Chapter 3: Climates of the Earth
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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 -
Midnight Sun and Northern Lights Name
volume 3 Midnight Sun and issue 5 Northern Lights It’s black, which absorbs the sun’s warmth. In fact, polar midnight, bears feel hot if the temperature rises above freezing. but the sun The polar nights are long and dark, but sometimes is shining there’s a light show in the sky. The northern lights, which brightly. Where are called the aurora, are often green or pink. They seem are you? You’re to wave and dance in the sky. Auroras are caused by gas in the Arctic, particles that were thrown off by the sun. These particles near the North collide in Earth’s atmosphere and make a beautiful show. Pole. During Few people live in the Arctic because it’s so cold, but the arctic Canada, Greenland, Norway, Iceland, and Russia are summer, the good places to see the midnight sun and the aurora. In ©2010 by Asbjørn Floden in Flickr. Some rights reserved http://creativecommons.org/licenses/by-nc/2.0/deed.en sun doesn’t fact, Norway is often called the Land of the Midnight set for months. Instead, it goes around the horizon. You Sun. could read outside at midnight. As you travel south The temperature stays warm, too, although not as from the North Pole, warm as where you live. The average temperature in there is less midnight sun the summer near the North Pole is about 32 degrees, and fewer northern lights. or freezing. That may sound cold to you, but it’s warm It gets warmer, too. Soon, in the Arctic. -
Midnight Sun, Part II by PA Lassiter
Midnight Sun, Part II by PA Lassiter . N.B. These chapters are based on characters created by Stephenie Meyer in Twilight, the novel. The title used here, Midnight Sun, some of the chapter titles, and all the non-interior dialogue between Edward and Bella are copyright Stephenie Meyer. The first half of Ms. Meyer’s rough-draft novel, of which this is a continuation, can be found at her website here: http://www.stepheniemeyer.com/pdf/midnightsun_partial_draft4.pdf 12. COMPLICATIONSPart B It was well after midnight when I found myself slipping through Bella’s window. This was becoming a habit that, in the light of day, I knew I should attempt to curb. But after nighttime fell and I had huntedfor though these visits might be irresponsible, I was determined they not be recklessall of my resolve quickly faded. There she lay, the sheet and blanket coiled around her restless body, her feet bound up outside the covers. I inhaled deeply through my nose, welcoming the searing pain that coursed down my throat. As always, Bella’s bedroom was warm and humid and saturated with her scent. Venom flowed into my mouth and my muscles tensed in readiness. But for what? Could I ever train my body to give up this devilish reaction to my beloved’s smell? I feared not. Cautiously, I held my breath and moved to her bedside. I untangled the bedclothes and spread them carefully over her again. She twitched suddenly, her legs scissoring as she rolled to her other side. I froze. “Edward,” she breathed. -
CERI Commodity Report — Natural Gas
June-July 2014 CERI Commodity Report — Natural Gas Hydrocarbon Gold under the Midnight Sun? exploration efforts will continue until 2018, with Jon Rozhon production potentially starting soon thereafter. For all practical intents and purposes, the Western Figure 1: Yukon’s Eight Hydrocarbons Basins Canadian Sedimentary Basin (WCSB) ends abruptly at the 60th parallel, along the border between British Columbia and the Yukon Territory. North of 60° there has been little exploration for oil and gas for over 30 years. South of 60°, especially in areas such as the Montney basin, oil and gas activity is now as busy as it has ever been. The difference is especially visible from the air: within Alberta and British Columbia you can see cut-lines crisscrossing the landscape; flying over the Yukon – the renowned Land of the Midnight Sun – the wilderness to this day still appears almost untouched. Of course, the geologic reality of the situation is that the WCSB extends further north, so there should be significant hydrocarbon resources within the Yukon. Governments know this, E&P companies know this, and so do stakeholders