El Complejo Hidroeléctrico De Hidroaysen En La Patagonia Chilena the Hidroaysén Hydroelectric Complex in Chilean Patagonia

Total Page:16

File Type:pdf, Size:1020Kb

El Complejo Hidroeléctrico De Hidroaysen En La Patagonia Chilena the Hidroaysén Hydroelectric Complex in Chilean Patagonia ART CASAS (19-38):C Y T.qxp 01/04/11 13:07 Página 19 Ciencia y Técnica de la Ingeniería Civil Revista de Obras Públicas El complejo hidroeléctrico de nº 3.520. Año 158 Abril 2011 ISSN: 0034-8619 Hidroaysen en la Patagonia chilena ISSN electrónico: 1695-4408 The HidroAysén Hydroelectric complex in Chilean Patagonia Antonio de las Casas Gómez. Ingeniero de Caminos, Canales y Puertos Madrid (España). [email protected] Resumen: El conocido como proyecto Hidroaysen consiste en la construcción de cinco centrales hidroeléctricas en los ríos Baker y Pascua en la Patagonia chilena, lo que aportará una potencia instalada de 2.750 MW, y una producción anual prevista de 18.430 GWh. La superficie ocupada por las cinco centrales es de 5.910 has lo cual supone una ocupación de 2,15 has/MW, cantidad mucho menor que la habitual en este tipo de proyectos. Para el traslado de la energía se prevé la construcción de una línea HVCD de 1912 km, 160 de los cuales submarinos. Tanto las centrales como una parte importante de la línea de transmisión discurren por zonas escasamente colonizadas y por tanto de un alto valor ecológico, por lo que el proyecto tiene que vencer la fuerte oposición de los grupos ecologistas. Palabras Clave: Hidroaysen; Patagonia; Chile; Centrales hidroeléctricas; Energías Renovables Abstract: The project known as Hidroaisen comprises the construction of five hydroelectric dams on the Baker and Pascua rivers in the Chilean Patagonia, with an installed capacity of 2.750 MW and the annual production expected is 18.430 GWh. The surface area occupied by the five plants is 5910 has, hence the occupancy is of 2.15ha/MW, far less than the usual for these type of projects. To transport the energy the construction of a HVCD line of 1.912 km, including 160 under the sea, is expected. Both the power plant and an important part of the transmission line go through sparsely populated areas which have a high ecological value. For this reason the project will have to overcome strong opposition from environmental groups. Keywords: Hidroaysen; Patagonia; Chile; Hidroelectric Power; Renewable Energies 1. Sector eléctrico en Chile 1. The electricity sector in Chile A abril de 2010, el sector eléctrico cuenta con 14.94 As of April 2010, the electricity sector in Chile had an GW de capacidad instalada. Éste se basa principal- installed capacity of 14.94 GW. This is primarily based on mente en la generación termoeléctrica (64,9%) e hi- thermal (64.9%) and hydropower generation (34%), in dráulica (34%),además de cerca de un 1% de centrales addition to nigh on 1% produced by wind power. As a eólicas. Producto de los cortes de gas que enfrentó a result of gas cuts in 2004, work was started on the partir de 2004, inició la construcción de dos terminales construction of two liquefied natural gas re-gasification regasificadores de GNL para permitir la importación de plants to allow the import of shipped natural gas. gas natural mediante barcos. The successful reform of the electricity sector in Chile La exitosa reforma del sector eléctrico de Chile, que was carried out in the first half of the 80’s and served as sirvió como modelo para otros países, se llevó a cabo a model for other countries and where the vertical and en la primera mitad de la década de los 80. La desa- horizontal unbundling of generation, transmission and gregación vertical y horizontal de la generación, trans- distribution together with large-scale privatization, all led misión y distribución, y la privatización a gran escala, to an increase in private investment. condujo al aumento de la inversión privada. 