Variations of Patagonian Glaciers, South America, Utilizing RADARSAT Images
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Patagonia Remote Wilderness of Chile & Argentina
PATAGONIA REMOTE WILDERNESS OF CHILE & ARGENTINA OVERLAND ADVENTURE 9 DAYS | 14 GUESTS CHILE ARGENTINA Itinerary Based on the expeditionary nature of our trips, there may be ongoing Los Glaciares ARGENTINA enhancements to this itinerary. National Park CHILE El Calafate Day 1 ARRIVE PUNTA ARENAS Fly independently to Punta Arenas. Enjoy great views of the Torres del Paine mountains as you soar over the Southern Patagonia Ice Field. Puerto Natales Spend two nights at the Hotel Diego de Almagro. (D) Magdalena Island Day 2 PORVENIR / PARQUE PINGUINO REY / Punta Arenas Parque Pinguino Rey Porvenir PUNTA ARENAS Fly to Porvenir in Tierra del Fuego. Drive along the shores of Bahia Inutil — “Useless Bay” — watching for an array of wildlife including guanaco, southern grey fox, upland goose and Chilean flamingo. JOURNEY BY LAND JOURNEY BY AIR Arrive at the private Parque Pinguino Rey, where we visit the world’s most accessible colony of king penguins. Fly back to Punta Arenas late this afternoon. (B,L,D) Experience the southernmost reach of the Andes on a Patagonia adventure spanning both Chile and Argentina. Days 3 & 4 MAGDALENA ISLAND / PUERTO NATALES Enjoy a rare opportunity to visit Tierra del Fuego’s Porvenir, Take a boat to Magdalena Island to visit the famous Magellanic home to the world’s most accessible colony of wild king penguin rookery, learning about their ecology. While visiting penguins. Hike the tundra of Torres del Paine, and travel to Estancia Cerro Negro, a typical working sheep-farming station, see El Calafate in Argentina for a full-day exploration of Los a shearing and sheep dog demonstration, followed by a delicious Glaciares National Park. -
Remote Sensing Study of Glacial Change in the Northern Patagonian Icefield
Advances in Remote Sensing, 2015, 4, 270-279 Published Online December 2015 in SciRes. http://www.scirp.org/journal/ars http://dx.doi.org/10.4236/ars.2015.44022 Remote Sensing Study of Glacial Change in the Northern Patagonian Icefield Lucy Dixon, Shrinidhi Ambinakudige Department of Geosciences, Mississippi State University, Starkville, MS, USA Received 23 October 2015; accepted 27 November 2015; published 30 November 2015 Copyright © 2015 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract The Patagonian Icefield has the largest temperate ice mass in the southern hemisphere. Using re- mote sensing techniques, this study analyzed multi-decadal glacial retreat and expansion of glaci- er lakes in Northern Patagonia. Glacial boundaries and glacier lake boundaries for 1979, 1985, 2000, and 2013 were delineated from Chilean topographic maps and Landsat satellite images. As- ter stereo images were used to measure mass balance from 2007 to 2012. The highest retreat was observed in San Quintin glacier. The area of glacier lakes increased from 13.49 km2 in 1979 to 65.06 km2 in 2013. Four new glacier lakes formed between 1979 and 2013. Between 2007 and 2012, significant glacial thinning was observed in major glaciers, including HPN1, Pared Norte, Strindberg, Acodado, Nef, San Quintin, Colonia, HPN4, and Benito glaciers. Generally, ablation zones lost more mass than accumulation zones. Keywords Patagonia, Glaciers, South America, ASTER 1. Introduction Glaciers are key indicators for assessing climate change [1]-[3]. Beginning in the nineteenth century, glaciers in many parts of the world retreated significantly, which was a clear indicator of climate warming [3]-[7]. -
PATAGONIA Located in Argentina and Chile, Patagonia Is a Natural Wonderland That Occupies the Southernmost Reaches of South America
PATAGONIA Located in Argentina and Chile, Patagonia is a natural wonderland that occupies the southernmost reaches of South America. It is an extraordinary landscape of dramatic mountains, gigantic glaciers that calve into icy lakes, cascading waterfalls, crystalline streams and beech forests. It is also an area rich in wildlife such as seals, humpback whales, pumas, condors and guanacos. The best time to visit Patagonia is between October and April. Highlights Spectacular Perito Moreno Glacier; scenic wonders of Los Glaciares National Park; unforgettable landscapes of Torres del Paine; breathtaking scenery of the Lakes District. Climate The weather is at its warmest and the hours of daylight at their longest (18 hours) during the summer months of Nov-Mar. This is also the windiest and busiest time of year. Winter provides clear skies, less windy conditions and fewer tourists; however temperatures can be extremely cold. 62 NATURAL FOCUS – TAILOR-MADE EXPERIENCES Pristine Patagonia Torres Del Paine National Park in Patagonia was incredible! I had never seen anything like it before. This was one of the most awesome trips I have ever been on. Maria-Luisa Scala WWW.NATURALFOCUSSAFARIS.COM.AU | E: [email protected] | T: 1300 363 302 63 ARGENTINIAN PATAGONIA • PERITO MORENO Breathtaking Perito Moreno Glacier © Shutterstock PERITO MORENO GLACIER 4 days/3 nights From $805 per person twin share Departs daily ex El Calafate Price per person from: Twin Single Xelena (Standard Room Lake View) $1063 $1582 El Quijote Hotel (Standard Room) $962 $1423 -
