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NEW QUESTION: 1
드래그 앤 드롭 질문
액세스 제어 모델의 이름을 관련 제한과 일치시킵니다.
각 액세스 제어 모델을 오른쪽의 적절한 제한 액세스로 끕니다.

Answer:
Explanation:

NEW QUESTION: 2
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 ater 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.
According to the passage, the northern part of the high-altitude plateaus is characterized by which of the
following?
A. Fertile soil
B. Extremes in air temperature
C. An arid climate
D. High relative humidity
E. A succession of agricultural zones
Answer: A
Explanation:
The high-altitude plateaus are called altiplano(line 16). The passage states explicitly that the soil fertility in
the northern altiplanois generally good

NEW QUESTION: 3
What is the source IP address in an OSPF update?
A. 224.0.0.5
B. The unicast IP address of the interface the update is being sent on.
C. 224.0.0.6
D. The system address of the router
Answer: B

NEW QUESTION: 4
Which of the followings are not the operations that you can do on a cloud disk snapshot? (Choose two.)
A. snapshot download
B. snapshot deletion
C. snapshot duplicate
D. snapshot rollback
Answer: A,C