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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.
The passage mentions all the following as climatic factors in the Central Andes cordillera EXCEPT for
A. the Pacific Humboldt current
B. the Intertropical Convergence Zone
C. the rainshadow effect
D. the symmetry of the mountain ranges
E. the southern Pacific highpressure cell
Answer: D
Explanation:
Explanation/Reference:
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), and E are all mentioned in the passage as factors affecting the climate of the Central Andes cordillera.
NEW QUESTION: 2
Which three options are threefunctions of a Cisco UCS Invicta scaling system router? (Choose three.)
A. Replication
B. Mirror protection
C. RAID
D. Power fail data protection
E. Host connectivity
F. Error correction
Answer: A,B,E
NEW QUESTION: 3
Ihr Netzwerk enthält eine Active Directory-Domäne mit dem Namen contoso.com. Die Domäne enthält einen Server mit dem Namen Server1, auf dem Windows Server 2012 R2 ausgeführt wird.
Sie aktivieren und konfigurieren Routing und RAS (RRAS) auf Server1.
Sie erstellen ein Benutzerkonto mit Name User1.
Sie müssen sicherstellen, dass Benutzer1 VPN-Verbindungen zu Server1 herstellen kann.
Was tun?
A. Ändern Sie die Mitglieder der Gruppe Remoteverwaltungsbenutzer.
B. Erstellen Sie eine Verbindungsanforderungsrichtlinie.
C. Erstellen Sie eine Netzwerkrichtlinie.
D. Fügen Sie einen RADIUS-Client hinzu.
Answer: C
Explanation:
Erläuterung:
Netzwerkrichtlinien sind eine Reihe von Bedingungen, Einschränkungen und Einstellungen, mit denen Sie festlegen können, wer zum Herstellen einer Verbindung zum Netzwerk berechtigt ist und unter welchen Umständen eine Verbindung hergestellt werden kann oder nicht.
Netzwerkrichtlinien können als Regeln angesehen werden. Jede Regel hat eine Reihe von Bedingungen und Einstellungen.
Konfigurieren Sie Ihren VPN-Server für die Verwendung von NAP (Network Access Protection), um Richtlinien für Integritätsanforderungen durchzusetzen.
Verweise:
http: //technet. microsoft. com/en-us/library/hh831683. aspx
http: //technet. microsoft. com/en-us/library/cc754107. aspx
http: //technet. microsoft. com/en-us/library/dd314165%28v=ws. 10%29. aspx
http: //technet. microsoft. com/en-us/windowsserver/dd448603. aspx
http: //technet. microsoft. com/en-us/library/dd314165(v=ws. 10). aspx
http: //technet. microsoft. com/en-us/library/dd469733. aspx
http: //technet. microsoft. com/en-us/library/dd469660. aspx
http: //technet. microsoft. com/en-us/library/cc753603. aspx
http: //technet. microsoft. com/en-us/library/cc754033. aspx
http: //technet. microsoft. com/en-us/windowsserver/dd448603. aspx