Download presentation
Presentation is loading. Please wait.
Published byNathan O’Neal’ Modified over 9 years ago
2
Property of Lear Siegler
3
ATMOSPHERIC STABILITY & CLOUDS Property of Lear Siegler
4
T L O
5
ELO 1 Action: The student will identify the different states in which moisture is found in the atmosphere. Condition: Given pertinent information about moisture Standard: IAW FM 1-230 para 4-2
6
Moisture States VAPOR / GAS VAPOR / GAS LIQUID / VISIBLE LIQUID / VISIBLE SOLID SOLID Property of Lear Siegler
7
ELO 2 Action: The student will identify the changes moisture makes from one water state to another. Condition: Given pertinent information about states of moisture Standard: IAW FM 1-230 para 4-2
8
Changes in Moisture EvaporationCondensation Fusion (freezing) SublimationMelting
10
LATENT HEAT Heat energy taken in through evaporation and melting Heat energy taken in through evaporation and melting Heat energy released through condensation and fusion Heat energy released through condensation and fusion Property of Lear Siegler
13
ELO 3 Action: The student will identify the amount of water vapor contained in a portion of the atmosphere. Condition: Given pertinent information about the water vapor and the atmosphere Standard: IAW FM 1-230 para 4-3, and 4-4
14
WATER VAPOR CONTENT Property of Lear Siegler SATURATION DEW POINT
16
WATER VAPOR CONTENT RELATIVE HUMIDITY Property of Lear Siegler SATURATION SATURATION DEW POINT DEW POINT
17
0 o C 32° F 6 o C 43° F 10 o C 50° F 17 o C 61° F 20 o C 68° F 30 o C 86 o F Property of Lear Siegler
18
Moist air = less air density = less engine performance
19
ELO 4 Action: The student will identify the adiabatic process. Condition: Given pertinent information about the water vapor and the atmosphere Standard: IAW FM 1-230 para 3-6
20
15° 40° 15° ADIABATIC PROCESS When the temperature of a gas is changed without the addition or deletion of heat energy Property of Lear Siegler
21
OAT 20° C DEW POINT 14° C RELATIVE HUMIDITY = 70.4% Property of Lear Siegler
22
OAT 14° C DEW POINT 14° C RELATIVE HUMIDITY = 100% Property of Lear Siegler
23
OAT 10° C DEW POINT 10° C RELATIVE HUMIDITY = 100% Property of Lear Siegler
24
OAT 20° C RELATIVE HUMIDITY = 54% DEW POINT 10° C Property of Lear Siegler
28
ELO 5 Action: The student will identify the moist and dry adiabatic cooling rates. Condition: Given pertinent information about the adiabatic process Standard: IAW FM 1-230 para 3-6
29
Dry cooling rate – 3 o per 1,000 ft Dry cooling rate – 3 o per 1,000 ft Moist cooling rate – 1.5 o per 1,000 ft Moist cooling rate – 1.5 o per 1,000 ft
30
ELO 6 Identify the points where condensation and free convection take place
31
OLR=2° DP=14° 18° 16° 14° 12° 10° OLR=2° DEWPOINT=14° 12° 18° 16° 14° 10° 8° 6° 4° Property of Lear Siegler
32
OLR=2° DEWPOINT=14° 17 ° 14 ° DRY ADIABATIC LAPSE RATE 3°/1000’ 12° 18° 16° 14° 10° 8° 6° 4° Property of Lear Siegler
33
OLR=2° DEWPOINT=14° 17 ° 14 ° 12° 18° 16° 14° 10° 8° 6° 4° Property of Lear Siegler LEVEL OF CONDENSATION Temperature of the rising air and dew point are the same.
34
OLR=2° DEWPOINT=14° 17 ° 12° 18° 16° 14° 10° 8° 6° 4° Property of Lear Siegler MOIST LAPSE RATE 1.5°/1000’ 8°8° 12.5 ° 14 ° 9.5 ° 11 ° LEVEL OF FREE CONVECTION Temperature of the rising air is the same as the ambient air
35
OLR=2° DEWPOINT=14° 17 ° 12° 18° 16° 14° 10° 8° 6° 4° Property of Lear Siegler 12.5 ° 14 ° 9.5 ° 11 ° 8°8° 6.5 ° 5°5°
36
17 ° 14 ° DEWPOINT=14° OLR=2° 12.5 ° LEVEL OF CONDENSATION 12° 18° 16° 14° 10° 8° 6° 4° MOIST LAPSE RATE 1.5°/1000’ Property of Lear Siegler Temperature of the rising air and dew point are the same.
37
17 ° 14 ° DEWPOINT=14° OLR=2° 12.5 ° 11 ° 9.5 ° 8°8° 6.5 ° 5°5° LEVEL OF FREE CONVECTION 12° 18° 16° 14° 10° 8° 6° 4° Property of Lear Siegler Temperature of the rising air is the same as the ambient air
38
ELO 7 Action: The student will identify the factors that determine atmospheric stability. Condition: Given pertinent information about stability Standard: IAW FM 1-230 para 7-4
39
UNSTABLE – Air that moves vertically and will continue without any outside force OLR 3.0 or greater CONDITIONALLY UNSTABLE – Air parcel is neutral. Vertical movement depends on the conditions OLR between 1.5 and 3.0 STABLE – Resists vertical development OLR 1.5 or less
40
Air with high moisture content tends to be more unstable than dry air, if lifting action occurs.
