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NEW QUESTION: 1
Which phase of Fast Recovery rolls forward (restores) all transactions since the last checkpoint and rolls back any uncommitted transactions?
A. Physical Recovery
B. Dbspace Recovery
C. Logical Recovery
D. Transactional Recovery
Answer: C
NEW QUESTION: 2
On which Cisco Configuration Professional screen do you enable AAA
A. AAA Summary
B. Authorization Policies
C. AAA Servers and Groups
D. Authentication Policies
Answer: A
NEW QUESTION: 3
Which two descriptions of FlexConnect mode for Cisco APs are true? (Choose two.)
A. APs that operate in FlexConnect mode cannot detect rogue APs
B. FlexConnect mode is a wireless solution for branch office and remote office deployments
C. FlexConnect mode is used when the APs are set up in a mesh environment and used to bridge between each other.
D. When connected to the controller, FlexConnect APs can tunnel traffic back to the controller
E. FlexConnect mode is a feature that is designed to allow specified CAPWAP-enabled APs to exclude themselves from managing data traffic between clients and infrastructure.
Answer: B,D
Explanation:
FlexConnect is a wireless solution for branch office and remote office deployments. It enables customers to configure and control access points in a branch or remote office from the corporate office through a wide area network (WAN) link without deploying a controller in each office.
The FlexConnect access points can switch client data traffic locally and perform client authentication locally when their connection to the controller is lost. When they are connected to the controller, they can also send traffic back to the controller. In the connected mode, the FlexConnect access point can also perform local authentication.
Reference: https://www.cisco.com/c/en/us/td/docs/wireless/controller/7-
2/configuration/guide/cg/cg_flexconnect.html
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 ozone changes caused specifically by anthropogenic factors
B. Monitoring radiative feedbacks and forcings over a longer time period
C. Measuring variations in cloud density in relation to air temperature
D. Accounting for the altitude at which cloud formations appear
E. Isolating the cooling influence1 of ozone changes from their warming influence
Answer: E
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.