1 / 126

Review for Chapter 37 38

The Earth's oceans likely evolved. From the condensation of water vapor in the hyrogen-oxygen rich atmWith the accumulation of rainfallFrom the condensation of water vapor from volcanic eruptionsAs the Earth cooled. The Earth's oceans likely evolved. From the condensation of water vapor in the hy

terri
Download Presentation

Review for Chapter 37 38

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


    1. Review for Chapter 37 & 38 Mrs. Senger

    2. The Earths oceans likely evolved From the condensation of water vapor in the hyrogen-oxygen rich atm With the accumulation of rainfall From the condensation of water vapor from volcanic eruptions As the Earth cooled

    3. The Earths oceans likely evolved From the condensation of water vapor in the hyrogen-oxygen rich atm With the accumulation of rainfall From the condensation of water vapor from volcanic eruptions As the Earth cooled

    4. The earths earliest atm was lacking in Carbon dioxide Photosynthesis Free oxygen Hydrogen

    5. The earths earliest atm was lacking in Carbon dioxide Photosynthesis Free oxygen Hydrogen

    6. The process of photosynthesis is important because photosynthesis Allows plants to grow to larger size Is an energy source that drives the metabolic process Converts carbon dioxide and water to hydrogen & free oxygen All of these

    7. The process of photosynthesis is important because photosynthesis Allows plants to grow to larger size Is an energy source that drives the metabolic process Converts carbon dioxide and water to hydrogen & free oxygen All of these

    8. The atm is divided into several layers. The troposphere is the The atmosphere's 3rd layer and the thickest layer Lowest layer and the thickest layer, where earths weather occurs Lowest layer and the thinnest, where the earths weather occurs None of these

    9. The atm is divided into several layers. The troposphere is the The atmosphere's 3rd layer and the thickest layer Lowest layer and the thickest layer, where earths weather occurs Lowest layer and the thinnest, where the earths weather occurs None of these

    10. The ozone layer is a region within the Ionosphere Troposphere Mesosphere Stratosphere

    11. The ozone layer is a region within the Ionosphere Troposphere Mesosphere Stratosphere

    12. The layers of the earths atm, from top to bottom, are the Troposphere, stratosphere, ozone layer, mesosphere, thermosphere, ionosphere and exosphere Exosphere, thermosphere, mesosphere, stratosphere, and troposphere Exosphere, ionosphere, thermosphere, mesosphere, ozonosphere, stratosphere and troposphere Troposphere, stratosphere, mesosphere, thermosphere and exosphere

    13. The layers of the earths atm, from top to bottom, are the Troposphere, stratosphere, ozone layer, mesosphere, thermosphere, ionosphere and exosphere Exosphere, thermosphere, mesosphere, stratosphere, and troposphere Exosphere, ionosphere, thermosphere, mesosphere, ozonosphere, stratosphere and troposphere Troposphere, stratosphere, mesosphere, thermosphere and exosphere

    14. The temperature in the thermosphere reaches a whooping 2000 degrees C. This extreme temperature has very little significance because The thermosphere is very far from the Earths surface There are not enough air molecules & atoms colliding with one another to generate heat energy There is very little ozone in the air to absorb the solar radiation Few atoms and air molecules in this region move slowly enough to absorb much solar radiation

    15. The temperature in the thermosphere reaches a whooping 2000 degrees C. This extreme temperature has very little significance because The thermosphere is very far from the Earths surface There are not enough air molecules & atoms colliding with one another to generate heat energy There is very little ozone in the air to absorb the solar radiation Few atoms and air molecules in this region move slowly enough to absorb much solar radiation

    16. The ionosphere Is produced by the action of solar radiation and atmospheric atoms Reflects solar ultraviolet & atmospheric atoms Consist of ozone ions Occurs at roughly the same altitude as high clouds

