Classic Antarctica Slide Show
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www.quarkexpeditions.com - an inside look at an expedition to the Antarctic Peninsula.
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Icebergs in Antarctica form stripes from layers of snow reacting to different conditions, with blue stripes forming from quick freezing sea water without bubbles, green stripes when algae-rich water freezes to the underside, and brown, black and yellow lines caused by sediment as the ice sheet grinds toward the sea.
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The document discusses evidence of global warming in Antarctica. It notes that the Antarctic Peninsula has warmed 2.5 degrees Celsius over the past 50 years, much faster than the global average. This rapid warming led to the Larsen B ice shelf, the size of Cornwall, breaking off in 2002. While temperatures have increased on the peninsula and parts of the West Antarctic ice sheet are thinning, the East Antarctic ice sheet does not show signs of warming. Global warming is also affecting the Southern Ocean by causing earlier sea ice melt and more ice-free areas in summer. This is impacting the Antarctic marine ecosystem as warmer waters reduce phytoplankton and krill populations.
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Greetings all,
What does your imagination tell you when you think about the Austral Ocean ? Perhaps this place reminds you of the “Roaring
Forties” and the “Screaming fifties”, the drift of the icebergs, the only passage free of ice to go around the earth, an inhospitable
area, the Antarctic continent, penguins… Actually, the Austral Ocean is a keystone for the interocean exchanges of heat,
freshwater and anthropogenic tracers: it is the meeting point of the Indian, Atlantic and Pacific Oceans. It also plays a key role in
the global carbon cycle.
This issue is dedicated to this particular place. It will present to us some of the important oceanographic projects concerning the
Austral Ocean: Flostral, Survostral, GoodHope, the Drake Campaign and analysis done to better understand its dynamic and its
role from model (Drakkar project, …) and observations (ARGO, dedicated campaigns, satellite data sets, …).
The first article, written by Pouget & al., focuses on the performances of one of the global Mercator 1/4° model (PSY3v1) at
Drake Passage by comparing it with in situ data gathered from R.V Polarsten in 2006.
The second one, from Le Sommer & al., presents an overview of some results obtained on the Southern Ocean processes and
climate variability through the use of the Drakkar hierarchy of ocean/ice models.
The next one explains what the Survostral and Flostral projects are and it gathers some results deduced from the data collected
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The last one, written by Speich S. and Arhan M., presents the GoodHope project and summarizes some results of the work
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In this issue, we would also like to approach a central topic on the future of operational oceanography: MyOcean: part of the
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Lolo is a little penguin who lives in Antarctica with its family which includes a mother, father, and brother penguin. Penguins live in large groups in Antarctica where it is always cold. They are black and white birds that cannot fly but use their flippers to swim and dive in the water, which they enjoy living in as well as the land. Penguins eat fish, which the father will help incubate eggs while the mother finds food.
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Greetings all,
What does your imagination tell you when you think about the Austral Ocean ? Perhaps this place reminds you of the “Roaring
Forties” and the “Screaming fifties”, the drift of the icebergs, the only passage free of ice to go around the earth, an inhospitable
area, the Antarctic continent, penguins… Actually, the Austral Ocean is a keystone for the interocean exchanges of heat,
freshwater and anthropogenic tracers: it is the meeting point of the Indian, Atlantic and Pacific Oceans. It also plays a key role in
the global carbon cycle.
This issue is dedicated to this particular place. It will present to us some of the important oceanographic projects concerning the
Austral Ocean: Flostral, Survostral, GoodHope, the Drake Campaign and analysis done to better understand its dynamic and its
role from model (Drakkar project, …) and observations (ARGO, dedicated campaigns, satellite data sets, …).
The first article, written by Pouget & al., focuses on the performances of one of the global Mercator 1/4° model (PSY3v1) at
Drake Passage by comparing it with in situ data gathered from R.V Polarsten in 2006.
The second one, from Le Sommer & al., presents an overview of some results obtained on the Southern Ocean processes and
climate variability through the use of the Drakkar hierarchy of ocean/ice models.
The next one explains what the Survostral and Flostral projects are and it gathers some results deduced from the data collected
during these campaigns. Authors of this article are Salle JB and Morrow R.
The last one, written by Speich S. and Arhan M., presents the GoodHope project and summarizes some results of the work
done from the hydrographic data sets obtained in the scope of this project.
In this issue, we would also like to approach a central topic on the future of operational oceanography: MyOcean: part of the
GMES European Projet. This subject is introduced in the News pages by Pierre Bahurel.
I hope you enjoy this issue.
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Our ship, the Corinthian II, took passengers on a Antarctic expedition from December 22, 2008 to January 1, 2009, making various stops along the way. Highlights included seeing hundreds of thousands of penguins at their rookeries, spectacular ice formations, climbing volcanic islands, and celebrating Christmas at sea, but the trip ended in tragedy when a 65-year-old passenger died in the hospital after becoming unconscious on the return trip to Ushuaia, Argentina.
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The document summarizes how animals survive freezing temperatures, the different types of penguins, the size of Antarctica, temperature extremes at the poles, and includes references. It discusses how most animals build nests or leave to stay warm, lists Emperor, King, Gentoo, and African penguins, notes Antarctica is Earth's 5th largest continent, and that recorded temperatures have been -128°C in Antarctica and -90°C at the North Pole.
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Glaciers are giant blocks of snow and ice that form over thousands of years in areas that receive snowfall year-round. As layers of snow accumulate and melt, the melted snow refreezes into layers of ice that build up and compress to form glaciers. Glaciers can be found on every continent except Australia, usually in polar or mountainous regions, and they move slowly due to the force of gravity pulling on melted ice at their edges.
What? Did You Say 365 Penguins?
This Web Quest was created for Pre-K to second grade students as an ATCP technology project. It is intended that students be able to identify the characteristics of different species of penguins, and present the findings to the class in the form of a Power Point, Kidpix etc. Most important is that students have exposure and experience in learning mathematical concepts using technology.
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Wayanad, nestled in Kerala's Western Ghats, is a lush paradise renowned for its scenic landscapes, rich biodiversity, and cultural heritage. From trekking Chembra Peak to exploring ancient Edakkal Caves, Wayanad offers thrilling adventures and serene experiences. Its vibrant economy, driven by agriculture and tourism, highlights a harmonious blend of nature, tradition, and modernity.
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The Power of a Glamping Go-To-Market Accelerator Plan.pptx
Unlock the secrets to success with our comprehensive 8-Step Glamping Accelerator Go-To-Market Plan! Watch our FREE webinar, where you'll receive expert guidance and invaluable insights on every aspect of launching and growing your glamping business.
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