Earth and Water Resources and Hazards in Central America
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Your Cruise Secrets of Central America
Secrets of Central America From 1/4/2022 From Colón Ship: LE CHAMPLAIN to 1/14/2022 to Puerto Caldera PONANT takes you to discover Panama and Costa Rica with an 11-day expedition cruise. A circuit of great beauty around the isthmus of Panama, a link between two continents, which concentrates a biodiversity that is unique in the world, from the Atlantic Ocean to the Pacific Ocean between dream islands, natural reserves and encounters with the fascinating local communities. Your journey in Central America will begin with an all-new port of call in the magnificent Portobelo Bay, between mangroves, tropical forest and discovery of the Congo culture. The fortifications of this former gateway to the New World are a UNESCO World Heritage Site. You will then discover the golden sand and crystal-clear waters of the coral islets of the San Blas Islands. The Kuna live among the palm trees and pirogues; this people perpetuates, among other things, the traditional craft of molas, weaved textiles in sparkling colours. After sailing through the world-famous Panama Canal, your ship will stop in the Pearl Islands, which nestle in the Gulf of Panama. Your ship will then head for the magnificent Darien National Park in Panama. This little corner of paradise is a UNESCO World Heritage site and home to remarkable plants and wildlife. Sandy beaches, rocky coastlines, mangroves, swamps and tropical rainforests vie with each other for beauty and offer a feast for photographers. This will also be the occasion for meeting the astonishing semi-nomadic Emberas community. In Casa Orquideas, in the heart of a region that is home to Costa Rica’s most beautiful beaches, you will have the chance to visit a botanical garden with a sublime collection of tropical flowers. -
Tinamiformes – Falconiformes
LIST OF THE 2,008 BIRD SPECIES (WITH SCIENTIFIC AND ENGLISH NAMES) KNOWN FROM THE A.O.U. CHECK-LIST AREA. Notes: "(A)" = accidental/casualin A.O.U. area; "(H)" -- recordedin A.O.U. area only from Hawaii; "(I)" = introducedinto A.O.U. area; "(N)" = has not bred in A.O.U. area but occursregularly as nonbreedingvisitor; "?" precedingname = extinct. TINAMIFORMES TINAMIDAE Tinamus major Great Tinamou. Nothocercusbonapartei Highland Tinamou. Crypturellus soui Little Tinamou. Crypturelluscinnamomeus Thicket Tinamou. Crypturellusboucardi Slaty-breastedTinamou. Crypturellus kerriae Choco Tinamou. GAVIIFORMES GAVIIDAE Gavia stellata Red-throated Loon. Gavia arctica Arctic Loon. Gavia pacifica Pacific Loon. Gavia immer Common Loon. Gavia adamsii Yellow-billed Loon. PODICIPEDIFORMES PODICIPEDIDAE Tachybaptusdominicus Least Grebe. Podilymbuspodiceps Pied-billed Grebe. ?Podilymbusgigas Atitlan Grebe. Podicepsauritus Horned Grebe. Podicepsgrisegena Red-neckedGrebe. Podicepsnigricollis Eared Grebe. Aechmophorusoccidentalis Western Grebe. Aechmophorusclarkii Clark's Grebe. PROCELLARIIFORMES DIOMEDEIDAE Thalassarchechlororhynchos Yellow-nosed Albatross. (A) Thalassarchecauta Shy Albatross.(A) Thalassarchemelanophris Black-browed Albatross. (A) Phoebetriapalpebrata Light-mantled Albatross. (A) Diomedea exulans WanderingAlbatross. (A) Phoebastriaimmutabilis Laysan Albatross. Phoebastrianigripes Black-lootedAlbatross. Phoebastriaalbatrus Short-tailedAlbatross. (N) PROCELLARIIDAE Fulmarus glacialis Northern Fulmar. Pterodroma neglecta KermadecPetrel. (A) Pterodroma -
Downloaded 09/25/21 09:51 PM UTC 800 MONTHLY WEATHER REVIEW VOLUME 131