1.1. Installed capacity 1.1. Capacidad instalada There are four separate electricity systems in Chile: the Hay cuatro sistemas de electricidad independientes Central Interconnected System (SIC, Sistema en Chile: el Sistema Interconectado Central, (SIC), el Interconectado Central), which serves the central part Se admiten comentarios a este artículo, que deberán ser remitidos a la Redacción de la ROP antes del 30 de junio de 2011. Recibido: enero/2011. Aprobado: febrero/2011 19 a 38 Revista de Obras Públicas/ISSN: 0034-8619/ISSN electrónico: 1695-4408/Abril 2011/Nº 3.520 19 ART CASAS (19-38):C Y T.qxp 01/04/11 13:07 Página 20 de las Casas, A. cual provee a la parte central del país (75,8% de la ca- of the county (75.8% of the total installed capacity and pacidad total instalada y el 93% de la población); el Sis- 93% of the population); the Large Northern tema Interconectado del Norte Grande (SING), el cual Interconnected System (SING Sistema Interconectado provee a las regiones de explotación minera del desier- del Norte Grande), which serves the desert mining to del norte (23,2% de la capacidad total instalada) y regions in the North (23.3% of the total installed los sistemas de Aysen (0,3% de la capacidad total) y capacity; and the Aysen (0.3% of total capacity) and Magallanes (0,6% de la capacidad total), los cuales Magallanes (0.6% of total capacity) systems, which proveen a las pequeñas áreas del extremo sur del país. serve small areas of the extreme southern part of the Las grandes distancias que existen entre los cuatro siste- country. The long distances existing among the four mas hacen que sea difícil la integración. systems make integration difficult. A abril de 2010, la capacidad total instalada nomi- As at April 2010 the nominal total installed capacity nal alcanzaba 14.940 MW. Del total de la misma 10.346 was 14,940 MW, of which 10,346 MW corresponded to MW corresponden a la generación térmica, 5.426 MW thermal generation, 5,425 MW to hydroelectricity and a la generación hidroeléctrica y 167 MW a la genera- 167 MW to wind power. There is no nuclear generated ción eólica. No hay generación de origen nuclear. La power. The total generation in 2008 was 58.7 TWh, 59% generación total en 2008 fue de 58,7 TWh, el 59,0% del of which was produced by thermal sources, 40.9% by cual fue aportado por las fuentes térmicas, 40,9% por hydropower and the remaining 0.1% by wind power. This las fuentes hidráulicas y 0,1% correspondió a energía corresponding to just over 3,400 kWh per capita. eólica. Esto corresponde a algo más de 3.400 kWh per At present, the prevailing technology considered for cápita. the expansion of the system is that of coal-fired thermal Actualmente la tecnología dominante en la expan- plants, which will take a significant share in the Chilean sión del sistema son las centrales térmicas a carbón, las energy system following plans to build new plants for a que aumentarán significativamente su participación en total of 11,852 MW as of April 2010. These are followed, la matriz energética chilena, con proyectos por 11.852 in terms of importance, by the hydroelectric plants MW a abril de 2010. Le siguen en importancia las cen- which at April 2010 amounted to 10,388 MW. At this trales hidráulicas proyectadas, que a abril de 2010 su- same time, wind power plants amounted to 2,497 MW maban 10.338 MW. Las centrales eólicas sumaban a la and geothermal plants to 270 MW. misma fecha 2.497 MW, y las centrales geotérmicas 270 Distribution losses in 2005 were 6.52%, down from 8% a MW. decade before and well below the 13.5% LAC average. Las pérdidas en distribución en 2005 fueron de Chile’s depends very heavily on foreign imports for 6,52%, una cifra inferior al 8% de la década anterior y energy and from where it gains 72% of all its energy. [1] bastante menor al promedio de ALyC de 