Changes in Andes Snow Cover from MODIS Data, 2000–2016
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Endangered Andean Cat Distribution Beyond the Andes in Patagonia
original contribution ANDRES NOVARO1,2, SUSAN WALKER2*, ROCIO PALACIOS1,3, SEBASTIAN DI MARTINO4, MARTIN MONTEVERDE5, SEBASTIAN CANADELL6, LORENA RIVAS1,2 AND DANIEL COSSIOS7 Endangered Andean cat distribution beyond the Andes in Patagonia The endangered Andean cat Leopardus jacobita was considered an endemic of the Andes at altitudes above 3,000 m, until it was discovered in the Andean foothills of central Argentina in 2004. We carried out surveys for Andean cats and sympatric small cats in the central Andean foothills and the adjacent Patagonian steppe, and found Andean cats outside the Andes at elevations as low as 650 m. We determined that Andean cats are widespread but rare in the northern Patagonian steppe, with a patchy distribution. Our findings suggest that the species’ distribution may follow that of its principal prey, the rock-dwelling mountain vizcacha. The Andean cat was previously believed to be distribution if it does indeed follow that of the endemic to the Andes above 3,000 m (Yensen mountain vizcacha. First, to avoid bias for par- & Seymour 2000), until an opportunistic pho- ticular habitats beyond the Andes we placed Fig. 1. Location of new records and un- tograph in 2004 produced the startling finding a 2 x 2 km grid over the area with ArcGIS. confirmed reports of Andean cats in Men- of two Andean cats at only 1,800 m, in the We selected 105 grid cells, using stratified doza and Neuquén provinces (black dots), Andean foothills of central Argentina (Sorli et random sampling to ensure broad geographic relative to previous known distribution in al. -
Climate, Tectonics, and the Morphology of the Andes
Climate, tectonics, and the morphology of the Andes David R. Montgomery Greg Balco Sean D. Willett Department of Geological Sciences, University of Washington, Seattle 98195-1310, USA ABSTRACT Large-scale topographic analyses show that hemisphere-scale climate variations are a ®rst-order control on the morphology of the Andes. Zonal atmospheric circulation in the Southern Hemisphere creates strong latitudinal precipitation gradients that, when incor- porated in a generalized index of erosion intensity, predict strong gradients in erosion rates both along and across the Andes. Cross-range asymmetry, width, hypsometry, and maximum elevation re¯ect gradients in both the erosion index and the relative dominance of ¯uvial, glacial, and tectonic processes, and show that major morphologic features cor- relate with climatic regimes. Latitudinal gradients in inferred crustal thickening and struc- tural shortening correspond to variations in predicted erosion potential, indicating that, like tectonics, nonuniform erosion due to large-scale climate patterns is a ®rst-order con- trol on the topographic evolution of the Andes. Keywords: geomorphology, erosion, tectonics, climate, Andes. INTRODUCTION we argue for the ®rst-order importance of earthquake cycle. Some studies have attribut- The presence or absence of mountain rang- large-scale climate zonations and resulting dif- ed local variations in structural, metamorphic, es at the global scale is determined by the lo- ferences in geomorphic processes to the mor- and geomorphic characteristics of the central cation and type of plate boundaries. Other fac- phology of mountain ranges. Andes to erosion (Gephart, 1994; Masek et al., tors become important in the evolution of 1994; Horton, 1999), but none has considered individual mountain systems. -
Area Changes of Glaciers on Active Volcanoes in Latin America Between 1986 and 2015 Observed from Multi-Temporal Satellite Imagery
