Informe PROPIR Año 2006
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Impacts of Climate Change on Marine Fisheries and Aquaculture in Chile
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/319999645 Impacts of Climate Change on Marine Fisheries and Aquaculture in Chile Chapter · September 2017 DOI: 10.1002/9781119154051.ch10 CITATIONS READS 0 332 28 authors, including: Nelson A Lagos Ricardo Norambuena University Santo Tomás (Chile) University of Concepción 65 PUBLICATIONS 1,052 CITATIONS 13 PUBLICATIONS 252 CITATIONS SEE PROFILE SEE PROFILE Claudio Silva Marco A Lardies Pontificia Universidad Católica de Valparaíso Universidad Adolfo Ibáñez 54 PUBLICATIONS 432 CITATIONS 70 PUBLICATIONS 1,581 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Irish moss - green crab interactions View project Influence of environment on fish stock assessment View project All content following this page was uploaded by Pedro A. Quijón on 11 November 2017. The user has requested enhancement of the downloaded file. 239 10 Impacts of Climate Change on Marine Fisheries and Aquaculture in Chile Eleuterio Yáñez1, Nelson A. Lagos2,13, Ricardo Norambuena3, Claudio Silva1, Jaime Letelier4, Karl-Peter Muck5, Gustavo San Martin6, Samanta Benítez2,13, Bernardo R. Broitman7,13, Heraldo Contreras8, Cristian Duarte9,13, Stefan Gelcich10,13, Fabio A. Labra2, Marco A. Lardies11,13, Patricio H. Manríquez7, Pedro A. Quijón12, Laura Ramajo2,11, Exequiel González1, Renato Molina14, Allan Gómez1, Luis Soto15, Aldo Montecino16, María Ángela Barbieri17, Francisco Plaza18, Felipe Sánchez18, -
Geotechnical Reconnaissance of the 2015 Mw8.3 Illapel, Chile Earthquake
GEOTECHNICAL EXTREME EVENTS RECONNAISSANCE (GEER) ASSOCIATION Turning Disaster into Knowledge Geotechnical Reconnaissance of the 2015 Mw8.3 Illapel, Chile Earthquake Editors: Gregory P. De Pascale, Gonzalo Montalva, Gabriel Candia, and Christian Ledezma Lead Authors: Gabriel Candia, Universidad del Desarrollo-CIGIDEN; Gregory P. De Pascale, Universidad de Chile; Christian Ledezma, Pontificia Universidad Católica de Chile; Felipe Leyton, Centro Sismológico Nacional; Gonzalo Montalva, Universidad de Concepción; Esteban Sáez, Pontificia Universidad Católica de Chile; Gabriel Vargas Easton, Universidad de Chile. Contributing Authors: Juan Carlos Báez, Centro Sismológico Nacional; Christian Barrueto, Pontificia Universidad Católica de Chile; Cristián Benítez, Pontificia Universidad Católica de Chile; Jonathan Bray, UC Berkeley; Alondra Chamorro, Pontificia Universidad Católica de Chile; Tania Cisterna, Universidad de Concepción; Fernando Estéfan Thibodeaux Garcia, UC Berkeley; José González, Universidad de Chile; Diego Inzunza, Universidad de Concepción; Rosita Jünemann, Pontificia Universidad Católica de Chile; Benjamín Ledesma, Universidad de Concepción; Álvaro Muñoz, Pontificia Universidad Católica de Chile; Antonio Andrés Muñoz, Universidad de Chile; José Quiroz, Universidad de Concepción; Francesca Sandoval, Universidad de Chile; Pedro Troncoso, Universidad de Concepción; Carlos Videla, Pontificia Universidad Católica de Chile; Angelo Villalobos, Universidad de Chile. GEER Association Report No. GEER-043 Version 1: December 10, 2015 FUNDING -
División Político Administrativa Y Censal Región De Coquimbo
