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NEW QUESTION: 1
Which three are features of the NBX Dial Plan timed routes? (Choose three.)
A. Can group time periods and point them to a specific route destination
B. Can disable specific routes for any time period, for example, holiday, night, etc.
C. Can designate a specific destination route for each time period
D. Can create route plans based on a specific date, for example, business, state or country holiday
E. Can create route plans based on specific time-of-day or day-of-week
F. Can create route plans based on pre-configured business hours - open, closed, lunch etc.
Answer: C,E,F

NEW QUESTION: 2
A SaaS provider specifies in a user agreement that the customer agrees that any misuse of the service will be the responsibility of the customer. Which of the following risk response methods was applied?
A. Mitigation
B. Acceptance
C. Transference
D. Avoidance
Answer: C

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. whether the amount of radiative change is specified or calculated
B. the altitude at which the radiative change occurs
C. whether the radiative change is directed toward or away from the earth
D. whether the radiative change is global or more localized
E. the precision with which the amounts of radiative change can be determined
Answer: A
Explanation:
According to the passage, radiative "forcings are quantities normally specified in global climate model
situations, while feedbacks are calculated quantities