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DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_000519 | image | question_images/rain_shadow_7532.png | rain_shadow_7532.png | 1 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_000524 | image | question_images/rain_shadow_7534.png | rain_shadow_7534.png | 0.83535 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_000541 | image | question_images/rain_shadow_8183.png | rain_shadow_8183.png | 0.829084 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_000536 | image | question_images/rain_shadow_7537.png | rain_shadow_7537.png | 0.799474 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DD_0024 | image | teaching_images/rain_shadow_8185.png | The diagram is a representation of how a rain shadow is formed. A rain shadow is a dry region of land on the side of a mountain range that is protected from the prevailing winds. Prevailing winds are the winds that occur most of the time in a particular location on the Earth. The protected side of a mountain range is also called the lee side or the down-wind side. Prevailing winds carry air toward the mountain range. As the air rises up over a mountain range, the air cools, water vapor condenses, and clouds form. On this side of the mountains, called the windward side, precipitation falls in the form of rain or snow. The windward side of a mountain range is moist and lush because of this precipitation. Once the air passes over the mountain range, it moves down the other side, warms, and dries out. This dry air produces a rain shadow. Land in a rain shadow is typically very dry and receives much less precipitation and cloud cover than land on the windward side of the mountain range. | 0.792557 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DD_0023 | image | teaching_images/rain_shadow_7524.png | This diagram shows the effect of rains on hills. The moist air from the green side of the hills rising up in the air and condenses as water vapor. This is called precipitation. The other side of the hill form the rain shadow region. Rain shadow region is a region having little rainfall because it is sheltered from prevailing rain-bearing winds by a range of hills. The dry air descends from this region. | 0.783287 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_000512 | image | question_images/rain_shadow_7529.png | rain_shadow_7529.png | 0.777301 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_009014 | image | question_images/cycle_water_4929.png | cycle_water_4929.png | 0.775978 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_000507 | image | question_images/rain_shadow_7525.png | rain_shadow_7525.png | 0.768386 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | DQ_000533 | image | question_images/rain_shadow_7536.png | rain_shadow_7536.png | 0.767955 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_0251 | text | null | Humidity is the amount of water vapor in the air. High humidity increases the chances of clouds and precipitation. | 0.660804 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_0914 | text | null | An air mass is a batch of air that has nearly the same temperature and humidity (Figure 1.1). An air mass acquires these characteristics above an area of land or water known as its source region. When the air mass sits over a region for several days or longer, it picks up the distinct temperature and humidity characteristics of that region. | 0.642709 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_0916 | text | null | Air masses are slowly pushed along by high-level winds. When an air mass moves over a new region, it shares its temperature and humidity with that region. So the temperature and humidity of a particular location depends partly on the characteristics of the air mass that sits over it. | 0.638723 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_1753 | text | null | The atmosphere is layered, corresponding with how the atmospheres temperature changes with altitude. By under- standing the way temperature changes with altitude, we can learn a lot about how the atmosphere works. | 0.637099 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_0262 | text | null | An air mass is a large body of air that has about the same conditions throughout. For example, an air mass might have cold dry air. Another air mass might have warm moist air. The conditions in an air mass depend on where the air mass formed. | 0.636901 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_1797 | text | null | The two types of air pollutants are primary pollutants, which enter the atmosphere directly, and secondary pollutants, which form from a chemical reaction. | 0.624519 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_1878 | text | null | At a stationary front the air masses do not move (Figure 1.1). A front may become stationary if an air mass is stopped by a barrier, such as a mountain range. A stationary front may bring days of rain, drizzle, and fog. Winds usually blow parallel to the front, but in opposite directions. After several days, the front will likely break apart. | 0.62358 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_1564 | text | null | Some precipitation forms in place. Dew forms when moist air cools below its dew point on a cold surface. Frost is dew that forms when the air temperature is below freezing. | 0.621428 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_0252 | text | null | Humidity usually refers to relative humidity. This is the percent of water vapor in the air relative to the total amount the air can hold. How much water vapor can the air hold? That depends on temperature. Warm air can hold more water vapor than cool air. You can see this in Figure 16.1. | 0.620761 |
