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The Earth’s Atmosphere Contents Part 3 ppt

The Earth’s Atmosphere Contents Part 3 ppt

The Earth’s Atmosphere Contents Part 3 ppt

... lingering close to the ground. As the day progresses, sunlight warms the surface and the surface warms the air above. As the air temperature near the ground increases, the lower atmosphere graduallybecomes ... Fig. 4 .33 ). The condensation may come di-rectly from the water vapor added to the air from engine ex-haust. In this case, there must be sufficient mixing of the hot exhaust gases with the cold ... of the drop and on its rate of fall: The greater its speed, the more air molecules the drop encounters each second. The speed of the falling drop increases until the air re-sistance equals the...
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The Earth’s Atmosphere Contents Part 1 pptx

The Earth’s Atmosphere Contents Part 1 pptx

... Appendix A.1 73 –100 –148– 130 –901 83 –112–801 93 –94–702 03 –76–58–60–50–40 30 2 13 2 23 233 2 43 –40–22–4–2014–102 53 2 63 2 73 2 83 2 93 3 03 3 23 333 34 3 35 301020 30 4050607080 32 50688610412214015817690100 36 3 37 3212194°F°CKBoiling ... temperature drops dramatically with height.Above the mesosphere lies the warmest part of the atmosphere, the thermosphere. At the top of the ther-mosphere is the exosphere, where collisions between gas ... andsymbols.Overview of the Earth’s Atmosphere Composition of the Atmosphere The Early Atmosphere Vertical Structure of the Atmosphere A Brief Look at Air Pressure and Air DensityLayers of the Atmosphere Focus...
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The Earth’s Atmosphere Contents Part 2 pdf

The Earth’s Atmosphere Contents Part 2 pdf

... –21 –26 31 36 –42 –47 –52 –57 – 63 –68 30 3 –8 –14 –20 –25 31 3743 –48 –54 –60 –65 –71 –7740 –5 –11 –17 – 23 –29 35 –41 –47 – 53 –59 –65 –71 –77 – 83 50 –6 –12 –18 –25 31 3743 –49 –56 ... –110 30 6 –2 –10 –18 –25 33 –41 –49 –56 –64 –71 –79 –86 – 93 –101 –109 –116 35 4 –4 –12 –20 –27 3543 –52 –58 –67 –74 –82 –89 –97 –105 –1 13 –12040 3 –5 – 13 –21 –29 37 –45 – 53 –60 –69 –76 –84 –92 ... about 3 percent, the energy that strikes the top of the earth’s atmosphere is almost 7 percentgreater on January 3 than on July 4. These statistics might48 Chapter 2 Warming the Earth and the Atmosphere Balance...
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The Earth’s Atmosphere Contents Part 4 pdf

The Earth’s Atmosphere Contents Part 4 pdf

... hourKnotsCalmCalm1–2 3 89–1415–2021–2526 31 32 37 3843 44–4950–5455–6061–6667–7172–7778– 83 84–89119–1 23 1–2 3 78–12 13 1718–22 23 2728 32 33 37 38 –42 43 4748–52 53 5758–62 63 6768–72 73 771 03 107HHL558056405700576058205880–10–15–20–25–20–15–10FIGURE ... hourKnotsCalmCalm1–2 3 89–1415–2021–2526 31 32 37 3843 44–4950–5455–6061–6667–7172–7778– 83 84–89119–1 23 1–2 3 78–12 13 1718–22 23 2728 32 33 37 38 –42 43 4748–52 53 5758–62 63 6768–72 73 771 03 107NL10121016 1020 10241012x'x1008100810041000996992988984980976972FIGURE ... greater the pressuregradient. The greater the pressure gradient, the stronger the pressure gradient force (PGF). The stronger the PGF, the greater the wind speed. The red arrows represent the relativemagnitude...
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The Earth’s Atmosphere Contents Part 5 potx

The Earth’s Atmosphere Contents Part 5 potx

... sky.” 30 29100910102215100726 23 10092418100927 23 10061004100810 03 1004100948464745P10051006544910085147P'00200100kmmiN 53 5022 35 35 33 32 27251005 32 32 10051002 31 30 10061007 37 37 32 32 10 03 38 38 1009 31 30 1006”••”2510091006kmFIGURE ... sky.” 30 29100910102215100726 23 10092418100927 23 10061004100810 03 1004100948464745P10051006544910085147P'00200100kmmiN 53 5022 35 35 33 32 27251005 32 32 10051002 31 30 10061007 37 37 32 32 10 03 38 38 1009 31 30 1006”••”2510091006kmFIGURE 8.14Surface weather associated with a typical warm front. (Green-shaded ... 510–6–14–29 37 17–2010561060H101210161810 36 2812 8– 23 33 1020104410401 036 16 3 1 032 1016 53 43 49441012100810041020102410281 032 6meted to a new low of –22°C (–7°F) for the airports...
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The Earth’s Atmosphere Contents Part 6 docx

