Free Access

Fig. 5

image

Left: modelled pre- and post-perihelion slopes (α) of water sublimation rate as a function of latitude averaged over several bins (see text for detailed description). Right: pre- and post-perihelion slopes of water production rate from the data derived from MIRO measurements. The error bars on the modelled data reflect longitudinal variability, which is very large in southern hemisphere owing to rapid temperature variations. The MIRO data error bars also reflect the data variability at 1σ level.

Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.

Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.

Initial download of the metrics may take a while.