DQ_000519 | What happens to moist air after it is blown upwards a mountain? | question_images/rain_shadow_7532.png | a. Dry air comes downwart on the opposite side of the mountain, b. Moist Air becomes rain, c. Moist air is absorbed by the mountain, d. Moist Air returns to the sea | a | T_0301 | text | null | Did you ever hike or drive up a mountain? Did you notice that it was cooler near the top? Climate is not just different on a mountain. Just having a mountain range nearby can affect the climate. | 0.61844 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_000519 | image | question_images/rain_shadow_7532.png | rain_shadow_7532.png | 1 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_000524 | image | question_images/rain_shadow_7534.png | rain_shadow_7534.png | 0.83535 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_000541 | image | question_images/rain_shadow_8183.png | rain_shadow_8183.png | 0.829084 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_000536 | image | question_images/rain_shadow_7537.png | rain_shadow_7537.png | 0.799474 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DD_0024 | image | teaching_images/rain_shadow_8185.png | The diagram is a representation of how a rain shadow is formed. A rain shadow is a dry region of land on the side of a mountain range that is protected from the prevailing winds. Prevailing winds are the winds that occur most of the time in a particular location on the Earth. The protected side of a mountain range is also called the lee side or the down-wind side. Prevailing winds carry air toward the mountain range. As the air rises up over a mountain range, the air cools, water vapor condenses, and clouds form. On this side of the mountains, called the windward side, precipitation falls in the form of rain or snow. The windward side of a mountain range is moist and lush because of this precipitation. Once the air passes over the mountain range, it moves down the other side, warms, and dries out. This dry air produces a rain shadow. Land in a rain shadow is typically very dry and receives much less precipitation and cloud cover than land on the windward side of the mountain range. | 0.792557 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DD_0023 | image | teaching_images/rain_shadow_7524.png | This diagram shows the effect of rains on hills. The moist air from the green side of the hills rising up in the air and condenses as water vapor. This is called precipitation. The other side of the hill form the rain shadow region. Rain shadow region is a region having little rainfall because it is sheltered from prevailing rain-bearing winds by a range of hills. The dry air descends from this region. | 0.783287 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_000512 | image | question_images/rain_shadow_7529.png | rain_shadow_7529.png | 0.777301 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_009014 | image | question_images/cycle_water_4929.png | cycle_water_4929.png | 0.775978 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_000507 | image | question_images/rain_shadow_7525.png | rain_shadow_7525.png | 0.768386 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | DQ_000533 | image | question_images/rain_shadow_7536.png | rain_shadow_7536.png | 0.767955 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_1800 | text | null | Most fossils are preserved by one of five processes outlined below (Figure 1.1): | 0.531376 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_2534 | text | null | Both types of reproduction have certain advantages. | 0.517494 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_3278 | text | null | What does population growth mean? You can probably guess that it means the number of individuals in a population is increasing. The population growth rate tells you how quickly a population is increasing or decreasing. What determines the population growth rate for a particular population? | 0.517138 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_1106 | text | null | Despite these problems, there is a rich fossil record. How does an organism become fossilized? | 0.503599 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_0332 | text | null | All living things need energy. They need it to power the processes of life. For example, it takes energy to grow. It also takes energy to produce offspring. In fact, it takes energy just to stay alive. Remember that energy cant be created or destroyed. It can only change form. Energy changes form as it moves through ecosystems. | 0.49993 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_3441 | text | null | How fast is evolution? Can you actually see evolution happening within your lifetime? Usually evolution takes a long time. So how can we visualize how it has happened? | 0.484205 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_1468 | text | null | Minerals are made by natural processes, those that occur in or on Earth. A diamond created deep in Earths crust is a mineral, but a diamond made in a laboratory by humans is not. Be careful about buying a laboratory-made diamond for jewelry. It may look pretty, but its not a diamond and is not technically a mineral. | 0.483777 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_1698 | text | null | How well soil forms and what type of soil forms depends on several different factors, which are described below. | 0.483475 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_0726 | text | null | Nuclear energy is produced by splitting the nucleus of an atom. This releases a huge amount of energy. | 0.481746 |
