• Lighter-than-air ships  
  • How man copes with the cold  
  • Organisation of the measurement flights  
  • Flying conditions and risks during the expedition  
  • The measurement campaign  
  • Communications - Safety - Emergency assistance  
  • Earth observation satellites  
  • Our airship  
  • The earth's atmosphere  
  • Weather forecasting and modeling  
  • The climate and the north pole  
  • The solar energy balance  
  • The greenhouse effect  
  • The ice pack: frozen saltwater  
  • Icebergs : frozen seawater  
  • The arctic ice: climate archives  
  • Ice ages and landscapes  
  • The Arctic Ocean and the ocean currents  
  • Genesis of the arctic ocean  
  • Arctic plankton  
  • Oceanic biodiversity and the food chain  
  • Whales and other cetaceans  
  • Seals and walruses  
  • Arctic flora  
  • Arctic fauna  
  • Polar bears  
  • Birds of the arctic  
  • Evolution of species and climate  
  • Geography of the Arctic regions  
  • Geographic North Pole and magnetic North Pole  
  • Who owns the arctic?  
  • Exploring the deep north  
  • The Inuit people  
  • The other peoples of the deep North  
  • The Arctic today  
  • Man and arctic biodiversity  
  • Pollution in the arctic  
  • Climate warming: the natural cycles  
  • The increase in the greenhouse effect  
  • The impact of global warming  
 

An airship at the North Pole
Earth observation satellites
 

Remote surveillance: the Earth seen from space
Artificial satellites have revolutionised the way we see our planet; they are now used to map the Earth, to trace roads, to monitor the spread of cities, to forecast crop harvests, and to monitor everything from volcanoes, clouds and forests to oceans and ice packs. Satellites can take measurements and make observations from far out in space without coming into contact with what they are monitoring; this is known as remote sensing or surveillance.

Satellite imagery, even at night
Earth observation satellites, often hundreds of kilometres out in space, orbit the Earth about 15 times every 24 hours. They closely observe each region on a regular basis. Some are simply designed to record the natural light that is reflected by the ground or the atmosphere. Others send down radar signals and record the echoes, this gathering data even at night and when the ground is obscured by cloud.

Ground-truthing on the ice pack
Once satellites send data back to Earth, it is processed into images with “false colours” depicting the different surfaces. Each type of surface (rock, water, cropland) sends back a different wave, called its spectral signature, which is allotted a colour. But in order to be sure the system works, the results must eventually be verified via “ground-truthing” by teams in the field. This is why the observations being made by Jean-Louis Etienne and his team on the pack ice are indispensable.

Studying the pack ice with QuikSCAT
The Arctic Ocean is a huge and inhospitable region that cannot easily be studied from the surface, so it is an ideal candidate for remote sensing. The American QuikSCAT satellite is equipped with a radar system that can use the surface appearance of a target zone to measure the speed and direction of wind on the ocean and can monitor the movement of polar pack ice. Using this satellite data, scientists can draw up ice maps to learn more about how the ice is changing and how it could react to climate variations.