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NEW QUESTION: 1
A. Option E
B. Option B
C. Option A
D. Option C
E. Option D
Answer: B,D
NEW QUESTION: 2
Rank the following funds in order of their relative risk, from highest to lowest:
I. growth fund
II. high-yield bond fund
III. high-grade bond fund
IV. international fund
A. IV, II, I, III
B. IV, I, II, III
C. II, IV, I, III
D. I, IV, III, II
Answer: B
Explanation:
The funds ordered by their relative risk from highest to lowest are IV, I, II, III. The highest
risk is an international fund that invests in foreign securities, which exposes the investor to more currency
exchange risk and some social and political risk as well. Next is the growth fund that invests most of its
funds in domestic stocks, which are riskier than bonds. The high-yield bond fund is a junk bond fund and,
as such, is next in the list. The high-grade bond fund invests mostly in investment-grade bonds, which
offer investors a moderate risk exposure and is the least risky of the choices listed.
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.
The passage mentions all the following as climatic factors in the Central Andes cordillera EXCEPT for
A. the Pacific Humboldt current
B. the symmetry of the mountain ranges
C. the rainshadow effect
D. the Intertropical Convergence Zone
E. the southern Pacific highpressure cell
Answer: B
Explanation:
The only discussion of mountain symmetry is in the first paragraph, which mentions the symmetry in
climate between the east and west flanks of the Northern Andes mountains. No mention is made
anywhere in the passage of any symmetry with respect to the Central Andes mountains. On the other
hand, choices (A), (B), (C), andE.are all mentioned in the passage as factors affecting the climate of the
Central Andes cordillera.
NEW QUESTION: 4
사용자가 몇 개의 그룹에 속할 수 있는지에 대한 제한이 있습니까?
A. 루트를 제외한 모든 사용자에 대해 예
B. 아니오
C. 모든 사용자에게 예
D. 특별 허가가 부여되지 않는 한 예
Answer: C