11› From: Schweiz. Z. Hydrol. 39: 12-45, 1977 1978

Total Page:16

File Type:pdf, Size:1020Kb

11› From: Schweiz. Z. Hydrol. 39: 12-45, 1977 1978 FISURIES AND MARINE SERVICE Translation Series No. 4374 Biology and management of the European lake char (Salvelinus alpinus L.) in Lake Zug (Switzerland) by Ch. Ruhle Original title: Biologie und Bewirtschaftung des Seesaiblings 11› (Salvelinus alpinus L.) im Zugersee From: Schweiz. Z. Hydrol. 39: 12-45, 1977 Translated by the Translation Bureau (VNN) Multilingual Services Division Department of the Secretary of State of Canada Department of the Environment Fisheries and Marine Service Biological Station St. John's, Mid. 1978 54 pages typescript DEPARTMENT OF THE SECRETARY OF STATE SECRÉTARIAT D'ÉTAT TRANSLATION BUREAU BUREAU DES TRADUCTIONS MULTILINGUAL SERVICES DIVISION DES SERVICES CANADA DIVISION MULTILINGUES L/ 7/ TRANSLATED FROM - TRADUCTION DE INTO - EN German English AUTHOR - AUTEUR Ch. Ruhle TITLE IN ENGLISH - TITRE ANGLAIS Biology and management of the European lake char (galvelinus capinus L.) in Lake Zug (Switzerland) TITLE IN FOREIGN LANGUAGE (TRANSLITERATE FOREIGN CHARACTERS) TITRE EN LANGUE ÉTRANGÉRE (TRANSCRIRE EN CARACTÈRES ROMAINS) Biologie und Bewirtschaftung des Seesaiblings (Salvelinus epinus L.) im Zugersee REFERENCE IN FOREIGN LANGUAGE (NAME OF BOOK OR PUBLICATION) IN FULL. TRANSLITERATE,FOREIGN CHARACTERS. RÉFÉRENCE EN LANGUE ÉTRANGÉRE (NOM DU LIVRE OU PUBLICATION), ,AU COMPLET, TRANSCRIRE EN CARACTÈRES ROMAINS. Schweizerische Zeitschrift fuer Hydrologie "EFERENCE IN ENGLISH - RÉFÉRENCE EN ANGLAIS ("Swiss Journal for Hydrology") PUBLISHER - ÉDI TEUR PAGE NUMBERS IN ORIGINAL DATE OF PUBLICATION NUMÉROS DES PAGES DANS not shown DATE DE PUBLICATION L'ORIGINAL YEAR ISSUE NO. 12 - 45 VOLUME PLACE OF PUBLICATION ANNÉE NUMÉRO NUMBER OF TYPED PAGES LIEU DE PUBLICATION NOMBRE DE PAGES not shown DACTYLOGRAPHIÉES 1977 39 1 50 REQUESTING DElliViTMENT DFE TRANSLATION BUREAU NO. 1486937 MINISTÈRE-CLIENT NOTRE DOSSIER NO Fisheries Branch, BRANCH OR DIVISION TRANSLATOR (INITIALS) V.N.N. DIRECTION OU DIVISION Nfld. Biological Station TRADUCTEUR (INITIALES) PERSON REQUESTING Brian Dempson ug 25 BiB DEMANDÉ PAR *t UN ED 0 TR A Pi.".U„ A YOUR NUMBER ;o:.m.7, -;ii:ei on!y VOTRE DOSSIER NO For tn 1 TRADUCTION NON RPVISEE DATE OF REQUEST 17. 07. 1978 Information seulomont iiiiDATE DE LA DEMANDE SOS-200-10.6 (REV. 2/88) 7030-21-029-5333 • Secretary Secrétariat of State d'Ètat TRANSLATION BUREAU BUREAU DES TRADUCTIONS MULTILINGUAL SERVICES DIVISION DES SERVICES • DIVISION MULTILINGUES CITY cuevcs NO. DEPARTMENT DIVISION/BRANCH VILLE N° DU CLIENT MINISTiRE DIVISION/DIRECTION Fisheries Branch D. F. E. St. John's, Nfld Nfld. Biological Station BUREAU NO. LANGUAGE TRANSLATOR (INITIALS) N° DU BUREAU LANGUE TRADUCTEUR (INITIALES) AUG 25 mu 1486937 German V.N.N. "Biologie und Bewirtschaftung des Seesaiblings (&alvelinus capinus L.) im .Zugersee," Schweizerische Zeitschrift fuer Hydrologie 39(1), 12 - 35, 1977 Biology and management of the European lake char (Scavelinus capinus L.) l in Lake Zug (Switzerland) 2 by • Ch. Ruhle From the Institut fuer Gewaesserschutz und Wassertechnologie and der ETH (Eidgenoessische Technische Hochschule) [Institut for Prevention of Water Pollution and Hydrotechnology, Swiss Federal Institute of Technology], Zurich, Switzerland (Received on 7 March 1977) Summary - During the past 70 years, yields of European lake char fishery in Lake Zug have dropped from some 100,000 to 5000 fish per year. The present work was aimed ar developing methods for retarding and, perhaps, reversing this downward trend. In order to arrive at a proper base for developing new methods of fish stock management, the biology of the lake char was investigated. It was found that this fish is able to utilize the increased supply of food available in this eutrophie lake, but that the probability of natural reproduction is very low under the environmental conditions presently prevailing in Lake Zug. On the basis of the findings 1 Translator's note: This fish is also know as the European sea trout, a landlocked species found in southern Bavaria, Switzerland, and the Austrian Alps [Scavelinus capinus scavelinus]. 