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Aviation-induced cirrus and radiation changes at diurnal timescales
2013
Journal of Geophysical Research - Atmospheres
1] The radiative forcing from aviation-induced cirrus is derived from observations and models. The annual mean diurnal cycle of airtraffic in the North Atlantic region exhibits two peaks in early morning and afternoon with different peak times in the western and eastern parts of the North Atlantic region. The same "aviation fingerprint" is found in 8 years (2004)(2005)(2006)(2007)(2008)(2009)(2010)(2011) of Meteosat observations of cirrus cover and OLR. The observations are related to
doi:10.1002/jgrd.50184
fatcat:kdq53dzzwnbozooy2skh7cozqm