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NEW QUESTION: 1
Which button permissions are defined in the JRDM template? There are 2 correct answers to this question.
A. Close
B. Decline
C. Reopen
D. Approve
Answer: A,C

NEW QUESTION: 2
Which three of the following Options should always be selected when configuring a SIP trunk for Cisco Unity Connection integration to Cisco Unified Communication Manager?
A. X.509Subject Name
B. Accept Unisolicited Notification
C. Enable Digest Authentication
D. Enable Application Level Authentication
E. Accept Out-of-Dialog REFER
F. Accept Replaces Header
G. Accept Presence Subscription
Answer: B,E,F
Explanation:
Refhttp://www.cisco.com/en/US/docs/voice_ip_comm/connection/2x/integration/cucm_sip/guide/cucint
cucmsip060.html

NEW QUESTION: 3
Which is a true statement about acceptance criteria?
A. Acceptance criteria are used to produce the customer's quality expectations
B. Once agreed, acceptance criteria CANNOT be changed
C. Acceptance criteria should be agreed between the customer and the supplier
D. Acceptance criteria are less specific and precise than customer's quality expectations
Answer: C

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 amount of radiative change is specified or calculated
B. whether the radiative change is global or more localized
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: A
Explanation:
Explanation/Reference:
Explanation:
According to the passage, radiative "forcings are quantities normally specified in global climate model situations, while feedbacks are calculated quantities