41
OLR=2° DP=14° 18° 16° 14° 12° 10° OLR=1.5° DEWPOINT=14° 11° 18.5° 17° 15.5° 14° 12.5° 9.5° 8° Property of Lear Siegler
42
OLR=1.5° DEWPOINT=14° 17 ° 14 ° DRY ADIABATIC LAPSE RATE 3°/1000’ 11° 18.5° 17° 15.5° 14° 12.5° 9.5° 8° Property of Lear Siegler
43
DEWPOINT=14° OLR=1.5° MOIST LAPSE RATE 1.5°/1000’ 17 ° 14 ° 12.5 ° 11 ° 9.5 ° 8°8° 6.5 ° 5°5° LEVEL OF CONDENSATION 11° 18.5° 17° 15.5° 14° 12.5° 9.5° 8°8° Property of Lear Siegler
44
17 ° 14 ° 12.5 ° 11 ° 9.5 ° 8°8° 6.5 ° 5°5° 11° 18.5° 17° 15.5° 14° 12.5° 9.5° 8°8° Property of Lear Siegler OLR=1.5° DEWPOINT=14° OLR 1.5 or less: STABLE conditions
45
OLR=2° DP=14° 18° 16° 14° 12° 10° OLR=3° DEWPOINT=14° 17° 2° 8° 14° 11° 5° -1° -4° Property of Lear Siegler
46
OLR=3° DEWPOINT=14° 17 ° 14 ° DRY ADIABATIC LAPSE RATE 3°/1000’ 17° 2° 8° 14° 11° 5° -1° -4° Property of Lear Siegler
47
17 ° 14 ° DEWPOINT=14° OLR=3° MOIST LAPSE RATE 1.5°/1000’ 12.5 ° 11 ° 9.5 ° 8°8° 6.5 ° 5°5° LEVEL OF CONDENSATION LEVEL OF FREE CONVECTION 17° 2° 8° 14° 11° 5° -1° -4° Property of Lear Siegler
48
17 ° 14 ° DEWPOINT=14° OLR=3° 12.5 ° 11 ° 9.5 ° 8°8° 6.5 ° 5°5° 17° 2° 8° 14° 11° 5° -1° -4° Property of Lear Siegler OLR 3 o or greater: UNSTABLE conditions LCL LFC
49
17 ° 14 ° DEWPOINT=14° OLR=2° 12.5 ° 11 ° 9.5 ° 8°8° 6.5 ° 5°5° 12° 18° 16° 14° 10° 8° 6° 4° Property of Lear Siegler OLR between 1.5 o and 3 o : CONDITIONALLY UNSTABLE LCL
52
ELO 8 Action: The student will identify how clouds are formed. Condition: Given pertinent information about clouds Standard: IAW FM 1-230 para 8-1
53
Extremely small condensed water vapor droplets suspended in the atmosphere (less than.002”) Property of Lear Siegler Direct result of saturation and saturation is the result of cooling Direct result of saturation and saturation is the result of cooling. Clouds
54
Cooling Process ADIABATIC NOCTURNAL ADVECTION Property of Lear Siegler
55
ELO 9 Action: The student will identify the basic types of clouds. Condition: Given pertinent information about clouds Standard: IAW FM 1-230 para 8-2
56
Cloud Catagories Cumulus Stratus
57
Property of Lear Siegler 1.Cumulus Indicating Unstable Conditions
58
Property of Lear Siegler 2. Stratus Indicating Stable Conditions
59
ELO 10 Action: The student will identify the classification of clouds in terms of the cloud’s altitude. Condition: Given pertinent information about clouds Standard: IAW FM 1-230 para 8-3,4,5
60
Cloud Descriptors (a) Nimbus / Nimbo (b) Fracto (c) Alto
61
(a) LOW: LESS THAN 6500’ (b) MIDDLE: 6,500 – 18,000 (c) HIGH: ABOVE, 18,000 Cloud Altitudes
62
ELO 11 Action: The student will identify cloud types by assigned abbreviations. Condition: Given pertinent information about clouds Standard: IAW FM 1-230 para 8-3,4,5
63
CumulonimbusCb StratusSt NimbostratusNs StratocumulusSc AltocumulusAc AltostratusAs CirrusCi CumulusCu CirrostratusCs CirrocumulusCc LOW, LESS THAN 6500’ MIDDLE, 6,500 –18,000 HIGH,ABOVE 18,000 Property of Lear Siegler
64
Cu Cumulus
65
Cb
67
Cumulonimbus Cumulus
70
Cumulus – Anvil
71
Cumulus
72
Cumulus - Anvil
74
Sc
76
sc Stratocumulus
77
sc
78
st
79
St Stratus
80
Ns Nimbostratus
81
cc
82
Altocumulus
83
Ac
84
AS
85
Ac
86
Ci Cirrus
88
cs
89
Cirrostratus
90
Cirrocumulus
92
cc
93
cc
94
Ci,Cs
101
ELO 12 Action: The student will identify the flight conditions that would be encountered in the two basic cloud types. Condition: Given pertinent information about clouds Standard: IAW FM 1-230 para 8-5, 6
102
Flight Conditions Cumulus / Cumulonimbus Cumulus / Cumulonimbus Stratus Stratus
103
Safety First… Takeoffs are optional… Landings are mandatory!
104
FM 1-230 References for today… Moisture Chapter 4 Moisture Chapter 4 Stability Chapter 7 Stability Chapter 7 Clouds Chapter 8 Clouds Chapter 8
105
FM 1-230 References for tomorrow… Frontal Weather Chapter 10 Frontal Weather Chapter 10
106
The end
107
STOP Abandon hope all ye who enter here You are entering the hidden slide Zone
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.