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Condensation trains seen from ISS. - Contrails over Rhone valley seen from ISS. - Condensation...
IMAGE
number
PIX4672384
Image title
Condensation trains seen from ISS. - Contrails over Rhone valley seen from ISS. - Condensation trains caused by air traffic. Upstairs, Leman Lake. Image obtained from the International Space Station on May 15, 2002. This digital photograph taken through the windows of the International Space Station on May 15, 2002, shows condensation trails over the Rhone Valley. Condensation trails - - or contrails - - are straight lines of ice crystals that form in the wake of jet liners where air temperatures at altitude are lower than about - 40* C. Newer contrails are thin whereas older trails have widened with time as a result of light winds. Because of this tendency for thin contrails to cover greater areas with time, it is estimated that these artificial clouds”” cover 0.1% of the planet's surface. Percentages are far higher in some places such as southern California, the Ohio River Valley and parts of Europe, as illustrated here.
Condensation trains seen from ISS. - Contrails over Rhone valley seen from ISS. - Condensation trains caused by air traffic. Upstairs, Leman Lake. Image obtained from the International Space Station on May 15, 2002. This digital photograph taken through the windows of the International Space Station on May 15, 2002, shows condensation trails over the Rhone Valley. Condensation trails - - or contrails - - are straight lines of ice crystals that form in the wake of jet liners where air temperatures at altitude are lower than about - 40* C. Newer contrails are thin whereas older trails have widened with time as a result of light winds. Because of this tendency for thin contrails to cover greater areas with time, it is estimated that these artificial clouds”” cover 0.1% of the planet's surface. Percentages are far higher in some places such as southern California, the Ohio River Valley and parts of Europe, as illustrated here.
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