    17. The ionosphere Is produced by the action of solar radiation and atmospheric atoms Reflects solar ultraviolet & atmospheric atoms Consist of ozone ions Occurs at roughly the same altitude as high clouds

    18. The tilt of the earths axis greatly affects the Change of the earths seasons Intensity of sunlight that reaches the earths surface Hours of daylight All of these

    19. The tilt of the earths axis greatly affects the Change of the earths seasons Intensity of sunlight that reaches the earths surface Hours of daylight All of these

    20. The angle of the suns rays striking the earths surface greatly affects the Earths seasons Intensity of solar energy received at the earths surface Equatorial and polar regions All of these

    21. The angle of the suns rays striking the earths surface greatly affects the Earths seasons Intensity of solar energy received at the earths surface Equatorial and polar regions All of these

    22. The lower atmosphere is directly warmed By the absorption of terrestrial radiation From the weight of the atmosphere above By the emission of terrestrial radiation By incoming solar radiation

    23. The lower atmosphere is directly warmed By the absorption of terrestrial radiation From the weight of the atmosphere above By the emission of terrestrial radiation By incoming solar radiation

    24. At the end of December, all the Southern Hemisphere is in Summer Winter Darkness Light

    25. At the end of December, all the Southern Hemisphere is in Summer Winter Darkness Light

    26. Almost all of the earths supply of energy come from The Sun Carbon dioxide The earths interior The oceans

    27. Almost all of the earths supply of energy come from The Sun Carbon dioxide The earths interior The oceans

    28. Air near the equator averages higher temperatures than air near the poles because The oceans near the equator are warmer than those near the poles Polar air is cooled by ice and snow on the ground Infrared radiation is absorbed more readily in equatorial air due to increased levels of carbon dioxide and water vapor Sunlight falls in more vertical position at the equator than near the poles

    29. Air near the equator averages higher temperatures than air near the poles because The oceans near the equator are warmer than those near the poles Polar air is cooled by ice and snow on the ground Infrared radiation is absorbed more readily in equatorial air due to increased levels of carbon dioxide and water vapor Sunlight falls in more vertical position at the equator than near the poles

    30. Wind is generated in response to Pressure differences Temperature differences The unequal heating of the earths surface All of these

    31. Wind is generated in response to Pressure differences Temperature differences The unequal heating of the earths surface All of these

    32. The Coriolis effect greatly affects the path of air circulation, and it is the result of The tilt of the earth The earths rotation Global winds All of these

    33. If a volume of air is warmed, it expands. After it expands the volume of air expands because it Cools Warms Neither cools or warms Does both

    34. If a volume of air is warmed, it expands. After it expands the volume of air expands because it Cools Warms Neither cools or warms Does both

    35. The wind blows in response to Pressure differences The earths rotation Temperature differences Pressure and temperature differences

    36. The wind blows in response to Pressure differences The earths rotation Temperature differences Pressure and temperature differences

    37. Fresh water leaves the ocean by Precipitation, evaporation and runoff Condensation Evaporation, sublimation and freezing Evaporation and formation of ice

    38. Fresh water leaves the ocean by Precipitation, evaporation and runoff Condensation Evaporation, sublimation and freezing Evaporation and formation of ice

    39. When precipitation at the ocean surface exceeds evaporation, the salinity of seawater Increases Decreases Stays the same Not enough info

    40. When precipitation at the ocean surface exceeds evaporation, the salinity of seawater Increases Decreases Stays the same Not enough info

    41. The two most abundant elements that make up the salinity of seawater are Sodium and potassium Chlorine and sulfur Chlorine and sodium Calcium and sulfur

    42. The two most abundant elements that make up the salinity of seawater are Sodium and potassium Chlorine and sulfur Chlorine and sodium Calcium and sulfur

    43. Most surface ocean currents are due to River flow into the oceans Melting polar glaciers Density differences in vertical profile of the oceans Winds

    44. Most surface ocean currents are due to River flow into the oceans Melting polar glaciers Density differences in vertical profile of the oceans Winds