DIVISIÓN POLÍTICO ADMINISTRATIVA Y CENSAL REGIÓN DE COQUIMBO DEPARTAMENTO DE GEOGRAFÍA INSTITUTO NACIONAL DE ESTADÍSTICAS Enero/ 2019 CHILE: División Político-Administrativa y Censal REGIÓN, PROVINCIAS, COMUNAS Y Superficie Población Censo 2017 Viviendas Censo 2017 DISTRITOS CENSALES Km2 Total Urbana Rural Total Urbana Rural 04 REGIÓN DE COQUIMBO 40.578,9 757.586 615.116 142.470 308.608 238.503 70.105 1 PROVINCIA ELQUI 17.095,7 496.337 443.484 52.853 197.281 171.416 25.865 04101 Comuna La Serena 1.901,5 221.054 200.640 20.414 87.464 78.787 8.677 Distrito Censal 01 Intendencia 1,2 1.455 1.455 0 564 564 0 02 Mercado 7,7 16.661 15.504 1.157 5.236 4.848 388 03 Francisco de Aguirre 4,0 10.950 10.950 0 6.485 6.485 0 04 Las Vegas 9,0 12.037 12.037 0 9.327 9.327 0 05 La Pampa 13,7 37.096 36.971 125 14.305 14.265 40 06 La Florida 47,4 20.705 16.564 4.141 7.002 6.215 787 07 Algarrobito 72,0 2.358 1.056 1.302 1.038 360 678 08 Porvenir 140,6 3.103 0 3.103 1.542 0 1.542 09 Las Rojas 90,5 3.370 1.292 2.078 1.319 418 901 10 Romero 181,7 3.974 0 3.974 1.734 0 1.734 11 Condoriaco 398,4 66 0 66 71 0 71 12 Almirante Latorre 314,8 107 0 107 140 0 140 13 Islón 220,0 1.920 0 1.920 678 0 678 14 La Compañía 378,4 24.308 22.058 2.250 10.142 8.527 1.615 15 Universidad 5,6 16.328 16.328 0 7.183 7.183 0 16 La Compañía Alta 8,3 45.781 45.703 78 14.071 14.015 56 17 El Olivar 8,1 20.039 19.926 113 6.393 6.346 47 99 Rezagados 796 796 0 234 234 0 04102 Comuna Coquimbo 1.425,1 227.730 214.550 13.180 89.499 82.063 7.436 Distrito Censal 01 Aduana 2,0 8.717 8.717 0 2.640 -
Damage Assessment of the 2015 Mw 8.3 Illapel Earthquake in the North‑Central Chile
Natural Hazards https://doi.org/10.1007/s11069-018-3541-3 ORIGINAL PAPER Damage assessment of the 2015 Mw 8.3 Illapel earthquake in the North‑Central Chile José Fernández1 · César Pastén1 · Sergio Ruiz2 · Felipe Leyton3 Received: 27 May 2018 / Accepted: 19 November 2018 © Springer Nature B.V. 2018 Abstract Destructive megathrust earthquakes, such as the 2015 Mw 8.3 Illapel event, frequently afect Chile. In this study, we assess the damage of the 2015 Illapel Earthquake in the Coquimbo Region (North-Central Chile) using the MSK-64 macroseismic intensity scale, adapted to Chilean civil structures. We complement these observations with the analysis of strong motion records and geophysical data of 29 seismic stations, including average shear wave velocities in the upper 30 m, Vs30, and horizontal-to-vertical spectral ratios. The calculated MSK intensities indicate that the damage was lower than expected for such megathrust earthquake, which can be attributable to the high Vs30 and the low predominant vibration periods of the sites. Nevertheless, few sites have shown systematic high intensi- ties during comparable earthquakes most likely due to local site efects. The intensities of the 2015 Illapel earthquake are lower than the reported for the 1997 Mw 7.1 Punitaqui intraplate intermediate-depth earthquake, despite the larger magnitude of the recent event. Keywords Subduction earthquake · H/V spectral ratio · Earthquake intensity 1 Introduction On September 16, 2015, at 22:54:31 (UTC), the Mw 8.3 Illapel earthquake occurred in the Coquimbo Region, North-Central Chile. The epicenter was located at 71.74°W, 31.64°S and 23.3 km depth and the rupture reached an extent of 200 km × 100 km, with a near trench rupture that caused a local tsunami in the Chilean coast (Heidarzadeh et al. -
Climatic Characteristics of the Semi-Arid Coquimbo Region in Chile
