Admission Test Admission Test Certification GRE-Verbal

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1년무료 업데이트 서비스란?

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Pass4Test는 고객님께서 GRE-Verbal첫번째 시험에서 패스할수 있도록 최선을 다하고 있습니다. 만일 어떤 이유로 인해 고객님이 GRE-Verbal시험에서 실패를 한다면 Pass4Test는 GRE-Verbal덤프비용 전액을 환불 해드립니다.

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최신 Admission Test Certification GRE-Verbal 무료샘플문제:

1. The Andean cordillera is made up of many interwoven mountain ranges, which include high intermundane
plateaus, basins, and valleys. The Northern Andes contain several broad ecosystems falling into four
altitudinal belts. Its northern subregion is distinguished by higher humidity and by greater climatic
symmetry between eastern and western flanks. The Central Andes are characterized by a succession of
agricultural zones with varied climatic conditions along the mountains' flanks and by large, highaltitude
plateaus, variously called puna or altiplano, which do not occur in the Northern Andes. The soil fertility of
the northern altiplano is generally good. The western Central Andean ranges are relatively arid with
desert-like soils, whereas the eastern ranges are more humid and have more diverse soils. The eastern
slopes of the Central Andes in many ways are similar to the wet forests of the Northern Andes. Unlike the
Northern Andes, however, these slopes have a dry season. In regions of gentle topography, such as the
Amazon basin, regional climatic variation can be determined from a few widely spaced measurements.
Regional projections in the Andean cordillera are quite difficult by comparison. For example, while air
temperature generally decreases with increasing altitude, variability of mountain topography can produce
much lower than expected air temperatures. Nevertheless, some general climatic patterns are discernible.
For example, with increasing distance south of the equator the seasonality of precipitation increases,
whereas the total annual amount generally decreases. Humidity commonly increases with increasing
altitude, but only to some intermediate altitude, above which it declines. The variability of mountain terrain
also affects precipitation, such that conditions of extreme wetness and aridity may exist in close proximity.
Related to this temperature gradient is a pattern of greater rainfall at the valley heads, and less rain at
lower altitudes, resulting in part from mountain rainshadow effect. The weather patterns of the Andean
cordillera and Amazon basin in general reflect movements of highand low-pressure cells associated with
the Intertropical Convergence Zone, a low-pressure trough that moves further north and south on a
seasonal basis. Precipitation is high throughout the year in the highlands and on the coast in the Northern
Andes. Coastal aridity increases south of central Ecuador, culminating in the Atacama desert of northern
Chile. In the Central Andes, highland precipitation is seasonal, and amounts are approximately half those
measured in the Northern Andes. The aridity of the Central Andean coastal zone is the result of the drying
effect of the cold Pacific Humboldt current and the southern Pacific high-pressure cell. Much of the
southern portion of the Central Andes in Bolivia is also arid. The dry season causes soil moisture deficits
and diminished stream flow part of each year.
The passage is primarily concerned with

A) comparing the climate and topography of the Northern Andes to those of the Central Andes
B) describing the climate and topography of various regions of the An dean cordillera
C) providing alternative explanations for the climatic diversity among different regions of the An dean
cordillera
D) discussing the factors affecting the climate of the An dean cordillera
E) examining the effects of topography on the climate and vegetation of the An dean cordillera

2. Radiative forcings are changes imposed on the planetary energy balance; radiative feedbacks are
changes induced by climate change. Forcings can arise from either natural or anthropogenic causes. For
example, the concentration of sulfate aerosols in the atmosphere can be altered by volcanic action or by
the burning of fossil fuels. The distinction between forcings and feedbacks is sometimes arbitrary;
however, forcings are quantities normally specified in global climate model simulations, while feedbacks
are calculated quantities. Examples of radiative forcings are greenhouse gases (such as carbon dioxide
and ozone), aerosols in the troposphere, and surface reflectivity. Radiative feedbacks include clouds,
water vapor in the troposphere, and sea-ice cover. The effects of forcings and feedbacks on climate are
complex. For example, clouds trap outgoing radiation, thus providing a warming influence, while also
reflecting incoming solar radiation and, thereby, providing a cooling influence. Current measurements
indicate that the net effect of clouds is to cool the earth. However, scientists are unsure if the balance will
shift in the future as the atmosphere and cloud formation are altered by the accumulation of greenhouse
gases. Similarly, the vertical distribution of ozone affects both the amount of radiation reaching the earth's
surface and the amount of reradiated radiation that is trapped by the greenhouse effect. These two
mechanisms affect the earth's temperature in opposite directions.
According to the passage, radiative forcings and radiative feedbacks can generally be distinguished from
each other by

A) the precision with which the amounts of radiative change can be determined
B) whether the radiative change is directed toward or away from the earth
C) whether the amount of radiative change is specified or calculated
D) whether the radiative change is global or more localized
E) the altitude at which the radiative change occurs

