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The solar internetwork is the site of vigorous flux emergence on small
spatial scales. Flux appears in supergranular cells in the form of
unipolar and bipolar patches, at a rate of 120 Mx cm-2 day-1. Upon
appearance, magnetic elements start to move toward the cell boundaries
- the network. Their mean lifetime is 7 minutes, but many of them
survive longer and interact with other features on their way to the
network. Bipolar structures, both small-scale magnetic loops with two
footpoints and clusters of opposite-polarity patches that emerge on
the same area of the solar surface within a short time interval, are
responsible for more than 50% of the total internetwork flux. These
are the longest-lived magnetic elements. They interact with
preexisting fields and produce brightenings in the chromosphere and
transition region as they rise into the atmosphere. Such elements may
be important contributors to chromospheric heating. The rest of the
flux appears in situ as unipolar features. They tend to be smaller and
have shorter lifetimes. Flux disappears from supergranular cells
through transfer to the network, fading, and cancellation, at a very
similar rate of 125 Mx cm-2 day-1. About 40% of the flux present in
the internetwork ends up in the network, supplying as much flux as it
contains on time scales of only 10 hours. Fading is an equally
important flux loss mechanism, followed by cancellations. The flux
appearance and disappearance rates are enormous. However, the fact
that a significant fraction of the internetwork flux shows up as
unipolar features and disappears by fading suggests that they are the
result of the concentration and dispersal of background flux which is
too weak to be detected above the noise level. This component is
probably flux recycled from the network, rather than newly emerged
flux. If so, the actual flux emergence and disappearance rates may be
smaller than implied by the observations. In this talk I will review
our current understanding of flux emergence processes and interactions
in the quiet Sun, using long-duration, high cadence, magnetograph
observations acquired by Hinode to illustrate the evolution of
small-scale magnetic elements in the solar atmosphere. |