3-11.
How do pressure changes associated
with a thunderstorm influence
aircraft altimeter readings?
1.
The altimeter reading decreases
as the storm approaches and
remains low until the storm
moves away
2.
The altimeter reading increases
as the storm approaches,
decreases while in the rain
showers, and returns to normal
as the storm moves away
3.
The altimeter reading decreases
in the cumulus stage of the
thunderstorm, increases in the
mature stage of the
thunderstorm, and returns to
normal in the dissipation stage
4.
The altimeter reflects
decreasing altitudes as the
aircraft approaches the
thunderstorm, increased
altitude as the aircraft flies
through the rain, and returns
to normal as the aircraft flies
away from the storm
3-12.
A pilot sets the altimeter
immediately before the passage of a
thunderstorm.
Following the
passage of the thunderstorm, what
should the altimeter read?
1.
High
2.
Low
3.
Accurate
3-13.
When the parcel method is analyzed
on a Skew T log P diagram and used
to forecast thunderstorms, which of
the following statements is valid?
1.
With a large positive area,
thunderstorms may be forecast
with a high degree of
confidence
2.
When thunderstorms are not
indicated, you may safely
assume that no thunderstorms
will occur
3.
The parcel method gives little
indication of stability or
instability when used alone as
a forecasting aid
4.
The size of the positive area
is a good indication of
instability,
but other factors,
such as the distribution of low
tropospheric moisture, should
be considered
3-14.
Which parcel method condition, when
considered alone, would NOT be
favorable for thunderstorm
development?
1.
The negative energy area
exceeds the positive energy
area
2.
The positive energy area
exceeds the negative energy
area
3. An ample supply of moisture is
uniformly distributed
throughout the lower
troposphere
4.
The parcel will rise to a
temperature level of -10°C
IN ANSWERING QUESTION 3-15, REFER TO
FIGURE 5-3 IN YOUR TRAMAN.
3-15.
From an analysis of figure 5-3, you
should draw which of the following
conclusions?
1.
The base of the inversion can
be safely assumed to be the top
of cumulus activity
2.
Sufficient heating during the
day will dissipate the low-
level inversion; therefore, a
forecast of thunderstorm
activity may be made
3.
In spite of favorable lapse
rate conditions, there is
insufficient moisture for
thunderstorm development
4.
Although the positive energy
areas exceed the negative
energy areas, due to the
intensity of the low-level
inversion,
thunderstorms would
probably not form
3-16.
When the parcel method for
mechanical lifting is used, what
level(s) is/are determined on the
Skew T log P diagram?
1.
LCL
2.
LFC
3.
Both 1 and 2 above
4. LND
17