) (2020) Late Glacial and early Holocene development of an oxbow lake in Central Europe (Poland) based on plant macrofossil and geochemical data. The Holocene, 30 (1). pp. 178-189. ISSN 0959-6836 https://doi.org/10.1177/0959683619875803 © The Author(s) 2019. This is an author produced version of a paper published in The Holocene. Reprinted by permission of SAGE Publications. Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ HOLOCENE Late Glacial and Early Holocene development of an oxbow lake in Central Europe (Poland) based on plant -
Załącznik Nr 1
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 ZAŁĄCZNIK NR 1 PROJEKT ISOK – RAPORT Z ZAKOŃCZENIA REALIZACJI ZADANIA 1.3.2 - PRZYGOTOWANIE DANYCH HYDROLOGICZNYCH W ZAKRESIE NIEZBĘDNYM DO MODELOWANIA HYDRAULICZNEGO Projekt ISOK – RAPORT Z ZAKOŃ CZEŃIA REALIZACJI ZADAŃIA 1.3.2 Projekt: Informatyczny system osłony kraju przed nadzwyczajnymi zagrożeniami Nr Projektu: POIG.07.01.00-00-025/09 Dokument: Raport Końcowy Metryka Dane Opis Tytuł dokumentu Raport końcowy Autor dokumentu (firma / IMGW PIB instytucja) Nazwa Projektu Informatyczny system osłony kraju przed nadzwyczajnymi zagrożeniami Nr Projektu POIG.07.01.00-00-025/09 Rodzaj Dokumentu Raport końcowy Poufność Nazwa i kod Produktu 1.3.2 Przygotowanie danych hydrologicznych w zakresie niezbędnym do Nazwa i kod Zadania modelowania hydraulicznego Historia zmian Wersja Autor Data Zmiana 0.01 TT 20131220 Recenzje dokumentu Recenzent Data 1 2 3 4 Odniesienia do innych dokumentów Data opracowania Nazwa dokumentu dokumentu Studium Wykonalności dla projektu w ramach VII osi POIG – „Informatyczny system osłony Marzec 2011 kraju przez nadzwyczajnymi zagrożeniami” Umowa o dofinansowanie nr POIG.07.01.00-00-025/09-00 zawarta pomiędzy WWPE a Lipiec 2010 IMGW 2 ISOK PR DIP - PZD Z4 -Raport_1 3 2_30052016 Projekt: Informatyczny system osłony kraju przed nadzwyczajnymi zagrożeniami Nr Projektu: POIG.07.01.00-00-025/09 Dokument: Raport Końcowy Spis treści 1 WPROWADZENIE 4 2 INFORMACJE OGÓLNE 5 3 CEL I ZAKRES ZADANIA 8 4 SYNTETYCZNY OPIS REALIZOWANYCH ZADAŃ 9 4.1 Charakterystyki hydrologiczne posterunków wodowskazowych 9 4.2 Stałe lub zmienne w czasie wartości przepływu Q [m3/s] 10 4.3 Rozkłady przepływów Q zgodnie z przyjętymi scenariuszami powodziowymi 11 4.4 Stałe lub zmienne w czasie wartości rzędnych zwierciadła wody H [cm] 13 4.5 Krzywe przepływu Q/H dla posterunków wodowskazowych udostępniane będą wraz z przekazanymi modeli hydraulicznymi. -
How History Matters for Student Performance: Lessons from the Partitions of Poland
Paweł Bukowski How history matters for student performance: lessons from the Partitions of Poland Article (Published version) (Refereed) Original citation: Bukowski, Paweł (2018) How history matters for student performance: lessons from the Partitions of Poland. Journal of Comparative Economics. pp. 1-40. ISSN 0147-5967 DOI: https://doi.org/10.1016/j.jce.2018.10.007 © 2018 The Author. Published by Elsevier Inc. on behalf of Association for Comparative Economic Studies This version available at: http://eprints.lse.ac.uk/90643 Available in LSE Research Online: November 2018 LSE has developed LSE Research Online so that users may access research output of the School. Copyright © and Moral Rights for the papers on this site are retained by the individual authors and/or other copyright owners. Users may download