The State of the Polar Oceans 2018 : Making Sense of Our Changing World
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North America Other Continents
Arctic Ocean Europe North Asia America Atlantic Ocean Pacific Ocean Africa Pacific Ocean South Indian America Ocean Oceania Southern Ocean Antarctica LAND & WATER • The surface of the Earth is covered by approximately 71% water and 29% land. • It contains 7 continents and 5 oceans. Land Water EARTH’S HEMISPHERES • The planet Earth can be divided into four different sections or hemispheres. The Equator is an imaginary horizontal line (latitude) that divides the earth into the Northern and Southern hemispheres, while the Prime Meridian is the imaginary vertical line (longitude) that divides the earth into the Eastern and Western hemispheres. • North America, Earth’s 3rd largest continent, includes 23 countries. It contains Bermuda, Canada, Mexico, the United States of America, all Caribbean and Central America countries, as well as Greenland, which is the world’s largest island. North West East LOCATION South • The continent of North America is located in both the Northern and Western hemispheres. It is surrounded by the Arctic Ocean in the north, by the Atlantic Ocean in the east, and by the Pacific Ocean in the west. • It measures 24,256,000 sq. km and takes up a little more than 16% of the land on Earth. North America 16% Other Continents 84% • North America has an approximate population of almost 529 million people, which is about 8% of the World’s total population. 92% 8% North America Other Continents • The Atlantic Ocean is the second largest of Earth’s Oceans. It covers about 15% of the Earth’s total surface area and approximately 21% of its water surface area. -
The Antarctic Treaty System And
The Antarctic Treaty System and Law During the first half of the 20th century a series of territorial claims were made to parts of Antarctica, including New Zealand's claim to the Ross Dependency in 1923. These claims created significant international political tension over Antarctica which was compounded by military activities in the region by several nations during the Second World War. These tensions were eased by the International Geophysical Year (IGY) of 1957-58, the first substantial multi-national programme of scientific research in Antarctica. The IGY was pivotal not only in recognising the scientific value of Antarctica, but also in promoting co- operation among nations active in the region. The outstanding success of the IGY led to a series of negotiations to find a solution to the political disputes surrounding the continent. The outcome to these negotiations was the Antarctic Treaty. The Antarctic Treaty The Antarctic Treaty was signed in Washington on 1 December 1959 by the twelve nations that had been active during the IGY (Argentina, Australia, Belgium, Chile, France, Japan, New Zealand, Norway, South Africa, United Kingdom, United States and USSR). It entered into force on 23 June 1961. The Treaty, which applies to all land and ice-shelves south of 60° South latitude, is remarkably short for an international agreement – just 14 articles long. The twelve nations that adopted the Treaty in 1959 recognised that "it is in the interests of all mankind that Antarctica shall continue forever to be used exclusively for peaceful purposes and shall not become the scene or object of international discord". -
Advances in Polar Ecology Series Ed.: D
Advances in Polar Ecology Series Ed.: D. Piepenburg In recent years, the polar regions have received increased scientific and public interest. Both the Arctic and Antarctic have been recognized as key regions in the regulation of the global climate and polar ecosystems have been identified to be particularly susceptible to the ongoing environmental changes. Consequently, the international efforts in polar research have been enhanced considerably, and a wealth of new findings is being produced at a growing rate by the international community of polar researchers. The aim of the book series Advances in Polar Ecology is to