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NEW QUESTION: 1
Match each application to its definition.
To answer, drag the appropriate application from the column on the left to its definition on the right. Each application may be used once, more than once, or not at all.
NOTE: Each correct match is worth one point.
Answer:
Explanation:
NEW QUESTION: 2
You use a contained database named ContosoDb within a domain.
You need to create a user who can log on to the ContosoDb database. You also need to ensure that you can port the database to different database servers within the domain without additional user account configurations.
Which type of user should you create?
A. User mapped to an asymmetric key
B. login mapped to a virtual account
C. SQL user without login
D. Domain user
Answer: D
Explanation:
If the service must interact with network services, access domain resources like file shares or if it uses linked server connections to other computers running SQL Server, you might use a minimally-privileged domain account. Many server-to-server activities can be performed only with a domain user account.
References:https://docs.microsoft.com/en-us/sql/database-engine/configure- windows/configure-windows-service-accounts-and-permissions
NEW QUESTION: 3
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. the altitude at which the radiative change occurs
B. whether the amount of radiative change is specified or calculated
C. whether the radiative change is directed toward or away from the earth
D. the precision with which the amounts of radiative change can be determined
E. whether the radiative change is global or more localized
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