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NEW QUESTION: 1
In FusionSphere solutions, VSA ManageDVS network is in the plane of the network with management can not be exchanged.
A. False
B. True
Answer: A
NEW QUESTION: 2
Which four actions are possible during an Online Data file Move operation?
A. Querying tables in the data file being moved
B. Flashing back the database
C. Performing file shrink of the data file being moved
D. Executing DML statements on objects stored in the data file being moved
E. Performing Block Media Recovery for a data block in the data file being moved
F. Creating and dropping tables in the data file being moved
Answer: A,D,E,F
Explanation:
- You con now move On line Datafile without hove to stop Monoged Recovery and manually copy and rename Files. This can even be used to move Datafiles from or to ASM.
-New in Oracle Database 12c: FROM METAUNK. Physical Standby Database is in Active Data Guard Mode (opened READ ONLY and Managed Recovery is running): It is now possible to online move a Datafile while Managed Recovery is running, ie. the Physical Standby Database is in Active Data Guard Mode. You con use this Command to move the Datafile
-A flashback operation does not relocate a moved data file to its previous location. If you move a data file online from one location to another and later flash back the database to a point in time before the move, then the Data file remains in the new location, but the contents of the Data file ore changed to the contents at the time specified in the flashback. Oracle0 Database Administrator's Guide 12c Release 1 (12.1)
NEW QUESTION: 3
You are designing a Web application by using Microsoft ASP.NET .
You add a master page and content pages to the application. The master page contains a Label control named lblTitle.
You need to reference lblTitle from the code within the content pages.
Which code segment should you use?
A. Dim lblTitle As Label lblTitle = DirectCast(Master.LoadControl("lblTitle"), Label)
B. Dim lblTitle As Label lblTitle = DirectCast(Master.FindControl("lblTitle"), Label)
C. Dim lblTitle As Label lblTitle = DirectCast(Master.ParseControl("lblTitle"), Label)
D. Dim lblTitle As Label lblTitle = DirectCast(Page.Form.FindControl("lblTitle"), Label)
Answer: B
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 directed toward or away from the earth
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. whether the radiative change is global or more localized
E. the altitude at which the radiative change occurs
Answer: B
Explanation:
Explanation/Reference:
Explanation:
According to the passage, radiative "forcings are quantities normally specified in global climate model situations, while feedbacks are calculated quantities