Journal of Glaciology (2019), 65(252) 542–556 doi: 10.1017/jog.2019.30 © The Author(s) 2019. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Area changes of glaciers on active volcanoes in Latin America between 1986 and 2015 observed from multi-temporal satellite imagery JOHANNES REINTHALER,1,2 FRANK PAUL,1 HUGO DELGADO GRANADOS,3 ANDRÉS RIVERA,2,4 CHRISTIAN HUGGEL1 1Department of Geography, University of Zurich, Zurich, Switzerland 2Centro de Estudios Científicos, Valdivia, Chile 3Instituto de Geofisica, Universidad Nacional Autónoma de México, Mexico City, Mexico 4Departamento de Geografía, Universidad de Chile, Chile Correspondence: Johannes Reinthaler <[email protected]> ABSTRACT. Glaciers on active volcanoes are subject to changes in both climate fluctuations and vol- canic activity. Whereas many studies analysed changes on individual volcanoes, this study presents for the first time a comparison of glacier changes on active volcanoes on a continental scale. Glacier areas were mapped for 59 volcanoes across Latin America around 1986, 1999 and 2015 using a semi- automated band ratio method combined with manual editing using satellite images from Landsat 4/5/ 7/8 and Sentinel-2. Area changes were compared with the Smithsonian volcano database to analyse pos- sible glacier–volcano interactions. Over the full period, the mapped area changed from 1399.3 ± 80 km2 − to 1016.1 ± 34 km2 (−383.2 km2)or−27.4% (−0.92% a 1) in relative terms. -
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. -
Why the Andes Matter
Sustainable Mountain Development RIO 2012 and beyond Why the Andes matter How the Andes contribute to sustainable development The Andes, covering a contiguous mountain region within Argentina, Bolivia, Chile, Colombia, Ecuador, Peru and Venezuela, occupy more than 2,500,000 km² and have The Andes, covering 33% of the area of the Ande- a population of about 85 million (45% of total country an countries, are vital for the livelihoods of the ma- populations), with the northern Andes as one of the most jority of the region’s population and the countries’ densely populated mountain regions in the world. At economies. However, increasing pressure, fuelled least a further 20 million people are also dependent on mountain resources and ecosystem services in the large by growing population numbers, changes in land cities along the Pacific coast of South America. use, unsustainable exploitation of resources, and climate change, could have far-reaching negati- The Andes play a vital part in national economies, ve impacts on ecosystem goods and services. To accounting for a significant proportion of the region’s achieve sustainable development, policy action is GDP, providing large agricultural areas, mineral resources, required regarding the protection of water resour- and water for agriculture, hydroelectricity (Figure 1), ces, responsible mining practices, adaptation to cli- domestic use, and some of the largest business centres in South America. However, some of the region’s poorest mate change and mechanisms to generate and use areas are also located in the mountains. knowledge for sound decision making. The region is highly diverse in terms of landscape, biodi- versity including agro-biodiversity, languages, peoples and cultures. -
Glacier Fluctuations During the Past 2000 Years
