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The Earth’s Atmosphere Contents Part 4 pdf
The Earth’s Atmosphere Contents Part 4 pdf
... 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 ... The difference in wind pressure fromone side of a cup to the other causes the cups to spinabout the shaft. The rate at which they rotate is directlyproportional to the speed of the wind. The ... weather map in Fig. 6.12. Notice that the Why the Wind Blows 149 HPGFPGFPGFPGFPGFPGF1016102010 24 MAP VIEW0200 40 0600Scale (km)FIGURE 6.11 The closer the spacing of the isobars, the...
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The Earth’s Atmosphere Contents Part 2 pdf
... –22 –26 –31 –35 40 44 49 –5320 0 –5 –10 –15 –21 –26 –31 –36 42 47 –52 –57 –63 –6830 –3 –8 – 14 –20 –25 –31 –37 43 48 – 54 –60 –65 –71 –77 40 –5 –11 –17 –23 –29 –35 41 47 –53 –59 –65 –71 ... 41 49 –56 – 64 –71 –79 –86 –93 –101 –109 –11635 4 4 –12 –20 –27 –35 43 –52 –58 –67 – 74 –82 –89 –97 –105 –113 –120 40 3 –5 –13 –21 –29 –37 45 –53 –60 –69 –76 – 84 –92 –100 –107 –115 –123 45 ... 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 might 48 Chapter 2 Warming the Earth and the Atmosphere Balance...
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The Earth’s Atmosphere Contents Part 1 pptx
... 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 ... – 148 –130–90183–112–80193– 94 70203–76–58–60–50 40 –30213223233 243 40 –22 4 –20 14 –10253263273283293303323333 343 3530102030 40 50607080325068861 04 122 140 158176901003633732121 94 °F°CKBoiling ... 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 3 ppt
... in a conditionallyunstable atmosphere over the GreatPlains. Notice that, in the distance, the cumulonimbus with the anvil top hasreached the stable part of the atmosphere. to peer into a tornado-generating ... 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 ... actually become warmer than the air around it. Since the lifted air can rise on its own ac-cord, the atmosphere is now unstable. The level in the atmosphere where the air parcel, after being...
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The Earth’s Atmosphere Contents Part 5 potx
... 8–233310201 044 1 040 103616 31032101653 43 49 44 1012100810 04 102010 24 102810326meted to a new low of –22°C (–7°F) for the airports in Philadelphia and Baltimore.Toward the end of the month, the ... sky.”3029100910102215100726231009 24 1810092723100610 04 1008100310 04 1009 48 46 47 45 P10051006 54 49100851 47 P'00200100kmmiN53502235353332272510053232100510023130100610073737323210033838100931301006”••”2510091006kmFIGURE ... oppositeends of the Pacific Ocean during the SouthernOscillation?(c) Describe how an ENSO event may influence the weather in different parts of the world.19.What are the conditions over the tropical...
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The Earth’s Atmosphere Contents Part 6 docx
... 10.32Some 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 of the thunderstorm. ... 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 ... 245 Miles(statute)per hourKnotsCalmCalm1–23–89– 14 15–2021–2526–3132–3738 43 44 49 50– 54 55–6061–6667–7172–7778–83 84 89119–1231–23–78–1213–1718–2223–2728–3233–3738 42 43 47 48 –5253–5758–6263–6768–7273–77103–107LL 546 0552055805 640 57005760FIGURE...
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The Earth’s Atmosphere Contents Part 7 doc
... the broad belt around the earth known as the trop-ics the region 231⁄2° north and south of the equator— the weather is much different from that of the middlelatitudes. In the tropics, the ... do theyform? And why do they strike the east coast of the UnitedStates more frequently than the west coast? These aresome of the questions we will consider in this chapter.Tropical WeatherIn ... 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
... 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 ... Waialeale on the island of Kauai, Hawaii, has the greatest annual average rainfall on record:1168 cm (46 0 in.). Cherrapunji, on the crest of the southern slopes of the KhasiHills in northeastern ... winter.In the late 1800s, the average global temperaturebegan to rise (see Fig. 14. 5). From about 1900 until about1 940 , the average temperature of the lower atmosphere rose nearly 0.5°C. Following the...
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The Earth’s Atmosphere Contents Part 9 potx
... 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 ... (eccentricity) of the earth’s orbitabout the sun2. precession of the earth’s axis of rotation, or wobbling3. changes in the tilt (obliquity) of the earth’s axisIn the 1970s, scientists of the CLIMAP ... 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
... 38 37 36 33 30 26 22 17 11 45 44 44 43 43 42 42 41 40 40 39 36 33 29 25 21 15 47 .5 47 46 46 45 45 44 44 43 42 42 39 35 32 28 24 1950 49 49 48 48 47 47 46 45 45 44 41 38 35 31 28 23TABLE D.1 ... DePaola.CHAPTER 4 Figs. 4. 7a, 4. 7b, 4. 9, 4. 11, 4. 13, 4. 14, 4. 16, 4. 18, 4. 19, 4. 20, 4. 21, 4. 22, 4. 23, 4. 24, 4. 25, 4. 26, 4. 27, 4. 31, and 4. 33 Photos by author.Fig. 4. 12 Photo by Ross DePaola.Fig. 4. 15 © ... 53 51 49 47 45 43 40 38 35 32 29 25 21 17 11 4 65 63 62 60 59 57 55 53 51 49 47 45 42 40 37 34 31 27 24 1970 69 67 65 64 62 61 59 57 55 53 51 49 47 44 42 39 36 33 3075 74 72 71 69 68 66 64 63...
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