|
| |
Complex Flows that Influence Dispersion at the Rocky Flats Plant
L. Olivier,
R. Banta,
D. Levinson (CIRES)
and
W. Neff
|
Mesofront
|
|
strong westerly flow at the RFP was a result of upper level winds being channeled by the canyon rather than thermally induced
|
|
|
a small-scale frontal feature completely reversed the winds over the RFP region in a short time period
|
|
|
the shallowness of the event was important because the tracer studies showed that the tracer remained below 150 m in most cases
|
|
ETL /
Review /
Complex Flows that Influence Dispersion at the Rocky Flats Plant
/ Figure:
Introduction,
1,
Thermally Forced Flows,
2,
3,
4,
5,
Mesofront,
6,
7,
Flow Interaction Case,
8,
9,
Summary
|