2 This work has been carried out at the Eidgenoessische Anstalt fuer Nasser- versorgung, Abwasserreinigung und Gewaesserschutz [Swiss Federal Institute of Water Supply, Wastewater Purification, and Prevention of Water Pollu- tion] (EAWAG), CH-8600 Duebendorf, Switzerland L5 ;\IEDI T .)- TR /M--i ;2:r ; • I For 'Tf;ADIC.1.1"..);`; NON SEC 5-25T (6/76) .Informailon • - 2 - obtained, the following measures have been recommended for improving lake char yields: (1) Intensified stocking (using yearlings, if possible); (2) use of gill nets with larger mesh size (35 mm); (3) discontinuation of fishing outside of the spawning season; and (4) setting up of new (ar- tificial) spawning grounds in shallow water zones with good oxygenation conditions. The measures for improving the stock of lake char will be expensive. Even with maximum yields, the cost-benefit balance of lake char management will be negative. It is concluded that only the histori- cal significance of European lake char fishery in Lake Zug can justify the great expenditure of public funds involved. 1. Introduction The Lake Zug lake char is a fish with tradition. It has been mentioned for the first time in a treaty written in the year 1281, which document settled an important transaction between the House of Habsburg and the Austrians (31), and, as in that document, the lake char has been mentioned • in various other documents from the late Middle Ages as tithe or tribute by subordinate courts. In the years 1759 and 1788, the council of Zug had to deal with this fish (30); these two council matters dealt with the mutual rights and duties of line-fishermen and net-fishermen, requiring official regulations for the common practuce of lake char fishing. The renewal of these regulations led in 1844 to the foundation of a fishermen's association in Walchwil, which was still in existence one hundred years later. These rather incomplete data in the role playes by the lake char in the local history of Zug explain why the people of that region--although they are now working chiefly in administration, commerce and industry--still possess a strongly developed "lake char awareness." That awareness not only finds expression in the fact that this fish has been raised to the rank of a historical curiosity; it is also expressed in the enactment of • official regulations dealing with the specific promotion of this "typical" fish. And, last but not least, that awareness is reflected in the desire, above all, of the local government of Zug, but also of many businesses, associations and individuals to be able to enjoy that historic delicacy at least once a year during the lake char season. Around the turn of the century and during the first decades of this century, the fishermen of Lake Zug were still able to catch relatively large numbers of lake char. In the fishery lake classification (27; 63), Lake Zug was listed as one of the characteristic lake char lakes. Yields of 90,000 to 100,000 lake chars per year, representing 85 per cent of the total catch (58), confirmed the validity of the assignment of Lake Zug to that lake type, which is distinguished by steno-oligothrophic properties, cor- responding depth as well as as continuously low temperatures and high oxygen • contents across the entire profile (27). As is indicated by the data plotted in Figure 1, the situation has greatly changed since then; in the average of the last ten years, only 8400 lake chars have been caught per year; that number of lake chars corresponds to about two to three per cent of the total catch taken from the Lake. For some time now, these catches are no longer large enough to satisfy the demands of the local market, which have been estimated to amount to approximately 20,000 lake char per year (46). That situation (and the high proce resulting from the discrepancy between supply and demand) as well as the conviction of the most important buyers--the restaurant and hotel owners--that the native fish, for reasons of quality, cannot simply be re- placed by lake char caught in other lakes have already led to a number of attempts to revitalize lake char fishery and management in Lake Zug. How- • ever, the goals aimed at have not been reached. For that reason, it became • - 3 - Figure 1 - Yields (numbers of fish caught) of lake char fishery, 1900 - 1974. Key: 1, Illegible; 2, Year. • necessary to study the biology of the lake char in Lake Zug within a wider 14 framework than had been done in the past, and to work out management mea- sures, insitution of which would prevent a further decrease of the yieldd and, perhaps, even make possible an increase. 2. Description of Lake Zug 2.1. Geography, geology, morphometry, and hydrology Lake Zug is a lake of the Alpine foothills (middle of its longitudinal axis: latitude 47 ° 04' north, longitude 8 ° 29' east), located between the Rigi Mountain (approximately 1800 m above sea level), the Ross Mountain (1600 m), the Zug Mountain (1000 m), and the foothills of the Root Mountain (850 m) (Figure 2). Two peninsulas project into the lake from the west; the bigger one of these peninsulas, the Kiemen (Chiemen), divides the lake into two, morpho- • • Figure 2 - Lake Zug. Table 1 - Morphometric and hydrological data of Lake Zug. Key: 1, Alti- tude above sea level; 2, Maximal length; 3, Maximal width; 4, Minimal width; 5, Maximal depth; 6, Mean depth; 7, Lake surface; 8, Lake volume; 9, Catchment area; 10, Inflow; 11, Inflow into the upper lake; 12, Inflow into the lower lake; 13, Residence time (theoretical); 14, Residence time; 15, Upper lake; 16, Lower lake. • "1 '. Nleereshübe 413 m 2 . Grüsste Lânge 13.4 km 3. Grüsste Breite 4,6 km 4 . Kleinste Breite 0.8 krn 5 • Gri.iste Tiefe- . 198 m .. Mittlere Tiefe ; . ' ; 80 .nt . 7.
Recommended publications
  • Pelagic Phytoplankton Community Change‐Points Across
    Freshwater Biology (2017) 62, 366–381 doi:10.1111/fwb.12873 Pelagic phytoplankton community change-points across nutrient gradients and in response to invasive mussels † † , ‡ KATYA E. KOVALENKO*, EUAN D. REAVIE*, J. DAVID ALLAN , MEIJUN CAI*, SIGRID D. P. SMITH AND LUCINDA B. JOHNSON* *Natural Resources Research Institute, University of Minnesota Duluth, Duluth, MN, U.S.A. † School of Natural Resources and Environment, University of Michigan, Ann Arbor, MI, U.S.A. SUMMARY 1. Phytoplankton communities can experience nonlinear responses to changing nutrient concentrations, but the nature of species shifts within phytoplankton is not well understood and few studies have explored responses of pelagic assemblages in large lakes. 2. Using pelagic phytoplankton data from the Great Lakes, we assessed phytoplankton assemblage change-point responses to nutrients and invasive Dreissena, characterising community responses in a multi-stressor environment and determine whether species responses to in situ nutrients can be approximated from nutrient loading. 3. We demonstrate assemblage shifts in phytoplankton communities along major stressor gradients, particularly prominent in spring assemblages, providing insight into community thresholds at the lower end of the phosphorus gradient and species-stressor responses in a multi-stressor environment. We show that responses to water nutrient concentrations could not be estimated from large-scale nutrient loading data likely due to lake-specific retention time and long-term accumulation of nutrients. 4. These findings highlight the potential for significant accumulation of nitrates in ultra-oligotrophic systems, nonlinear responses of phytoplankton at nutrient concentrations relevant to current water quality standards and system-specific (e.g. lake or ecozone) differences in phytoplankton responses likely due to differences in nutrient co-limitation and effects of dreissenids.
