PROGRAM
Rear Flank Downdraft (RFD)
17 May - 2018 - South Dakota
A supercell can be recognized by identifying the RFD. That's a dark threatening horizontal band of clouds that spirals inward to the center of the storm. It's the boundary between cool air associated with the evaporation of raindrops near the rear of the storm and the warm and humid air the flows into the storm. RFD winds can be destructive and will normally be from the west, while inflow will be from the south, south-east or east. We look for tornado (T) genesis precisely at the location where the RFD spiralles inward. The Forward Flank Downdraft (FFD) is associated with the general downward flow of rain fromt the center of the storm and intersects with the RFD close the where the location of tornado genesis.
GOOD TO KNOW
You travel to distant regions with sometimes exceptional circumstances. Often you need a visa, but you will certainly have to take into account clothing. In addition, many countries have different electricity plugs. Because we do not yet know exactly what our destination is during this trip, you will be informed well in advance about a number of requirements.
What has to be arranged before are visa for the United States and Canada.