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

NEW QUESTION: 2
네트워크에는 contoso.com과 adatum.com이라는 두 개의 Active Directory 포리스트가 있습니다. 모든 서버는 Windows Server 2012 R2를 실행합니다.
contoso.com과 adatum.com간에 단방향 외부 트러스트가 존재합니다.
Adatum.com에는 Group1이라는 유니버설 그룹이 포함되어 있습니다. contoso.com의 리소스에 대한 액세스를 제공하기 위해 Group1을 사용하지 못하게 해야 합니다.
어떻게 해야 합니까?
A. adatum.com에서 허용 된 인증 권한을 수정하십시오.
B. Group1의 유형을 배포로 변경하십시오.
C. Group1의 관리 대상 설정을 수정하십시오.
D. Group1의 이름을 수정하십시오.
Answer: A
Explanation:
설명
* 고객의 Active Directory에 액세스해야하는 계정에는 인증 허용이라는 특별 권한이 부여됩니다. 그런 다음이 권한은 계정이 액세스해야 하는 고객 Active Directory 내의 컴퓨터 개체 (Active Directory 도메인 컨트롤러 및 AD RMS 서버)에 적용됩니다.
* 트러스트 된 Windows Server 2008 또는 Windows Server 2003 도메인 또는 포리스트의 사용자가 트러스트 인증 설정이 선택적 인증으로 설정된 트러스트 된 Windows Server 2008 또는 Windows Server 2003 도메인 또는 포리스트의 리소스에 액세스하려면 각 사용자가 트러스 팅 도메인 또는 포리스트에 있는 컴퓨터 개체 (자원 컴퓨터)의 보안 설명자에 대한 인증 허용 권한을 명시 적으로 부여해야 합니다.

NEW QUESTION: 3
You create an Ubuntu Linux virtual machine (VM) by using the Azure Portal. You do not specify a password when you create the VM.
You need to connect to the terminal of the VM.
Solution: You connect to the public IP address of the VM by using Secure Shell (SSH) and specify your private key.
Does the solution meet the goal?
A. No
B. Yes
Answer: A