Three three-dimensional trajectory models (LAGRANTO, TRAJKS and FLEXTRA), a
ll driven with analysis wind fields from the European Centre for Medium-Ran
ge Weather Forecasts, are intercompared. The comparison has three parts: fi
rst, a case study of strong ascent in a warm conveyor belt is performed; se
cond, a large set of back trajectories from the tropopause region over Euro
pe and the mid-latitude Atlantic Ocean is investigated third:, a set of low
-level trajectories is compared The intercomparison shows that all three mo
dels have been implemented correctly. The degree of model accordance depend
s on the interpolation methods used Deviations between the results from a s
ingle model using different interpolation schemes are of the same magnitude
as the deviations of different models. If all models use linear spatial in
terpolation, their respective trajectories closely agree with each other, w
ith deviations of 2% or less for the average distance between the starting
and the ending positions in the free atmosphere after 48 h. Close to the su
rface, where the differences in the model formulations are largest, average
horizontal position deviations may be up to 10%. Compared with other sourc
es of errors, such as inaccuracies in the wind fields or insufficient tempo
ral and spatial resolution of the data Set, these differences are much smal
ler Non-linear spatial interpolation lead to stronger vertical motions than
linear interpolation and in the case study, enhanced the quality of the re
sults.