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NEW QUESTION: 1
DRAG DROP
Your network contains servers that run Windows Server 2012. The network contains two servers named Server1 and Server2 that are connected to a SAS storage device. The device only supports two connected computers.
Server1 has the iSCSI Target Server role service installed. Ten application servers use their iSCSI Initiator to connect to virtual disks in the SAS storage device via iSCSI targets on Server1.
Currently, Server2 is used only to run backup software.
You install the iSCSI Target Server role service on Server2.
You need to ensure that the iSCSI targets are available if Server1 fails.
Which five actions should you perform?
To answer, move the five appropriate actions from the list of actions to the answer area and arrange them in the correct order.
Select and Place:
Answer:
Explanation:
Explanation/Reference:
References: http://blogs.msdn.com/b/clustering/archive/2012/05/01/10299698.aspx
NEW QUESTION: 2
A. Option A
B. Option D
C. Option C
D. Option B
Answer: A
NEW QUESTION: 3
What is a risk when initiating the containment of a rogue AP?
A. disassociating clients of valid access points that are operated by a neighboring organization
B. disrupting transmission of neighboring AP clients
C. breaking the radio of the containing AP
D. breaking the rogue client radio or its firmware
Answer: A
Explanation:
Rogue Containment Caveats
Reference: http://www.cisco.com/c/en/us/support/docs/wireless/4400-series-wireless-lan
controllers/112045-handling-rogue-cuwn-00.html
NEW QUESTION: 4
Radiative forcings are changes imposed on the planetary energy balance; radiative feedbacks are
changes induced by climate change. Forcings can arise from either natural or anthropogenic causes. For
example, the concentration of sulfate aerosols in the atmosphere can be altered by volcanic action or by
the burning of fossil fuels. The distinction between forcings and feedbacks is sometimes arbitrary;
however, forcings are quantities normally specified in global climate model simulations, while feedbacks
are calculated quantities. Examples of radiative forcings are greenhouse gases (such as carbon dioxide
and ozone), aerosols in the troposphere, and surface reflectivity. Radiative feedbacks include clouds,
water vapor in the troposphere, and sea-ice cover. The effects of forcings and feedbacks on climate are
complex. For example, clouds trap outgoing radiation, thus providing a warming influence, while also
reflecting incoming solar radiation and, thereby, providing a cooling influence. Current measurements
indicate that the net effect of clouds is to cool the earth. However, scientists are unsure if the balance will
shift in the future as the atmosphere and cloud formation are altered by the accumulation of greenhouse
gases. Similarly, the vertical distribution of ozone affects both the amount of radiation reaching the earth's
surface and the amount of reradiated radiation that is trapped by the greenhouse effect. These two
mechanisms affect the earth's temperature in opposite directions.
According to the passage, radiative forcings and radiative feedbacks can generally be distinguished from
each other by
A. whether the radiative change is global or more localized
B. whether the amount of radiative change is specified or calculated
C. the precision with which the amounts of radiative change can be determined
D. the altitude at which the radiative change occurs
E. whether the radiative change is directed toward or away from the earth
Answer: B
Explanation:
According to the passage, radiative "forcings are quantities normally specified in global climate model
situations, while feedbacks are calculated quantities