Quaternary Science Reviews 149 (2016) 61e90 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Invited review Glacier fluctuations during the past 2000 years * Olga N. Solomina a, , Raymond S. Bradley b, Vincent Jomelli c, Aslaug Geirsdottir d, Darrell S. Kaufman e, Johannes Koch f, Nicholas P. McKay e, Mariano Masiokas g, Gifford Miller h, Atle Nesje i, j, Kurt Nicolussi k, Lewis A. Owen l, Aaron E. Putnam m, n, Heinz Wanner o, Gregory Wiles p, Bao Yang q a Institute of Geography RAS, Staromonetny-29, 119017 Staromonetny, Moscow, Russia b Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA c Universite Paris 1 Pantheon-Sorbonne, CNRS Laboratoire de Geographie Physique, 92195 Meudon, France d Department of Earth Sciences, University of Iceland, Askja, Sturlugata 7, 101 Reykjavík, Iceland e School of Earth Sciences and Environmental Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA f Department of Geography, Brandon University, Brandon, MB R7A 6A9, Canada g Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, CC 330 Mendoza, Argentina h INSTAAR and Geological Sciences, University of Colorado Boulder, USA i Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway j Uni Research Climate AS at Bjerknes Centre for Climate Research, Bergen, Norway k Institute of Geography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria l Department of Geology, -
Sunny Islands & Andes
SUNNY ISLANDS & ANDES FEATURING PANAMA CANAL TRANSIT aboard Marina SANTIAGO TO MIAMI • JANUARY 3–22, 2020 BOOK BY JUN 6, 2019 2-FOR-1 CRUISE FARES & FREE UNLIMITED INTERNET Featuring OLife Choice: INCLUDES ROUND-TRIP AIRFARE* PLUS, CHOICE OF 8 FREE SHORE EXCURSIONS**, OR FREE BEVERAGE PACKAGE***, OR $800 SHIPBOARD CREDIT ABOVE OFFERS ARE PER STATEROOM, BASED ON DOUBLE OCCUPANCY SPONSORED BY: FOLLOW GO NEXT TRAVEL: VOTED ONE OF THE WORLD'S BEST CRUISE LINES SUNNY ISLANDS & ANDES 18 NIGHTS ABOARD MARINA • JANUARY 3–22, 2020 SANTIAGO TO MIAMI FEATURING: COQUIMBO • LIMA • SALAVERRY • MANTA • FUERTE AMADOR PUERTO LIMÓN • ROATÁN • HARVEST CAYE • COSTA MAYA • COZUMEL 2-FOR-1 CRUISE FARES & FREE UNLIMITED INTERNET Featuring OLife Choice: INCLUDES ROUND-TRIP AIRFARE* PLUS, CHOICE OF 8 FREE SHORE EXCURSIONS**, OR FREE BEVERAGE PACKAGE***, OR $800 SHIPBOARD CREDIT ABOVE OFFERS ARE PER STATEROOM, BASED ON DOUBLE OCCUPANCY IF BOOKED BY JUNE 6, 2019 R1 PRSRT STD U.S. POSTAGE PAID 340-2 SunnyIslands &Andes R1 PERMIT #32322 Virginia Tech Alumni Association TWIN CITIES, MN Holtzman Alumni Center (0102) 901 Prices Fork Road Costa Maya, Mexico Blacksburg, Virginia 24061 Cover Image: DEAR ALUMNI AND FRIENDS, Explore a variety of cultural traditions, exotic landscapes, and historic archaeological sites cruising the western coast of South America, Central America, and the Caribbean. Arrive in Santiago de Chile, a city of dazzling skyscrapers surrounded by the snow-capped Andes, and travel to Coquimbo to bask in the comfortable desert climate. In vibrant Lima, enjoy baroque architecture or pay homage to pre-Columbian history at the ruins of Huaca Pucllana. -
Voyage Calendar
February 2016 March 2016 April 2016 May 2016 June 2016 July 2016 August 2016 September 2016 October 2016 November 2016 December 2016 January 2017 February 2017 March 2017 April 2017 May 2017 June & July 2017 Alluring Andes & Majestic Fjords Journey Through the Amazon Mayan Mystique Northwest Wonders Coastal Alaska Coastal Alaska Coastal Alaska Accent on Autumn Beacons of Beauty Celebrate the Sunshine Pacific Holidays Baja & The Riviera Amazon Exploration Patagonian Odyssey Southern Flair The Great Northwest Lima to Buenos Aires Rio de Janeiro to Miami Miami to Miami San Francisco to Vancouver Seattle to Seattle Seattle to Seattle Seattle to Seattle New York to Montreal New York to Montreal Miami to Miami Miami to Los Angeles Los Angeles to Los Angeles Miami to Rio de Janeiro Buenos Aires to Lima Miami to Miami San Francisco to Vancouver 21 days | February 7 22 days | March 11 10 days | April 2 10 days | May 10 7 