    [Show full text]
  • Goose Lake Nutrient Study (Marquette County, Michigan)
    MI/DEQ/WD-04/013 Goose Lake Nutrient Study (Marquette County, Michigan) Prepared by: White Water Associates, Inc. 429 River Lane Amasa, Ml 49903 (SUBCONTRACTOR) Great Lakes Environmental Center 739 Hastings Street Traverse City, Ml 49686 (PRIME CONTRACTOR) Prepared for: Michigan Department of Environmental Quality Water Division Lansing, Michigan 48933-7773 Lead Staff Person: Sarah Walsh View of Goose Lake looking northwest from the Goose Lake Outlet (Marquette County). Photo by D Premo Contract Number: 071B1001643, Project Number: 03-02 Date: December 31, 2003 Goose Lake Nutrient Study (Marquette County, Michigan) Prepared by: White 'Nater Associates, Inc. 429 River Lane Amasa, rv11 49903 (SUBCONTRACTOR) Great Lakes Environmental Center 739 Hastings Street Traverse City, Ml 49686 (PRIME CONTRACTOR) Contacts: Dean B. Premo, Ph.D., White Water Associates Phone: (906) 822-7889; Fax: (906) 822-7977 E-mail: [email protected] Dennis McCauley, Great Lakes Environmental Center Phone. (231) 941-2230; Fax: (231) 941-2240 E-mail: [email protected] Prepared for: Michigan Department of Environmental Quality Water Division Lansing, Michigan 48933-7773 Lead Staff Person: Sarah Walsh Contract Number: 07181001643 Project Number: 03-02 Date: December 31, 2003 Goose Lake Nutrient Study (Marquette County, Michigan) Fieldwork: Dean Premo, Senior Ecologist David Tiller, Field Biologist Report: Dean Premo, Ph.D., Senior Ecologist Kent Premo, M.S., Technical Support Scientist Bette Premo, Ph.D., Limnologist Cite as: Premo, Dean, Kent Premo, and Bette Premo. 2003. Goose Lake Nutrient Study (Marquette County, Michigan). White Water Associates, Inc. Contents of Appendix A - Exhibits Exhibit 1. Map of the Goose Lake Study Landscape and Four Sampling Stat(ons.
    [Show full text]
  • Schwyz-Zug–ZVV
    Schwyz-Zug–ZVV 116 Uhwiesen Schloss Laufen a. Rh. For journeys to neighbouring Dachsen Wildensbuch Benken ZH fare networks Neubrunn- Ulmenhof 162 Rheinau Rudolfingen Trüllikon Stammheim For travel to neighbouring fare networks, the Marthalen Guntalingen Oerlingen Truttikon Waltalingen following guidelines apply: Ossingen Oberstamm- Marthalen heim – Please purchase or validate your ticket prior 161 Rafz 115 Oberneunforn to boarding. Wil ZH – Travel between the point of departure and Kleinandelfingen destination is always comprised of multiple Hüntwangen 114 Andelfingen Gütighausen Wasterkingen Adlikon zones. Hüntwangen-Wil Rüdlingen 124 Thalheim – When you purchase a Z-Pass ticket, the Altikon 113 Flaach Volken Dorf Kaiserstuhl AG Buchberg 160 Thalheim-Altikon appropriate zones will be automatically cal- Ellikon Humlikon Henggart an der Thur Zweidlen Berg am culated. Eglisau Irchel Dägerlen Dinhard Rickenbach ZH – Zones that are not directly linked by public Buch am Teufen Aesch bei Weiach Irchel Neftenbach 163 h Glattfelden Hettlingen transportation cannot be directly combined. Seuzach Windlac 118 t Rickenbach-Attikon – The zones and period of validity can be found Freienstein Neftenbach Gundetswil Rorbas Reutlingen on the tickets. Stadel Bülach bei Niederglat Hochfelden 123 Dättlikon Wallrüti Embrach-Rorbas – Tickets valid according to calendar day (e.g. s Wiesendangen iederweningen ach Bachenbülach Oberwinterthur N B Neerach Pfungen day passes, travelcards) may be used up to Höri Elsau Embrach Wülflingen Grüze Hegi Elgg NiederweningenSchöfflisdorf- Dorf 5.00 a.m. on the following day. Oberweningen 112 Winterthur Räterschen Schottikon Winkel Lufingen – Within the zones covered by your ticket, you Steinmaur Töss Schleinikon Niederglatt Oberembrach Seen 164 may make as many journeys as you wish on g Dielsdorf 120* Hofstetten Schlatt all available means of transport.