13,5%. The Chilean economy is undergoing rapid growth and La dependencia exterior de Chile en el campo de the National Energy Commission consider that the la energía es muy grande, el 72% de la energía es im- country will double consumption by 2020 and triple portada. [1] consumption by 2030 and this growth will have to be La economía de Chile está en franco crecimiento matched by an urgent increase in the country’s por lo que Comisión Nacional de Energía considera que electricity generating capacity. In view of current para 2020 se duplicará el consumo y se multiplicará por technological development, when excluding nuclear 3 para 2030, por lo tanto el aumento de la capacidad power for the time being on account of the excessive generadora de electricidad no puede considerarse un time required to develop this form of power even if were tema menor. Con el desarrollo tecnológico actual, ex- to be considered, this response may only be met by the cluida de momento la utilización de energía nuclear, greater development of hydropower and the installation cuyo desarrollo, en caso de optarse por este camino, of thermal plants. The most efficient of these plants, gas- aún llevaría bastantes años, solamente puede producir- fired plants, have to resort to imported fuel. This fuel is se con un mayor aprovechamiento de la energía hidro- subject to large price variations and uncertain supply eléctrica y con la instalación de plantas térmicas. Las from the neighbouring countries of Argentina and Bolivia más eficientes entre ellas, las que utilizan gas, deben re- and appears to be a very complicated option in both currir a un combustible importado por tanto sujeto a cases. This was demonstrated in the crisis of 2004 when una gran variación de los precios, que eventualmente Argentina unilaterally stopped the service in spite of the 20 Revista de Obras Públicas/ISSN: 0034-8619/ISSN electrónico: 1695-4408/Abril 2011/Nº 3.520 19 a 38 ART CASAS (19-38):C Y T.qxp 01/04/11 13:07 Página 21 El complejo hidroeléctrico de Hidroaysen en la Patagonia chilena The HidroAysén Hydroelectric complex in Chilean Patagonia podría llegar de los países vecinos, Argentina y Bolivia, contracts in place.
Recommended publications
  • Circling Lake Chelenko
    Circling Lake Chelenko Ingewtaik gego-gunu-munee. Route: Coyhaique – Chile Chico –Los Antiguos (Argentina). 6 Days, 6 Nights We invite you to travel around South Carretera Austral in Chilean Patagonia, home of Glaciers, millenary Ice fields and the land of the Tehuelches. Wild life and biosphere of the world. This wonderfull route will lead you to unknown and relevant locations such as Saint Raphael’s Glacier; Exploradores Glacier; the Marble Chapel Natural Monument; Baker river, the largest river in Chile; and to discover prehistoric vestiges of Ammonites and ancestral Dinosaurs found in the area. You will also navigate the Chelenko Lake (Ingewtaik gego-gunu- munee in Tehuelche language) to visit the town of Puerto Ibañez with its traditional craftsmanship, liquors and leather tannery. Enjoy the pleasures of the local Mate and Gaucho way of life… we invite you to live new traditions, experiences and landscapes. “Come and live Aysén Patagonia” 1 Itinerary Day 1: Coyhaique – Rio Tranquilo Port 07:30 am Coyhaique – Villa Cerro Castillo: Breakfast at a local restaurant, short visit to the local Museum and a 10-minute walk to “Alero de las manos Tehuelches”. Photo stops in several Lookout spots like Bosque Muerto, El Ibañez 1, Rio Murta Valley and Chelenko Lake lookout. 13:30 pm Puerto Tranquilo Marble cavern. (Boat) 1 hour and 30-minute ride to visit the inside of the Cavern’s tunnels, chapels and Marble Cathedral Lunch in a local restaurant upon return, consisting in native food and products and Patagonian dishes (Vegan and vegetarian alternatives also available). El Abuelo pathway scheduled after lunch.
