Fig. B.16

Posterior distribution of isothermal line retrieval with an added vertical wind in the upper atmosphere. The parameter on the right h is then used to calculate the pressure where the vertical velocity is added via Eq. (9). The fraction of the atmosphere below that pressure has no winds. The distribution of h shows that the retrieval shows a clear preference for high vertical winds for pressures below h = −6, but is unable to discriminate between the wind patterns in the lower parts of the atmosphere.
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