foster the progress in the scientific knowledge about the polar and sub-polar regions of both hemispheres by contributing to the fast and wide-ranging dissemination of novel scientific information gained from recent studies of sea, freshwater and land biota among polar researchers, environmental managers and policy makers. Advances in Polar Ecology’s broad ecology- oriented scope encompasses environmental and biological research of both recent and past ecosystems. The Series offers an outlet to publish contributions (monographs, edited works, conference proceedings, etc.) addressing scientific topics that need more comprehensive and in-depth analysis than the length of typical journal articles allow for. These include, but are not limited to, thorough accounts of the current status of active research areas of wide importance that outline promising perspectives for future research. An international editorial board oversees the rigorous peer review that all contributions will be subjected to. Springer books available as Recently published: Printed book Available from springer.com/shop J. Berge, G. Johnsen, J. -
Mitigation of Arctic Tundra Surface Warming by Plant Evapotranspiration: Complete Energy Balance Component Estimation Using LANDSAT Satellite Data
remote sensing Article Mitigation of Arctic Tundra Surface Warming by Plant Evapotranspiration: Complete Energy Balance Component Estimation Using LANDSAT Satellite Data Václav Nedbal 1,* , Kamil Láska 2,3 and Jakub Brom 1 1 Faculty of Agriculture, University of South Bohemia in Ceskˇ é Budˇejovice,Studentská 1668, 370 05 Ceskˇ é Budˇejovice,Czech Republic; [email protected] 2 Department of Geography, Faculty of Science, Masaryk University, Kotláˇrská 2, 611 37 Brno, Czech Republic; [email protected] 3 Centre for Polar Ecology, Faculty of Science, University of South Bohemia in Ceskˇ é Budˇejovice,Na Zlaté stoce 3, 370 05 Ceskˇ é Budˇejovice,Czech Republic * Correspondence: [email protected] Received: 19 September 2020; Accepted: 14 October 2020; Published: 16 October 2020 Abstract: Global climate change is expected to cause a strong temperature increase in the polar regions, accompanied by a reduction in snow cover. Due to a lower albedo, bare ground absorbs more solar energy and its temperature can increase more. Here, we show that vegetation growth in such bare ground areas can efficiently mitigate surface warming in the Arctic, thanks to plant evapotranspiration. In order to establish a comprehensive energy balance for the Arctic land surface, we used an ensemble of methods of ground-based measurements and multispectral satellite image analysis. Our estimate is that the low vegetation of polar tundra transforms 26% more solar energy into evapotranspiration than bare ground in clear sky weather. Due to its isolation properties, vegetation further reduces ground heat flux under the surface by ~4%, compared to bare areas, thus lowering the increase in subsurface temperature. -
Antarctic Primer
Antarctic Primer By Nigel Sitwell, Tom Ritchie & Gary Miller By Nigel Sitwell, Tom Ritchie & Gary Miller Designed by: Olivia Young, Aurora Expeditions October 2018 Cover image © I.Tortosa Morgan Suite 12, Level 2 35 Buckingham Street Surry Hills, Sydney NSW 2010, Australia To anyone who goes to the Antarctic, there is a tremendous appeal, an unparalleled combination of grandeur, beauty, vastness, loneliness, and malevolence —all of which sound terribly melodramatic — but which truly convey the actual feeling of Antarctica. Where else in the world are all of these descriptions really true? —Captain T.L.M. Sunter, ‘The Antarctic Century Newsletter ANTARCTIC PRIMER 2018 | 3 CONTENTS I. CONSERVING ANTARCTICA Guidance for Visitors to the Antarctic Antarctica’s Historic Heritage South Georgia Biosecurity II. THE PHYSICAL ENVIRONMENT Antarctica The Southern Ocean The Continent Climate Atmospheric Phenomena The Ozone Hole Climate Change Sea Ice The Antarctic Ice Cap Icebergs A Short Glossary of Ice Terms III. THE BIOLOGICAL ENVIRONMENT Life in Antarctica Adapting to the Cold The Kingdom of