Simulations of contrail-to-cirrus transition over up to 6 h wereperformed using a LES-model. The sensitivity of microphysical, opticaland geometric contrail properties to relative humidity RH(i),temperature T and vertical wind shear s was investigated in an extensiveparametric study. The dominant parameter for contrail evolution isrelative humidity. Substantial spreading is only visible for RH(i)greater than or similar to 120%. Vertical wind shear has a smallereffect on optical properties than human observers might expect from thevisual impression. Our model shows that after a few hours the watervapour removed by falling ice crystals from the contrail layer can beseveral times higher than the ice mass that is actually present in thecontrail at any instance.
CITATION STYLE
Unterstrasser, S., & Gierens, K. (2010). Numerical simulations of contrail-to-cirrus transition - Part 1: An extensive parametric study. ATMOSPHERIC CHEMISTRY AND PHYSICS, 10(4), 2017–2036.
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