LINKS CHAPTER 6 HUMIDITY, SATURATION, AND STABILITY Books [~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~] Class Meetings Course 1. The largest fresh water reservoir in the global Description hydrologic cycle: Course Schedule oceans Grading lakes Learning ice sheets and glaciers Objectives ground water Photographs Practice 2. On the continents over the course of a year, annual Questions precipitation _______ annual evapotranspiration. Special Notice equals Student is greater than Responsibilities is less than is much less than Access to Online Daily Weather 3. Rain may Summary and infiltrate the soil. Learning run off into rivers and lakes. Activities evaporate. some combination of the above is correct National Weather Service - Green 4. The saturation vapor pressure is _______ proportional Bay to air temperature. directly Home inversely not 5. The saturation mixing ratio is _______ proportional to air temperature. directly inversely not 6. The mixing ratio is 10 g/kg and the relative humidity is 40%. What is the saturation mixing ratio? 4 g/kg 25 g/kg 2.5 g/kg 50 g/kg 7. The vapor pressure is 3 mb and the saturation vapor pressure is 12 mb. What is the relative humidity? 25% 100% 33.3% 2.5% 8. The vapor pressure is 18 mb and the saturation vapor pres-sure is 18 mb. What is the relative humidity? 25% 100% 40% 6.8% 9. Relative humidity is _______ proportional to air tempera-ture. directly inversely not 10. On a clear and calm day, the relative humidity has its lowest value at sunrise. around 3 A.M. when air temperature is maximum just after sunset. 11. The relative humidity increases when the vapor pressure is constant and the air temperature rises. the saturation vapor pressure increases. the air cools None of the above is correct. 12. The relative humidity increases when the temperature is constant and the vapor pressure decreases. the saturation vapor pressure increases. the mixing ratio increases the saturation mixing ratio increases. 13. As saturated (cloudy) air ascends within the atmosphere, its temperature rises. it expands and cools its relative humidity increases. its saturation vapor pressure increases. 14. As unsaturated air ascends within the atmosphere, its tem-perature rises at 10 Celsius degrees per 1000 meters. does not change. drops at 6 Celsius degrees per 1000 meters falls at the dry adiabatic lapse rate 15. An unsaturated air parcel at an initial temperature of 5 C is forced to ascend 2500 meters. Following ascent, the air parcel has a temperature of 5 C 30 C -20 C -10 C 16. The moist adiabatic lapse rate is constant. is about 10 Celsius degrees per 1000 meters. equals the dry adiabatic lapse rate. ranges from about 4 Celsius degrees per 1000 m to almost 9 Celsius degrees per 1000 m 17. Atmospheric stability can change with altitude time location any of the above is correct 18. Which one of the following soundings indicates an atmosphere that is unstable for both cloudy and clear air parcels. -12 Celsius degrees per 1000 m -10 Celsius degrees per 1000 m +1 Celsius degree per 1000 m +6 Celsius degrees per 1000 m 19. In an inversion, air temperature _______ with increasing altitude. rises drops does not change 20. A temperature inversion indicates _______ atmospheric condi-tions. stable neutral unstable Score = Correct answers: [~ ~ ~ ~ ~ ~ Back to Top ~ ~ ~ ~ ~ ~] Web Site created by David Dimmer Last Updated on December 11, 1998