Krill IV. THE WILDLIFE Antarctic Squids Antarctic Fishes Antarctic Birds Antarctic Seals Antarctic Whales 4 AURORA EXPEDITIONS | Pioneering expedition travel to the heart of nature. CONTENTS V. EXPLORERS AND SCIENTISTS The Exploration of Antarctica The Antarctic Treaty VI. PLACES YOU MAY VISIT South Shetland Islands Antarctic Peninsula Weddell Sea South Orkney Islands South Georgia The Falkland Islands South Sandwich Islands The Historic Ross Sea Sector Commonwealth Bay VII. FURTHER READING VIII. WILDLIFE CHECKLISTS ANTARCTIC PRIMER 2018 | 5 Adélie penguins in the Antarctic Peninsula I. CONSERVING ANTARCTICA Antarctica is the largest wilderness area on earth, a place that must be preserved in its present, virtually pristine state. -
Dynamics of CO2 Evolution of Arctic Soils from Northern Siberia and Scandinavia
Dynamics of CO2 evolution of Arctic soils from Northern Siberia and Scandinavia Manfred Bölter*, Rolf Möller, Wiebke Müller-Lupp, and Nathalie Soethe Institute for Polar Ecology, University Kiel, Wischhofstr. 1-3, Bldg. 12, 24148 Kiel, Germany *Corresponding author: [email protected] 1. INTRODUCTION Growing interest in soil respiration in Arctic environments has opened wide research fields in microbial physiology and models associated therewith (Shivaji 2004). Much interest has been focused on metabolism in cold environments, with special emphasis on CO2 and CH4 evolution from tundra soils (Nadelhoffer et al. 1997, Vourlitis and Oechel 1997a,b). For modeling approaches, however, it is important to include the variability of microbial communities and their reactions to temperature shifts, i.e., the possible individual adaptations to temperature spans and related shifts in Q10 values of metabolic activity, which may indicate significant alterations in metabolic processes that point to important ecological factors to consider in the study of soil biological processes (Nadelhoffer et al. 1991, Sjögertsen and Wookey 2002). Special attention must be paid to processes at the cellular and subcellular level, and to the enzymes and substrates involved: an investigative effort that constitutes a crucial step in linking landscape modeling to small-scale processes. Soil carbon loss, generally termed soil respiration, is principally due to microbial and root respiration. Its measure can be defined in three ways (Haber 1958), i) the “physiological line”, ii) the “physical line”, and iii) the “ecological line”. The physiological line is mainly focused on the efficiency of soil organisms (and roots) and the reaction potential to the various environmental influences. -
Climate Change and Southern Ocean Resilience
No.No. 52 5 l l JuneMay 20202021 POLARKENNAN PERSPECTIVES CABLE Adélie penguins on top of an ice flow near the Antarctic Peninsula. © Jo Crebbin/Shutterstock Climate Change and Southern Ocean Resilience REPORT FROM AN INTERDISCIPLINARY SCIENTIFIC WORKSHOP, MARCH 30, 2021 Andrea Capurroi, Florence Colleoniii, Rachel Downeyiii, Evgeny Pakhomoviv, Ricardo Rourav, Anne Christiansonvi i. Boston University Frederick S. Pardee Center for the Study of the Longer-Range Future ii. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale Antarctic and Southern Ocean Coalition iii. Australian National University iv. University of British Columbia v. Antarctic and Southern Ocean Coalition vi. The Pew Charitable Trusts CONTENTS I. INTRODUCTION BY EVAN T. BLOOM 3 II. EXECUTIVE SUMMARY 5 III. CLIMATE CHANGE AND SOUTHERN OCEAN RESILIENCE 7 A. CLIMATE CHANGE AND THE SOUTHERN OCEAN 7 B. CONNECTION OF REGIONAL SOUTHERN OCEAN PROCESS TO GLOBAL SYSTEMS 9 C. UNDERSTANDING PROCESS CHANGES IN THE SOUTHERN OCEAN 10 D. ANTARCTIC GOVERNANCE AND DECISION MAKING 15 E. CONCLUSION 18 F. REFERENCES 19 POLAR PERSPECTIVES 2 No. 5 l June 2021 I. INTRODUCTION BY EVAN T. BLOOM vii Fig 1: Southern Ocean regions proposed for protection A network of MPAs could allow for conservation of distinct areas, each representing unique ecosystems As the world prepares for the Glasgow Climate Change Conference in November 2021, there is considerable focus on the Southern Ocean. The international community has come to realize that the polar regions hold many of the keys to unlocking our understanding of climate-related phenomena - and thus polar science will influence policy decisions on which our collective futures depend. -
