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NEW QUESTION: 1
You use Azure Machine Learning to train and register a model.
You must deploy the model into production as a real-time web service to an inference cluster named service-compute that the IT department has created in the Azure Machine Learning workspace.
Client applications consuming the deployed web service must be authenticated based on their Azure Active Directory service principal.
You need to write a script that uses the Azure Machine Learning SDK to deploy the model. The necessary modules have been imported.
How should you complete the code? To answer, select the appropriate options in the answer area.
NOTE: Each correct selection is worth one point.

Answer:
Explanation:

Explanation:
Box 1: AksCompute
Example:
aks_target = AksCompute(ws,"myaks")
# If deploying to a cluster configured for dev/test, ensure that it was created with enough
# cores and memory to handle this deployment configuration. Note that memory is also used by
# things such as dependencies and AML components.
deployment_config = AksWebservice.deploy_configuration(cpu_cores = 1, memory_gb = 1) service = Model.deploy(ws, "myservice", [model], inference_config, deployment_config, aks_target) Box 2: AksWebservice Box 3: token_auth_enabled=Yes Whether or not token auth is enabled for the Webservice.
Note: A Service principal defined in Azure Active Directory (Azure AD) can act as a principal on which authentication and authorization policies can be enforced in Azure Databricks.
The Azure Active Directory Authentication Library (ADAL) can be used to programmatically get an Azure AD access token for a user.
Incorrect Answers:
auth_enabled (bool): Whether or not to enable key auth for this Webservice. Defaults to True.
Reference:
https://docs.microsoft.com/en-us/azure/machine-learning/how-to-deploy-azure-kubernetes-service
https://docs.microsoft.com/en-us/azure/databricks/dev-tools/api/latest/aad/service-prin-aad-token

NEW QUESTION: 2
You intend to introduce ordering in message processing for your JMS destination by creating a destination key.
Which statement is true about the JMS Destination Key configuration? (Choose the best answer.)
A. A JMS Destination Key allows a user-defined sort key.
B. A JMS Destination Key cannot be specified using WLST.
C. A JMS Destination Key cannot be used to sort messages in a Last In First Out order.
D. A Destination Key can be applied to the message body.
Answer: B
Explanation:
Explanation/Reference:
The WebLogic Server Administration Console enables you to configure, modify, target, and delete destination key resources in a system module.
Incorrect Answers:
B: As messages arrive on a specific destination, by default they are sorted in FIFO (first-in, first-out) order, which sorts ascending based on each message's unique JMSMessageID. However, you can use a destination key to configure a different sorting scheme for a destination, such as LIFO (last-in, first-out).
C: Attribute Sort Key: The message sort key or the name of a message header field on which to sort.
Message header field keys start with the letters JMS and ignore the key type setting.
Valid values only (user-defined sort key not possible):
JMSMessageID

JMSTimestamp

JMSCorrelationID

JMSPriority

JMSExpiration

JMSType

JMSRedelivered

JMSDeliveryTime

Reference: https://docs.oracle.com/cd/E13222_01/wls/docs90/jms_admin/basic_config.html#1105573

NEW QUESTION: 3
展示を参照してください。

この構成に基づいて正確なステートメントはどれですか？
A. スポーク2は認証をハブに渡し、フェーズ2に正常に進みます
B. スポーク1は認証をハブに渡し、フェーズ2に正常に進みます
C. 認証方法が正しくないため、スポーク1は認証に失敗します
D. リモート認証方法が正しくないため、スポーク2は認証に失敗します
Answer: C
Explanation:
Explanation
Spoke 1 should be configured as the following, otherwise it will fails the authentication because the authentication methods are incorrect with the perspective of Hub configurations authentication local pre-shared-key cisco authentication remote rsa-sig ?

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.
According to the passage, radiative forcings and radiative feedbacks can generally be distinguished from each other by
A. whether the radiative change is global or more localized
B. the altitude at which the radiative change occurs
C. whether the radiative change is directed toward or away from the earth
D. the precision with which the amounts of radiative change can be determined
E. whether the amount of radiative change is specified or calculated
Answer: E
Explanation:
Explanation/Reference:
Explanation:
According to the passage, radiative "forcings are quantities normally specified in global climate model situations, while feedbacks are calculated quantities

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