    [Show full text]
  • Plecoptera Y Aeglidae
    Revista Chilena de Historia Natural ISSN: 0716-078X [email protected] Sociedad de Biología de Chile Chile VALDOVINOS, CLAUDIO; KIESSLING, ANDREA; MARDONES, MARÍA; MOYA, CAROLINA; OYANEDEL, ALEJANDRA; SALVO, JACQUELINE; OLMOS, VIVIANA; PARRA, ÓSCAR Distribución de macroinvertebrados (Plecoptera y Aeglidae) en ecosistemas fluviales de la Patagonia chilena: ¿Muestran señales biológicas de la evolución geomorfológica postglacial? Revista Chilena de Historia Natural, vol. 83, núm. 2, 2010, pp. 267-287 Sociedad de Biología de Chile Santiago, Chile Disponible en: http://www.redalyc.org/articulo.oa?id=369944294009 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto DISTRIBUCIÓN DE MACROINVERTEBRADOS EN RÍOS PATAGÓNICOS 267 REVISTA CHILENA DE HISTORIA NATURAL Revista Chilena de Historia Natural 83: 267-287, 2010 © Sociedad de Biología de Chile ARTÍCULO DE INVESTIGACIÓN Distribución de macroinvertebrados (Plecoptera y Aeglidae) en ecosistemas fluviales de la Patagonia chilena: ¿Muestran señales biológicas de la evolución geomorfológica postglacial? Distribution of macroinvertebrates (Plecoptera and Aeglidae) in fluvial ecosystems of the Chilean Patagonia: Do they show biological signals of the postglacial geomorphological evolution? CLAUDIO VALDOVINOS1, 2, *, ANDREA KIESSLING1, MARÍA MARDONES3,
    [Show full text]
  • PATAGONIA: Wild, Remote, Extreme…UNIQUE
    PATAGONIA: Wild, Remote, Extreme…UNIQUE CHILEAN PATAGONIA Threats • Warming – glacier shrinkage (Rivera et al 2007) – accelerated flow and sediment fluxes in rivers – Increased frequency of glacial-lake outburst floods • Combined hazard factors – Tectonic/volcanic activity – Slope instability – Increased intense rainfall UNEP (2010) from Dyurgerov & Meier (2005) Glacier O’Higgins (South Patagonian Icefield SPI)… Extreme Events Droughts: reduced seasonal precipitation (A. Rivera, CECS) 1. Outburst Floods: Baker Basin • Baker River Q ~ 1,100 m3/s , largest in Chile by flow and quite pristine • Outlet of Carrera Lake: 1900 km2, second largest in South America Baker river in summer (Photo: Juan E. Undurraga) Since 2008: >24 Lago Cachet 2 outbursts Glacial-Lake Outburst Floods G lacial • GLOFs down Colonia River into Baker L ake O utburst River (>24 events since April 2008) F lood GLOF 17 Sept. 2009 in Colonia-Baker confluence As opposed to Low flow Cachet 2 Lake CACHET2 LAKE FULL CACHET2 LAKE EMPTY • L ~ 5km, W ~ 1km, D~50m 3 • GLOFs: ~ 200 Hm (J. Lleidich) Receding GLOF into Río Baker Lake Cachet2 emptying… 8 Oct 2008 in Colonia-Baker confluence (DGA Aysén) Colonia Baker gauge Baker (A. Rivera, CECS) Geomorphological Indicators Cachet 2 outbursts – impacts to identify water levels Palaeofloods • Colonia Lake outlet o palaeo-channel: 3 Qp > 15,000 m /s 1.7 m (Benito et al 2014) • Bakerlonia samples o Q > 5000 m3/s (1800 to 1937) o Q > 7000 m3/s (1635 to 1677) GLOFs: SUMMARY & POTENTIAL ! IMPLICATIONS After 40 years of hiatus (1968-2008), 24+
    [Show full text]
  • The Environmental Impact Assessment………………………………………………………………
    Sustainable Energy Development in Chilean Patagonia: A Comprehensive Critique of the August 2008 HidroAysén Environmental Impact Assessment Graham Scholars Program Winter 2009 CEE 490: Sustainable Energy Development in South America Courtney Doman Shawn Kinkema Aubrey Parker Amy Fingerle Annette Kosin Matthew Raubinger Matthew Gacioch Rachel Lauderdale Sarah Robb Walter Graf Mary Lemmer Eric Sauck Alexander Harris Amy Mikus Jill Schlechtweg Greta Jankoviak John Monaghan Angela Wyse Professors Steven Wright and Sara Adlerstein-Gonzalez 1 Preface This report represents a course project prepared by a group of 17 undergraduate students and 1 graduate student at the University of Michigan enrolled in the course CEE 490 – Sustainable Energy Development in South America during the winter semester of 2009. In addition to studies of relevant documents, the students visited the Aysén region in February 2009 including some of the areas that would be impacted by the proposed projects, and participated in discussions and presentations with a number of