• 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  
 

Atmosphere and weather
Weather forecasting and modeling
 

What’s the weather tomorrow?
Meteorologists are getting better and better at answering this question, but forecasting more than 5 days ahead is still very uncertain. This is because the Earth’s climate is such a complex overall system: each cloud, each storm, each plot of farmland, each built-up area, each ocean current (even down deep) and each stretch of polar pack ice affects our climate. And no-one can know what’s going on all over the globe, from pole to Equator… It is possible to forecast seasonal trends, but no-one can say what the weather will be like in 2 weeks time on a particular beach.

A worldwide observation network
Dotted across all the continents on Earth there is a network of thousands of weather observation stations recording measurements such as temperature, wind speed, pressure, humidity, etc. Aircraft and weather balloons are used to take measurements at altitude, while ships and weather buoys send back the same data, plus information on ocean currents. All this data is fed into computers used to draw up weather forecasts.

Weather satellites too
Even out in space, weather satellites orbit the Earth in mobile and geo-stationary satellites orbit (geo-stationary satellites orbit at the same speed as the Earth’s rotation, so they remain above a fixed spot) the globe sending back real-time images of atmospheric conditions. This constantly updated overall picture, combined with data from surface facilities, has been a big factor in improving weather forecasting.

More reliable weather models
The computers used by meteorologists draw up forecasts according to predetermined methods and using parameters already implanted in their memory. In order to simulate the circulation of the various earthly fluids, the atmosphere and the oceans are cut up into compartments and the computer calculates the impact of each one on the adjacent compartments. But when calculating forecasts several hours ahead, any variation in the initial stages can produce a totally different result. The only solution here is to fine-tune the compartments to factor in the influence of landscape relief, living organisms etc., and to develop even more powerful “number-crunchers”.