Daily Program Friday, 24.02.2017 – Embarkation Ushuaia
DAILY PROGRAM FRIDAY, 24.02.2017 – EMBARKATION USHUAIA RESTAURANT TIMINGS TEA,COFFEE & COOKIES 15:00 – 17:30 PANORAMA LOUNGE, DECK 7 BUFFET DINNER 18:00 – 21:00 RESTAURANT, DECK 4 15:00 Check-In 21:30 Captain’s Cocktails. Our Expedition Jackets and Check in is on deck 3 and 4. Captain Raymond Martinsen Rubber Boots will be available Suites can check in on deck 7. would like to welcome you on for collection over the coming board and present his officers days. 15:00-17:30 Medical Forms and the Expedition Team. At Please deliver your medical the same time we'll give some We may have the opportunity forms to the Doctor in the information regarding our to stamp your passport at an lobby on deck 4. voyage, in the Panorama Antarctic base during our Lounge, deck 7. voyage. If you would NOT like 15:00-17:30 If you would like a stamp, please see to learn more about our FRAM goes paperless! On Reception, Deck 4. voyage then why not come your first day you will receive and meet some of the the Daily program in printed Most of the time we will use Expedition Team members in version. From tomorrow on our PolarCirkle boats for the Panorama Lounge on deck you will find the daily landings. For organizational 7. information on your cabin’s TV purposes we are going to screen as well as in all public separate you into groups of Approx. 17:30 Mandatory spaces. By doing so we avoid approximately 30 passengers. -
A Database of Plant Traits Spanning the Tundra Biome
Received: 15 November 2017 | Revised: 11 July 2018 | Accepted: 20 July 2018 DOI: 10.1111/geb.12821 DATA PAPER Tundra Trait Team: A database of plant traits spanning the tundra biome Anne D. Bjorkman1,2,3 | Isla H. Myers‐Smith1 | Sarah C. Elmendorf4,5,6 | Signe Normand2,7,8 | Haydn J. D. Thomas1 | Juha M. Alatalo9 | Heather Alexander10 | Alba Anadon‐Rosell11,12,13 | Sandra Angers‐Blondin1 | Yang Bai14 | Gaurav Baruah15 | Mariska te Beest16,17 | Logan Berner18 | Robert G. Björk19,20 | Daan Blok21 | Helge Bruelheide22,23 | Agata Buchwal24,25 | Allan Buras26 | Michele Carbognani27 | Katherine Christie28 | Laura S. Collier29 | Elisabeth J. Cooper30 | J. Hans C. Cornelissen31 | Katharine J. M. Dickinson32 | Stefan Dullinger33 | Bo Elberling34 | Anu Eskelinen35,23,36 | Bruce C. Forbes37 | Esther R. Frei38,39 | Maitane Iturrate‐Garcia15 | Megan K. Good40 | Oriol Grau41,42 | Peter Green43 | Michelle Greve44 | Paul Grogan45 | Sylvia Haider22,23 | Tomáš Hájek46,47 | Martin Hallinger48 | Konsta Happonen49 | Karen A. Harper50 | Monique M. P. D. Heijmans51 | Gregory H. R. Henry39 | Luise Hermanutz29 | Rebecca E. Hewitt52 | Robert D. Hollister53 | James Hudson54 | Karl Hülber33 | Colleen M. Iversen55 | Francesca Jaroszynska56,57 | Borja Jiménez‐Alfaro58 | Jill Johnstone59 | Rasmus Halfdan Jorgesen60 | Elina Kaarlejärvi14,61 | Rebecca Klady62 | Jitka Klimešová46 | Annika Korsten32 | Sara Kuleza59 | Aino Kulonen57 | Laurent J. Lamarque63 | Trevor Lantz64 | Amanda Lavalle65 | Jonas J. Lembrechts66 | Esther Lévesque63 | Chelsea J. Little15,67 | Miska Luoto49 | Petr Macek47 | Michelle C. Mack52 | Rabia Mathakutha44 | Anders Michelsen34,68 | Ann Milbau69 | Ulf Molau70 | John W. Morgan43 | Martin Alfons Mörsdorf30 | Jacob Nabe‐Nielsen71 | Sigrid Schøler Nielsen2 | Josep M. Ninot11,12 | Steven F. Oberbauer72 | Johan Olofsson16 | Vladimir G. Onipchenko73 | Alessandro Petraglia27 | Catherine Pickering74 | Janet S. -
Arctic Policy &