and/or print one copy of any article(s) in LSE Research Online to facilitate their private study or for non-commercial research. You may not engage in further distribution of the material or use it for any profit-making activities or any commercial gain. You may freely distribute the URL (http://eprints.lse.ac.uk) of the LSE Research Online website. Journal of Comparative Economics xxx (xxxx) xxx–xxx Contents lists available at ScienceDirect Journal of Comparative Economics journal homepage: www.elsevier.com/locate/jce How history matters for student performance. lessons from the ☆ Partitions of Poland Paweł Bukowski Centre for Economic Performance, The London School of Economics and Political Science, Houghton Street, London, WC2A 2AE, the United Kingdom ARTICLE INFO ABSTRACT JEL classification: This paper examines the effect on current student performance of the 19th century Partitions of N30 Poland among Austria, Prussia and Russia. -
The Effect of Geography and Institutions on Economic
Journal of Interdisciplinary History, XLVIII:4 (Spring, 2018), 523–538. Joanna Dzionek-Kozlowska, Kamil Kowalski, and Rafal Matera The Effect of Geography and Institutions on Economic Development: The Case of Lodz One of the longest, most heated, and still unsettled debates in economics is about pinpointing the factors responsible for economic develop- ment. What are the main factors that cause some areas to prosper whereas others do not? Two distinct approaches have emerged from this debate—the geography hypothesis that holds natural resources accountable for economic performance and the institu- tions hypothesis that credits socio-economic conditions as the major determinants of economic progress. Using Lodz, one of the largest cities in Poland as a case study, this research note demonstrates that progress is a function of a combination of geographical and institutional factors. The history of Lodz provides an excellent opportunity to identify the extent to which these two types of factors serve as incentives for, or hin- drances to, economic development. We focus on the period from the 1820s to World War I, during which the foundations of the city’s later economic performance were laid.1 What explains the city’s economic stagnation for the four first centuries of its existence and its subsequent rapid growth, the pace of which, expressed in terms of population growth, was the fastest Joanna Dzionek-Kozlowska is Assistant Professor, Dept. of the History of Economic Thought and Economic History, University of Lodz. She is the author of “Economics in Times of Crisis: In Search of a New Paradigm in Economic Sciences,” Journal of Philosophical Economics: Reflections on Economic and Social Issues, XCI (2015), 52–72; co-author, with Rafal Matera, of Ethics in Economic Thought: Selected Issues and Various Perspectives (Lodz, 2015). -
Załącznik Nr 7
