- Page 2: The Earth’s Atmosphere Contents O
- Page 6: substances, producing oxides. It is
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- Page 14: within its hot interior escaped thr
- Page 18: Altitude (km) 120 110 100 90 80 70
- Page 22: Focus on an Observation THE RADIOSO
- Page 26: Weather and Climate When we talk ab
- Page 30: winds are light and skies are gener
- Page 34: Up to this point, we have looked at
- Page 38: side of the coin, the bitter cold w
- Page 44: 22 Chapter 1 The Earth’s Atmosphe
- Page 50: Warming the Earth and the Atmospher
- Page 54: A formula for converting °C to °F
- Page 58: important mechanism for the relocat
- Page 62: Parcel of air Focus on a Special To
- Page 66: Focus on a Special Topic SUN BURNIN
- Page 70: ture. For example, a black object i
- Page 74: Incoming solar energy (a) Without g
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- Page 86: Focus on an Observation THE AURORA
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22, the earth will have moved so th
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Focus on a Special Topic IS DECEMBE
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kinetic energy temperature absolute
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54 Chapter 3 Air Temperature Air te
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56 Chapter 3 Air Temperature Focus
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58 Chapter 3 Air Temperature Focus
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60 Chapter 3 Air Temperature FIGURE
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62 Chapter 3 Air Temperature Becaus
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64 Chapter 3 Air Temperature Focus
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66 Chapter 3 Air Temperature 4 0 0.
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68 Chapter 3 Air Temperature TABLE
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70 Chapter 3 Air Temperature Focus
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72 Chapter 3 Air Temperature frostb
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Humidity, Condensation, and Clouds
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Groundwater FIGURE 4.1 The hydrolog
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Water vapor Nitrogen Oxygen Air par
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Temperature Relative humidity Tempe
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moisture does not readily evaporate
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Does a volume of hot, humid air rea
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FIGURE 4.13 The high relative humid
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tact with the ground to increase. T
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Steam fog may form above a wet surf
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■ Visible white frost forms in sa
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FIGURE 4.20 Cirrostratus clouds wit
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the heavy, showery variety. The bas
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FIGURE 4.27 Cumulus congestus. This
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FIGURE 4.30 Lenticular clouds formi
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FIGURE 4.32 Mammatus clouds. Clouds
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that these clouds are composed of t
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10. Go to the Sky Identification/Na
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110 Chapter 5 Cloud Development and
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112 Chapter 5 Cloud Development and
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114 Chapter 5 Cloud Development and
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116 Chapter 5 Cloud Development and
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118 Chapter 5 Cloud Development and
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120 Chapter 5 Cloud Development and
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122 Chapter 5 Cloud Development and
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124 Chapter 5 Cloud Development and
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126 Chapter 5 Cloud Development and
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128 Chapter 5 Cloud Development and
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130 Chapter 5 Cloud Development and
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132 Chapter 5 Cloud Development and
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134 Chapter 5 Cloud Development and
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136 Chapter 5 Cloud Development and
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Air Pressure and Winds Contents Atm
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Air column 1 Air column 2 • •
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in. Hg mb 32.78 32.48 32.19 31.89 3
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Protective case Amplifying levers A
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Focus on a Special Topic ISOBARIC M
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faster the water moves. In a simila
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✈ ✈ ✈ tion). On the equator,
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similar to water in a stream flowin
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-15 -10 H the isobars, blowing from
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1008 1004 1008 1004 1000 • Santia
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WNW W WSW NW 315° 360° half of th
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Focus on a Special Topic WIND POWER
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16. What does the Coriolis force do
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166 Chapter 7 Atmospheric Circulati
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168 Chapter 7 Atmospheric Circulati
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170 Chapter 7 Atmospheric Circulati
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172 Chapter 7 Atmospheric Circulati
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174 Chapter 7 Atmospheric Circulati
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176 Chapter 7 Atmospheric Circulati
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178 Chapter 7 Atmospheric Circulati
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180 Chapter 7 Atmospheric Circulati
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182 Chapter 7 Atmospheric Circulati
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184 Chapter 7 Atmospheric Circulati
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186 Chapter 7 Atmospheric Circulati
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188 Chapter 7 Atmospheric Circulati
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190 Chapter 7 Atmospheric Circulati
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192 Chapter 7 Atmospheric Circulati
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194 Chapter 7 Atmospheric Circulati
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Air Masses, Fronts, and Middle-Lati
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with different physical properties
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Sinking air develops above the larg
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Focus on a Special Topic THE RETURN
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easters (or nor’easters) bringing
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A weak, but often persistent, flow
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H 1020 mP 34 25 A -8 -12 cP B 1024
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showers and thunderstorms, called a
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TABLE 8.3 Typical Weather Condition
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In a warm occlusion, the upper-leve
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usually most intense, with clouds a
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When a storm develops or intensifie
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Focus on a Special Topic A CLOSER L
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H C MAX (a) Day 1 (b) Day 2 L D Jet
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12. Describe the characteristics of
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228 Chapter 9 Weather Forecasting W
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230 Chapter 9 Weather Forecasting U
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232 Chapter 9 Weather Forecasting g
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234 Chapter 9 Weather Forecasting s
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236 Chapter 9 Weather Forecasting L
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238 Chapter 9 Weather Forecasting F
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240 Chapter 9 Weather Forecasting T