Arctic Policy & Law References to Selected Documents Edited by Wolfgang E. Burhenne Prepared by Jennifer Kelleher and Aaron Laur Published by the International Council of Environmental Law – toward sustainable development – (ICEL) for the Arctic Task Force of the IUCN Commission on Environmental Law (IUCN-CEL) Arctic Policy & Law References to Selected Documents Edited by Wolfgang E. Burhenne Prepared by Jennifer Kelleher and Aaron Laur Published by The International Council of Environmental Law – toward sustainable development – (ICEL) for the Arctic Task Force of the IUCN Commission on Environmental Law The designation of geographical entities in this book, and the presentation of material, do not imply the expression of any opinion whatsoever on the part of ICEL or the Arctic Task Force of the IUCN Commission on Environmental Law concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers and boundaries. The views expressed in this publication do not necessarily reflect those of ICEL or the Arctic Task Force. The preparation of Arctic Policy & Law: References to Selected Documents was a project of ICEL with the support of the Elizabeth Haub Foundations (Germany, USA, Canada). Published by: International Council of Environmental Law (ICEL), Bonn, Germany Copyright: © 2011 International Council of Environmental Law (ICEL) Reproduction of this publication for educational or other non- commercial purposes is authorized without prior permission from the copyright holder provided the source is fully acknowledged. Reproduction for resale or other commercial purposes is prohibited without the prior written permission of the copyright holder. Citation: International Council of Environmental Law (ICEL) (2011). -
The Southern Ocean 118 Worldwide Review of Bottom Fisheries in the High Seas
THE SOUTHERN OCEAN 118 Worldwide review of bottom fisheries in the high seas 30°W 15°W 0° 15°E 30°E °S °S 10 10 47 °S a n t i c °S A t l O c e a 20 n 20 t h o u 41 S Bouvet Prince Edward 51 Island Islands R i d i a g So t e ut S o hern Crozet °S c O o °S S South Georgia ce 30 Island an Islands u 30 t h 48 I n d Kerguelen e Islands g i id a McDonald R g Islands r n Weddell e Heard b Sea Island ss u O 5858 a -G en c el u e rg Bellingshausen e a K 87 n 87 Sea Davis Amundsen Sea n a Sea e c S O o n Ross r e u h S Sea t t outh u o h e 88 S rn O P c ea a n c i °S f °S i M 30 c 30 a O c c qu Macquarie e a a r Island 81 n ie R 57 i d g e °S °S 20 20 Tasman 77 Sea °S °S 10 150°W 165°W 180° 165°E 150°E 10 Antarctic Convergence FAO Fishing Areas 200 nautical miles arcs CCAMLR Regulatory Area Map Projection: Lambert Azimuthal equal area FAO, 2008 MAP 1 The Southern Ocean 119 Southern Ocean FAO Statistical Areas 48, 58 and 88 GEOGRAPHIC DESCRIPTION OF THE REGION The Southern Ocean surrounds the continent of Antarctica, and constitutes about 15 percent of the world’s total ocean surface (CCAMLR, 2000). -
The Ice of the Southern Ocean
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by National Institute of Polar Research Repository The Ice of the Southern Ocean A. F. TRESHNIKOV The Arctic and Antarctic Research Institute, Leningrad, USSR Abstract: Regular sea ice observations off the coasts of Antarctica in the Mirny Station area have been made by the Soviet Antarctic Expedition since 1956. For eight years air ice reconnaissance over the Davis Sea has been made from Mirny Station during all the seasons of the year from the shore to the ice edge. During the voyages of the d/e ship OB special observations on sea ice and icebergs have been made in the coastal zone of Antarctica. Physical properties, formation and desintegration of sea ice have been studied. The data obtained on sea ice peculiarities may be spread over a vast water area of the Southern Ocean. For many years the author has studied sea ice in the Arctic Ocean. The paper deals with general features of sea ice existence in the Antarctic and with differ ences. The formation and growth of ice from sea water both in the Arctic and Ant arctic depend mainly upon air temperature and heat content in the sea. Disinte gration and melting of ice in the Antarctic occur differently. Solar radiation, a great amount of diatoms included in the ice thickness and currents carrying ice out to the north into more warm waters play most important part here. The amount of old ice remaining in the Antarctic waters after the summer season is considerably less than in the Arctic waters.