    45. Because the Coriolis effect, a wind in the Northern Hemisphere is deflected Upward Downward Toward the right Toward the left

    46. Because the Coriolis effect, a wind in the Northern Hemisphere is deflected Upward Downward Toward the right Toward the left

    47. Air currents are sensitive to changes in pressure and temperature. In general, air moves from regions of Low pressure to regions of high pressure High temperatures and low pressure to regions of low temperature and high pressure Low temperature and high pressure to regions of high temperature and low pressure High pressure to regions of low pressure

    48. Air currents are sensitive to changes in pressure and temperature. In general, air moves from regions of Low pressure to regions of high pressure High temperatures and low pressure to regions of low temperature and high pressure Low temperature and high pressure to regions of high temperature and low pressure High pressure to regions of low pressure

    49. The ocean has many layers amongst itself. The layers form due to differences in Salinity Temperature Both neither

    50. The ocean has many layers amongst itself. The layers form due to differences in Salinity Temperature Both neither

    51. What is the driving force of energy in the planets hydrologic cycle? Solar energy Wind Precipitation of water over the oceans The balance of precipitation and evaporation

    52. What is the driving force of energy in the planets hydrologic cycle? Solar energy Wind Precipitation of water over the oceans The balance of precipitation and evaporation

    53. The Coriolis effect greatly affects the path of circulation, and is the result of what? The Earths rotation The tilt of the earth Global winds Wind changes

    54. The Coriolis effect greatly affects the path of circulation, and is the result of what? The Earths rotation The tilt of the earth Global winds Wind changes

    55. The changing of a substance from a liquid into a vapor or gas is called Dew point Evaporation Condensation Saturation point

    56. The changing of a substance from a liquid into a vapor or gas is called Dew point Evaporation Condensation Saturation point

    57. The changing of a vapor into a liquid is called Saturation point Dew point Evaporation Condensation

    58. The changing of a vapor into a liquid is called Saturation point Dew point Evaporation Condensation

    59. The amount of water vapor the air can hold depends on the air temperature. At higher temperatures the air Is saturated Holds water at dew point Holds less water Can hold more water

    60. The amount of water vapor the air can hold depends on the air temperature. At higher temperatures the air Is saturated Holds water at dew point Holds less water Can hold more water

    61. The temperature to which air must be cooled for saturation to occur is called Relative humidity Dew point Precipitation Condensation point

    62. The temperature to which air must be cooled for saturation to occur is called Relative humidity Dew point Precipitation Condensation point

    63. The limit at which the air contains as much moisture as it can hold for a given temperature is called Dew point Saturation Evaporation point Sublimation point

    64. The limit at which the air contains as much moisture as it can hold for a given temperature is called Dew point Saturation Evaporation point Sublimation point

    65. We feel uncomfortably warm on a muggy day because water molecules are Jostling about Preventing evaporation from our body Condensing on our skin Evaporating from out body

    66. We feel uncomfortably warm on a muggy day because water molecules are Jostling about Preventing evaporation from our body Condensing on our skin Evaporating from out body

    67. Evaporation of rain drops in the atmosphere Is greatest above the polar ice caps Does not happen; rain always reaches the earth Cools the air Warms the air

    68. Evaporation of rain drops in the atmosphere Is greatest above the polar ice caps Does not happen; rain always reaches the earth Cools the air Warms the air

    69. As air temperature decreases, relative humidity Stays the same Drops Decreases Increases

    70. As air temperature decreases, relative humidity Stays the same Drops Decreases Increases

    71. As air rises, it Compresses and cools Compresses and warms Expands and cools Expands and warms

    72. As air rises, it Compresses and cools Compresses and warms Expands and cools Expands and warms

    73. We are warmed by condensation because water molecules in the air that strike our bodies Gain kinetic energy as they change state Transfer kinetic energy to us Form an insulating layer on our bodies None of these

