26.07.2013 Views

Training Guide in Surface Weather Observations - Multiple Choices

Training Guide in Surface Weather Observations - Multiple Choices

Training Guide in Surface Weather Observations - Multiple Choices

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

layer aloft will be considered as midway between the time the balloon beg<strong>in</strong>s to fade until the time the<br />

balloon completely disappears.<br />

Once you have determ<strong>in</strong>ed the amount and height of each layer present at the station you will know what<br />

layer the ceil<strong>in</strong>g will be. If you have learned to evaluate the sky cover and record it correctly, then<br />

determ<strong>in</strong><strong>in</strong>g the ceil<strong>in</strong>g is relatively easy. The ceil<strong>in</strong>g is the lowest layer reported as broken or overcast,<br />

or if the sky is totally obscured, the height of the vertical visibility shall be the ceil<strong>in</strong>g.<br />

When the cloud height is vary<strong>in</strong>g rapidly while you are try<strong>in</strong>g to obta<strong>in</strong> a height, report the average of<br />

all observed values as the height of the layer. If it is the ceil<strong>in</strong>g layer and the average height is less than<br />

3,000 feet and the amount of change is accord<strong>in</strong>g to the criteria given <strong>in</strong> your station’s WSOH, a remark<br />

shall be <strong>in</strong>cluded <strong>in</strong> column 14 of MF1M-10 giv<strong>in</strong>g the range of variability. For example, “CIG<br />

005V010” would <strong>in</strong>dicate a ceil<strong>in</strong>g that was vary<strong>in</strong>g between 500 and 1,000 feet.<br />

5.3.1 Methods Used When Determ<strong>in</strong><strong>in</strong>g Cloud and Ceil<strong>in</strong>g Heights<br />

Determ<strong>in</strong>ation of heights should be supplemented by visual observations and not left solely to<br />

<strong>in</strong>struments themselves. To determ<strong>in</strong>e the height of layers aloft and the vertical visibility <strong>in</strong>to surfacebased<br />

phenomena, the follow<strong>in</strong>g methods can be used.<br />

a. Ceil<strong>in</strong>g Light and Cl<strong>in</strong>ometer. At night, sky cover height and vertical visibility values may be<br />

determ<strong>in</strong>ed with a cl<strong>in</strong>ometer and a projector by us<strong>in</strong>g the follow<strong>in</strong>g procedures:<br />

1. Allow the pendant to sw<strong>in</strong>g freely; sight through the cl<strong>in</strong>ometer center<strong>in</strong>g the <strong>in</strong>tersection<br />

of the cross-hair:<br />

(a) Upon the brightest portion of the light beam spot when the sky cover layer is aloft (see<br />

Figure 5-13), or<br />

(b) On the upper limit of the light beam penetration when the sky is completely obscured<br />

by a surface-based layer (see Figures 5-12 and 5-14).<br />

2. When the pendant has come to rest, lock it <strong>in</strong> position without mov<strong>in</strong>g the cl<strong>in</strong>ometer.<br />

3. Read the <strong>in</strong>dicated angle to the nearest whole degree and release the pendant clutch.<br />

4. Repeat steps 1 through 3 three times, then determ<strong>in</strong>e an average angular read<strong>in</strong>g.<br />

5. Refer to a table appropriate for the basel<strong>in</strong>e used for the equivalent height value of this<br />

average read<strong>in</strong>g.<br />

5-18

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!