RAPORT Z WYKONANIA MAP ZAGROŻENIA POWODZIOWEGO I MAP RYZYKA POWODZIOWEGO ZAŁĄCZNIK NR 7 WYKAZ OBSZARÓW BEZPOŚREDNIEGO ZAGROŻENIA POWODZIĄ WYZNACZONYCH W STUDIACH OCHRONY PRZECIWPOWODZIOWEJ DYREKTORÓW RZGW, OBOWIĄZUJĄCYCH JAKO OBSZARY SZCZEGÓLNEGO ZAGROŻENIA POWODZIĄ, PO OFICJALNYM PRZEKAZANIU MAP ZAGROŻENIA POWODZIOWEGO I MAP RYZYKA POWODZIOWEGO OPRACOWANYCH W I CYKLU PLANISTYCZNYM Wersja 2.00 (2017-04-19) Tabela 1. Wykaz obszarów bezpośredniego zagrożenia powodzią (OBZP) wyznaczonych w studiach ochrony przeciwpowodziowej Dyrektora RZGW we Wrocławiu, obowiązujących jako obszary szczególnego zagrożenia powodzią (OSZP) po oficjalnym przekazaniu map zagrożenia powodziowego i map ryzyka powodziowego opracowanych w I cyklu planistycznym. Odcinek dla którego został Nazwa Nr wyznaczony OBZP (OSZP) rzeki [km] Obszar dorzecza Odry Region wodny Środkowej Odry 1 Kamienica 0 - 15 2 Kamienny Potok 0 - 10 Tabela 2. Wykaz obszarów bezpośredniego zagrożenia powodzią (OBZP) wyznaczonych w studiach ochrony przeciwpowodziowej Dyrektora RZGW w Szczecinie, obowiązujących jako obszary szczególnego zagrożenia powodzią (OSZP) po oficjalnym przekazaniu map zagrożenia powodziowego i map ryzyka powodziowego opracowanych w I cyklu planistycznym. Nazwa Odcinek dla którego został Nr rzeki / obszaru / zbiornika wodnego wyznaczony OBZP (OSZP) (dodatkowe informacje) [km] Obszar dorzecza Odry Region wodny Dolnej Odry i Przymorza Zachodniego 1 Czerwona 0 - 24 2 Dzierżęcinka 0 - 18 3 Ilanka (dopływ Odry) 0 - 59 4 Ina 101 - 118 5 Kanał Luboński 0 - 8 6 Konotop 0 - 18 7 Krąpiel 0 - 41 8 Kurzyca 0 - 22 9 Mała Ina 0 - 56 10 Myśla 0 - 80 11 Pliszka 0 - 70 2 Nazwa Odcinek dla którego został Nr rzeki / obszaru / zbiornika wodnego wyznaczony OBZP (OSZP) (dodatkowe informacje) [km] 12 Płonia 8 - 73 13 Rurzyca 0 - 46 14 Słubia 0 - 32 15 Struga Malechowska 0 - 5 16 Struga Popowska (Młyńska Struga) 0 - 12 17 Strzeżenica 0 - 11 18 Tymienica 0 - 14 19 Tywa 0 - 52 20 Unieść 9 - 12 21 Jezioro Jamno całe Przymorze od Malechowskiej Strugi 22 całe do jeziora Bukowo Tabela 3. -
Spatial Differentiation of the Maximum River Runoff Synchronicity in The
water Article Spatial Differentiation of the Maximum River Runoff Synchronicity in the Warta River Catchment, Poland Adam Perz * , Leszek Sobkowiak and Dariusz Wrzesi ´nski Institute of Physical Geography and Environmental Planning, Adam Mickiewicz University, Krygowskiego 10, 61-680 Pozna´n,Poland; [email protected] (L.S.); [email protected] (D.W.) * Correspondence: [email protected] Received: 8 May 2020; Accepted: 19 June 2020; Published: 23 June 2020 Abstract: Based on daily flows recorded in the period 1971–2010, the synchronous occurrence of the annual (AMAXq), winter (WMAXq), and summer (SMAXq) maximum specific runoffs in 39 sub-catchments of the Warta River catchment (WRC) in Poland was analyzed. First, trends in the flows were detected using the non-parametric Mann–Kendall (M-K) test. Then, the degree of the synchronous and asynchronous occurrences of the maximum specific runoffs (MAXq) in respective sub-catchments in relation to the Gorzów Wielkopolski gauge closing the WRC was calculated. Finally, the reasons for the detected spatial and temporal differences were discussed. The study revealed a noticeable variability of the analyzed parameters. The highest synchronicity of AMAXq and WMAXq in relation to the closing Gorzów Wielkopolski gauge was revealed in the man-made Ko´scia´nskiand Mosi´nskicanals and in the sub-catchments of the Note´c,Wełna, and lower Prosna rivers. While compared to AMAXq and WMAXq, the summer maxima showed relatively lower degrees of synchronicity, an increase in the synchronous occurrence of SMAXq in the southern part of WRC, and a decrease in its central part were identified. It was concluded that the stronger synchronicity of WMAXq resulted from the nival regime of the investigated rivers.