such as First Nations, land owners, and other local residents. Northern Cross Energy, an affiliate of the Chinese National Overseas Oil Corporation (CNOOC), is one company that has been doing much work in the Yukon’s Eagle Plain basin. In 2011, boosted with a cash infusion from CNOOC, the company was granted exploration permits from the Government of Yukon and dedicated a Sources: Government of Yukon, CERI total of $22 million in work commitments. Since then, Northern Cross has spent more than $100 million in What will Northern Cross do with any discovered oil and Eagle Plain, and though the company states results of its gas resources? Chinese State-Owned Enterprises such as work “are still being analyzed”, their continued and CNOOC are busy throughout the world diversifying their 1 resource holdings with a view to ensuring the country’s increasing funding indicates cause for optimism. -
Patagonia Travel Guide
THE ESSENTIAL PATAGONIA TRAVEL GUIDE S EA T TLE . RIO D E J A NEIRO . BUENOS AIRES . LIMA . STUTTGART w w w.So u t h A mer i c a.t r av e l A WORD FROM THE FOUNDERS SouthAmerica.travel is proud of its energetic Team of travel experts. Our Travel Consultants come from around the world, have traveled extensively throughout South America and work “at the source" from our operations headquarters in Rio de Janeiro, Lima and Buenos Aires, and at our flagship office in Seattle. We are passionate about South America Travel, and we're happy to share with you our favorite Buenos Aires restaurants, our insider's tips for Machu Picchu, or our secret colonial gems of Brazil, and anything else you’re eager to know. The idea to create SouthAmerica.travel first came to Co-Founders Juergen Keller and Bradley Nehring while traveling through Brazil's Amazon Rainforest. The two noticed few international travelers, and those they did meet had struggled to arrange the trip by themselves. Expertise in custom travel planning to Brazil was scarce to nonexistent. This inspired the duo to start their own travel business to fill this void and help travelers plan great trips to Brazil, and later all South America. With five offices on three continents, as well as local telephone numbers in 88 countries worldwide, the SouthAmerica.travel Team has helped thousands of travelers fulfill their unique dream of discovering the marvelous and diverse continent of South America. Where will your dreams take you? Let's start planning now… “Our goal is to create memories that -
Intertextuality, Masculinity, and Desire in the Twilight Series
Virtue as Adventure and Excess: Intertextuality, Masculinity, and Desire in the Twilight Series By Claudia Lindén Abstract The vampire is still primarily a literary figure. The vampires we have seen on TV and cinema in recent years are all based on literary models. The vampire is at the same time a popular cultural icon and a figure that, especially women writers, use to problematize gender, sexuality and power. As a vampire story the Twilight se- ries both produces and problematizes norms in regard to gender, class and ethnici- ty. As the main romantic character in Twilight, Edward Cullen becomes interest- ing both as a vampire of our time and as a man. In a similar way as in the 19th century novel the terms of relationship are negotiated and like his namesake Ed- ward Rochester, Edward Cullen has to change in important ways for the “happy ending” to take place. In spite of a strong interest in sexuality and gender norms in relation to vampires very few studies have focused exclusively on masculinity. This article examines the construction of masculinity in relation to vampirism in the Twilight series. It offers an interpretation of Stephenie Meyer’s novels and the character of Edward as part of a broader field of feminist (re-)uses of the vampire in modern literature with its roots in the literary tradition from Austen and the Brontë-sisters as well as from classic Gothic fiction. Keywords: Twilight Series, Stephenie Meyer, masculinity, vampires, were- wolves, Midnight Sun, Jane Austen, Pride and Prejudice, Charlotte Brontë, Jane Eyre, feminist theory, queer theory, gothic. -
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. -
The Idea of the North Transcript
