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NEW QUESTION: 1
In reviewing a JavaScript file, you notice a built-in object named: qsvc. Describe how this object was made available to JavaScript.
A. A class named "qsvc" extended the BaseProcessorExtension class and a bean with a parent of "qsvc" deployed this class.
B. A class extended the ScriptAPI class and a bean definition deployed this class.
C. A class named "qsvc" extended the BaseProcessorExtension class and a bean deployed this class.
D. A new class extended the BaseProcessorExtension class and a bean definition specified the name "qsvc".
Answer: D

NEW QUESTION: 2
WX is considering an investment in ST.
At 31 December 20X2 ST had the following balances in its statement of financial position:

Which of the following would cause ST to become an associate investment of WX?
A. WX purchases 50,000 of ST's $1 preference shares.
B. WX purchases 75,000 of ST's $1 equity shares.
C. WX purchases 25,000 of ST's $1 equity shares.
D. WX purchases 15,000 of ST's $1 equity shares and 20,000 of ST's $1 preference shares.
Answer: C

NEW QUESTION: 3
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. Accounting for the altitude at which cloud formations appear
B. Measuring variations in cloud density in relation to air temperature
C. Isolating the cooling influence1 of ozone changes from their warming influence
D. Isolating ozone changes caused specifically by anthropogenic factors
E. Monitoring radiative feedbacks and forcings over a longer time period
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: 4
You have the followings commands on your Cisco Router:
ip ftp username admin
ip ftp password backup
You have been asked to switch from FTP to HTTP. Which two commands will you use to replace the existing commands?
A. ip http client username admin
B. ip http username admin
C. ip http server username admin
D. ip http password backup
E. ip http client password backup
F. ip http server password backup
Answer: A,E
Explanation:
Configuring the HTTP Client
Perform this task to enable the HTTP client and configure optional client characteristics.
The standard HTTP 1.1 client and the secure HTTP client are always enabled. No commands exist to disable the HTTP client. For information about configuring optional characteristics for the HTTPS client, see the HTTPS-HTTP Server and Client with SSL 3.0, Release 12.2(15)T, feature module.
SUMMARY STEPS
1. enable

2. configure terminal

3. ip http client cache {ager interval minutes | memory {file file-size-limit | pool pool-size-limit}

4. ip http client connection {forceclose | idle timeout seconds | retry count | timeout seconds}

5. ip http client password password

6. ip http client proxy-server proxy-name proxy-port port-number

7. ip http client response timeout seconds

8. ip http client source-interface type number

9. ip http client username username

Incorrect Answers:
A: The correct sytax is "ip http client username admin" not "ip http username admin" C: The correct syntax is "ip http client password backup" not "ip http password backup" E, F: "ip http server" commands are not valid for this configuration task.
Reference: HTTP 1.1 Web Server and Client
.http://www.cisco.com/en/US/docs/ios/netmgmt/configuration/guide/nm_http_web.html