METEO MIDTERM Flashcards

1
Q

Used to measure the wind,
temperature, moisture, and
pressure in vertical levels.

A

Skew-T Diagram

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2
Q

itis the processed output of
upper-air soundings.

A

Skew-T Diagram

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3
Q

A weather balloon costs around

A

18k - 20k per launch

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4
Q

The data processed by the skew-t
is from __________

A

the different upper air
stations of the Philippine
Atmospheric, Geophysical and
Astronomical Services
Administration (PAGASA).

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5
Q

PAGASA has seven upper-air
stations situated at ____

A

Laoag, Baguio,
Tanay, Legaspi, Cebu, Puerto
Princesa and Davao.

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6
Q

All stations are required to launch
a weather balloon ___ a day
during _____

A

2, (00Z and 12Z).

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7
Q

Weather balloons, which are made of _________, are filled with ___ instead of helium to reach greater heights. This is done using water electrolysis.

A

latex or synthetic rubber (neoprene),,,,,, hydrogen

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8
Q

The balloons, which start out
measuring about 6 ft. wide before
release, expand as they rise to about ___. in diameter.

A

20 ft

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9
Q

An instrument called ____ is attached to the balloon to measure pressure,temperature and relative humidity as it ascends up into the atmosphere.

A

radiosonde

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10
Q

Radiosondes and weather balloons are used to measure upper-air data. The ____ measures the weather parameters and transmits the data back to a server.

A

radiosonde

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11
Q

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.

A

Convective Available Potential Energy (CAPE)

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12
Q

the energy that inhibits the
process of convection which means the higher the _____,the lower the possibility to have a thunderstorm.

A

Convective Inhibition (CIN)

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13
Q

its about the instability. The more negative the value of __, the higher the possibility to have a thunderstorm.

A

Lifted Index (LI)

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14
Q

the two levels are important as it determine the intensity of the storm or the thunderstorm that will be form.

A

Mid-level (850 to 500 hpa) moisture and wind-shear

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15
Q

it is the line of constant
pressure.

A

Isobars

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16
Q

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.

A

Isobars

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17
Q

it is the line of constant
temperature.

A

Isotherms

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18
Q

On the skew-T diagram,
these are straight, solid
lines, sloping from the lower left
to upper right.

A

Isotherms

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19
Q

it is the line of constant
potential temperature.

A

Dry Adiabats

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20
Q

On the skew-T diagram, these are the slightly-curved, solid lines sloping from the lower
right to upper left.

A

Dry Adiabats

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21
Q

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

A

Dry Adiabats

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22
Q

also known as moist adiabats or saturation pseudo-adiabats, represent lines of constant equivalent potential temperature.

A

Saturation Adiabats

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23
Q

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

A

Saturation Adiabats

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24
Q

also known as humidity mixing ratio lines

A

Saturation Mixing Ratio

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25
On the skew-t diagram lines are the slightly-curved, dashed lines sloping from the lower left to upper right.
Saturation Mixing Ratio
26
They are labeled at the bottom of the diagram for a range of 0.1 to 40.0 grams per kilogram
Saturation Mixing Ratio
27
___ is the difference in wind speed and/or direction between two identified levels.
Wind Shear
28
____ wind shears will support convection.
Weak
29
Strong wind shears will ____ convection
inhibit, hinder
30
is the ratio of the mass of water vapor (Mv) to the mass of dry air (Md) in a parcel of air at saturation.
saturation mixing ratio (ws)
31
It is the maximum amount of water vapor that a parcel can hold without condensation.
SATURATION MIXING RATIO (Ws)
32
formula of SATURATION MIXING RATIO (Ws) and the mixing ratio (w)
ws or w = Mv / Md
33
is the ratio of the mass of water vapor (Mv) to the mass of dry air (Md)
the mixing ratio (w)
34
it measures the actual amount of water vapor present
the mixing ratio (w)
35
_____ is the ratio of the amount of water vapor in a given volume of air to the amount that volume would hold if the air were saturated.
Relative humidity (RH)
36
formula of RH
RH = 100* (W/Ws
37
Saturated conditions have a DD of ____
zero
38
_____ have a large DD.
dry condition
39
____ is the height at which a parcel of air becomes saturated when it is lifted dry adiabatically.
lifting condensation level (LCL)
40
Height to which a parcel of air, if heated sufficiently from below, will rise adiabatically until it is just saturated.
CONVECTIVE CONDENSATION LEVEL (CCL)
41
This is the cloud base.
CONVECTIVE CONDENSATION LEVEL (CCL)
42
Height at which a parcel of air, when lifted, becomes warmer than its surroundings.
LEVEL OF FREE CONVECTION (LFC)
43
The parcel is lifted dry adiabatically until saturate and then moist-adiabatically thereafter
LEVEL OF FREE CONVECTION (LFC)
44
Height where the temperature of a buoyantly rising parcel again equals the temperature of the environment.
EQUILIBRIUM LEVEL (EL)
45
Can be identified either through the use of LCL or CCL.
EQUILIBRIUM LEVEL (EL)
46
This is referred as the cloud top.
EQUILIBRIUM LEVEL (EL)
47
Amount of buoyant energy available as the parcel is accelerated upward.
CONVECTIVE AVAILABLE POTENTIAL ENERGY
48
CAPE value 0 means
Stable
49
what is the stability of CAPE value 0 - 1000
Marginally Unstable
50
what is the stability of CAPE value 1000 - 2500
Moderately Unstable
51
what is the stability of CAPE value 2500 0 3500
Very Unstable
52
what is the stability of CAPE value 3500 or greater
Extremely Unstable
53
Amount of energy required to lift the parcel to the LFC
CONVECTIVE INHIBITION (CIN)
54
The larger the____ the higher the CIN value, and the lower the likelihood of convective storms
negative area,
55
difference between the observed temperature at 500 hPa and the temperature of an air parcel lifted to 500 hPa from near the surface.
LIFTED INDEX (LI)
56
The lower the value of LI, the _____
higher the possibility of thunderstorms.
57
LI VALUE; -2, WHAT IS THE SEVERE WEATHER POTENTIAL
WEAK
58
LI VALUE; - 3 to -5, WHAT IS THE SEVERE WEATHER POTENTIAL
MODERATE
59
LI VALUE; -6 OR LESS, WHAT IS THE SEVERE WEATHER POTENTIAL
STRONG
60
Using a certain programming language (Python), one can automatically compute the parameters to create an early warning system (EWS) that can provide automated risk analysis at a specific area of interest.
FORECASTING
61
in launching weather ballon how many are launched for normal condition and extreme condition per day
normal condition: 2x a day extreme condition: hourly
62
measures the amount of water vapor that would be present at saturation.
saturation mixing ratio