The Idea of the North Transcript Date: Friday, 19 June 2009 - 12:00AM Location: Barnard's Inn Hall The Idea of the North City of London Festival 2009 by Peter Davidson 19 June 2009 Snowlight and Evening: The Fall of Northern Light If I were at home in Aberdeenshire in the evening of a day so near to midsummer as today, the daylight would be undiminished until about ten. It would feel as if time itself were stretching and slowing in the endless northern evening. It is difficult to exaggerate the way in which the presence and absence of light governs the life of the north. On such an evening it is hard to stay in the house, hard to waste the daylight, because in the north you are always aware of the dark biding its time. In a week or two, the prodigious light will already be dwindling: in the words of that splendidly miserable old sod Professor Housman The dark Has passed its nadir and begun to climb. We would go out just as, at last, the sun begins to go down. Out into the cooling air and the level light, into the scents of the clove pinks in the bed beside the greenhouse. Viridian shadows are beginning to deepen under the trees on the lawn. We walk away from the house, between the beech hedges which lead out of the clearing at the end of the garden, and down the broad steps into the wood. A grass path stretches away to the north of us, into the sunlight which still sends its last low rays over the stream and amongst the trunks of the trees. -
Detecting Glacier Surface Motion by Optical Flow
Detecting Glacier Surface Motion by Optical Flow M.G. Lenzano, E. Lannutti, C. Toth, A. Rivera, and L. Lenzano Abstract In this study, we assessed the feasibility of using optical flow, objects, the temporal aspects of the mapping are equally in particular, large displacement optical flow (LDOF) method important, and therefore, the revisit time of satellite plat- as a possible solution to obtain surface movement data to forms may present some disadvantages. A permanent sensor derive ice flow velocities in a glacier. Tests were carried installation could offer unprecedented temporal resolution out at the Viedma Glacier, located at the South Patagonia and observation capabilities (Toth and Jóźków, 2016), and us- Icefield, Argentina, where terrestrial monoscopic image ing time-lapse imagery provides a viable approach to glacier sequences were acquired by a calibrated camera from April change detection (Harrison, 1992; Hashimoto et al., 2009; Ahn 2014 until April 2016. As for preprocessing, the Correlated and Box, 2010; Maas et al, 2010; Rivera et al., 2012b; Daniel- Analysis method was implemented to avoid and minimize son and Sharp, 2013; Lenzano et al., 2014). errors due to the measurable changes in lighting, shad- The dynamics of glaciers has noticeably changed due to ows, clouds, and snow. The results show a flow field with a global warming during in the late 20th and 21st centuries (Oer- maximum surface velocity value of 3.5 m/d. The errors were lemans, 2005; Bolch et al., 2012), and thus, to properly assess minimized by averaging the image sequence results based and monitor their dynamics requires the detailed mapping on seasons, in which the Total Error Reconstruction yielded of surface velocities and changes in geometry (Howat et al., fairly good mean accuracy (0.36 m/d). -
Latitude/Longitude of the Exact Opposite Place LONGITUDE on Earth to Sydney, Australia, 33° 55‘ S, 151° 17‘ E 90° N 180° Sydney LATITUDE 151° 17’ E
GEO 101, January 16, 2014, Latitude and Longitude Finding your way … How geographers locate where things are… Most common locational system Best reference points are ends of rotational axis Latitude and Longitude Measures angular distance in degrees, not distance in miles or km Basic geometry: circle has 360 degrees Babylonians (≈600 BC) chose the number 360. The reason is that their number system was based on 60. To compare, we base our number system on 10. For us, 10 is a nice, round number and we find it very convenient to count in multiples of 10. But the Babylonians liked 60. LATITUDE Midway between N & S pole is Equator = 0° 90° N 0° 90° S 1 Latitude of Mobile ≈ 30° 42’ N. Parallels of latitude measure the angular distance (degrees) north or south of the Equator. Expressed in degrees, minutes, & seconds 60 minutes in 1 degree 60 seconds in 