Journal of Arid Environments 126 (2016) 7e11 Contents lists available at ScienceDirect Journal of Arid Environments journal homepage: www.elsevier.com/locate/jaridenv Climatic characteristics of the semi-arid Coquimbo Region in Chile * S. Montecinos a, b, , J.R. Gutierrez c, d, e,F.Lopez-Cort es c,D.Lopez d a Departamento de Física y Astronomía, Universidad de La Serena, Avenida Juan Cisternas 1200, La Serena, Chile b Centro Estudio Recursos de Energía, Universidad Arturo Prat (CERE-UNAP), Avda. Arturo Prat 2120, Iquique, Chile c Departamento de Biología, Universidad de La Serena, Raúl Bitran 1305, La Serena, Chile d Centro de Estudios Avanzados en Zonas Aridas (CEAZA), Raúl Bitran 1305, La Serena, Chile e Instituto de Ecología y Biodiversidad (IEB), Casilla 653, Santiago, Chile article info abstract Article history: The climate of the Coquimbo Region, north-central Chile is driven by atmospheric, oceanic and Received 17 December 2014 orographic factors. The southeast Pacific anticyclone, the cold Humboldt Current and the rugged Received in revised form topography that characterize the zone, determine thermally induced wind regimes and the formation of 5 May 2015 low stratocumulus along the coastline. Low precipitation and high solar radiation cause important cli- Accepted 30 September 2015 matic altitudinal gradients, especially on temperature and humidity, thus different climatic areas can be Available online 17 October 2015 identified in the region. We summarized the general climatic characteristics of the study area and analyzed meteorological data to understand the behavior of the environmental variables. We used Keywords:: Atmospheric modeling mesoscale modeling to evaluate the spatial characteristics of the mean air temperature, humidity and Semi-arid zones wind. -
First Meeting “Cystic Echinococcosis in Chile, Update in Alternatives for Control and Diagnostics in Animals and Humans” Cristian A
Alvarez Rojas et al. Parasites & Vectors (2016) 9:502 DOI 10.1186/s13071-016-1792-y MEETINGREPORT Open Access First meeting “Cystic echinococcosis in Chile, update in alternatives for control and diagnostics in animals and humans” Cristian A. Alvarez Rojas1*, Fernando Fredes2, Marisa Torres3, Gerardo Acosta-Jamett4, Juan Francisco Alvarez5, Carlos Pavletic6, Rodolfo Paredes7* and Sandra Cortés3,8 Abstract This report summarizes the outcomes of a meeting on cystic echinococcosis (CE) in animals and humans in Chile held in Santiago, Chile, between the 21st and 22nd of January 2016. The meeting participants included representatives of the Departamento de Zoonosis, Ministerio de Salud (Zoonotic Diseases Department, Ministry of Health), representatives of the Secretarias Regionales del Ministerio de Salud (Regional Department of Health, Ministry of Health), Instituto Nacional de Desarrollo Agropecuario (National Institute for the Development of Agriculture and Livestock, INDAP), Instituto de Salud Pública (National Institute for Public Health, ISP) and the Servicio Agrícola y Ganadero (Animal Health Department, SAG), academics from various universities, veterinarians and physicians. Current and future CE control activities were discussed. It was noted that the EG95 vaccine was being implemented for the first time in pilot control programmes, with the vaccine scheduled during 2016 in two different regions in the South of Chile. In relation to use of the vaccine, the need was highlighted for acquiring good quality data, based on CE findings at slaughterhouse, previous to initiation of vaccination so as to enable correct assessment of the efficacy of the vaccine in the following years. The current world’s-best-practice concerning the use of ultrasound as a diagnostic tool for the screening population in highly endemic remote and poor areas was also discussed. -
Linea Base Limnologica De Los Humedales De Tongoycomplementaria Solicitud De Sitio Ramsar