MAY 2003 MAPES ET AL. 799 Diurnal Patterns of Rainfall in Northwestern South America. Part I: Observations and Context BRIAN E. MAPES NOAA±CIRES Climate Diagnostics Center, Boulder, Colorado THOMAS T. W ARNER AND MEI XU Program in Atmospheric and Oceanic Sciences, University of Colorado, and Research Applications Program, National Center for Atmospheric Research,* Boulder, Colorado ANDREW J. NEGRI NASA Goddard Space Flight Center, Laboratory for Atmospheres, Greenbelt, Maryland (Manuscript received 10 January 2002, in ®nal form 29 August 2002) ABSTRACT One of the rainiest areas on earth, the Panama Bight and Paci®c (western) littoral of Colombia, is the focal point for a regional modeling study utilizing the ®fth-generation Pennsylvania State University±NCAR Mesoscale Model (MM5) with nested grids. In this ®rst of three parts, the observed climatology of the region is presented. The seasonal march of rainfall has a northwest±southeast axis, with western Colombia near the center, receiving rain throughout the year. This study focuses on the August±September season. The diurnal cycle of rainfall over land exhibits an afternoon maximum over most of South and Central America, typically composed of relatively small convective cloud systems. Over some large valleys in the Andes, and over Lake Maracaibo, a nocturnal maximum of rainfall is observed. A strong night/morning maximum of rainfall prevails over the coastal ocean, propagating offshore and westward with time. This offshore convection often takes the form of mesoscale convective systems with sizes comparable to the region's coastal concavities and other geographical features. The 10-day period of these model studies (28 August±7 September 1998) is shown to be a period of unusually active weather, but with a time-mean rainfall pattern similar to longer-term climatology. -
Earthquake-Induced Landslides in Central America
Engineering Geology 63 (2002) 189–220 www.elsevier.com/locate/enggeo Earthquake-induced landslides in Central America Julian J. Bommer a,*, Carlos E. Rodrı´guez b,1 aDepartment of Civil and Environmental Engineering, Imperial College of Science, Technology and Medicine, Imperial College Road, London SW7 2BU, UK bFacultad de Ingenierı´a, Universidad Nacional de Colombia, Santafe´ de Bogota´, Colombia Received 30 August 2000; accepted 18 June 2001 Abstract Central America is a region of high seismic activity and the impact of destructive earthquakes is often aggravated by the triggering of landslides. Data are presented for earthquake-triggered landslides in the region and their characteristics are compared with global relationships between the area of landsliding and earthquake magnitude. We find that the areas affected by landslides are similar to other parts of the world but in certain parts of Central America, the numbers of slides are disproportionate for the size of the earthquakes. We also find that there are important differences between the characteristics of landslides in different parts of the Central American isthmus, soil falls and slides in steep slopes in volcanic soils predominate in Guatemala and El Salvador, whereas extensive translational slides in lateritic soils on large slopes are the principal hazard in Costa Rica and Panama. Methods for assessing landslide hazards, considering both rainfall and earthquakes as triggering mechanisms, developed in Costa Rica appear not to be suitable for direct application in the northern countries of the isthmus, for which modified approaches are required. D 2002 Elsevier Science B.V. All rights reserved. Keywords: Landslides; Earthquakes; Central America; Landslide hazard assessment; Volcanic soils 1. -
Synopsis Sheets CANAL DE PANAMA UK
Synopsis sheets Rivers of the World THE PANAMA CANAL Initiatives pour l’Avenir des Grands Fleuves The Panama Canal 80 km long, the Panama Canal links the Pacific and Atlantic Oceans, forming a faster transoceanic route for merchant shipping than by passing via Cape Horn, at the southernmost tip of South America. A strategic hub for the world’s maritime trade, 15,000 ships pass through it every year. In 2016, a huge project of Canal’s enlargement was completed to double its capacity and accommodate the new generation ships, larger and longer, the Post Panamax. Now it has to face new challenges: competing projects are emerging and new shipping routes can be opened that would reduce the supremacy of the Panama Canal. A strategic route The origins Océan Atlantique The first attempt to build the canal dates back to 1880. France entrusted Ferdinand de Lesseps with the responsibility of its design and amassed considerable funds. However, the technical difficulties and above all a major financial scandal revealed in 1889 led to the bankruptcy of the Compagnie Universelle du Canal Inter-océanique du Panamá. The new Panama Canal Company took over but met the same fate, and in 1903 the treaty of Hay- Bunau-Varilla officialised the transfer of the operating and building rights to the canal to the United States. Built under the direction of G.W. Goethals, at the head of the U.S. Army Corps of Engineers, the canal opened in 1914 and was finally handed over to Panama in 1999 by virtue of the Torrijos-Carter Treaty. -
