Reading Passage Question
The transfer of heat and water vapor from the ocean to the air above it depends on a disequilibrium at the interface of the water and the air. Within about a millimeter of the water, air temperature is close to that of the surface water, and the air is nearly saturated with water vapor. But the differences, however small, are crucial, and the disequilibrium is maintained by air near the surface mixing with air higher up, which is typically appreciably cooler and lower in water-vapor content. The air is mixed by means of turbulence that depends on the wind for its energy. As wind speed increases, so does turbulence, and thus the rate of heat and moisture transfer. Detailed understanding of this phenomenon awaits further study. An interacting-and complicating-phenomenon is wind-to-water transfer of momentum that occurs when waves are formed. When the wind makes waves, it transfers important amounts of energy--energy that is therefore not available to provide turbulence.
“The transfer of heat and water vapor from the ocean to the air above”- is a GMAT reading comprehension passage with answers. Candidates need a strong knowledge of English GMAT reading comprehension.
This GMAT Reading Comprehension consists of 4 comprehension questions. The GMAT Reading Comprehension questions are designed for the purpose of testing candidates’ abilities in understanding, analyzing, and applying information or concepts. Candidates can actively prepare with the help of GMAT Reading Comprehension Practice Questions.
Solution and Explanation
Question 1:The primary purpose of the passage is to
(A) resolve a controversy
(B) describe a phenomenon
(C) outline a theory
(D) confirm research findings
(E) classify various observations
Answer: B
Explanation: As the passage states. “The transfer of heat and water vapour from the ocean to the air above it depends on a disequilibrium at the interface of the water and the air.” Wind-to-water momentum transfer is a phenomenon that interacts and complicates wave formation. Significant quantities of energy are transferred when the wind creates waves; this energy is not then accessible to create turbulence. The response is best supported by Option B.
Question 2: According to the passage, wind over the ocean generally does which of the following?
- Causes relatively cool, dry air to come into proximity with the ocean surface.
- Maintains a steady rate of heat and moisture transfer between the ocean and the air.
- Causes frequent changes in the temperature of the water at the ocean's surface.
(A) I only
(B) II only
(C) I and II only
(D) II and III only
(E) I, II, and III
Answer: A
Explanation: As mentioned, the air is substantially saturated with water vapour and is approximately the same temperature as the surface water within a millimetre of the water. The disequilibrium is maintained by mixing air near the surface with air higher above, which is often noticeably colder and lower in water-vapour concentration. However, the variations, however tiny, are significant.
Question 3: It can be inferred from the passage that the author regards current knowledge about heat and moisture transfer from the ocean to air as
(A) revolutionary
(B) inconsequential
(C) outdated
(D) derivative
(E) incomplete
Answer: E
Explanation: According to the author, turbulence and, consequently, the rate of heat and moisture transfer, rise as wind speed rises. This phenomena has to be studied more thoroughly. When waves are created, there is a wind-to-water momentum transfer that interacts and complicates the event.
Question 4: The passage suggests that if on a certain day the wind were to decrease until there was no wind at all, which of the following would occur?
(A) The air closest to the ocean surface would become saturated with water vapor.
(B) The air closest to the ocean surface would be warmer than the water.
(C) The amount of moisture in the air closest to the ocean surface would decrease.
(D) The rate of heat and moisture transfer would increase.
(E) The air closest to the ocean would be at the same temperature as air higher up.
Answer: A
Explanation: "Within about a millimetre of the water, air temperature is close to that of the surface water, and the air is nearly saturated with water vapour. But the differences, however small, are crucial, and the disequilibrium is maintained by air near the surface mixing with air higher up, which is typically appreciably cooler and lower in water-vapour content". As a result, we may infer that there is an unbalance, which is why the air close to the surface is only "almost" saturated. The statement "the differences, however tiny, are essential" serves as proof. Turbulence from the wind maintains this state of disequilibrium. The water is now totally saturated rather than just "almost" saturated.
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