Unit 5

Moist Air

So far we only considered dry air, but already learned that moisture affects pressure, the molecular weight of the air parcel and hence its individual gas constant.

Moist air is important for weather, climate, air quality despite its low, strongly varying fraction of 0 to 4% as we had discussed in Unit 1. Besides its role in the water cycle, water vapor is also playing a large role in the energy-, and trace gas cycle. Water vapor is involved in cloud and precipitation formation, affects radiation, and many gas-phase chemical and aerosol processes.

Water is the only atmospheric constituent that occurs in all its phases in the troposphere. For simplicity we will deal with the moist atmosphere first before, in a later unit, we address phase transition processes between gaseous, liquid & solid states of water. The moisture measures we define in this unit only apply to water vapor.

Mean water vapor distribution in the Northern and Southern hemisphere in the annual cycle
Mean water vapor distribution in the Northern and Southern hemisphere in the annual cycle for various years

Learning goal

Describing the moist atmosphere quantitatively and qualitatively.

Students’ Tasks

  1. Watch the videos on the material
  2. Read chapter 2.7 to 2.7.6 (included) of Lectures in Meteorology
  3. ATM401 students: Answer the questionnaire by Thursday 2359 AST . ATM601, CHEM601 students:  Copy your summary of the material in this form and answer the  by Thursday 2359 AST .
  4. All students: Solve the problems listed in this unit5.

Supplemental material

In case you want to take notes on the slides used in the video, here they are.

Worked example problem

Show that water vapor pressure decreases when the air parcel expands under isotherm conditions.

©Nicole Mölders 2018