DQ_000520 | How many stages are there in the process? | question_images/rain_shadow_7532.png | a. 1, b. 4, c. 2, d. 3 | d | T_3941 | text | null | Why do different states of matter have different properties? Its because of differences in energy at the level of atoms and molecules, the tiny particles that make up matter. | 0.481196 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_000519 | image | question_images/rain_shadow_7532.png | rain_shadow_7532.png | 1 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_000524 | image | question_images/rain_shadow_7534.png | rain_shadow_7534.png | 0.83535 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_000541 | image | question_images/rain_shadow_8183.png | rain_shadow_8183.png | 0.829084 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_000536 | image | question_images/rain_shadow_7537.png | rain_shadow_7537.png | 0.799474 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DD_0024 | image | teaching_images/rain_shadow_8185.png | The diagram is a representation of how a rain shadow is formed. A rain shadow is a dry region of land on the side of a mountain range that is protected from the prevailing winds. Prevailing winds are the winds that occur most of the time in a particular location on the Earth. The protected side of a mountain range is also called the lee side or the down-wind side. Prevailing winds carry air toward the mountain range. As the air rises up over a mountain range, the air cools, water vapor condenses, and clouds form. On this side of the mountains, called the windward side, precipitation falls in the form of rain or snow. The windward side of a mountain range is moist and lush because of this precipitation. Once the air passes over the mountain range, it moves down the other side, warms, and dries out. This dry air produces a rain shadow. Land in a rain shadow is typically very dry and receives much less precipitation and cloud cover than land on the windward side of the mountain range. | 0.792557 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DD_0023 | image | teaching_images/rain_shadow_7524.png | This diagram shows the effect of rains on hills. The moist air from the green side of the hills rising up in the air and condenses as water vapor. This is called precipitation. The other side of the hill form the rain shadow region. Rain shadow region is a region having little rainfall because it is sheltered from prevailing rain-bearing winds by a range of hills. The dry air descends from this region. | 0.783287 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_000512 | image | question_images/rain_shadow_7529.png | rain_shadow_7529.png | 0.777301 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_009014 | image | question_images/cycle_water_4929.png | cycle_water_4929.png | 0.775978 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_000507 | image | question_images/rain_shadow_7525.png | rain_shadow_7525.png | 0.768386 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | DQ_000533 | image | question_images/rain_shadow_7536.png | rain_shadow_7536.png | 0.767955 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_0301 | text | null | Did you ever hike or drive up a mountain? Did you notice that it was cooler near the top? Climate is not just different on a mountain. Just having a mountain range nearby can affect the climate. | 0.695442 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_0799 | text | null | Many processes create mountains. Most mountains form along plate boundaries. A few mountains may form in the middle of a plate. For example, huge volcanoes are mountains formed at hotspots within the Pacific Plate. | 0.674885 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_1818 | text | null | A volcano is a vent through which molten rock and gas escape from a magma chamber. Volcanoes differ in many features, such as height, shape, and slope steepness. Some volcanoes are tall cones and others are just cracks in the ground (Figure 1.1). As you might expect, the shape of a volcano is related to the composition of its magma. | 0.661552 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_1855 | text | null | Volcanoes erupt because mantle rock melts. This is the first stage in creating a volcano. Remember from the chapter Materials of Earths Crust that mantle may melt if temperature rises, pressure lowers, or water is added. Be sure to think about how and why melting occurs in the settings where there is volcanism mentioned in the next few concepts. | 0.660053 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_0058 | text | null | The most destructive types of mass movement are landslides and mudslides. Both occur suddenly. | 0.657657 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_1476 | text | null | Converging plates create the worlds largest mountain ranges. Each combination of plate types continent- continent, continent-ocean, and ocean-ocean creates mountains. | 0.651444 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_0293 | text | null | Climate is the average weather of a place over many years. It includes average temperatures. It also includes average precipitation. The timing of precipitation is part of climate as well. What determines the climate of a place? Latitude is the main factor. A nearby ocean or mountain range can also play a role. | 0.628504 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_1853 | text | null | A volcano is a vent from which the material from a magma chamber escapes. Volcanic eruptions can come from peaky volcanic cones, fractured domes, a vent in the ground, or many other types of structures. | 0.628238 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_0049 | text | null | When the wind deposits sand, it forms small hills of sand. These hills are called sand dunes. For sand dunes to form, there must be plenty of sand and wind. Sand dunes are found mainly in deserts and on beaches. You can see examples of sand dunes in Figure 10.23. | 0.627257 |
