The principal rationale for a dense network of soundings, profilers and
radars in Tier 1, together with rain gauges, is to describe and understand
the diurnal cycle of precipitation and the structure of precipitation in the
core region of the NAMS and to better understand regimes associated
with intra-seasonal variability, including the influences of surges, jets,
surface fluxes and topographic blocking. These observations are
critical for budget studies and model validation.
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