chapter 7: Jet and Jet streaks Flashcards
Weather processes strongly depend on
the structure and dynamics of jet streams
There are ………………….major ……………………jet streams in the upper ………………………in each hemisphere
two
westerly
troposphere
There are two major westerly jet streams in the upper troposphere in each hemisphere
– Polar jet stream
– Subtropical jet stream
The structure of jet streams are related to
temperature distribution through the thermal wind relationship
Warm air to the south results in
westerly geostrophic winds through the thermal wind relationship.
Draw the jet stream (box)
The thermal wind relationship also explains why
the jet stream tends to be collocated with the polar front.
Large horizontal temperature gradients > > >
large horizontal temperature gradients
Large thickness gradients>
Large horizontal pressure gradient aloft>
strong winds
The polar jet is the band of
(speed ) (found in)
meandering strong winds (~100 knots) found at the tropopause.
The polar jet moves
meridionally (30°-60° latitude) and vertically (10-15 km) with the seasons.
Large vertical extent: maximum usually near ……………….. but can be seen at ……………….
300 mb
200mb - 500mb
At times, the polar jet will split into …………………………….and possibly merge with ………………………..
northern and southern branches
the subtropical jet
Polar Jet and thermal wind balance:
it is associated with:
strong quasi-horizontal temperature gradients in the lower troposphere and strong vertical wind shear.
It is associated with strong quasi-horizontal temperature gradients in the lower troposphere and strong vertical wind shear.
• These features are often associated with
the polar front.
Meridional undulations of the jet stream are associated with
poleward and equatorward displacements of warm and cold air, respectively.