The Earth’s Atmosphere Contents Part 6 docx

... hourKnotsCalmCalm1–2 3 89–1415–2021–2526 31 32 37 3843 44–4950–5455–6061–6667–7172–7778– 83 84–89119–1 23 1–2 3 78–12 13 1718–22 23 2728 32 33 37 38 –42 43 4748–52 53 5758–62 63 6768–72 73 771 03 107LL546055205580564057005760FIGURE ... 10 .32 Some of the features associatedwith a tornado-breeding thunder-storm as viewed from the southeast. The thunderstorm ismoving to the northeast. The tornado forms in the southwest part ... rodFIGURE 10. 23 The lightning rod extends above the building, increasing the like-lihood that lightning will strike the rod rather than some other part of the structure. After lightning strikes the metal...
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The Earth’s Atmosphere Contents Part 7 doc

The Earth’s Atmosphere Contents Part 7 doc

... the broad belt around the earth known as the trop-ics the region 23 1⁄2° north and south of the equator— the weather is much different from that of the middlelatitudes. In the tropics, the ... stable atmosphere tends to spread horizontally, rather than mix vertically. The stability of the atmosphere is determined by the way the air temperature changes with height (the lapse rate). When the ... spell. The winds in the tropics generally blow from the east, northeast, or southeast the trade winds. Because the variation of sea-level pressure is normally quitesmall, drawing isobars on a weather...
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The Earth’s Atmosphere Contents Part 8 doc

The Earth’s Atmosphere Contents Part 8 doc

... (9 93 days)❶❷❸❹❺❻❼❽❾❿1168 cm (460 in.) 930 cm (36 6 in.) 135 cm ( 53 in.)109 cm ( 43 in.) 30 cm (12 in.) 3 cm (1.2 in.) 3 cm (1.2 in.)0.08 cm (0. 03 in.)2896 cm (1140 in.)991 cm (39 0 ... 18°C The Global Pattern of Climate 35 30510152025 30 °CDNOSAJJMAMFJ 02420 30 4050°FJFMAMJJASONDMean annual temperature: 23. 3°C (74°F)152025 30 35 68101214In.Cm60 35 Annual ... downwind.Either these particles and gases slowly settle to the ground in dry form (dry deposition) or they are re-moved from the air during the formation of cloud particles and then carried to the...
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The Earth’s Atmosphere Contents Part 9 potx

The Earth’s Atmosphere Contents Part 9 potx

... (eccentricity) of the earth’s orbitabout the sun2. precession of the earth’s axis of rotation, or wobbling 3. changes in the tilt (obliquity) of the earth’s axisIn the 1970s, scientists of the CLIMAP ... episodes during the past 2 mil-lion years are the result of small variations in the tilt of the earth’s axis and in the geometry of the earth’s orbitaround the sun. Another theory suggests ... then reflected off the back-side of the droplet. The light thenexits at the other side of the droplet, being refracted onceagain (see Fig. 3) . The colorfulrings may be due to the variousangles...
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The Earth’s Atmosphere Contents Part 10 docx

The Earth’s Atmosphere Contents Part 10 docx

... 5 –5 32 30 29 29 28 27 27 26 25 25 24 23 19 14 9 2 –11 32 .5 32 31 31 30 29 29 28 27 26 26 22 18 13 7 –2 35 34 34 33 32 32 31 31 30 29 28 25 21 16 11 4 37 .5 37 36 36 35 34 34 33 32 32 31 28 24 ... 40 39 39 38 38 37 36 36 35 34 34 30 27 23 18 13 642.5 42 41 41 40 40 39 38 38 37 36 33 30 26 22 17 1145 44 44 43 43 42 42 41 40 40 39 36 33 29 25 21 1547.5 47 46 46 45 45 44 44 43 42 42 39 35 ... 21 17 13 7 0 –1140 38 35 33 30 28 25 21 18 13 7 –1 –1445 43 41 38 36 34 31 28 25 22 18 13 7 –1 –1450 48 46 44 42 40 37 34 32 29 26 22 18 13 8 0 – 13 55 53 51 50 48 45 43 41 38 36 33 30 27 24...
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