READING SECTION READING PRACTICE TEST (2) CAMBRIDGE PREPARATION FOR THE TOEFL® IBT TEST

 

CAMBRIDGE PREPARATION FOR THE TOEFL® IBT TEST READING SECTION READING PRACTICE TEST (2)

 

Directions In this section, you will read three passages and answer reading comprehension about each passage. Most questions are worth one point. The directions indicate how many points you may receive. You have 60 minutes to read all of the passages and answer the questions. Some passages include a word or phrase followed by an asterisk (*). Go to the bottom of the page to see a definition or an explanation of these words or phrases.   Questions 14-26 The Coriolis Force In the early part of the twentieth century, the Norwegian scientist and polar explorer Fridtjof Nansen noted that icebergs did not follow the path of the wind as common sense had assumed. Instead they tended to move to the right side of the direction in which the wind blew. A student of Nansen's, V. W. Ekman, showed that the rotation of the Earth leading to an inertial force known as the Coriolis force was responsible for this phenomenon. He further demonstrated that in the Northern Hemisphere the deflection was toward the right of the prevailing wind, and in the Southern Hemisphere the deflection was toward the left. The icebergs observed by Nansen were moved by ocean currents that also moved at an angle to the prevailing wind. The Coriolis force itself is caused by the fact that the Earth rotates on its axis once per day, and hence all points on the planet have the same rotational velocity; that is, they take one whole day to complete a rotational circle. However, since a complete rotation around the Earth is shorter the further one is away from the equator, different points on the Earth travel at different speeds depending on degree of latitude. For example, a point on the equator travels the whole distance around the sphere (about 40,000 kilometers), whereas a point near the poles will travel a much shorter distance. Therefore, we can say that the linear speed of a point depends on its latitude above or below the equator. Thus the actual linear speed of a point on the surface is faster the nearer that point is to the equator. Now if an untethered object (or current) is moving northward away from the equator in the Northern Hemisphere, it will also maintain the initial speed imparted to it by the eastward rotation of the Earth. That eastward deflection is faster at the equator than at more northerly (or southerly) latitudes, and thus, when the object reaches a more northerly point, it will be traveling faster in an eastward direction than the surrounding ground or water. The moving object will appear to be forced away from its path by some mysterious phenomenon. In reality the ground is simply moving at a different speed from the original speed at the object's (or current's) home position. The resulting direction of movement will therefore be at an angle of about 45 degrees to the original direction, so an object traveling north will move to the right in the Northern Hemisphere and to the left in the Southern Hemisphere with respect to the rotating Earth. An object traveling south will be deflected to the left in the Northern Hemisphere and to the right in the Southern Hemisphere. As the surface water in the ocean is moved by the wind, it tends to veer* off at an angle of 45 degrees to the right or left. This movement exerts a drag on the water immediately below it, and the Coriolis force causes this layer to move and also to deflect to the right or left. This layer in turn drags the layer below, which in turn is deflected. At successively deeper layers, the water is deflected in relation to the layer above until at a depth of around 150 meters, the water is moving in a direction opposite to the surface water. At successively greater depths. the frictional forces between layers reduce the energy of the flow, causing water to move more slowly the deeper the layer. The resulting deflections produce a spiral pattern known as the Ekman spiral. The net movement of water is roughly at 90 degrees from the wind direction and is known as Ekman transport. This phenomenon is an important factor in the movement of water in the oceans. Among other things, it creates zones of upwelling by forcing surface waters apart and other zones of downwelling by forcing surface waters together. For example, wind blowing parallel to the shore may create a net movement of water at 90 degrees away from the shore. Nutrient-rich deeper ocean water will upwell to take the place of the displaced water and thus profoundly influence the marine ecosystem. *veer: to suddenly change direction   14 The phrase "path of the wind" in the passage is closest in meaning to In the early part of the twentieth century, the Norwegian scientist and polar explorer Fridtjof Nansen noted that icebergs did not follow the path of the wind as common sense had assumed. Instead they tended to move to the right side of the direction in which the wind blew. A student of Nansen's, V. W. Ekman, showed that the rotation of the Earth leading to an inertia! force known as the Coriolis force was responsible for this phenomenon. He further demonstrated that in the Northern Hemisphere the deflection was