stakeholders. The course was sponsored by the Graham Environmental Sustainability Institute; the views expressed in this report do not represent an official position of the University of Michigan or the Graham Environmental Sustainability Institute. Most of the students participating in the course were not fluent in Spanish and the review of lengthy documents in that language posed significant difficulties in ensuring accurate interpretation of the fundamental information that was analyzed in this report. There have been considerable efforts made to ensure the accuracy of the contents of this report but it is possible that relevant information was not located within the documents or was incorrectly translated.
    [Show full text]
  • Rivers of Patagonia Fact Sheet
    PATAGONIA’S WILD RIVERS G R O . UNDER SIEGE N R I . W W W | 5 5 1 1 - 8 4 8 - 0 1 5 | Rio Baker at its source. Photo Glenn Switkes, IRN 3 0 7 4 9 atagonia is a region of mystery and striking diversity, one of the precious few places on A C , the planet where the array of natural beauty still defies humankind’s imagination. Y P E L Stretching for about 386,000 square miles on both the Argentine and Chilean sides of the E K R E Andes Mountains, Patagonia is a place where fiords, glaciers, coastal rainforests, dry steppes, B , Y pristine lakes, and rushing rivers can all be found within a short distance of each other. A W Y The wild rivers of Patagonia are highly regarded for Saltón. The dams would flood the most fertile farming E L E eco-adventures – the Futalefu, Baker, Pascua and and ranching lands in the valley, and would form an K R other rivers are a daunting challenge for even the most enormous pool of stagnant water reaching to the E B experienced river runners. Introduced trout species Bertrand Lake, from which the Baker springs. The 7 4 have flourished in Patagonia, attracting fly fishermen Baker River region is considered a priority for conser- 8 1 from around the world. Hikers and campers have vation, and the region of steppes and mountains hosts | K made Patagonia’s ecotourism industry a rapidly grow- some of the last habitat of the huemul deer, a symbol R O ing source of income for the local economy.
    [Show full text]
  • Triggering Mechanism and Depositional Processes of a Late Holocene Megaturbidite in Baker Fjord, Chilean Patagonia
    FACULTEIT WETENSCHAPPEN Opleiding Master of Science in de geologie Triggering mechanism and depositional processes of a late Holocene megaturbidite in Baker fjord, Chilean Patagonia Loïc Piret Academiejaar 2015–2016 Scriptie voorgelegd tot het behalen van de graad Van Master of Science in de geologie Promotor: Prof. Dr. S. Bertrand Begeleider: Prof. Dr. S. Bertrand Leescommissie: Dr. C. Kissel, Dr. M. Van Daele Cover image. Bathymetric map of the Baker/Martinez fjord complex. II ACKNOWLEDGEMENTS I was amazed by the amount of people that provided excellent help and guidance through the course of making this thesis and furthermore through my entire education. In this section I’d like to express my gratitude towards these people. First, I’d like to thank my promoter, Sébastien Bertrand (aka Seb). Your support and readiness to answer my questions are greatly appreciated. From the lab work in Paris, over figuring out how to exactly make a bathymetric map to teaching me how to properly write a scientific text, you gave me a great and educational experience. And most important, you guided me to become a young scientist. The sampling trip to Paris (Gif sur Yvette) was very pleasant and gave me some initial insight in the way of working and the larger context of the project. I would like to thank Catherine Kissel for her guidance and of course also for providing the magnetic data and radiocarbon dates. Also I would like to thank Camille Wandres for preparing the U-channels, making my lab work so much easier. All the people who provided essential data for this thesis are acknowledged: Ricardo de Pol Holz for the radiocarbon dates, Alvaro Tamayo for the foram data, Carlos Moffat & Lorena Rebolledo for the bathymetrical data, Xavier Morin of Ipev for the sub-bottom profiles.