    [Show full text]
  • Central Switzerland
    File16-central-swiss-loc-swi7.dwg Book Initial Mapping Date Road Switzerland 7 Peter 21/11/11 Scale All key roads labelled?Hierarchy Hydro ChapterCentral Switzerland Editor Cxns Date Title Spot colours removed?Hierarchy Symbols Author MC Cxns Date Nthpt Masking in Illustrator done? Sally O'Brien Book Off map Inset/enlargement correct?dest'ns BorderCountry LocatorKey A1None Author Cxns Date Notes Basefile08-geneva-loc-swi6.dwgFinal Ed Cxns Date KEY FORMAT SETTINGS New References09-geneva-loc-swi7.dwg Number of Rows (Lines) Editor Check Date MC Check Date Column Widths and Margins MC/CC Signoff Date ©Lonely Planet Publications Pty Ltd CentralPOP 718,400 / AREA 4484 SQ KM / LANGUAGESwitzerland GERMAN Includes ¨ Why Go? Lucerne . 192 To the Swiss, Central Switzerland – green, mountainous Lake Lucerne . 198 and soothingly beautiful – is the very essence of ‘Swissness’. Lake Uri . 202 It was here that the pact that kick-started a nation was signed in 1291; here that hero William Tell gave a rebel yell Brunnen . 203 against Habsburg rule. Geographically, politically, spiritual- Schwyz . 204 ly, this is the heartland. Nowhere does the flag fly higher. Einsiedeln . 205 You can see why locals swell with pride at Lake Lucerne: Engelberg . 206 enigmatic in the cold mist of morning, molten gold in the Zug . 209 dusky half-light. The dreamy city of Lucerne is small enough for old- Andermatt . 211 world charm yet big enough to harbour designer hotels and a world-class gallery full of Picassos. From here, cruise to resorts like Weggis and Brunnen, or hike Mt Pilatus and Mt Rigi. Northeast of Lucerne, Zug has Kirschtorte Best Places to Eat (cherry cake) as rich as its residents and medieval herit- age.
    [Show full text]
  • Effects of Eutrophication on Sedimentary Organic Carbon Cycling in Five Temperate Lakes
    Research Collection Journal Article Effects of eutrophication on sedimentary organic carbon cycling in five temperate lakes Author(s): Fiskal, Annika; Deng, Longhui; Michel, Anja; Eickenbusch, Philip; Han, Xingguo; Lagostina, Lorenzo; Zhu, Rong; Sander, Michael; Schroth, Martin Herbert; Bernasconi, Stefano M.; Dubois, Nathalie; Lever, Mark Publication Date: 2019-09-30 Permanent Link: https://doi.org/10.3929/ethz-b-000370204 Originally published in: Biogeosciences 16(19), http://doi.org/10.5194/bg-16-3725-2019 Rights / License: Creative Commons Attribution 4.0 International This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Biogeosciences, 16, 3725–3746, 2019 https://doi.org/10.5194/bg-16-3725-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Effects of eutrophication on sedimentary organic carbon cycling in five temperate lakes Annika Fiskal1, Longhui Deng1, Anja Michel1, Philip Eickenbusch1, Xingguo Han1, Lorenzo Lagostina1, Rong Zhu1, Michael Sander1, Martin H. Schroth1, Stefano M. Bernasconi3, Nathalie Dubois2,3, and Mark A. Lever1 1Institute of Biogeochemistry and Pollutant Dynamics (IBP), ETH Zurich, Universitätstrasse 16, 8092 Zurich, Switzerland 2Surface Waters Research – Management, Eawag, Swiss Federal Institute of Aquatic Science and Technology, Überlandstrasse 133, 8600 Dübendorf, Switzerland 3Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8092 Zurich, Switzerland Correspondence: Annika Fiskal (annika.fi[email protected]) and Mark A. Lever ([email protected]) Received: 25 March 2019 – Discussion started: 27 March 2019 Revised: 2 September 2019 – Accepted: 4 September 2019 – Published: 30 September 2019 Abstract. Even though human-induced eutrophication has rate.