toward the right of the prevailing wind, and in the Southern Hemisphere the deflection was toward the teft. The icebergs observed by Nansen were moved by ocean currents that also moved at an angle to the prevailing wind. A wind strength B wind variation C wind direction D wind phenomenon   15 The phrase "this phenomenon" in the passage refers to In the early part of the twentieth century, the Norwegian scientist and polar explorer Fridtjof Nansen noted that icebergs did not follow the path of the wind as common sense had assumed. Instead they tended to move to the right side of the direction in which the wind blew. A student of Nansen's, V. W. Ekman, showed that the rotation of the Earth leading to an inertial force known as the Coriolis force was responsible for this phenomenon. He further demonstrated that in the Northern Hemisphere the deflection was toward the right of the prevailing wind, and in the Southern Hemisphere the deflection was toward the left. The icebergs observed by Nansen were moved by ocean currents that also moved at an angle to the prevailing wind. A the movement of icebergs B the rotation of the Earth C the direction of the wind D the inertial Coriolis force   16 The word "rotates" in the passage is closest in meaning to The Coriolis force itself is caused by the fact that the Earth rotates on its axis once per day. and hence all points on the planet have the same rotational velocity; that is. they take one whole day to complete a rotational circle. However. since a complete rotation around the Earth is shorter the further one is away from the equator, different points on the Earth travel at different speeds depending on degree of latitude. For example, a point on the equator travels the whole distance around the sphere (about 40,000 kilometers). whereas a point near the poles will travel a much shorter distance. Therefore, we can say that the linear speed of a point depends on its latitude above or below the equator. Thus the actual linear speed of a point on the surface is faster the nearer that point is to the equator. A spins B travels C twirls D swivels   17 We can infer that rotational velocity is [Refer to the full passage.] A the same as speed in kph B different at different latitudes C the same at different latitudes D dependent on latitude   18 In paragraph 2, the author explains the differences in linear speed by → The Coriolis force itself is caused by the fact that the Earth rotates on its axis once per day, and hence all points on the planet have the same rotational velocity; that is, they take one whole day to complete a rotational circle. However. since a complete rotation around the Earth is shorter the further one is away from the equator, different points on the Earth travel at different speeds depending on degree of latitude. For example, a point on the equator travels the whole distance around the sphere (about 40,000 kilometers). whereas a point near the poles will travel a much shorter distance. Therefore, we can say that the linear speed of a point depends on its latitude above or below the equator. Thus the actual linear speed of a point on the surface is faster the nearer that point is to the equator. A arguing that an object moving north moves faster B describing the linear velocity of the Earth C identifying the eastward deflection of a current D relating speed to the distance of a point from the equator Paragraph 2 is marked with an arrow [→]. 19 According to the passage, a point near the equator in the Northern Hemisphere travels [Refer to the full passage.] A at the same speed as any other point B faster than a point at a higher latitude C slower than a point in the Southern Hemisphere D at different speeds in different seasons   20 Look at the four squares [■] that indicate where the following sentence could be added to the passage.   And conversely, if the object is traveling southward toward the equator, it will be moving more slowly than the surrounding land or water.   Where would the sentence best fit? Choose the letter of the square that shows where the sentence should be added. Now if an untethered object (or current) is moving northward away from the equator in the Northern Hemisphere, it will also maintain the initial speed imparted to it by the eastward rotation of the Earth. [A] That eastward deflection is faster at the equator than at more northerly (or southerly) latitudes, and thus, when the object reaches a more northerly point, it will be traveling faster in an eastward direction than the surrounding ground or water. [B] The moving object will appear to be forced away from its path by some mysterious phenomenon. In reality the ground is simply moving at a different speed from the original speed at the object's (or current's) home position. [C] The resulting direction of movement will therefore be at an angle of about 45 degrees to the original direction, so an object traveling north will move to the right in the Northern Hemisphere and to the left in the Southern Hemisphere with respect to the rotating Earth. [D] An object traveling south will be deflected to the left in the Northern Hemisphere and to the right in the Southern Hemisphere. O A O B O C O D   21 According to paragraph 4, where does water move in a direction