Glacial Lakes of the Central and Patagonian Andes
Aberystwyth University Glacial lakes of the Central and Patagonian Andes Wilson, Ryan; Glasser, Neil; Reynolds, John M.; Harrison, Stephan; Iribarren Anacona, Pablo; Schaefer, Marius; Shannon, Sarah Published in: Global and Planetary Change DOI: 10.1016/j.gloplacha.2018.01.004 Publication date: 2018 Citation for published version (APA): Wilson, R., Glasser, N., Reynolds, J. M., Harrison, S., Iribarren Anacona, P., Schaefer, M., & Shannon, S. (2018). Glacial lakes of the Central and Patagonian Andes. Global and Planetary Change, 162, 275-291. https://doi.org/10.1016/j.gloplacha.2018.01.004 Document License CC BY General rights Copyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the Aberystwyth Research Portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. tel: +44 1970 62 2400 email: [email protected] Download date: 09. Jul. 2020 Global and Planetary Change 162 (2018) 275–291 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Glacial lakes of the Central and Patagonian Andes T ⁎ Ryan Wilsona, , Neil F. -
Tours and Activities Season 2020-2021
Tours and Activities Season 2020-2021 Activities at Other activities Activities at EOLO Los Glaciares National Park in the area Tours and Activities Through the following guide, we expose the most representative activities in the area, in order to explore the surroundings of EOLO and Los Glaciares National Park. At EOLO, we can help you design the program that best suits your preferences, physical condition and duration of the stay, thus achieving an optimal itinerary to discover southern Patagonia and all its attractions. General notes . All activities are subject to availability, which is why we suggest booking in advance. Being outdoor activities, weather conditions could cause possible cancellations, changes or adjustments on the itinerary. The activities that take place in the National Park are conducted by companies designated by the National Park Administration. How to use the tours and activities guide: . The activities are grouped according to four main areas: Activities at EOLO, Perito Moreno Glacier area, Punta Bandera Port area, Other activities. We recommend to engage in one activity per area. It is required to hire a shuttle and an authorized guide to access the Perito Moreno glacier area. Both services are booked separately from the tours. To access Punta Bandera port area, it is also required to hire a shuttle, booked separately from the tours. El Chaltén Lago Vie dm a Upsala Glacier CHILE Estancia Cristina Spegazzini Glacier Lago Argentino Airport Punta Bandera El Calafate EOLO Perito Moreno Glacier Roca Lake 20 km 10 ml Google Activities at EOLO The land where the hotel stands extends to 10.000 acres, 30 minutes away from El Calafate, TREKKING on the way to Perito Moreno glacier. -
The 2015 Chileno Valley Glacial Lake Outburst Flood, Patagonia
Aberystwyth University The 2015 Chileno Valley glacial lake outburst flood, Patagonia Wilson, R.; Harrison, S.; Reynolds, John M.; Hubbard, Alun; Glasser, Neil; Wündrich, O.; Iribarren Anacona, P.; Mao, L.; Shannon, S. Published in: Geomorphology DOI: 10.1016/j.geomorph.2019.01.015 Publication date: 2019 Citation for published version (APA): Wilson, R., Harrison, S., Reynolds, J. M., Hubbard, A., Glasser, N., Wündrich, O., Iribarren Anacona, P., Mao, L., & Shannon, S. (2019). The 2015 Chileno Valley glacial lake outburst flood, Patagonia. Geomorphology, 332, 51-65. https://doi.org/10.1016/j.geomorph.2019.01.015 Document License CC BY General rights Copyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the Aberystwyth Research Portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. tel: +44 1970 62 2400 email: [email protected] Download date: 09. Jul. 2020 Geomorphology 332 (2019) 51–65 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph The 2015 Chileno Valley glacial lake outburst flood, Patagonia R. -
Getting to the Core of Climate Change
