CSI CSC2 Q&A - in .pdf

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NEW QUESTION: 1
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. air pressure
B. mountain elevation
C. prevailing wind direction
D. aridity
E. precipitation levels
Answer: B
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.

NEW QUESTION: 2
Your network contains an Active Directory domain named contoso.com. All servers run Windows Server 2012 R2. The domain contains a file server named Server1. The domain contains a domain controller named DC1. Server1 contains three shared folders. The folders are configured as shown in the following table.

Folder2 has a conditional expression of User.Department= = MMarketing".
You discover that a user named User1 cannot access \\Server1\folder2. User1 can access \\Server1\folderl and \\Server1\folder3.
You verify the group membership of User1 as shown in the Member Of exhibit. (Click the Exhibit button.)

You verify the organization information of User1 as shown in the Organization exhibit. (Click the Exhibit button.)

You verify the general properties of User1 as shown in the General exhibit. (Click the Exhibit button.)

You need to ensure that User1 can access the contents of \\Server1\folder2.
What should you do?
A. Remove User11from the Accounting global group.
B. Change the department attribute of User1.
C. Grant the Full Control NTFS permissions on Folder2 to User1.
D. From a Group Policy object (GPO), set the Support for Dynamic Access Control and Kerberos armoring setting to Always provide claims.
Answer: B
Explanation:
B. Conditional Expression and users Department must match http://technet.microsoft.com/en-us/library/jj134043.aspx

NEW QUESTION: 3
자동 확장은 자동으로 태그를 리소스에 할당합니까?
A. 예. 기본적으로
B. 아니요. API를 통해 구성하지 않는 한 아닙니다.
C. 그렇습니다.
D. 아니요. 그렇지 않습니다.
Answer: C
Explanation:
설명:
태그는 Amazon EC2에 의미 적 의미가 없으며 엄격하게 문자열로 해석됩니다.
태그는 Auto Scaling 그룹에서 생성 한 인스턴스에 자동으로 할당됩니다. Auto Scaling은 aws : autoscaling : groupName 키와 Auto Scaling 그룹 이름 값을 사용하여 인스턴스에 태그를 추가합니다.
http://docs.amazonwebservices.com/AWSEC2/latest/UserGuide/Using_Tags.html

NEW QUESTION: 4
Which two statements about stateless firewalls are true? (Choose two.)
A. Cisco IOS cannot implement them because the platform is stateful by nature.
B. They cannot track connections.
C. They compare the 5-tuple of each incoming packet against configurable rules.
D. They are designed to work most efficiently with stateless protocols such as HTTP or HTTPS.
E. The Cisco ASA is implicitly stateless because it blocks all traffic by default.
Answer: B,C
Explanation:
Explanation/Reference:
Explanation:
However, since iptables and Netfilter were introduced and connection tracking in particular, this option was
gotten rid of. The reason for this is that connection tracking can not work properly without defragmenting
packets, and hence defragmenting has been incorporated into conntrack and is carried out automatically. It
can not be turned off, except by turning off connection tracking. Defragmentation is always carried out if
connection tracking is turned on.
Reference: http://www.iptables.info/en/connection-state.html

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