    74. We are warmed by condensation because water molecules in the air that strike our bodies Gain kinetic energy as they change state Transfer kinetic energy to us Form an insulating layer on our bodies None of these

    75. Warm air rises and cools as it expands. Warm air will continue to rise as long as it is Snowing Warmer and more dense than the air above Warmer and less dense than the surrounding air Denser than the surrounding air

    76. Warm air rises and cools as it expands. Warm air will continue to rise as long as it is Snowing Warmer and more dense than the air above Warmer and less dense than the surrounding air Denser than the surrounding air

    77. An air parcel expands and cools, or compresses and warms, with no interchange of heat with its surroundings, the situation is called An adiabatic process Temperature equilibrium Lapse rate Stable equilibrium

    78. An air parcel expands and cools, or compresses and warms, with no interchange of heat with its surroundings, the situation is called An adiabatic process Temperature equilibrium Lapse rate Stable equilibrium

    79. When a volume of air is compressed, its temperature Decreases Increases Both None of these

    80. When a volume of air is compressed, its temperature Decreases Increases Both None of these

    81. A drop in pressure is an indication of Sunny skies and clear weather Adiabetic warming Cloudy weather None of these

    82. A drop in pressure is an indication of Sunny skies and clear weather Adiabetic warming Cloudy weather None of these

    83. A rise in pressure indicates Adiabatic warming Cloudy weather Sunny skies and clear weather None of these

    84. A rise in pressure indicates Adiabatic warming Cloudy weather Sunny skies and clear weather None of these

    85. Clouds occur when moist air is cooled by Compression when it rises Expansion when it rises Expansion when it falls Compression when it falls

    86. Clouds occur when moist air is cooled by Compression when it rises Expansion when it rises Expansion when it falls Compression when it falls

    87. Warm humid air is characteristic of a Continental polar air mass Maritime polar air mass Maritime tropical air mass Continental tropical air mass

    88. Warm humid air is characteristic of a Continental polar air mass Maritime polar air mass Maritime tropical air mass Continental tropical air mass

    89. When an air mass is pushed upward over an obstacle, it undergoes Orographical lifting Convectional lifting Adiabatic lifting Frontal lifting

    90. When an air mass is pushed upward over an obstacle, it undergoes Orographical lifting Convectional lifting Adiabatic lifting Frontal lifting

    91. An air mass with circulatory motion is called Frontal Adiabatic Orographic Convectional

    92. An air mass with circulatory motion is called Frontal Adiabatic Orographic Convectional

    93. Atmspheric lifting resulting from the convergence of 2 different air masses is called Orographic lifting Convectional lifting Frontal lifting Adiabatic lifting

    94. Atmspheric lifting resulting from the convergence of 2 different air masses is called Orographic lifting Convectional lifting Frontal lifting Adiabatic lifting

    95. When a cold air mass moves into a region occupied by a warm air mass, the contact zone is called A warm front A cold front An occluded front A stationary front

    96. When a cold air mass moves into a region occupied by a warm air mass, the contact zone is called A warm front A cold front An occluded front A stationary front

    97. When a warm air mass moves into a region occupied by a cold air mass, the contact zone is called A warm front A cold front An occluded front A stationary front

    98. When a warm air mass moves into a region occupied by a cold air mass, the contact zone is called A warm front A cold front An occluded front A stationary front

    99. Lower temperatures can be expected Ahead of an advancing cold front Behind an advancing cold front Behind a stationary warm front Behind an advancing warm front

    100. Lower temperatures can be expected Ahead of an advancing cold front Behind an advancing cold front Behind a stationary warm front Behind an advancing warm front

    101. Towering cumulonimbus clouds are a common feature in regions where moist unstable air is heated from below. Such clouds are produced by Frontal lifting Orographic lifting Convectional lifting None of these

