lecture 11-12 water vapour as a major energy carrier

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Terrestrial Energy Systems Lecture

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  • CIV300 Terrestrial Energy Systems

    Water Vapour as a Major Energy Carrier Lecture 11 - 12

    1

  • l Humidity Ra+o = Mass of vapour / mass of dry air (g/kg or no dims)

    l This is the absolute amount of water vapour in the airand we represent this as a percentage of the total possible with the relaNve humidity (RH as a %).

    l Atmospheric pressure varies with atmospheric humidity (Daltons Law of ParNal Pressures)

    l E = Actual Vapour Pressure

    l E* = Saturated Vapour Pressure

    How to Dene Humidity? 2

  • E* is the saturated vapour pressure

    SaturaNon Vapour Pressure Curve 3

  • Psychrometric Chart 4

    Dry Bulb Temperature

    Humidity RaNo (g/kg)

    Enthalpy (kJ/kg of dry air)

    SaturaNon temperature

  • l Chart has a bewildering range of potenNal measurements

    l Focus on dry bulb, wet bulb, relaNve humidity, dew point, humidity raNo, enthalpy

    l Psychrometric Chart provides a graphic relaNonship of the condiNon of air

    Key Items 5

  • l Wet Bulb temperature relates relaNve humidity to the dry air temperature (Dry Bulb) via the energy, or Enthalpy (kJ/kg) - a measure of how it feels

    l A direct measure of the ability to evaporate and therefore cool a thermometer. The higher the RH, the less the ability to evaporate and cool

    l The drier the air the more rapid evaporaNon on a thermometer the lower the wet bulb. OR the moister the air, the closer dry bulb to wet bulb.

    l Dry Bulb Temperature (deg C) = Web Bulb temperature at 100% RH follow the enthalpy lines to the curve to read it.

    Wet Bulb 6

  • Wet Bulb Temperature Measurement 7

  • l ASHRAE states we need to meet 27oC dry bulb / 21oC wet bulb

    l Equates to 27oC / 58% RH

    Toronto Design Day 8

  • l ASHRAE states we need to meet 30oC dry bulb / 25oC wet bulb

    Equates to 30oC / 67% RH

    Melbourne, FL Design Day 9

  • How Air CondiNoning Works. 10

  • 11

  • 12

  • Reading from the Chart.

    Air at 30oC/50% RH? 22oC wet bulb 65 kJ/kg enthalpy 0.013 kg/kg dry air moisture content

    13

  • l Dead of winter

    l Tropical summer

    l Desert heat

    l Humidity in the home

    Real Life 14

  • l Can now see why we get dew and frost

    l AdiabaNc cooling forces RH to 100% condensaNon

    l Find the dry bulb and RH, follow the line horizontally as it cools, unNl it meets the curve

    l If ambient temperature is

  • Dew point

    Frost point

    16

  • Reading from the Chart.

    0.013 humidity raNo 18oC dew point

    17

  • l Which window got caulked?

    ! !!

    18

  • Light Relief

    l What is the Humidex? 19

  • So the humidex IS related to the wet bulb in laymans terms

    Humidex 20

  • The humidex 21

  • 1. Radia+on fog

    Ground cools o at night. Reduces temperature of moist air which then reaches the dew point. Fog.

    l Why does fog burn o in sunlight?

    Types of Fog 22

  • 2. Advec+on fog

    Moist air blows across cold surface.

    Welcome to Newfoundland.

    Types of Fog 23

  • Catch the Fog 24

  • l Warm moist air rises up e.g. summer over Lake Ontario

    l What happens on the chart?

    Low Level Cloud FormaNon 25

  • 26

  • Air Mass and Mountains

    l The moist wind approaches from the westor east in Nanaimo

    l Recall psychrometrics

    l What happens when it hits the dew point?

    27

  • 28

  • How Air CondiNoning Weather Works. 29