An examination of the convective charging hypothesis: Cloud charge structure and Maxwell currents.
Helsdon, J.H., Jr., S. Gattaleeradapan, R.D. Farley, and C.C. Waits, 2002
(JGR-Atmospheres, in press.)
Abstract
An
examination of the convective charging hypothesis is undertaken using our
three-dimensional Storm Electrification Model.
In an attempt to cover the range of storm conditions over which the
convective mechanism might be expected to operate, two storms are simulated: a
small, weak storm and a larger, severe storm.
Elements of the model relevant to the convective hypothesis are the full
treatment of small ions, including attachment to hydrometeors; the inclusion of
field-dependent surface point discharge; and the components of the Maxwell
current. For comparison purposes, each storm is also simulated using a
noninductive mechanism. Results
from both the small and large storm simulations using convective-only charging
indicate disorganized, weak electrical structures during the mature and
dissipating stages. Conversely, the
use of noninductive charging produces strong electrification in both storms.
Maxwell current analysis shows that, for the most part, currents within
the storm are dissipative and that the cloud acts as a barrier to the external
conduction current when convective-only charging is considered.
For the noninductive simulations the Maxwell current is that of a
generator. The treatment of small
ions and their attachment to hydrometeors accounts for the formation of
screening layers, thus this aspect of the convective charging mechanism still
plays an important role in the modeling of thunderstorm charge structures. However, since the convective charging hypothesis, by itself,
is unable to produce significant charging or strong electric fields in either
simulated cloud, we conclude that it is not a viable mechanism for thunderstorm
electrification.
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