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NEW QUESTION: 1
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. Accounting for the altitude at which cloud formations appear
C. Isolating ozone changes caused specifically by anthropogenic factors
D. Measuring variations in cloud density in relation to air temperature
E. Monitoring radiative feedbacks and forcings over a longer time period
Answer: A
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.

NEW QUESTION: 2
You are a system administrator responsible for maintaining Microsoft Dynamics 365 at your company.
Management wants a new application built that allows them to manage requests for vendors.
You need to use the app designer to build the new application on Microsoft Dynamics 365.
What are three items that can be configured in the app designer? Each correct answer presents a complete solution.
A. a dashboard for the new app
B. a site map for the new app
C. a role to be used by the new app
D. a workflow for the new app
E. a business rule for the new app
Answer: A,B,C

NEW QUESTION: 3

A. Option B
B. Option D
C. Option A
D. Option C
Answer: D
Explanation:
To add a node to an existing SQL Server failover cluster, you must run SQL Server Setup on the node that is to be added to the SQL Server failover cluster instance. Do not run Setup on the active node.
The Installation Wizard will launch the SQL Server Installation Center. To add a node to an existing failover cluster instance, click Installation in the left-hand pane. Then, select Add node to a SQL Server failover cluster.