days | June 9 7 days | July 8 7 days | August 4 12 days | September 18 10 days | October 12 12 days | November 5 16 days | December 22 10 days | January 7 23 days | February 2 22 days | March 7 10 days | April 14 11 days | May 10 Radiant Rhythms Atlantic Charms Majesty of Alaska Glacial Explorer Majestic Beauty Glaciers & Gardens Fall Medley Landmarks & Lighthouses Caribbean Charisma Panama Enchantment Ancient Legends Palms in Paradise Buenos Aires to Rio de Janeiro Miami to Miami Vancouver to Seattle Seattle to Seattle Seattle to Seattle Seattle to Vancouver Montreal to New York Montreal to Miami Miami to Miami Los Angeles to -
Estrategia Nacional De Glaciares Fundamentos
REPÚBLICA DE CHILE MINISTERIO DE OBRAS PÚBLICAS DIRECCIÓN GENERAL DE AGUAS ESTRATEGIA NACIONAL DE GLACIARES FUNDAMENTOS REALIZADO POR: CENTRO DE ESTUDIOS CIENTÍFICOS - CECS S.I.T. N° 205 Santiago, Diciembre 2009 MINISTERIO DE OBRAS PÚBLICAS Ministro de Obras Públicas Ingeniero Civil Industrial Sr. Sergio Bitar Ch. Director General de Aguas Abogado Sr. Rodrigo Weisner L. Jefe Unidad de Glaciología y Nieves Geógrafo Sr. Gonzalo Barcaza S. Inspectores Fiscales Ingeniero Civil Sr. Fernando Escobar C. Ingeniero Civil Sr. Cristóbal Cox O. CENTRO DE ESTUDIOS CIENTÍFICOS Jefe de Proyecto Dr. Andrés Rivera (Glaciólogo) Profesionales MSc Francisca Bown (Glacióloga) Claudio Bravo (Geógrafo) Daniela Carrión (Licenciada en Geografía) Dr. Gino Casassa (Glaciólogo) Claudia Flores (Secretaria) Dra. Paulina López (Hidroglacióloga) MSc Camilo Rada (Geofísico) Sebastián Vivero (Licenciado en Geografía) Pablo Zenteno (Geógrafo) Índice 1. INTRODUCCIÓN ..................................................................................................................6 1.1. ORIGEN DEL PROYECTO Y TRATAMIENTO GENERAL DEL TEMA .............................................6 1.2. HIPÓTESIS DE TRABAJO .........................................................................................................6 1.3. OBJETIVOS ............................................................................................................................7 1.4. ¿P OR QUÉ UNA ESTRATEGIA NACIONAL DE GLACIARES ? .....................................................8 2. GLACIARES -
Glacier Changes in the Semi-Arid Huasco Valley, Chile, Between 1986 and 2016
geosciences Article Glacier Changes in the Semi-Arid Huasco Valley, Chile, between 1986 and 2016 Katharina Hess 1,*, Susanne Schmidt 2,* , Marcus Nüsser 1,2 , Carina Zang 1 and Juliane Dame 1,2 1 Heidelberg Center for the Environment (HCE), Heidelberg University, 69120 Heidelberg, Germany; [email protected] (M.N.); [email protected] (C.Z.); [email protected] (J.D.) 2 Department of Geography, South Asia Institute (SAI), Heidelberg University, 69115 Heidelberg, Germany * Correspondence: [email protected] (K.H.); [email protected] (S.S.); Tel.: +49-(0)6221-54-15240 (S.S.) Received: 30 July 2020; Accepted: 26 October 2020; Published: 29 October 2020 Abstract: In the semi-arid and arid regions of the Chilean Andes, meltwater from the cryosphere is a key resource for the local economy and population. In this setting, climate change and economic activities foster water scarcity and resource conflicts. The study presents a detailed glacier and rock glacier inventory for the Huasco valley (28–29◦ S) in northern Chile based on a multi-temporal remote sensing approach. The results indicate a glacier-covered area of 16.35 3.06 km2 (n = 167) and, ± additionally, 50 rock glaciers covering an area of about 8.6 km2 in 2016. About 81% of the ice-bodies are smaller than 0.1 km2, and only four glaciers are larger than 1 km2. The change analysis reveals a more or less stable period between 1986 and 2000 and a drastic decline in the glacier-covered area by about 35% between 2000 and 2016. -