    [Show full text]
  • This Is an Accepted Manuscript of an Article Published by Taylor & Francis in HYDROLOGICAL SCIENCES JOURNAL on 10/10/2012, A
    This is an Accepted Manuscript of an article published by Taylor & Francis in HYDROLOGICAL SCIENCES JOURNAL on 10/10/2012, available online: http://www.tandfonline.com/10.1080/02626667.2012.726993 1 Hydrological regime of remote catchments with extreme gradients under accelerated change: the Baker basin in Patagonia Alejandro Dussaillant J.1,4, Wouter Buytaert2, Claudio Meier3,4 and Fabián Espinoza5 1 Civil Engineering Deparment, University of Greenwich, UK [email protected] 2 Imperial College London, UK 3 Depto. Ingeniería Civil, Universidad de Concepción, Concepción, Chile 4 Centro de Investigación en Ecosistemas de la Patagonia, Coyhaique, Chile 5 Dirección General de Aguas, región Aysén, Coyhaique, Chile Received 7 June 2010; accepted 2 April 2012; open for discussion until Editor Z.W. Kundzewicz Citation , 2012. Hydrological Sciences Journal, 57 (?), ???–???. Abstract The Baker basin (27 000 km2) is located in one of the most unique and remote areas of the planet. Its hydrological regime is poised to undergo dramatic changes in the near future due to hydropower development and climate change. The basin contains the second largest lake in South America, and part of a major icefield. This study documents the natural baseline of the Baker River basin, discusses the main hydrological modes and analyses the potential for sustainable management. Annual precipitation varies several-fold from the eastern Patagonian steppes to the North Patagonian Icefield. The westernmost sub- basins are strongly governed by glacier-melt with a peak discharge in the austral summer (January–March). The easternmost sub-basins have a much more seasonal response governed by quicker snowmelt in spring (November–December), while they exhibit low flows typical for semi-arid regions during summer and autumn.
    [Show full text]
  • Hydro-Transitions: an Environmental History of Chilean Electrification
    HYDRO-TRANSITIONS: AN ENVIRONMENTAL HISTORY OF CHILEAN ELECTRIFICATION by Peter B. de Montmollin B.A., Syracuse University, 2009 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in The Faculty of Graduate and Postdoctoral Studies (Geography) THE UNIVERSITY OF BRITISH COLUMBIA (Vancouver) January 2021 © Peter B. de Montmollin, 2021 ii The following individuals certify that they have read, and recommend to the Faculty of Graduate and Postdoctoral Studies for acceptance, the thesis entitled: Hydro-Transitions: An Environmental History of Chilean Electrification submitted by Peter B. de Montmollin in partial fulfillment of the requirements for the degree of Master of Arts in Geography Examining Committee: Matthew Evenden, Geography Department, UBC Supervisor Juanita Sundberg, Geography Department, UBC Supervisory Committee Member iii Abstract This thesis examines the history of electrification and hydropower in Chile during the 20th century. Drawing from environmental history, technology history, and science and technology studies, it asks three central questions: How did technology, nature and society interact and shape the hydro-electrification of Chile? What were the economic, environmental and political consequences of damming Chilean rivers for power? And, more broadly, how did rivers, hydroelectric stations and power lines influence territorial and developmental imaginaries and policies over this period? The empirical foundations of the research are primary documents consulted at various archives and libraries in Santiago, Chile, as well as some online repositories. The thesis is structured loosely around the 1943 national electrification plan, which set the terms for constructing a large technological system to exploit Chile’s rivers for power. It explores the origins and creation of the plan, the execution of a key project on the Laja River in south-central Chile, and the failure of another project in Aysén in southern Patagonia.
