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STRANGE CLOUDS (Chaps. 5 & 6).

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Presentation on theme: "STRANGE CLOUDS (Chaps. 5 & 6)."— Presentation transcript:

1 STRANGE CLOUDS (Chaps. 5 & 6)

2

3

4 Contrails

5 Contrails

6 p. 134

7 This enhanced infrared image from NASA's Terra satellite shows a widespread outbreak of contrails over the southeastern United States during the morning of January 29, Satellite data are critical for studying the effects of contrails. The crisscrossing white lines are contrails that form from planes flying in different directions at different altitudes. Each contrail spreads and moves with the wind. Contrails often form over large areas during winter and spring. CREDIT: NASA

8 Distrail (Dissipation Trail, Canal Cloud)

9 Hole Punch Cloud

10

11 © Vicki Harrison

12 Mountain Waves and Lee Waves (Lenticular)
Page: 161 FIGURE 6.24 Lenticular clouds that form in the wave directly over the mountain are called mountain wave clouds, whereas those that form downwind of the mountain are called lee wave clouds. On the underside of the lee wave’s crest a turbulent rotor cloud may form.

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14 p. 161 Mark J. Madigan, Walsenburg, CO

15 Pileus

16

17 Pileus Formation

18 p. 132

19 Lenticular Clouds FIGURE 6.25 Lenticular clouds forming one on top of the other over the Sierra Nevada.

20 Lenticular Clouds

21 Lenticular Clouds

22 Lenticular Cloud

23 Lenticular Cloud p. 132, 161 © Brian Holden

24

25 Cumulus Castellanus

26 Entrainment Mixing of drier, cooler air along cloud edges. Can cause cloud droplets to evaporate. Entrainment is greater with stronger rising motion in cloud. p. 158

27 Cumulus Castellanus p. 164–165

28 Mammatus

29 Pendules on Contrail

30 Mammatus

31 Mammatus

32 Mammatus

33 Mammatus p. 132

34 Fractostratus (“Scud”)
p. 130

35 Fractostratus (“Scud”)

36 Virga

37 Virga p. 179

38 Billows

39

40 Billows Vertical Wind Shear strong wind weak wind p. 164, 235

41 Billows Page: 164 FIGURE 6.27 Billow clouds forming in a region where wind speed changes rapidly with altitude. This is a region of strong vertical wind shear. (More on the topic of wind shear and the formation of these clouds is given in Chapter 9, p. 235.)

42 Cloud Streets

43 Cloud Streets STABLE UNSTABLE cold ice warm water wind

44 Cloud Streets p. 164, 300


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