INFORME FINAL LINEA BASE LIMNOLOGICA DE LOS HUMEDALES DE TONGOYCOMPLEMENTARIA SOLICITUD DE SITIO RAMSAR Carlos Zuleta Ramos, Víctor Bravo Naranjo &Alex Cea Villablanca Universidad de La Serena Centro de Estudios Ambientales del Norte de Chile DICIEMBRE 2016 ÍNDICE Página 1 INTRODUCCIÓN 6 RESULTADOS 7 Paisajes 7 Riqueza faunística 10 Herpetofauna 10 Mastozoofauna 10 Avifauna 11 Fauna acuática 12 Riqueza Florística 14 HUMEDALES DE TONGOY 15 Estero Tongoy 18 Salinas Chica 21 Salinas Grande 24 Pachingo 27 CONCLUSIONES 31 REFERENCIAS BIBLIOGRÁFICAS 32 ANEXOS Anexo 1. Línea base Herpetofauna de los humedales de Tongoy (Coquimbo) 34 Anexo 2. Línea base Mastozoofauna de los humedales de Tongoy (Coquimbo) 35 Anexo 3: Línea base Ornitofauna de los humedales de Tongoy (Coquimbo) 36 Anexo 3: Línea base Flora de los humedales de Tongoy (Coquimbo) 40 2 TABLAS Página Tabla 1. Riqueza taxonómica registrada para los humedales costeros de Tongoy 10 Tabla 2. Riqueza de fauna acuática de los humedales costeros de la Bahía de Tongoy 13 Tabla 3. Riqueza taxonómica registrada para el humedal Estero Tongoy 18 Tabla 4. Riqueza de la Flora vascular del Estero Tongoy. Se indica el Origen (A=Adventicia, E=Endémica, N=Nativa), Formas de Vida (T=Arbol, F=Fanerofita (arbusto), S=Sufrútice, H= Hierba perenne, HB=Hierba bi-anual, A=Hierba anual, K=Cactácea) según Squeo et al (2001) 20 Tabla 5. Riqueza taxonómica de Vertebrados registrada para el humedal Salinas Chica 21 Tabla 6. Riqueza taxonómica de vertebrados registrada para el humedal Salinas Grande 24 Tabla 7. Riqueza taxonómica de Vertebrados registrada para el humedal Pachingo 27 Tabla 8. -
Estratigrafía Sísmica Y Evidencias Submarinas De Tectónica Activa En La Falla Puerto Aldea, Tongoy, IV Región De Coquimbo, Chile
O EOL GIC G A D D A E D C E I H C I L E O S F u n 2 d 6 la serena octubre 2015 ada en 19 Estratigrafía sísmica y evidencias submarinas de tectónica activa en la falla Puerto Aldea, Tongoy, IV Región de Coquimbo, Chile Julio Avilés*, Gabriel Vargas, Cristina Ortega Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile *email: [email protected] Resumen. Estudios previos indican que la actividad de la consideración de antecedentes de testigos de sedimento falla Puerto Aldea habría cesado al menos hace 230 ka en cortos (<1 m de largo) obtenidos en la bahía, en este la Bahía de Tongoy (Saillard, 2012), sin embargo, el trabajo se definen las unidades que constituyen el subsuelo análisis de perfiles acústicos de alta resolución evidencia del fondo marino, se interpreta su génesis y se caracteriza tectónica activa durante el Cuaternario tardío. la deformación que las afecta. La estratigrafía del subsuelo marino de la bahía de Tongoy, muestra 3 unidades sismo-estratigráficas. La unidad intermedia 2 es de tipo agradacional y desarrolla onlap, por En particular, se interpreta la actividad Cuaternaria tardía lo que se interpreta como producto de la transgresión de la falla Puerto Aldea, denotando su carácter activo. global post-glacial en el Pleistoceno tardío-Holoceno temprano. La unidad 3 sobreyace a la anterior, es de tipo progradacional-agradacional, desarrolla toplap y se asocia 2 Antecedentes Geológicos al alto estadio marino desde el Holoceno medio al presente. Estas dos unidades se encuentran afectadas por La falla Puerto Aldea constituye una de las principales fallas normales que deforman estratos y se asocian a estructuras geológicas de la costa semiárida de Chile. -
Hotelera Nacional De Chile" (HONSA): Modern Tourism in the Desert Territory in Northern Chile