    [Show full text]
  • Seasonal Thermal Structure and Exchange in Baker Channel, Chile
    Dynamics of Atmospheres and Oceans 58 (2012) 1–19 Contents lists available at SciVerse ScienceDirect Dynamics of Atmospheres and Oceans journal homepage: www.elsevier.com/locate/dynatmoce Seasonal thermal structure and exchange in Baker Channel, Chile a,b,∗ Christopher M. Aiken a Estación Costera de Investigaciones Marinas, Pontificia Universidad Católica de Chile, Las Cruces, Chile b Centro de Investigación en Ecosistemas de la Patagonia, Coyhaique, Chile a r t i c l e i n f o a b s t r a c t Article history: A series of four field campaigns undertaken between November Received 10 October 2011 2007 and August 2008 in the Baker Channel fjord complex in south- Received in revised form 31 May 2012 ern Chile provide a unique record of the seasonal evolution of its Accepted 12 July 2012 vertical and axial structure. The observations document the warm- Available online 21 July 2012 ing of subsurface waters during the summer and autumn of 2008 creating a subsurface temperature maximum that persists at the Keywords: channel head until the following spring. An analysis of the observed Fjord dynamics horizontal and vertical structure is used to infer that the subsurface Renewal heating owes to the seasonal intrusion of relatively warm water River plumes from Penas Gulf. A series of numerical simulations provide support Mathematical models Chile for the hypothesis that seasonal density fluctuations in the Penas Gulf are responsible for modulating the exchange of intermediary Baker Channel ◦ ◦ 48 S 74 W waters and maintaining anomalously warm water at the channel head from autumn until the following spring.
    [Show full text]
  • Downloaded 10/02/21 11:37 PM UTC FEBRUARY 2015 K R O G H E T a L
    172 JOURNAL OF HYDROMETEOROLOGY VOLUME 16 Physically Based Mountain Hydrological Modeling Using Reanalysis Data in Patagonia SEBASTIAN A. KROGH Department of Civil Engineering, Universidad de Chile, Santiago, Chile JOHN W. POMEROY Centre for Hydrology, University of Saskatchewan, Saskatoon, Saskatchewan, Canada JAMES MCPHEE Department of Civil Engineering, and Advanced Mining Technology Center, Universidad de Chile, Santiago, Chile (Manuscript received 30 October 2013, in final form 15 August 2014) ABSTRACT A physically based hydrological model for the upper Baker River basin (UBRB) in Patagonia was de- veloped using the modular Cold Regions Hydrological Model (CRHM) in order to better understand the processes that drive the hydrological response of one of the largest rivers in this region. The model includes a full suite of blowing snow, intercepted snow, and energy balance snowmelt modules that can be used to describe the hydrology of this cold region. Within this watershed, snowfall, wind speed, and radiation are not measured; there are no high-elevation weather stations; and existing weather stations are sparsely distributed. The impact of atmospheric data from ECMWF interim reanalysis (ERA-Interim) and Climate Forecast System Reanalysis (CFSR) on improving model performance by enhancing the representation of forcing variables was evaluated. CRHM parameters were assigned for local physiographic and vegetation characteristics based on satellite land cover classification, a digital elevation model, and parameter transfer from cold region environ- ments in western Canada. It was found that observed precipitation has almost no predictive power [Nash– Sutcliffe coefficient (NS) , 0.3] when used to force the hydrologic model, whereas model performance using any of the reanalysis products—after bias correction—was acceptable with very little calibration (NS .
