Plotted on upper-air maps are temperature (?C), dewpoint (?C), wind speed (kts), wind direction, and the height of the pressure surface above sea level (m). The upper-air station model depicted in Figure 8A-4, is similar but distinct from surface station models. If the wind speed reaches 50kts, a flag is added to the wind shaft. Temperature (?C) Dewpoint (?C)? Altitude ( tens m)=5490 m Wind (southeast, 65kts)? Figure 8A-4. Upper-air station model legend (500 mb). Table 8A-1 Standard Atmosphere altitude of the pressure surface and the missing digits needed to decode the three plotted numbers (xxx). *If the 700-mb level is below 3000 m, it requires a 2 in front of the values. Conditions at 500-mb are in the middle troposphere, however weather systems extend well into the troposphere, and a three-dimensional understanding of them is necessary for making accurate weather forecasts. Figure 8A-5 is the 500-mb constant-pressure map for 00Z14 March 2021, the upper-air conditions over the coterminous U.S. and adjacent areas of Canada and Mexico.
Figure 8A-5. Analyzed upper-air weather map with height contours (isohypses), isotherms, and 500 mb radiosonde data for O0Z 14 MAR 2021. 15. Recalling that the heights plotted at individual stations on 500 -mb maps are in tens of meters (place a 0 to the right of the three plotted digits), the coded height at Midland-Odessa (MAF), in west Texas ("572") indicated 500mb occurred at m above sea level. a. 57.2 b. 572 c. 5720 d. 57,200 16. On the 500?mb map, the station observation for Midland-Odessa shows that, at the 500?mb pressure level over the station, the temperature was ?C. a. -11 b. -13 c. -25 d. -57
17. The dewpoint at 500mb over Midland-Odessa was ?C. One of the driest reports on the map! a. -25 b. -31 c. -45 d. -57 18. The wind at Midland-Odessa was generally from the southwest at knots. (The wind being reported has one flag, and four long feathers.) a. 25 b. 30 c. 45 d. 75 e. 90