Getting to the Core of SCOPE ON THE SKIES Climate Change BY BOB RIDDLE hat image may come to and permafrost. As such, the cryo- that study the climate history of mind when the word sphere is part of the hydrosphere the cryosphere (paleoclimatol- Wglacier is heard? Before and could be thought of as the ogy) study global ice in a variety answering that question, here is “frozen water” part of the Earth. of ways, including data and ob- another one: glaciers are part of The cryosphere plays a signifi- servations from Earth’s orbit, fly- the Earth’s “cryosphere”—so what cant role in our planet’s climate, overs with instrument-equipped is the cryosphere? The cryosphere and an understanding of how cli- airplanes, and a ground-based includes any place on our planet’s mate has changed in the past may collection of observations and surface covered with water in the provide information about what data (see Hunting for Ice on Hud- form of snow, ice on land or sea, to expect in the future. Scientists son Bay in Resources). NASA’s Operation IceBridge is an airborne flyover of the ice at | FIGURE 1: Ice core sample. both the North and South Pole. (Source: climate.nasa.gov/system/news_items/main_images/2616_ A variety of instruments docu- p1000526-1280px-90.jpg) mented changes in the gain or loss in the thickness and mass of ice on land and sea as well as gla- ciers. Data collected by IceBridge is added to data from previous and current NASA satellite mis- sions, ICESat, ICESat-2, and the ESA’s satellite missions Cryo-Sat and CryoSat-2 (see Resources). -
South America Cryonet Meeting, 27-29 October 2014, Santiago De
TECHNICAL REPORT No. 2013- xx Insert title of report ....... WORLD METEOROLOGICAL ORGANIZATION GLOBAL CRYOSPHERE WATCH REPORT No. 8 CryoNet South America Workshop First Session Santiago de Chile, Chile 27-29 October 2014 © World Meteorological Organization, 2014 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate this publication in part or in whole should be addressed to: Chair, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 8403 P.O. Box 2300 Fax: +41 (0) 22 730 8040 CH-1211 Geneva 2, Switzerland E-mail: [email protected] NOTE The designations employed in WMO publications and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of WMO concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products does not imply that they are endorsed or recommended by WMO in preference to others of a similar nature which are not mentioned or advertised. The findings, interpretations and conclusions expressed in WMO publications with named authors are those of the authors alone and do not necessarily reflect those of WMO or its Members. FINAL -
A Review of the Current State and Recent Changes of the Andean Cryosphere
feart-08-00099 June 20, 2020 Time: 19:44 # 1 REVIEW published: 23 June 2020 doi: 10.3389/feart.2020.00099 A Review of the Current State and Recent Changes of the Andean Cryosphere M. H. Masiokas1*, A. Rabatel2, A. Rivera3,4, L. Ruiz1, P. Pitte1, J. L. Ceballos5, G. Barcaza6, A. Soruco7, F. Bown8, E. Berthier9, I. Dussaillant9 and S. MacDonell10 1 Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, Mendoza, Argentina, 2 Univ. Grenoble Alpes, CNRS, IRD, Grenoble-INP, Institut des Géosciences de l’Environnement, Grenoble, France, 3 Departamento de Geografía, Universidad de Chile, Santiago, Chile, 4 Instituto de Conservación, Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia, Chile, 5 Instituto de Hidrología, Meteorología y Estudios Ambientales (IDEAM), Bogotá, Colombia, 6 Instituto de Geografía, Pontificia Universidad Católica de Chile, Santiago, Chile, 7 Facultad de Ciencias Geológicas, Universidad Mayor de San Andrés, La Paz, Bolivia, 8 Tambo Austral Geoscience Consultants, Valdivia, Chile, 9 LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France, 10 Centro de Estudios Avanzados en Zonas Áridas (CEAZA), La Serena, Chile The Andes Cordillera contains the most diverse cryosphere on Earth, including extensive areas covered by seasonal snow, numerous tropical and extratropical glaciers, and many mountain permafrost landforms. Here, we review some recent advances in the study of the main components of the cryosphere in the Andes, and discuss the Edited by: changes observed in the seasonal snow and permanent ice masses of this region Bryan G. Mark, The Ohio State University, over the past decades. The open access and increasing availability of remote sensing United States products has produced a substantial improvement in our understanding of the current Reviewed by: state and recent changes of the Andean cryosphere, allowing an unprecedented detail Tom Holt, Aberystwyth University, in their identification and monitoring at local and regional scales. -
168 2Nd Issue 2015