    [Show full text]
  • Buenos Aires
    Geomorphic Records along the General Carrera (Chile)–Buenos Aires (Argentina) Glacial Lake (46°-48°S), Climate Inferences, and Glacial Rebound for the Past 7–9ka Jacques Bourgois, Maria Eugenia Cisternas, Regis Braucher, Didier Bourles, José Frutos To cite this version: Jacques Bourgois, Maria Eugenia Cisternas, Regis Braucher, Didier Bourles, José Frutos. Geomorphic Records along the General Carrera (Chile)–Buenos Aires (Argentina) Glacial Lake (46°-48°S), Climate Inferences, and Glacial Rebound for the Past 7–9ka . Journal of Geology, University of Chicago Press, 2016, 124 (1), pp.27-53. 10.1086/684252. hal-01271536 HAL Id: hal-01271536 https://hal.archives-ouvertes.fr/hal-01271536 Submitted on 9 Feb 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Manuscript Click here to download Manuscript: DOC 3 NEW TEXT SEPT 2015.doc 1 Geomorphic records along the General Carrera (Chile)-Buenos Aires 2 (Argentina) glacial lake (46-48°S), climate inferences and glacial rebound 3 for the past 7-9 ka 4 5 a,b, *Jacques Bourgois, cMaria Eugenia Cisternas, dRégis Braucher, dDidier Bourlès, eJose 6 Frutos 7 8 aSorbonne Universités, UPMC Univ Paris 06, UMR 7193, Institut des Sciences de la Terre 9 Paris (iSTeP), F-75005, Paris, France.
    [Show full text]
  • Latitudinal Patterns of Export Production Recorded in Surface Sediments of the Chilean Patagonian Fjords (41–55°S) As a Respo
    Continental Shelf Research 31 (2011) 340–355 Contents lists available at ScienceDirect Continental Shelf Research journal homepage: www.elsevier.com/locate/csr Research papers Latitudinal patterns of export production recorded in surface sediments of the Chilean Patagonian fjords (41–551S) as a response to water column productivity Claudia Aracena a,n, Carina B. Lange b,c, Jose´ Luis Iriarte c,d, Lorena Rebolledo e, Silvio Pantoja b,c a Programa de Postgrado en Oceanografı´a, Departamento de Oceanografı´a, Universidad de Concepcio´n, Casilla 160-C, Concepcio´n, Chile b Departamento de Oceanografı´a and Centro de Investigacio´n Oceanogra´fica en el Pacı´fico Sur-Oriental (COPAS), Universidad de Concepcio´n, Casilla 160-C, Concepcio´n, Chile c Programa COPAS Sur-Austral, Universidad de Concepcio´n, Casilla 160-C, Concepcio´n, Chile d Instituto de Acuicultura, Universidad Austral de Chile, Casilla 1327, Puerto Montt, Chile e Instituto de Biologı´a Marina, Facultad de Ciencias, Universidad Austral de Chile, Casilla 567, Valdivia, Chile article info abstract Article history: The Chilean Patagonian fjords region (41–561S) is characterized by highly complex geomorphology and Received 23 November 2009 hydrographic conditions, and strong seasonal and latitudinal patterns in precipitation, freshwater Received in revised form discharge, glacier coverage, and light regime; all of these directly affect biological production in the 9 August 2010 water column. In this study, we compiled published and new information on water column properties Accepted 18 August 2010 (primary production, nutrients) and surface sediment characteristics (biogenic opal, organic carbon, 13 molar C/N, bulk sedimentary d Corg) from the Chilean Patagonian fjords between 411S and 551S, Keywords: describing herein the latitudinal pattern of water column productivity and its imprint in the underlying Biogenic opal sediments.
    [Show full text]