Trans-Andean Passage of Migrating Arctic Terns Over Patagonia
Duffy et al.: Arctic Tern migration over Patagonia 155 TRANS-ANDEAN PASSAGE OF MIGRATING ARCTIC TERNS OVER PATAGONIA DAVID CAMERON DUFFY1, ALY MCKNIGHT2 & DAVID B. IRONS2 1Pacific Cooperative Studies Unit, Department of Botany, University of Hawaii, 3190 Maile Way, Honolulu, HI 96822, USA ([email protected]) 21011 E. Tudor Rd. Migratory Bird Management, US Fish and Wildlife Service, Anchorage, AK 99503, USA Received 19 April 2013; accepted 17 June 2013 SUMMARY DUFFY, D.C., MCKNIGHT, A. & IRONS, D.B. 2013. Trans-Andean passage of migrating Arctic Terns over Patagonia. Marine Ornithology 41: 155–159. We assessed migration routes of Arctic Terns Sterna paradisaea breeding in Prince William Sound, Alaska, by deploying geolocator tags on 20 individuals in June 2007, recovering six upon their return in 2008 and 2009. The terns migrated south along the North and South American coastlines. As they neared the southern end of the Humboldt Current upwelling off Chile, they stopped their over-water migration and turned eastward, crossing the Andes to reach rich foraging areas in the South Atlantic Ocean off the coast of Argentina. Challenging sea and weather conditions, rather than paucity of food, likely deterred further movement south along the Chilean coast. Key words: Alaska, Arctic Tern, Andes, Argentina, Chile, geolocation, Humboldt Current, migration, Patagonia, Sterna paradisaea INTRODUCTION the tags’ view of the horizon and displaced positions calculated during the crossing, we defined the crossing distance as the distance Arctic Terns Sterna paradisaea have the longest known migration between the last Pacific point and the first Atlantic point, ignoring of any bird species, from the Arctic to the Antarctic, covering up intermediate points occurring on land. -
Introduction
Limarí River Basin Study Phase I – Current conditions, history and plans Authors: Alexandra Nauditt, Nicole Kretschmer and Lars Ribbe Introduction For the SERIDAS project, the semiarid Central Chilean region was selected as its water bodies are highly modified to irrigate intensive agriculture and water resources availability is expected to decrease due to climate change triggered temperature rise and seasonal precipitation shifts. The drought prone agricultural areas are supplied with water from mountainous headwater catchments. Stream runoff in Central Chile mainly consists of snow melt, ablation of glaciers and rock glaciers and other melting permafrost and ground ice (Arenson&Jakob 2010) which are especially vulnerable to climatic changes (Barnet et al., 2005; Bates et al., 2008). The following figure shows the Central Chilean semiarid catchments from Copiapo, Huasco, Elqui, Limarí, Choapa, Petorca-La Ligua, Aconcagua and Maipo and their snow cover after a wet winter year 2002 and a dry year 2006 respectively: Figure 1: Snow cover in a dry and in a wet year in Central Chile The Limarí River basin was selected as an example to describe the regional characteristics: 1. Physical and human geography 1.1 River and tributaries The Limarí River is formed by the confluence of the Grande and Hurtado rivers. The Grande River drains the central parts of the basin (Commune of Monte Patria), whereas the Hurtado drains the northern part (Commune of Hurtado). Both rivers originate in the Andean Cordillera, with headwaters at 4,500 m.a.s.l., thus snowfall makes an important contribution to their discharge. The Hurtado River does not have any important tributaries, and its course is intercepted by the Recoleta dam.