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NEW QUESTION: 1
The IT Management team is interested in the new features of the Check Point R80 Management and wants to upgrade but they are concerned that the existing R77.30 Gaia Gateways cannot be managed by R80 because it is so different. As the administrator responsible for the Firewalls, how can you answer or confirm these concerns?
A. R80 Management requires the separate installation of compatibility hotfix packages for managing the earlier versions of Check Point Gateways prior to R80. Consult the R80 Release Notes for more information.
B. R80 Management cannot manage earlier versions of Check Point Gateways prior to R80. Only R80 and above Gateways can be managed. Consult the R80 Release Notes for more information.
C. R80 Management was designed as a completely different Management system and so can only monitor Check Point Gateways prior to R80.
D. R80 Management contains compatibility packages for managing earlier versions of Check Point Gateways prior to R80. Consult the R80 Release Notes for more information.
Answer: D
Explanation:
Explanation/Reference:
Explanation:
Reference: http://dl3.checkpoint.com/paid/1f/1f7e21da67aa992954aa12a0a84e53a8/ CP_R80_ReleaseNotes.pdf?HashKey=1479838085_d6ffcb36c6a3128708b3f6d7bcc4f94e&xtn=.pdf
NEW QUESTION: 2
A. Option D
B. Option C
C. Option A
D. Option B
Answer: D
Explanation:
http://technet.microsoft.com/en-us/library/ms191545.aspx
NEW QUESTION: 3
Goal plan templates can be deleted?
Response:
A. True
B. False
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.
Based solely on the information in the passage, which of the following research methods, if implemented, would be most likely to yield a more accurate prediction of the extent and direction of the greenhouse effect?
A. Isolating the cooling influence1 of ozone changes from their warming influence
B. Measuring variations in cloud density in relation to air temperature
C. Isolating ozone changes caused specifically by anthropogenic factors
D. Monitoring radiative feedbacks and forcings over a longer time period
E. Accounting for the altitude at which cloud formations appear
Answer: A
Explanation:
Explanation/Reference:
Explanation:
According to the passage, a given vertical distribution of ozone affects atmospheric temperatures in both directions at once. Accordingly, by isolating the cooling influence of a given distribution of ozone from its warming influence, scientists might better predict whether changes in the vertical distribution of ozone will have a net cooling or a net warming effect.
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