DQ_000521 | In the diagram, how many slopes does the mountain have? | question_images/rain_shadow_7532.png | a. 3, b. 4, c. 2, d. 1 | c | T_0049 | text | null | When the wind deposits sand, it forms small hills of sand. These hills are called sand dunes. For sand dunes to form, there must be plenty of sand and wind. Sand dunes are found mainly in deserts and on beaches. You can see examples of sand dunes in Figure 10.23. | 0.627257 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_000519 | image | question_images/rain_shadow_7532.png | rain_shadow_7532.png | 1 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_000524 | image | question_images/rain_shadow_7534.png | rain_shadow_7534.png | 0.83535 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_000541 | image | question_images/rain_shadow_8183.png | rain_shadow_8183.png | 0.829084 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_000536 | image | question_images/rain_shadow_7537.png | rain_shadow_7537.png | 0.799474 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DD_0024 | image | teaching_images/rain_shadow_8185.png | The diagram is a representation of how a rain shadow is formed. A rain shadow is a dry region of land on the side of a mountain range that is protected from the prevailing winds. Prevailing winds are the winds that occur most of the time in a particular location on the Earth. The protected side of a mountain range is also called the lee side or the down-wind side. Prevailing winds carry air toward the mountain range. As the air rises up over a mountain range, the air cools, water vapor condenses, and clouds form. On this side of the mountains, called the windward side, precipitation falls in the form of rain or snow. The windward side of a mountain range is moist and lush because of this precipitation. Once the air passes over the mountain range, it moves down the other side, warms, and dries out. This dry air produces a rain shadow. Land in a rain shadow is typically very dry and receives much less precipitation and cloud cover than land on the windward side of the mountain range. | 0.792557 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DD_0023 | image | teaching_images/rain_shadow_7524.png | This diagram shows the effect of rains on hills. The moist air from the green side of the hills rising up in the air and condenses as water vapor. This is called precipitation. The other side of the hill form the rain shadow region. Rain shadow region is a region having little rainfall because it is sheltered from prevailing rain-bearing winds by a range of hills. The dry air descends from this region. | 0.783287 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_000512 | image | question_images/rain_shadow_7529.png | rain_shadow_7529.png | 0.777301 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_009014 | image | question_images/cycle_water_4929.png | cycle_water_4929.png | 0.775978 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_000507 | image | question_images/rain_shadow_7525.png | rain_shadow_7525.png | 0.768386 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | DQ_000533 | image | question_images/rain_shadow_7536.png | rain_shadow_7536.png | 0.767955 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_1701 | text | null | The steeper the slope, the less likely material will be able to stay in place to form soil. Material on a steep slope is likely to go downhill. Materials will accumulate and soil will form where land areas are flat or gently undulating. | 0.636256 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_0777 | text | null | Plates move apart at divergent plate boundaries. This can occur in the oceans or on land. | 0.629434 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_1578 | text | null | The atmosphere has different properties at different elevations above sea level, or altitudes. | 0.611375 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_1780 | text | null | The tidal range is the difference between the ocean level at high tide and the ocean level at low tide (Figure 1.2). The tidal range in a location depends on a number of factors, including the slope of the seafloor. Water appears to move a greater distance on a gentle slope than on a steep slope. | 0.60686 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_0049 | text | null | When the wind deposits sand, it forms small hills of sand. These hills are called sand dunes. For sand dunes to form, there must be plenty of sand and wind. Sand dunes are found mainly in deserts and on beaches. You can see examples of sand dunes in Figure 10.23. | 0.603389 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_0049 | text | null | When the wind deposits sand, it forms small hills of sand. These hills are called sand dunes. For sand dunes to form, there must be plenty of sand and wind. Sand dunes are found mainly in deserts and on beaches. You can see examples of sand dunes in Figure 10.23. | 0.603389 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_0058 | text | null | The most destructive types of mass movement are landslides and mudslides. Both occur suddenly. | 0.599048 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_0075 | text | null | Sediments were deposited in ancient seas in horizontal, or flat, layers. If sedimentary rock layers are tilted, they must have moved after they were deposited. | 0.59784 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_1698 | text | null | How well soil forms and what type of soil forms depends on several different factors, which are described below. | 0.595643 |
