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NEW QUESTION: 1
ユーザー定義のローカルプロセスを実行するAzure Databricksクラスターを設計しています。
次の要件を満たすクラスター構成を推奨する必要があります。
*クエリの待ち時間を最小限に抑えます。
*全体的なコストを削減します。
*クラスターで同時にクエリを実行できるユーザーの数を最大化します。
どのクラスタータイプをお勧めしますか？
A. 自動スケーリングによる高い同時実行性
B. 自動終了のある標準
C. 自動スケーリングの標準
D. 自動終了による高い同時実行性
Answer: A
Explanation:
Explanation
High Concurrency clusters allow multiple users to run queries on the cluster at the same time, while minimizing query latency. Autoscaling clusters can reduce overall costs compared to a statically-sized cluster.
References:
https://docs.azuredatabricks.net/user-guide/clusters/create.html
https://docs.azuredatabricks.net/user-guide/clusters/high-concurrency.html#high-concurrency
https://docs.azuredatabricks.net/user-guide/clusters/terminate.html
https://docs.azuredatabricks.net/user-guide/clusters/sizing.html#enable-and-configure-autoscaling

NEW QUESTION: 2
Refer to the Exhibit:

Users at each end of this VPN tunnel cannot communicate with each other. Which cause of this behavior is true?
A. Phase 1 is not completed and troubleshooting is required.
B. The Diffie-Hellman groups configured are different
C. The pre shared key does not match.
D. The issue occurs in phase 2 of the tunnel.
Answer: A

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. precipitation levels
B. aridity
C. prevailing wind direction
D. air pressure
E. mountain elevation
Answer: E
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.