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You need to be responsible for your life.
NEW QUESTION: 1
There ere various security threats in the use of the server. Which of the following options is not a server securitythreat?
A. Natural disasters
B. Malicious programs
C. DDos attack
D. Hacking
Answer: A
NEW QUESTION: 2
감사 수행 중에 다음 중 핵심 고려 사항은 무엇입니까?
* 필요한 샘플링 계획은 무엇입니까?
* 감사 일정은 계획대로 진행되고 있습니까?
* 기술 전문가가 필요합니까?
* 준수 수준이 만족 스러운가?
A. I, II and III only
B. I and IV only
C. II and IV only
D. I, II, III 및 IV
Answer: C
NEW QUESTION: 3
The Andean cordillera is made up of many interwoven mountain ranges, which include high intermontane
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.
It can be inferred from the passage that air temperatures in the Andean cordillera are often "lower than
expected" (line 39) probably due to wide variations in
A. mountain elevation
B. prevailing wind direction
C. aridity
D. air pressure
E. precipitation levels
Answer: A
Explanation:
The passage points out that while air temperature generally decreases as altitude increases, "variability of
mountain topography"-i.e., dramatic changes in elevation-makes it difficult to determine temperature in
any given spot from widely spaced measurements. It can be reasonably inferred from this information that
an unexpected temperature would probably be the result of unexpected altitude.
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