1 minute The lines themselves run east - west like the rungs on a ladder Find distance in miles between Latitude can be used to approximate Mobile and the Galapagos Islands, distances based on following: which is almost due south of Mobile 360° in a circle Galapagos 0° 10’ S Mobile 30° 42’ N ≈ 25,000 miles around earth 25,000 miles / 360° ≈ 69 miles in 1° Difference 30° 52’ or 30 + 52/60 degrees = 30.87° One degree of latitude always ≈ 69 miles This is true because parallels of latitude 30.87° x 69 mi/degree = 2130 miles stay same distance apart LONGITUDE Arbitrary starting place at Greenwich (London), England 180° = International Date Line East West N P 0° = Prime Meridian 2 One degree of longitude ONLY EQUALS 69 Meridians of longitude measure the miles, at the Equator. -
AAR Chapter 2
Go back to opening screen 9 Chapter 2 Physical/Geographical Characteristics of the Arctic –––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––– Contents 2.2.1. Climate boundaries 2.1. Introduction . 9 On the basis of temperature, the Arctic is defined as the area 2.2. Definitions of the Arctic region . 9 2.2.1. Climate boundaries . 9 north of the 10°C July isotherm, i.e., north of the region 2.2.2. Vegetation boundaries . 9 which has a mean July temperature of 10°C (Figure 2·1) 2.2.3. Marine boundary . 10 (Linell and Tedrow 1981, Stonehouse 1989, Woo and Gre- 2.2.4. Geographical coverage of the AMAP assessment . 10 gor 1992). This isotherm encloses the Arctic Ocean, Green- 2.3. Climate and meteorology . 10 2.3.1. Climate . 10 land, Svalbard, most of Iceland and the northern coasts and 2.3.2. Atmospheric circulation . 11 islands of Russia, Canada and Alaska (Stonehouse 1989, 2.3.3. Meteorological conditions . 11 European Climate Support Network and National Meteoro- 2.3.3.1. Air temperature . 11 2.3.3.2. Ocean temperature . 12 logical Services 1995). In the Atlantic Ocean west of Nor- 2.3.3.3. Precipitation . 12 way, the heat transport of the North Atlantic Current (Gulf 2.3.3.4. Cloud cover . 13 Stream extension) deflects this isotherm northward so that 2.3.3.5. Fog . 13 2.3.3.6. Wind . 13 only the northernmost parts of Scandinavia are included. 2.4. Physical/geographical description of the terrestrial Arctic 13 Cold water and air from the Arctic Ocean Basin in turn 2.4.1. -
Model Research Investigation
National Aeronautics and Space Administration EXPEDITION EARTH AND BEYOND Student Scientist Guidebook Model Research Investigation Written and Developed by: Paige Valderrama Graff, Science Education Specialist, Expedition Earth and Beyond Director Astromaterials Research and Exploration Science (ARES) Directorate ARES Education Program, NASA Johnson Space Center JACOBS - Engineering Science Contract Group (ESCG) Edited and reviewed by the following individuals within the Astromaterials Research and Exploration Science (ARES) Directorate at the NASA Johnson Space Center: Marshalyn Baker, Classroom Teacher Tim McCollum, Classroom Teacher Trevor Graff, Planetary Scientist William Stefanov, Chief Scientist Charles Lindgren, Classroom Teacher Susan Runco, Physical Scientist Michele Mailhot, Classroom Teacher Kim Willis, Principal Geoscientist Additional reviewers include: Joshua Bandfield, Research Assistant Professor Earth and Space Sciences, University of Washington © 2013 Astromaterials Research and Exploration Science (ARES) Education Program. All rights reserved. This document may be freely distributed for non-commercial use only. National Aeronautics and Space Administration EXPEDITION EARTH AND BEYOND Student Scientist Guidebook Model Research Investigation The Expedition Earth and Beyond Student Scientist Guidebook Model Research Investigation is designed to help student researchers model the process of science and conduct a research investigation. This Model Research Investigation includes a complete and thorough research investigation that can be used as an example as you progress through each step of your research. The Table of Contents listed below outlines the steps included in this guidebook. T A B L E O F C O N T E N T S Section Subtitles Page Overview of Section Getting Actively Involved in General overview of Expedition Earth and Beyond and the modeled 9-step NASA Exploration, Discovery 3 - 6 process of science.