3. The Galapagos Islands are in the Pacific Ocean, off the western coast of South America.
They are a rocky, lonely spot, but they are also one of the most unusual places in the world. One reason is
that they are the home of some of the last giant tortoises left on earth. Weighing hundreds of pounds,
these tortoises, or land turtles, wander slowly around the rocks and sand of the islands. Strangely, each of
these islands has its own particular kinds of tortoises. There are seven different kinds of tortoises on the
eight islands, each kind being slightly different from the other. Hundreds of years ago, thousands of
tortoises wandered around these islands. However, all that changed when people started landing there.
When people first arrived in 1535, their ships had no refrigerators. This meant that fresh food was always
a problem for the sailors on board.
The giant tortoises provided a solution to this problem. Ships would anchor off the islands, and crews
would row ashore and seize as many tortoises as they could. Once the animals were aboard the ship, the
sailors would roll the tortoises onto their backs. The tortoises were completely helpless once on their
backs, so they could only lie there until used for soups and stews. Almost 100,000 tortoises were carried
off in this way. The tortoises faced other problems, too. Soon after the first ships, settlers arrived bringing
pigs, goats, donkeys, dogs and cats. All of these animals ruined life for the tortoises.
Donkey and goats ate all the plants that the tortoises usually fed on, while the pigs. Dogs and cats
consumed thousands of baby tortoises each year. Within a few years, it was hard to find any tortoise
eggs-or even any baby tortoises. By the early 1900s, people began to worry that the last of the tortoises
would soon die out. No one, however, seemed to care enough to do anything about the problem. More
and more tortoises disappeared, even though sailors no longer needed them for food. For another fifty
years, this situation continued. Finally, in the 1950s, scientist decided that something must be done. The
first part of their plan was to get rid of as many cats, dogs and other animals as they could.
Next, they tried to make sure that more baby tortoises would be born. To do this, they started looking for
wild tortoise eggs. They gathered the eggs and put them in safe containers. When the eggs hatched, the
scientists raised the tortoises in special pens. Both the eggs and tortoises were numbered so that the
scientists knew exactly which kinds of tortoises they had-and which island they came from. Once the
tortoises were old enough and big enough to take care of themselves, the scientists took them back to
their islands and set them loose. This slow, hard work continues today, and, thanks to it, the number of
tortoises is now increasing every year.
What happened last?

A) Scientists took away other animals.
B) The number of tortoises began to grow.
C) The number of tortoises began to decrease.
D) Tortoises were taken back to their home islands.
E) The tortoises began to disappear.

4. What if someone told you about a kind of grass that grows as tall as the tallest trees? A grass that can be
made as strong as steel? A grass from which houses, furniture, boats, and hundreds of other useful things
can be made? A grass that you would even enjoy eating? Would you believe that person? You should, for
that grass is bamboo, the "wood" of 1,001 uses. Bamboo may look like wood, but it is part of the family of
plants that includes wheat, oats, and barley. It is a kind of grass. This grass is not just a material for
making useful products. Young bamboo is eaten, often mixed with other vegetables, in many Asian foods.
Bamboo grows in many parts of the world. In the United States it grows in an area from Virginia west to
Indiana and south to Florida, Louisiana, and Texas. Most bamboo, however, is found in warm, wet
climates, especially in Asia and on the islands of the South Pacific Ocean. In most Asian countries,
bamboo is nearly as important as rice. Many Asians live in bamboo houses. They sit on bamboo chairs
and sleep on bamboo mats. They fence their land with bamboo and use the wood for cages for chickens
and pigs. Bamboo is used to build large buildings as well as homes. When it is glued in layers, it becomes
as strong as steel. On some islands in the South Pacific, bamboo is even used for water pipes. This
extraordinary material has many other uses. It is used to make musical instruments, such as flutes and
recorders. Paper made from bamboo has been highly prized by artists for thousands of years. Bamboo is
light and strong, and it bends without breaking. It is cheap, floats on water, almost never wears out, and is
easy to grow. Nothing else on earth grows quite so fast as bamboo. At times you can even see it grow!
Botanists have recorded growths of more than three feet in just twenty-four hours! Bamboo is hollow and
has a strong root system that almost never stops growing and spreading. In fact, only after it flowers, an
event that may happen only once every thirty years, will bamboo die. There are more than a thousand
kinds of bamboo. The smallest is only three inches tall and one-tenth of an inch across. The largest
reaches more than two hundred feet in height and seven inches in diameter. No wonder, then, that the
lives of nearly half the people on earth would change enormously if there were no longer any bamboo. No
wonder, too, that to many people bamboo is a symbol of happiness and good fortune.
What is the main idea of this passage?

A) Bamboo is an amazing grass that can be used in multiple ways.
B) Bamboo grows at an amazing rate and is found primarily in Asia.
C) There are at least a 1,000 types of bamboo.
D) Bamboo has at least 2,000 uses.
E) Bamboo could be considered a flower in some cases.

5. SCULPTURE : SHAVING ::

A) analysis : insight
B) therapy : comfort
C) burglary : arrest
D) experiment : hypothesis
E) education : opportunity

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