The "Hotelera Nacional de Chile" (HONSA): modern tourism in the desert territory in northern Chile. Claudio Galeno-Ibaceta Universidad Católica del Norte, Escuela de Arquitectura, Av. Angamos 0610, 1270709, Antofagasta, Chile. e-mail: [email protected] Abstract: The modern leisure habits result of the right to spare time, increased mobility due to improved transport, education through travel, and enhancement of healthy environments, consolidated in the Chilean desert, a series of modern architectures linked to its context. In November 1933 the Ferrocarriles del Estado began publishing the magazine En Viaje (On Tour), which was the means of disseminating the values and tourism ventures in the country. The magazine precedes the enactment of the law of the annual holiday in January 1934. Since then, the State implemented a territorial politics implementation of tourist services, but takes on greater emphasis from the foundation of the Consorcio Hotelero in 1944, which declares its desire to build hotels in Northern Chile. That entity then joins with the Organización Nacional Hotelera, and together they are called Hotelera Nacional S.A. (HONSA). Keywords: tourism, Chile, hotel, desert, modernity. 01. Tourism in Chile. In Chile, a territorial politics of implementation of tourist architecture promoted by the State was executed; that in addition led all those dispersed national efforts to promote the tourism. The process began from mid thirties, but it had major institutionalism from the foundation of the Consorcio Hotelero de Chile, in 1944, that promoted new constructions, as well as it linked itself to existing entrepreneurship, generating a merge among the State, the local governments and the private world. -
Covid-19 Global Port Restrictions Chile
COVID-19 GLOBAL PORT RESTRICTIONS CHILE Chile General Information 931.939 accumulated confirmed cases have been registered in Chile so far, where there are 37.958 active cases of coronavirus, and 22.279. (Coronavirus arrived in Chile on the 3rd of March 2020). The nationwide nighttime curfew is maintained from 23:00 to 5:00 Chilean Local Time. The Ministry of Health has announced updates regarding the Step-by-Step plan, which comes into effect on the 20th of March, at 06:00 hrs LT: • The following areas are bacK to Transition phase: Diego de Almagro and Vallenar (Atacama region); Combarbalá (CoQuimbo region); Olmué (Valparaíso region); Graneros (O’Higgins region); Santa Juana (Biobío region); Pucón and Gorbea (Araucanía region). • The following areas are moving bacK to Quarantine phase: Iquique and Alto Hospicio (Tarapacá region); Concón, Quilpué, Villa Alemana, Nogales and Viña del Mar (Valparaíso region); Curacaví, María Pinto, Buin, Calera de Tango, La Cisterna, Talagante, Santiago and San Ramón (Metropolitan region); Chépica and Chimbarongo (O’Higgins region); San Ignacio (Ñuble region); Florida and Los Álamos (Biobío region); Curarrehue, Curacautín and Lautaro (La Araucanía region); Río Negro (Los Lagos region). • Interregional travel is authorized between zones that are in stages 3, 4, 5. The permit for interregional travel can be reQuested as many times as reQuired and must be reQuested 24 hours before. Case Types And COVID-19 Contact Confirmed Case: Any person who meets the definition of SUSPECTED CASE in which the specific test for SARS-CoV2 was "positive" (RT-PCR). In addition, there is the ASYMPTOMATIC CONFIRMED CASE: any person without symptoms, identified through an active search strategy that the SARS-CoV2 test was "positive" (RT-PCR) Medical Certificate: The treating doctor must issue a medical license for 11 days, with code CIE10 U0.1 (confirmed cases of Coronavirus), which can be extended remotely in the case of electronic medical license, without the presence of the employee. -