contrary to surface layers of water? → As the surface water in the ocean is moved by the wind, it tends to veer off at an angle of 45 degrees to the right or left. This movement exerts a drag on the water immediatety below it, and the Coriolis force causes this layer to move and also to deflect to the right or left. This layer in turn drags the layer below, which in turn is deflected. At successively deeper layers, the water is deflected in relation to the layer above until at a depth of around 150 meters, the water is moving in a direction opposite to the surface water. At successively greater depths, the frictional forces between layers reduce the energy of the flow, causing water to move more slowly the deeper the layer. The resulting deflections produce a spiral pattern known as the Ekman spiral. The net movement of water is roughly at 90 degrees from the wind direction and is known as Ekman transport. A Directly below the surface B At 90 degrees to the surface C At all depths below the surface D At 150 meters below the surface Paragraph 4 is marked with an arrow [→]. 22 In paragraph 4, why does the author explain that the wind tends to deflect the water to the right or left? → As the surface water in the ocean is moved by the wind, it tends to veer off at an angle of 45 degrees to the right or left. This movement exerts a drag on the water immediately below it, and the Coriolis force causes this layer to move and also to deflect to the right or left. This layer in turn drags the layer below, which in turn is deflected. At successively deeper layers, the water is deflected in relation to the layer above until at a depth of around 150 meters, the water is moving in a direction opposite to the surface water. At successively greater depths, the frictional forces between layers reduce the energy of the flow, causing water to move more slowly the deeper the layer. The resulting deflections produce a spiral pattern known as the Ekman spiral. The net movement of water is roughly at 90 degrees from the wind direction and is known as Ekman transport. A To explain the concept of upwelling B To demonstrate the effect of the Coriolis force C To point out causes of rotational velocity D To introduce the movement of ocean currents Paragraph 4 is marked with an arrow [→] 23 The word "deflected" in the passage is closest in meaning to As the surface water in the ocean is moved by the wind, it tends to veer off at an angle of 45 degrees to the right or left. This movement exerts a drag on the water immediately below it, and the Coriolis force causes this layer to move and also to deflect to the right or left. This layer in turn drags the layer below, which in turn is deflected. At successively deeper layers, the water is deflected in relation to the layer above until at a depth of around 150 meters, the water is moving in a direction opposite to the surface water. At successively greater depths, the frictional forces between layers reduce the energy of the flow, causing water to move more slowly the deeper the layer. The resulting deflections produce a spiral pattern known as the Ekman spiral. The net movement of water is roughly at 90 degrees from the wind direction and is known as Ekman transport. A turned B pushed C shoved D urged   24 Based on the information in paragraphs 1 and 4, which of the following best explains the term "Coriolis force"? [Refer to the full passage.] A The force that creates currents B The force that moves icebergs C The force that opposes wind movement D The force that deflects ocean water   25 According to the passage, the Ekman spiral may affect [Refer to the full passage.] A the distribution of ocean life forms B the direction of the wind C the speed of ocean currents D the frictional forces of water layers     26 Directions: An introductory sentence for a brief summary of the passage is provided below. Complete the summary by selecting the THREE answer choices that express the most important ideas in the passage. Some sentences do not belong in the summary because they express ideas that are not presented in the passage or are minor ideas in the passage. This question is worth 2 points. Write the letters of the answer choices in the spaces where they belong. Refer to the full passage. Different linear speeds at different latitudes on the Earth cause the prevailing winds in the Earth's Northern and Southern Hemispheres to deflect water movements, thus creating Ekman spirals. Answer choices   A Due to the Coriolis force, icebergs move at a right angle to the prevailing wind. • _________________________ B Because of the Earth's rotation, objects moving away from or toward the equator travel at different speeds in relation to fixed points at different latitudes. • _________________________ C In order to reach the correct destination, an airplane pilot must adjust direction to compensate for the Coriolis force. • _________________________ D Because of deflection and differences in linear speed, ocean currents move at an angle to the wind.   E Water at successively lower levels is deflected at an angle to the layer immediately above it, and this creates a spiral.   F Due to upwelling of water, marine life is rich in areas where Ekman spirals operate.

ANSWER KEYS AND EXPLANATION