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242 Chapter 9 Weather Forecasting u
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244 Chapter 9 Weather Forecasting G
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246 Chapter 9 Weather Forecasting H
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248 Chapter 9 Weather Forecasting A
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250 Chapter 9 Weather Forecasting a
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Thunderstorms and Tornadoes Content
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The appearance of the downdraft mar
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do not have enough time to form. Ap
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Microbursts are capable of blowing
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generate new updrafts on the right
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derstorm development. The moisture
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Focus on a Special Topic THE TERRIF
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frequency of thunderstorms is near
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_ + + _ + + _ + _ _ _ _ _ _ _ Stepp
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the tip and follow the metal rod ha
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Now that we have looked at thunders
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36 tornadoes, more typical of those
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Statistics reveal that the majority
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the winter, tornadoes are most like
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FIGURE 10.33 A wall cloud photograp
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FIGURE 10.35 A tornado-spawning thu
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than tornadoes and they only last f
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4. Use the Severe Weather/Lightning
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290 Chapter 11 Hurricanes Born over
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292 Chapter 11 Hurricanes Southern
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294 Chapter 11 Hurricanes The amoun
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296 Chapter 11 Hurricanes results u
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298 Chapter 11 Hurricanes Focus on
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300 Chapter 11 Hurricanes 20-foot w
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302 Chapter 11 Hurricanes Focus on
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304 Chapter 11 Hurricanes several b
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306 Chapter 11 Hurricanes FIGURE 11
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308 Chapter 11 Hurricanes Number of
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310 Chapter 11 Hurricanes 7. (a) De
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Air Pollution Contents A Brief Hist
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The first major documented air poll
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dangerous substances include asbest
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Carbon monoxide (CO), a major pollu
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disappointing because ozone, as we
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where it formed tiny droplets of su
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In Mexico City, Mexico, air polluti
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pollutants by spreading them apart
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Cubatao, Brazil, just may be the mo
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Focus on an Observation FIVE DAYS I
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Country breeze downwind from this c
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Estimates are that acid rain has se
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18. Give several reasons why taller
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340 Chapter 13 Global Climate Our o
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342 Chapter 13 Global Climate FIGUR
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344 Chapter 13 Global Climate North
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346 Chapter 13 Global Climate Focus
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348 Chapter 13 Global Climate FIGUR
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350 Chapter 13 Global Climate 64°F
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352 Chapter 13 Global Climate Tropi
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354 Chapter 13 Global Climate FIGUR
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356 Chapter 13 Global Climate FIGUR
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358 Chapter 13 Global Climate Focus
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360 Chapter 13 Global Climate is ca
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362 Chapter 13 Global Climate Humid
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364 Chapter 13 Global Climate °F 6
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366 Chapter 13 Global Climate J F M
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368 Chapter 13 Global Climate Quest
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Climate Change Contents The Earth
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(a) 10 15 20 25 25 20 15 10 10 20 2
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ended abruptly, and by 8000 y.a. th
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Focus on a Special Topic THE GREENH
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(a) (b) FIGURE 14.6 Geographical di
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Axis now 231/2° (a) Axis in approx
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light, which warms the air around t
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changes brought on by the Pinatubo
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To sum up, fluctuations in solar ou
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ation from the earth than they emit
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CO 2 levels increase, more precipit
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precipitation across the United Sta
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Focus on a Special Topic The Sahel
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16. Explain how the ocean’s conve
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400 Chapter 15 Light, Color, and At
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402 Chapter 15 Light, Color, and At
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404 Chapter 15 Light, Color, and At
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406 Chapter 15 Light, Color, and At
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408 Chapter 15 Light, Color, and At
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410 Chapter 15 Light, Color, and At
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412 Chapter 15 Light, Color, and At
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414 Chapter 15 Light, Color, and At
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416 Chapter 15 Light, Color, and At
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418 Chapter 15 Light, Color, and At
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420 Chapter 15 Light, Color, and At
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438 Additional Reading Material De
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422 Appendix A Mass 1 gram (g) = 0.
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APPENDIX B Equations and Constants
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426 Appendix B Relative Humidity Th
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428 Appendix C Wind Entries Miles (
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430 Appendix D TABLE D.2 Relative H
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TABLE D.4 Relative Humidity (Percen
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APPENDIX F Heat Index (HI) Table TA
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APPENDIX H Standard Atmosphere 436
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Glossary Absolute humidity The mass
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Cap cloud See Pileus cloud. Carbon
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long enough to cause serious effect
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Heating degree-day A form of the de
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cycle of an air-mass thunderstorm.
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elative to one another across the s
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Snow A solid form of precipitation
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Transpiration The process by which