Regional Centers for Scientific And
REGIONAL Program CONICYT REGIONAL CENTERS FOR SCIENTIFIC AND TECHNOLOGICAL DEVELOPMENT Decentralizing science to serve the regions A joint initiative of CONICYT’s Regional Program and the regional governments REGIONAL PROGRAM 1 Comisión Nacional de Investigación 2 Científica y Tecnológica - CONICYT REGIONAL PROGRAM 3 The National Commission for Scientific and Technological Research, CONICYT was created in 1967 as an advisory organization for the Presidency in matters of scientific development. It is an autonomous public institution under the Ministry of Education. It organizes its work under two main strategic pillars: strengthening Chile’s scientific and technological base and promoting advanced human capital training. In order to achieve these strategic goals CONICYT has a variety of programs guided by the principles of open tendering and excellency via open calls. The projects are evaluated through different stages until their awarding, based on evaluations that follow international practices. Amongst our programs, the Regional Program for Scientific and Technological Research is of note. It began in 2000 thanks to an initiative by the Undersecretary of Regional Development and Administration. The instrument “Creation of regional centers for scientific and technological research” was co-funded by regional governments (GORE) with the aim of expanding and decentralizing the distribution of human, financial and material resources, from a geographic and institutional perspective. Thereby, the goal is to direct research towards the relevant subjects for the development of the regions where research institutions are located. Also, we hope to stimulate the development of disciplines or specific areas throughout the country with the purpose of helping the regional centers to become national leaders in their specific fields. -
Reconstructing Past Variations in Environmental Conditions and Paleoproductivity Over the Last ∼ 8000 Years Off North-Central Chile (30◦ S)
Biogeosciences, 17, 5763–5785, 2020 https://doi.org/10.5194/bg-17-5763-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Reconstructing past variations in environmental conditions and paleoproductivity over the last ∼ 8000 years off north-central Chile (30◦ S) Práxedes Muñoz1,2, Lorena Rebolledo3,4, Laurent Dezileau5, Antonio Maldonado2,6, Christoph Mayr7,8, Paola Cárdenas4, Carina B. Lange4,10,11, Katherine Lalangui9, Gloria Sanchez12, Marco Salamanca10, Karen Araya1,13, Ignacio Jara2, Gabriel Easton14, and Marcel Ramos1,2 1Departamento de Biología Marina, Universidad Católica del Norte, Larrondo 1281, Coquimbo, Chile 2Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena, Coquimbo, Chile 3Departamento Científico, Instituto Antártico Chileno, Punta Arenas, Chile 4Centro FONDAP de Investigación Dinámica de Ecosistemas Marinos de Altas Latitudes (IDEAL), Universidad Austral de Chile, Campus Isla Teja, Valdivia, Chile 5Normandy University, UNICAEN, UNIROUEN, CNRS, M2C, 14000 Caen, France 6Instituto de Investigación Multidisciplinario en Ciencia y Tecnología, Universidad de La Serena, La Serena, Chile 7Institut für Geographie, FAU Erlangen-Nürnberg, 91058 Erlangen, Germany 8Department of Earth and Environmental Sciences and GeoBio-Center, LMU Munich, 80333 Munich, Germany 9Planta de Alimentos Pargua, AquaChile, Puerto Montt, Chile 10Departamento de Oceanografía, Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, Casilla 160C, Concepción, Chile 11Centro de Investigación