Fishes-Of-The-Salish-Sea-Pp18.Pdf
NOAA Professional Paper NMFS 18 Fishes of the Salish Sea: a compilation and distributional analysis Theodore W. Pietsch James W. Orr September 2015 U.S. Department of Commerce NOAA Professional Penny Pritzker Secretary of Commerce Papers NMFS National Oceanic and Atmospheric Administration Kathryn D. Sullivan Scientifi c Editor Administrator Richard Langton National Marine Fisheries Service National Marine Northeast Fisheries Science Center Fisheries Service Maine Field Station Eileen Sobeck 17 Godfrey Drive, Suite 1 Assistant Administrator Orono, Maine 04473 for Fisheries Associate Editor Kathryn Dennis National Marine Fisheries Service Offi ce of Science and Technology Fisheries Research and Monitoring Division 1845 Wasp Blvd., Bldg. 178 Honolulu, Hawaii 96818 Managing Editor Shelley Arenas National Marine Fisheries Service Scientifi c Publications Offi ce 7600 Sand Point Way NE Seattle, Washington 98115 Editorial Committee Ann C. Matarese National Marine Fisheries Service James W. Orr National Marine Fisheries Service - The NOAA Professional Paper NMFS (ISSN 1931-4590) series is published by the Scientifi c Publications Offi ce, National Marine Fisheries Service, The NOAA Professional Paper NMFS series carries peer-reviewed, lengthy original NOAA, 7600 Sand Point Way NE, research reports, taxonomic keys, species synopses, fl ora and fauna studies, and data- Seattle, WA 98115. intensive reports on investigations in fi shery science, engineering, and economics. The Secretary of Commerce has Copies of the NOAA Professional Paper NMFS series are available free in limited determined that the publication of numbers to government agencies, both federal and state. They are also available in this series is necessary in the transac- exchange for other scientifi c and technical publications in the marine sciences. -
Table 2. Geographic Areas, and Biography
Table 2. Geographic Areas, and Biography The following numbers are never used alone, but may be used as required (either directly when so noted or through the interposition of notation 09 from Table 1) with any number from the schedules, e.g., public libraries (027.4) in Japan (—52 in this table): 027.452; railroad transportation (385) in Brazil (—81 in this table): 385.0981. They may also be used when so noted with numbers from other tables, e.g., notation 025 from Table 1. When adding to a number from the schedules, always insert a decimal point between the third and fourth digits of the complete number SUMMARY —001–009 Standard subdivisions —1 Areas, regions, places in general; oceans and seas —2 Biography —3 Ancient world —4 Europe —5 Asia —6 Africa —7 North America —8 South America —9 Australasia, Pacific Ocean islands, Atlantic Ocean islands, Arctic islands, Antarctica, extraterrestrial worlds —001–008 Standard subdivisions —009 History If “history” or “historical” appears in the heading for the number to which notation 009 could be added, this notation is redundant and should not be used —[009 01–009 05] Historical periods Do not use; class in base number —[009 1–009 9] Geographic treatment and biography Do not use; class in —1–9 —1 Areas, regions, places in general; oceans and seas Not limited by continent, country, locality Class biography regardless of area, region, place in —2; class specific continents, countries, localities in —3–9 > —11–17 Zonal, physiographic, socioeconomic regions Unless other instructions are given, class -
Caribbean and Pacific Coastal Marine System