    102. Towering cumulonimbus clouds are a common feature in regions where moist unstable air is heated from below. Such clouds are produced by Frontal lifting Orographic lifting Convectional lifting None of these

    103. If a cool dry day was followed by a warm humid day, you might expect the air masses to have been Continental polar and maritime tropical Continental tropical and continental polar Maritime tropical and continental polar Maritime polar and maritime tropical

    104. If a cool dry day was followed by a warm humid day, you might expect the air masses to have been Continental polar and maritime tropical Continental tropical and continental polar Maritime tropical and continental polar Maritime polar and maritime tropical

    105. Daily afternoon thunderstorms along the Gulf coast are most likely caused by a Maritime tropical air mass Maritime polar air mass Continental tropical air mass Continental polar air mass

    106. Daily afternoon thunderstorms along the Gulf coast are most likely caused by a Maritime tropical air mass Maritime polar air mass Continental tropical air mass Continental polar air mass

    107. Drought conditions and high temperatures over the Great Plains are most likely caused by a Maritime tropical air mass Maritime polar air mass Continental tropical air mass Continental polar air mass

    108. Drought conditions and high temperatures over the Great Plains are most likely caused by a Maritime tropical air mass Maritime polar air mass Continental tropical air mass Continental polar air mass

    109. Cold damp weather along the eastern coast of the United States is most likely caused by a Maritime tropical air mass Maritime polar air mass Continental tropical air mass Continental polar air mass

    110. Cold damp weather along the eastern coast of the United States is most likely caused by a Maritime tropical air mass Maritime polar air mass Continental tropical air mass Continental polar air mass

    111. When a funnel cloud touches the ground, it becomes a Cyclone Tornado Hurricane Thunderstorm

    112. When a funnel cloud touches the ground, it becomes a Cyclone Tornado Hurricane Thunderstorm

    113. Hurricanes are generated In tropical areas As moist thermal winds converge in tropical storms From tropical storms with high levels of moisture and thermal energy By all of these

    114. Hurricanes are generated In tropical areas As moist thermal winds converge in tropical storms From tropical storms with high levels of moisture and thermal energy By all of these

    115. Lightning occurs as water droplets become electrically charged. Energy that is positively charged is found Throughout the cloud Surrounding the cloud At the top of the cloud At the base of the cloud

    116. Lightning occurs as water droplets become electrically charged. Energy that is positively charged is found Throughout the cloud Surrounding the cloud At the top of the cloud At the base of the cloud

    117. The fundamental source of energy released by a tropical hurricane come from The Sun Warm moist air The convergence of maritime polar and maritime tropical air masses The trade winds

    118. The fundamental source of energy released by a tropical hurricane come from The Sun Warm moist air The convergence of maritime polar and maritime tropical air masses The trade winds

    119. The atmospheric condition at a particular location moment in time is called Climate Weather Average temperature Average precipitation level

    120. The atmospheric condition at a particular location moment in time is called Climate Weather Average temperature Average precipitation level

    121. In general, warm days are associated with Summer storms Low surface pressure High surface pressure Negative change in pressure gradient

    122. In general, warm days are associated with Summer storms Low surface pressure High surface pressure Negative change in pressure gradient

    123. All of the Earths weather occurs in the Lower levels of the atmosphere Troposphere Troposphere and stratosphere Tropopause

    124. All of the Earths weather occurs in the Lower levels of the atmosphere Troposphere Troposphere and stratosphere Tropopause

    125. Which of the following has the greatest impact on generating waves in the ocean The movement of sea life causes disturbances in the water The density differences of the water due to the oceans salinity Magma at ocean ridges causing the warm water to rise and cool water to sink Friction with the wind at the surface of the ocean

    126. Which of the following has the greatest impact on generating waves in the ocean The movement of sea life causes disturbances in the water The density differences of the water due to the oceans salinity Magma at ocean ridges causing the warm water to rise and cool water to sink Friction with the wind at the surface of the ocean

More Related