DQ_000522 | The dry leeward slope sits in what area in the diagram? | question_images/rain_shadow_7532.png | a. eye of the storm, b. windward slope, c. rain shadow, d. central air rising | c | T_0392 | text | null | As we mentioned above, topographic maps show the shape of the land. You can determine a lot of information about the landscape using a topographic map. These maps are invaluable for Earth scientists. | 0.594279 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_000519 | image | question_images/rain_shadow_7532.png | rain_shadow_7532.png | 1 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_000524 | image | question_images/rain_shadow_7534.png | rain_shadow_7534.png | 0.83535 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_000541 | image | question_images/rain_shadow_8183.png | rain_shadow_8183.png | 0.829084 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_000536 | image | question_images/rain_shadow_7537.png | rain_shadow_7537.png | 0.799474 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DD_0024 | image | teaching_images/rain_shadow_8185.png | The diagram is a representation of how a rain shadow is formed. A rain shadow is a dry region of land on the side of a mountain range that is protected from the prevailing winds. Prevailing winds are the winds that occur most of the time in a particular location on the Earth. The protected side of a mountain range is also called the lee side or the down-wind side. Prevailing winds carry air toward the mountain range. As the air rises up over a mountain range, the air cools, water vapor condenses, and clouds form. On this side of the mountains, called the windward side, precipitation falls in the form of rain or snow. The windward side of a mountain range is moist and lush because of this precipitation. Once the air passes over the mountain range, it moves down the other side, warms, and dries out. This dry air produces a rain shadow. Land in a rain shadow is typically very dry and receives much less precipitation and cloud cover than land on the windward side of the mountain range. | 0.792557 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DD_0023 | image | teaching_images/rain_shadow_7524.png | This diagram shows the effect of rains on hills. The moist air from the green side of the hills rising up in the air and condenses as water vapor. This is called precipitation. The other side of the hill form the rain shadow region. Rain shadow region is a region having little rainfall because it is sheltered from prevailing rain-bearing winds by a range of hills. The dry air descends from this region. | 0.783287 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_000512 | image | question_images/rain_shadow_7529.png | rain_shadow_7529.png | 0.777301 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_009014 | image | question_images/cycle_water_4929.png | cycle_water_4929.png | 0.775978 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_000507 | image | question_images/rain_shadow_7525.png | rain_shadow_7525.png | 0.768386 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | DQ_000533 | image | question_images/rain_shadow_7536.png | rain_shadow_7536.png | 0.767955 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_1753 | text | null | The atmosphere is layered, corresponding with how the atmospheres temperature changes with altitude. By under- standing the way temperature changes with altitude, we can learn a lot about how the atmosphere works. | 0.62929 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_0301 | text | null | Did you ever hike or drive up a mountain? Did you notice that it was cooler near the top? Climate is not just different on a mountain. Just having a mountain range nearby can affect the climate. | 0.607377 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_1048 | text | null | Before we develop some hypotheses, lets find a new question that we want to answer. What we just learned that atmospheric CO2 has been increasing at least since 1958. This leads us to ask this question: Why is atmospheric CO2 increasing? | 0.606915 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_0229 | text | null | Air temperature in the stratosphere layer increases with altitude. Why? The stratosphere gets most of its heat from the Sun. Therefore, its warmer closer to the Sun. The air at the bottom of the stratosphere is cold. The cold air is dense, so it doesnt rise. As a result, there is little mixing of air in this layer. | 0.603417 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_0966 | text | null | Why is such a small amount of carbon dioxide in the atmosphere even important? Carbon dioxide is a greenhouse gas. Greenhouse gases trap heat energy that would otherwise radiate out into space, which warms Earth. These gases were discussed in the chapter Atmospheric Processes. | 0.60169 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_1050 | text | null | Atmospheric CO2 has increased over the past five decades, because the amount of CO2 gas released by volcanoes has increased. | 0.599293 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_0916 | text | null | Air masses are slowly pushed along by high-level winds. When an air mass moves over a new region, it shares its temperature and humidity with that region. So the temperature and humidity of a particular location depends partly on the characteristics of the air mass that sits over it. | 0.598105 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_0914 | text | null | An air mass is a batch of air that has nearly the same temperature and humidity (Figure 1.1). An air mass acquires these characteristics above an area of land or water known as its source region. When the air mass sits over a region for several days or longer, it picks up the distinct temperature and humidity characteristics of that region. | 0.597163 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_0226 | text | null | Sometimes air doesnt mix in the troposphere. This happens when air is cooler close to the ground than it is above. The cool air is dense, so it stays near the ground. This is called a temperature inversion. An inversion can trap air pollution near the surface. Temperature inversions are more common in the winter. Can you explain why? | 0.589973 |
DQ_000523 | What happens when air rises over mountains and cools? | question_images/rain_shadow_7532.png | a. It results to precipitation., b. It results to vaporization., c. It results to evaporation., d. It results to humidity. | a | T_1578 | text | null | The atmosphere has different properties at different elevations above sea level, or altitudes. | 0.589008 |
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