C. Birkeland Caribbean and Pacific Coastal marine system: similarities and differences A goal that scientists set for themselves is to find general Magnitude of rate of nutrient input principles with broad relevance and applicability. This devotion to generality can lead to serious error. For A primary factor in bringing about differences in the example, the harvesting techniques that are very successful functional organization of coral-reef communities in on the temperate Great Plains may not be applicable to the different geographic regions is the magnitude of the rate of Amazonian rain forest. In the rain forest, where the nutrient input and the degree to which the input nutrients are bound into the biomass and are sparse in the is concentrated into pulses. John Ryther of Woods Hole soil, pruning may be a more workable pattern of resource Oceanographic Institute calculated that over half the world utilization than reaping. Reaping works well on the prairie, fishery catch comes from upwelling regions, although the but is likely to do extensive, practically irreparable, regions of upwelling occupy only about one-tenth of 1% damage to the tropical rain forest system. of the ocean surface. Coral-reef ecosystems are even more productive than are regions of upwelling in terms of rates Differences of gross primary productivity per unit area. Relatively pristine coral reefs maintain a large standing-stock Functional differences exist within types of tropical biomass of fish. Yet coral reefs are particularly vulnerable coastal ecosystems among different regions of the world to overexploitation while the regions of upwelling are that are analogous to the tropical rainforest/ temperate heavily exploited year after year. -
Costa Rica and Panama Canal Expedition
COSTA RICA AND PANAMA CANAL EXPEDITION Immerse yourself in the remarkable coastlines of Costa Rica and Panama. Costa Rica (‘rich coast’) is one of the most biodiverse regions on earth. Explore the lush jungle, tropical rainforest and inviting turquoise waters surrounded by a truly outstanding variety of wildlife, brilliant birds and flamboyant flora. In Panama, discover pristine coral reefs, meet the Emberá Mogue indigenous community and cross the historic Panama Canal. ITINERARY Day 1 San Jose Upon your arrival at San José International Airport, use the complimentary airport transfer service provided by Double Tree Cariari by Hilton and transfer to the hotel. The hotel offers a free airport shuttle service departing every hour starting at 4.30 am until 10.30 pm. As you exit the international terminal, the pick-up point for the transfer is located in front of El Malinche restaurant. Upon check-in, please remind reception staff to provide you with your Aurora Expeditions cabin tags. Please fill out the luggage tags clearly, showing your name and cabin number so that we can deliver your luggage to your cabin ahead of your arrival. Enjoy the remainder of the day at leisure. Accommodation: Double Tree by Hilton Hotel Cariari (or similar) Day 2 Puerto Caldera, embark Greg Mortimer 0800 945 3327 (within New Zealand) | +64 (0) 3 365 1355 | 1800 107 715 (within Australia) [email protected] | wildearth-travel.com After a leisurely buffet breakfast, transfer to Puerto Caldera (2-hours) where Days 5-6 Osa Peninsula & Golfo Dulce your vessel awaits. After boarding, you’ll have time to settle into your cabin before participating in important safety briefings. -
An Integrated Structural and GPS Study of the Jalpatagua Fault, Southeastern Guatemala
Research Paper GEOSPHERE An integrated structural and GPS study of the Jalpatagua fault, southeastern Guatemala 1 1 2 1 1 1,3 4 4 GEOSPHERE, v. 17, no. 1 Bridget Garnier , Basil Tikoff , Omar Flores , Brian Jicha , Charles DeMets , Beatriz Cosenza-Muralles , Douglas Hernandez , Griselda Marroquin , Luis Mixco4, and Walter Hernandez4 https://doi.org/10.1130/GES02243.1 1Department of Geoscience, University of Wisconsin–Madison, 1215 West Dayton St., Madison, Wisconsin 53706, USA 2Centro de Estudios Superiores de Energías y Minas–Facultad de Ingeniería, Universidad de San Carlos, Ciudad Universitaria, Zona 12, Edificio T-1, tercer nivel, Ciudad de Guatemala 01012, Guatemala 3Instuto de Invesgación en Ciencias Físicas y Matemácas, Escuela de Ciencias Físicas y Matemácas, Universidad de San Carlos, Ciudad Universitaria, Zona 12, Edificio T-1, segundo nivel, Ciudad 13 figures; 6 tables; 1 supplemental