    [Show full text]
  • Change of Phytoplankton Composition and Biodiversity in Lake Sempach Before and During Restoration
    Hydrobiologia 469: 33–48, 2002. S.A. Ostroumov, S.C. McCutcheon & C.E.W. Steinberg (eds), Ecological Processes and Ecosystems. 33 © 2002 Kluwer Academic Publishers. Printed in the Netherlands. Change of phytoplankton composition and biodiversity in Lake Sempach before and during restoration Hansrudolf Bürgi1 & Pius Stadelmann2 1Department of Limnology, ETH/EAWAG, CH-8600 Dübendorf, Switzerland E-mail: [email protected] 2Agency of Environment Protection of Canton Lucerne, CH-6002 Lucerne, Switzerland E-mail: [email protected] Key words: lake restoration, biodiversity, evenness, phytoplankton, long-term development Abstract Lake Sempach, located in the central part of Switzerland, has a surface area of 14 km2, a maximum depth of 87 m and a water residence time of 15 years. Restoration measures to correct historic eutrophication, including artificial mixing and oxygenation of the hypolimnion, were implemented in 1984. By means of the combination of external and internal load reductions, total phosphorus concentrations decreased in the period 1984–2000 from 160 to 42 mg P m−3. Starting from 1997, hypolimnion oxygenation with pure oxygen was replaced by aeration with fine air bubbles. The reaction of the plankton has been investigated as part of a long-term monitoring program. Taxa numbers, evenness and biodiversity of phytoplankton increased significantly during the last 15 years, concomitant with a marked decline of phosphorus concentration in the lake. Seasonal development of phytoplankton seems to be strongly influenced by the artificial mixing during winter and spring and by changes of the trophic state. Dominance of nitrogen fixing cyanobacteria (Aphanizomenon sp.), causing a severe fish kill in 1984, has been correlated with lower N/P-ratio in the epilimnion.
    [Show full text]
  • Discussion Paper on Brackish Urban Lake Water Quality in South East Queensland Catalano, C.L
    Discussion Paper on Brackish Urban Lake Water Quality in South East Queensland Catalano, C.L. 1, Dennis, R.B. 2, Howard, A.F.3 Cardno Lawson Treloar12, Cardno3 Abstract Cardno has been involved in the design and monitoring of a number of urban lakes and canal systems within south east Queensland for over 30 years. There are now many urban lakes in South East Queensland and the majority have been designed on the turnover or lake flushing concept, whereby it is considered that, if the lake is flushed within a nominal timeframe, then there is a reasonable expectation that the lake will be of good health. The designs have predominately been based on a turnover or residence time of around 20-30 days and some of the lakes reviewed are now almost 30 years old. This paper reviews this methodology against collected water quality data to provide comment on the effectiveness of this method of design for brackish urban lakes in South East Queensland and also to indicate where computational modelling should be used instead of, or to assist with, this methodology. 1. Introduction Lakeside developments are very popular in South-East Queensland. The lake is generally artificial, created out of a modification of an existing watercourse or lowland area for a source of fill for the surrounding residential construction. They are used to provide visual and recreational amenity, sometimes including boat navigation and mooring areas, and can also serve as detention basins and water quality polishing devices. As with anypermanent water feature, they inevitability also become an aquatic habitat.
