METEO MIDTERM Flashcards
Used to measure the wind,
temperature, moisture, and
pressure in vertical levels.
Skew-T Diagram
itis the processed output of
upper-air soundings.
Skew-T Diagram
A weather balloon costs around
18k - 20k per launch
The data processed by the skew-t
is from __________
the different upper air
stations of the Philippine
Atmospheric, Geophysical and
Astronomical Services
Administration (PAGASA).
PAGASA has seven upper-air
stations situated at ____
Laoag, Baguio,
Tanay, Legaspi, Cebu, Puerto
Princesa and Davao.
All stations are required to launch
a weather balloon ___ a day
during _____
2, (00Z and 12Z).
Weather balloons, which are made of _________, are filled with ___ instead of helium to reach greater heights. This is done using water electrolysis.
latex or synthetic rubber (neoprene),,,,,, hydrogen
The balloons, which start out
measuring about 6 ft. wide before
release, expand as they rise to about ___. in diameter.
20 ft
An instrument called ____ is attached to the balloon to measure pressure,temperature and relative humidity as it ascends up into the atmosphere.
radiosonde
Radiosondes and weather balloons are used to measure upper-air data. The ____ measures the weather parameters and transmits the data back to a server.
radiosonde
The energy supports the creation of convection thatis vital in creating a thunderstorm which means the higher the ___ ,the higher the possibility to have a thunderstorm.
Convective Available Potential Energy (CAPE)
the energy that inhibits the
process of convection which means the higher the _____,the lower the possibility to have a thunderstorm.
Convective Inhibition (CIN)
its about the instability. The more negative the value of __, the higher the possibility to have a thunderstorm.
Lifted Index (LI)
the two levels are important as it determine the intensity of the storm or the thunderstorm that will be form.
Mid-level (850 to 500 hpa) moisture and wind-shear
it is the line of constant
pressure.
Isobars
they nearly horizontal lines that
spaced logarithmically from
about 1050 hPa at the bottom
to 100 hPa at the top. They are
plotted every 50 hPa.
Isobars
it is the line of constant
temperature.
Isotherms
On the skew-T diagram,
these are straight, solid
lines, sloping from the lower left
to upper right.
Isotherms
it is the line of constant
potential temperature.
Dry Adiabats
On the skew-T diagram, these are the slightly-curved, solid lines sloping from the lower
right to upper left.
Dry Adiabats
it indicate the rate of temperature change in a parcel of dry air rising or descending adiabatically, with no loss or gain of heat by the parcel
Dry Adiabats
also known as moist adiabats or saturation pseudo-adiabats, represent lines of constant equivalent potential temperature.
Saturation Adiabats
On the skew-T diagram, they are the slightly curved lines. It represent the rate of temperature change in a rising parcel of saturated air
Saturation Adiabats
also known as humidity mixing ratio lines
Saturation Mixing Ratio