file de Guatemala, Guatemala 4Dirección del Observatorio, Ministerio de Medio Ambiente y Recursos Naturales, Km. 5½ carretera a Santa Tecla, colonio y calle Las Mercedes, San Salvador, El Salvador CORRESPONDENCE: [email protected] ABSTRACT ■ INTRODUCTION Guzmán-Speziale et al., 2005; Lyon-Caen et al., 2006; CITATION: Garnier, B., Tikoff, B., Flores, O., Jicha, B., DeMets, C., Cosenza-Muralles, B., Hernandez, D., Franco et al., 2012). The dextral forearc fault system Marroquin, G., Mixco, L., and Hernandez, W., 2021, An The Jalpatagua fault in Guatemala accommodates Moving forearc slivers typically result from is the widest in Nicaragua, with NE-oriented sinistral integrated structural and GPS study of the Jalpatagua dextral movement of the Central America forearc. We strain partitioning due to oblique convergence faults that suggest bookshelf faulting may accom- fault, south eastern Guatemala: Geosphere, v. -
The Conservation Status of North American, Central American, and Caribbean Chondrichthyans the Conservation Status Of
The Conservation Status of North American, Central American, and Caribbean Chondrichthyans The Conservation Status of Edited by The Conservation Status of North American, Central and Caribbean Chondrichthyans North American, Central American, Peter M. Kyne, John K. Carlson, David A. Ebert, Sonja V. Fordham, Joseph J. Bizzarro, Rachel T. Graham, David W. Kulka, Emily E. Tewes, Lucy R. Harrison and Nicholas K. Dulvy L.R. Harrison and N.K. Dulvy E.E. Tewes, Kulka, D.W. Graham, R.T. Bizzarro, J.J. Fordham, Ebert, S.V. Carlson, D.A. J.K. Kyne, P.M. Edited by and Caribbean Chondrichthyans Executive Summary This report from the IUCN Shark Specialist Group includes the first compilation of conservation status assessments for the 282 chondrichthyan species (sharks, rays, and chimaeras) recorded from North American, Central American, and Caribbean waters. The status and needs of those species assessed against the IUCN Red List of Threatened Species criteria as threatened (Critically Endangered, Endangered, and Vulnerable) are highlighted. An overview of regional issues and a discussion of current and future management measures are also presented. A primary aim of the report is to inform the development of chondrichthyan research, conservation, and management priorities for the North American, Central American, and Caribbean region. Results show that 13.5% of chondrichthyans occurring in the region qualify for one of the three threatened categories. These species face an extremely high risk of extinction in the wild (Critically Endangered; 1.4%), a very high risk of extinction in the wild (Endangered; 1.8%), or a high risk of extinction in the wild (Vulnerable; 10.3%). -
Pacific Offshore Record of Plinian Arc Volcanism in Central America: 2
Article Geochemistry 3 Volume 9, Number 2 Geophysics 8 February 2008 Q02S02, doi:10.1029/2007GC001791 GeosystemsG G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Pacific offshore record of plinian arc volcanism in Central America: 2. Tephra volumes and erupted masses S. Kutterolf SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany ([email protected]) A. Freundt SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany W. Pere´z SFB574 at Kiel University/IFM-GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany [1] Sediment gravity cores collected from the Pacific seafloor offshore Central America contain numerous distal ash layers from plinian-type eruptions at the Central American Volcanic Arc dating back to more than 200 ka. In part 1 of this contribution we have correlated many of those ash layers between cores and with 26 tephras on land. The marine ash layers cover areas of up to 106 km2 in the Pacific Ocean and represent a major fraction (60–90%) of the erupted tephra volumes because the Pacific coast lies within a few tens of kilometers downwind from the volcanic arc. Combining our own mapping efforts on land and published mapping results with our marine data yields erupted volumes of all major tephras along the arc that range from 1 to 420 km3. Recalculated to erupted magma mass, the widespread tephras account for 65% of the total magma output at the arc.