    [Show full text]
  • Newman Lake Total Phosphorus TMDL
    Newman Lake Total Phosphorus Total Maximum Daily Load Water Quality Improvement Report November 2007 Publication Number 06-10-045 Newman Lake Total Phosphorus Total Maximum Daily Load Water Quality Improvement Report Prepared by: Anthony J. Whiley and Ken Merrill Washington State Department of Ecology Water Quality Program November 2007 Publication Number 06-10-045 You can print or download this document from our Web site at http://www.ecy.wa.gov/biblio/0610045.html For more information contact: Department of Ecology Water Quality Program Watershed Management Section P.O. Box 47600 Olympia, WA 98504-7600 Telephone: 360-407-6404 Headquarters (Lacey) 360-407-6000 Regional Whatcom Pend San Juan Office Oreille location Skagit Okanogan Stevens Island Northwest Central Ferry 425-649-7000 Clallam Snohomish 509-575-2490 Chelan Jefferson Spokane K Douglas i Bellevue Lincoln ts Spokane a Grays p King Eastern Harbor Mason Kittitas Grant 509-329-3400 Pierce Adams Lacey Whitman Thurston Southwest Pacific Lewis 360-407-6300 Yakima Franklin Garfield Wahkiakum Yakima Columbia Walla Cowlitz Benton Asotin Skamania Walla Klickitat Clark Persons with a hearing loss can call 711 for Washington Relay Service. Persons with a speech disability can call 877-833-6341. If you need this publication in an alternate format, please call the Water Quality Program at 360-407-6404. Persons with hearing loss can call 711 for Washington Relay Service. Persons with a speech disability can call 877-833-6341 Table of Contents List of Figures and Tables..............................................................................................................iii
    [Show full text]
  • Element Transport in a River-Lake Continuum Across Forest- Dominated Landscapes: a Case Study in Central Louisiana
    Louisiana State University LSU Digital Commons LSU Doctoral Dissertations Graduate School March 2020 Element Transport in A River-lake Continuum across Forest- dominated Landscapes: A Case Study in Central Louisiana Zhen Xu Louisiana State University and Agricultural and Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_dissertations Part of the Environmental Indicators and Impact Assessment Commons, Environmental Monitoring Commons, Geochemistry Commons, and the Hydrology Commons Recommended Citation Xu, Zhen, "Element Transport in A River-lake Continuum across Forest-dominated Landscapes: A Case Study in Central Louisiana" (2020). LSU Doctoral Dissertations. 5181. https://digitalcommons.lsu.edu/gradschool_dissertations/5181 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Doctoral Dissertations by an authorized graduate school editor of LSU Digital Commons. For more information, please [email protected]. ELEMENT TRANSPORT IN A RIVER-LAKE CONTINUUM ACROSS FOREST-DOMINATED LANDSCAPES: A CASE STUDY IN CENTRAL LOUISIANA A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The School of Renewable Natural Resources by Zhen Xu B.S., College of Idaho, 2012 M.S., Louisiana State University, 2014 May 2020 ACKNOWLEDGEMENTS I would like to thank everyone who helped and supported me on this lifetime achievement. First and foremost, thank you to my major advisor, Dr. Yi-Jun Xu, whose training set the foundation for this achievement. You let me swim upriver on my own, yet were always willing to pull me out of unhappy waters when I floundered.
    [Show full text]
  • Validation of the Swiss Methane Emission Inventory by Atmospheric Observations and Inverse Modelling
    Atmos. Chem. Phys., 16, 3683–3710, 2016 www.atmos-chem-phys.net/16/3683/2016/ doi:10.5194/acp-16-3683-2016 © Author(s) 2016. CC Attribution 3.0 License. Validation of the Swiss methane emission inventory by atmospheric observations and inverse modelling Stephan Henne1, Dominik Brunner1, Brian Oney1, Markus Leuenberger2, Werner Eugster3, Ines Bamberger3,4, Frank Meinhardt5, Martin Steinbacher1, and Lukas Emmenegger1 1Empa Swiss Federal Laboratories for Materials Science and Technology, Überlandstrasse 129, Dübendorf, Switzerland 2Univ. of Bern, Physics Inst., Climate and Environmental Division, and Oeschger Centre for Climate Change Research, Bern, Switzerland 3ETH Zurich, Inst. of Agricultural Sciences, Zurich, Switzerland 4Institute of Meteorology and Climate Research Atmospheric Environmental Research (IMK-IFU), Karlsruhe Institute of Technology (KIT), Garmisch-Partenkirchen, Germany 5Umweltbundesamt (UBA), Kirchzarten, Germany Correspondence to: Stephan Henne ([email protected]) Received: 30 October 2015 – Published in Atmos. Chem. Phys. Discuss.: 16 December 2015 Revised: 10 March 2016 – Accepted: 14 March 2016 – Published: 21 March 2016 Abstract. Atmospheric inverse modelling has the potential emissions by 10 to 20 % in the most recent SGHGI, which is to provide observation-based estimates of greenhouse gas likely due to an overestimation of emissions from manure emissions at the country scale, thereby allowing for an inde- handling. Urban areas do not appear as emission hotspots pendent validation of national emission inventories. Here, we in our posterior results, suggesting that leakages from nat- present a regional-scale inverse modelling study to quantify ural gas distribution are only a minor source of CH4 in the emissions of methane (CH4) from Switzerland, making Switzerland. This is consistent with rather low emissions of use of the newly established CarboCount-CH measurement 8.4 Ggyr−1 reported by the SGHGI but inconsistent with the network and a high-resolution Lagrangian transport model.
