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Microsoft Identity and Access Administrator

  • Exam Number/Code : SC-300
  • Exam Name : Microsoft Identity and Access Administrator
  • Questions and Answers : 213 Q&As
  • Update Time: 2019-01-10
  • Price: $ 99.00 $ 39.00

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NEW QUESTION: 1
A good MBO (management by objectives) shares all of the following aspects EXCEPT:
A. Periodic feedback about objectives
B. Goals which are measurable
C. Goals are established by the supervisor/manager
D. Goals which align with corporate level goals and strategies
Answer: C

NEW QUESTION: 2
あなたは侵入テスターであり、特定のサーバーでスキャンを実行しようとしています。クライアントと署名した契約には、スキャンに関する次の特定の条件が含まれています。「攻撃者は、スプーフィングされたソースIPアドレスのセットを使用して、サーバー上のすべてのポートを数回スキャンする必要があります。」このスキャンを実行するためにNmapを使用しているとします。この要件を満たすためにどのフラグを使用しますか?
A. -Aフラグ
B. -gフラグ
C. -fフラグ
D. -Dフラグ
Answer: B
Explanation:
flags -source-port and -g are equivalent and instruct nmap to send packets through a selected port. this option is used to try to cheat firewalls whitelisting traffic from specific ports. the following example can scan the target from the port twenty to ports eighty, 22, 21,23 and 25 sending fragmented packets to LinuxHint.

NEW QUESTION: 3
The UIMA standard allows ______________________.
A. importing of text annotators from other sources
B. importing of physical models from other applications
C. importing of cubes from other applications
D. importing of logical models fromother applications
Answer: A

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. Monitoring radiative feedbacks and forcings over a longer time period
B. Measuring variations in cloud density in relation to air temperature
C. Accounting for the altitude at which cloud formations appear
D. Isolating the cooling influence1 of ozone changes from their warming influence
E. Isolating ozone changes caused specifically by anthropogenic factors
Answer: D
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.