ISSN 0019–1043 Ice News Bulletin of the International Glaciological Society Number 168 2nd Issue 2015 Contents 2 From the Editor 25 Annals of Glaciology 56(70) 5 Recent work 25 Annals of Glaciology 57(71) 5 Chile 26 Annals of Glaciology 57(72) 5 National projects 27 Report from the New Zealand Branch 9 Northern Chile Annual Workshop, July 2015 11 Central Chile 29 Report from the Kathmandu Symposium, 13 Lake district (37–41° S) March 2015 14 Patagonia and Tierra del Fuego (41–56° S) 43 News 20 Antarctica International Glaciological Society seeks a 22 Abbreviations new Chief Editor and three new Associate 23 International Glaciological Society Chief Editors 23 Journal of Glaciology 45 Glaciological diary 25 Annals of Glaciology 56(69) 48 New members Cover picture: Khumbu Glacier, Nepal. Photograph by Morgan Gibson. EXCLUSION CLAUSE. While care is taken to provide accurate accounts and information in this Newsletter, neither the editor nor the International Glaciological Society undertakes any liability for omissions or errors. 1 From the Editor Dear IGS member It is now confirmed. The International Glacio be moving from using the EJ Press system to logical Society and Cambridge University a ScholarOne system (which is the one CUP Press (CUP) have joined in a partnership in uses). For a transition period, both online which CUP will take over the production and submission/review systems will run in parallel. publication of our two journals, the Journal Submissions will be twotiered – of Glaciology and the Annals of Glaciology. ‘Papers’ and ‘Letters’. There will no longer This coincides with our journals becoming be a distinction made between ‘General’ fully Gold Open Access on 1 January 2016. -
Argentina SOLAR ECLIPSE ADVENTURE December 9-19, 2020 | 11 Days
Argentina SOLAR ECLIPSE ADVENTURE December 9-19, 2020 | 11 days TRIP ITINERARY 1.800.941.8010 | www.boundlessjourneys.com How we deliver THE WORLD’S GREAT ADVENTURES A passion for travel. Simply put, we love to travel, and that Small groups. Although the camaraderie of a group of like- infectious spirit is woven into every one of our journeys. Our minded travelers often enhances the journey, there can be staff travels the globe searching out hidden-gem inns and too much of a good thing! We tread softly, and our average lodges, taste-testing bistros, trattorias, and noodle stalls, group size is just 8–10 guests, allowing us access to and discovering the trails and plying the waterways of each opportunities that would be unthinkable with a larger group. remarkable destination. When we come home, we separate Flexibility to suit your travel style. We offer both wheat from chaff, creating memorable adventures that will scheduled, small-group departures and custom journeys so connect you with the very best qualities of each destination. that you can choose which works best for you. Not finding Unique, award-winning itineraries. Our flexible, hand- exactly what you are looking for? Let us customize a journey crafted journeys have received accolades from the to fulfill your travel dreams. world’s most revered travel publications. Beginning from Customer service that goes the extra mile. Having trouble our appreciation for the world’s most breathtaking and finding flights that work for you? Want to surprise your interesting destinations, we infuse our journeys with the traveling companion with a bottle of champagne at a tented elements of adventure and exploration that stimulate our camp in the Serengeti to celebrate an important milestone? souls and enliven our minds. -
Surface Energy Fluxes on Chilean Glaciers
The Cryosphere, 14, 2545–2565, 2020 https://doi.org/10.5194/tc-14-2545-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Surface energy fluxes on Chilean glaciers: measurements and models Marius Schaefer1, Duilio Fonseca-Gallardo1, David Farías-Barahona2, and Gino Casassa3,4 1Instituto de Ciencias Físicas y Matemáticas, Facultad de Ciencias, Austral University of Chile, Valdivia, Chile 2Institut für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, Germany 3Dirección General de Aguas, Ministerio de Obras Públicas, Santiago, Chile 4Centro de Investigación Gaia Antártica, Universidad de Magallanes, Punta Arenas, Chile Correspondence: Marius Schaefer ([email protected]) Received: 12 March 2019 – Discussion started: 13 June 2019 Revised: 15 May 2020 – Accepted: 14 June 2020 – Published: 10 August 2020 Abstract. The surface energy fluxes of glaciers determine 1 Introduction surface melt, and their adequate parametrization is one of the keys to a successful prediction of future glacier mass balance Glaciers are retreating and thinning in nearly all parts of and freshwater discharge. Chile hosts glaciers in a large range the planet, and it is expected that these processes are go- of latitudes under contrasting climatic settings: from 18◦ S ing to continue under the projections of global warming in the Atacama Desert to 55◦ S on Tierra del Fuego. Using (IPCC, 2019). For mountain glaciers melt is mostly deter- three different methods, we computed surface energy fluxes mined by the energy exchange with the atmosphere at their for five glaciers which represent the main glaciological zones surfaces. The processes leading to this exchange of energy of Chile.