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NEW QUESTION: 1
Refer to the exhibit. All switches have default bridge priorities, and originate BPDUs with MAC addresses as indicated. The numbers shown are STP link metrics. Which two ports are in blocking state after STP converges? (Choose two.)
A. the port on switch SWF that connects to switch SWG
B. the port on switch SWD that connects to switch SWE
C. the port on switch SWD that connects to switch SWC
D. the port on switch SWB that connects to switch SWD
Answer: C,D
NEW QUESTION: 2
트래픽을 전달할수 있어야 하는 3 개의 VPC가 있습니다. 이것을 어떻게 달성할수 있습니까?
두 가지 정답을 선택하십시오.
A. 각 VPC를 다른 모든 VPC에 피어링하여 전체 메시 피어링을 만듭니다.
B. 그들 사이에 VPN을 생성하고 그에 따라 라우팅 테이블을 조정하십시오.
C. 전 이적 피어링을 활성화하려면 AWS에 문의하십시오.
D. VPC 피어링은 2017 년 12 월 기준으로 전 이적 피어링을 허용합니다.
Answer: A,B
Explanation:
VPN instances can be used to create transitive peering. Full mesh peering is the only way to use peering to allow all VPCs to communicate with all other VPCs. Transitive peering is not possible.
NEW QUESTION: 3
Refer to the exhibit.
Which result does the configuration show?
A. tenant interface
B. SVI configuration
C. border spine
D. border leaf
Answer: D
NEW QUESTION: 4
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. aridity
C. air pressure
D. precipitation levels
E. prevailing wind direction
Answer: A
Explanation:
Explanation/Reference:
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.