    [Show full text]
  • Retention Time of Lakes in the Larsemann Hills Oasis, East
    Retention time of lakes in the Larsemann Hills oasis, East Antarctica Elena Shevnina1, Ekaterina Kourzeneva1, Yury Dvornikov2, Irina Fedorova3 1Finnish Meteorological Institute, Helsinki, Finland. 2 Department of Landscape Design and Sustainable Ecosystems, Agrarian-Technological Institute, RUDN University, 5 Moscow, Russia 3Saint-Petersburg State University, St. Petersburg, Russia. Correspondence to: Elena Shevnina ([email protected]) Abstract. This study provides first estimates of water transport time scale for five lakes located in the Larsemann Hills oasis (69º23´S, 76º20´E) in East Antarctica. We estimated lake retention time (LRT) as a ratio of lake volume to the inflow and 10 outflow terms of a lake water balance equation. The LRT was evaluated for lakes of epiglacial and land-locked types, and it was assumed that these lakes are monomictic, with water exchange occurring during the warm season only. We used hydrological observations collected in 4 seasonal field campaigns to evaluate the LRT. For the epiglacial lakes Progress and Nella/Scandrett, the LRT was estimated at 12–13 and 4–5 years, respectively. For the land-locked lakes Stepped, Sarah Tarn and Reid, our results show a great difference in the LRT calculated from the outflow and inflow terms of the water balance 15 equation. The LRTs for these lakes vary depending on the methods and errors inherent to them. We relied on the estimations from the outflow terms, since they are based on hydrological measurements with better quality. Lake Stepped exchanged water within less than 1.5 years. Lake Sarah Tarn and Lake Reid are endorheic ponds, with water loss mainly through evaporation.
    [Show full text]
  • Queen of the Mountains
    Rigi Queen of the Mountains www.rigi.com Seewen Legende / Legend U r Muota m i Bergbahnen / mountain railways, cable cars b Bahnhof / railway station e r Unterkünfte / accommodations g Bushaltestelle / bus stop Restaurants / restaurants 447 e Urmiberg/Timpel 1135 m e Ingenbohl Wandertipps / hiking suggestions s Zahnradbahn / cogwheel railway r Gottertli 1396 m Aktivitäten im Sommer / summer activities e z Rigi Hochflue 1698 m Standseilbahn / cable car Wellness / wellness r Langberg Brunnen Steiner Aa Familien / families e Luftseilbahn / aerial cable car u a L Schiffstation / pier Autofähre / car ferry Treib Parkplatz / car park Lauerz Die detaillierte Rigikarte mit allen Wander- und Gätterlipass 1190 m Parkhaus / car park Themenwegen, Sehenswürdigkeiten sowie Unterhaltungs- Höcheli 1437 m und Verpflegungsmöglichkeiten erhalten Sie an allen 434 Aussichtspunkt / lookout point Bahnschaltern sowie in den Hotels, Restaurants und weiteren Verkaufsstellen. Chäppeliberg Rigi Burggeist 1551 m Rigi Scheidegg Tierpark 1656 m Gschwänd 1012 m Goldau Goldau A4 Hinder Dosse 1546 m Vitznauer-/Gersauerstock 1451 m Dosse 1685 m Oberarth Kräbel 759 m Fälmisegg 1176 m Rigi Kulm 1797 m Chäserenholz Schwendi Fruttli Gersau Arth Würzestock 1482 m Bruedersbalm Malchus Understette Hinderberge Trib Schild 1548 m Heiterenboden 413 Rigi Klösterli Steigelfadbalm Rigi Staffel Rigi First 1603 m Rotstock 1659 m Wissiflue Z u g e r s e e 945 m Ober-Äbnet Düssen Rigi Kaltbad Rigi Staffelhöhe Romiti 1433 m Freibergen Grubisbalm 1550 m Holderen Kuorez Felsetor Mittlerschwanden
    [Show full text]