prof. fred remer university of north dakota water in the atmosphere
TRANSCRIPT
![Page 1: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/1.jpg)
Prof. Fred RemerUniversity of North Dakota
Water in the AtmosphereWater in the Atmosphere
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Prof. Fred RemerUniversity of North Dakota
ReadingReading
Hess– pp 43 - 44– pp 58 – 60
Tsonis– pp 93 – 97
Wallace & Hobbs– pp 66 – 67– pp 79 – 84
Bohren & Albrecht– pp 181-188
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Prof. Fred RemerUniversity of North Dakota
ObjectivesObjectives
Be able to define water vapor pressure
Be able to define virtual temperature Be able to define specific humidity Be able to define mixing ratio
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Prof. Fred RemerUniversity of North Dakota
ObjectivesObjectives
Be able to calculate the water vapor pressure
Be able to calculate virtual temperature
Be able to calculate specific humidity Be able to calculate mixing ratio
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Prof. Fred RemerUniversity of North Dakota
Water In the AtmosphereWater In the Atmosphere
Unique Substance Occurs in Three Phases Under
Normal Atmospheric Pressures and Temperatures
Gaseous State– Variable 0 – 4%
HH HHOO
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Prof. Fred RemerUniversity of North Dakota
Water in the AtmosphereWater in the Atmosphere
Remember Dalton’s Law?– Law of Partial Pressures
– Let’s look at the contribution of water
p = p1 + p2 + p3 + ….p = p1 + p2 + p3 + ….
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
Ideal Gas Law for Dry Air
Ideal Gas Law for Water Vapor
TRp dd
TRe vv
p = pressure of dry airp = pressure of dry airdd = specific volume of dry air = specific volume of dry air
RRdd = gas constant for dry air = gas constant for dry air
e = vapor pressure of water vapore = vapor pressure of water vaporvv = specific volume of water vapor = specific volume of water vapor
RRvv = gas constant for water vapor = gas constant for water vapor
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
Partial pressure that water vapor exerts
Total PressureTotal Pressurep = pp = pOO22
+p+pNN22+p+pHH22OOvv
Water Vapor PressureWater Vapor Pressuree = pe = pHH22OOvv
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
Gas Constant of Water Vapor
HH HHOO
Wv M
RR
Molecular Weight Molecular Weight (M(Mw w ))
Hydrogen = 1kg kmolHydrogen = 1kg kmol-1 -1
Oxygen = 16 kg kmolOxygen = 16 kg kmol-1-1
Water = 18 kg kmolWater = 18 kg kmol-1-1
1
11
v kmolkg18
kmolKJ8314R
11v kgKJ461R
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
The temperature dry air must have in order to have the same density as moist air at the same pressure
Fictitious temperature
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Dry Air
Total Pressure = pTotal Pressure = p
Volume = VVolume = V
Temperature = TTemperature = T
Mass of Air = mMass of Air = mdd
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Moist Air (Mixture)
Total Pressure = pTotal Pressure = p
Volume = VVolume = V
Temperature = TTemperature = T
Mass of Air = mMass of Air = md d ++ mmvv
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Density of mixture
V
mm vd
vd
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Ideal Gas Law
– For Dry Air
– For Water Vapor Alone
TRp ddd
TRe vv
ororTR
p
d
dd
TR
e
vv oror
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Substitute into density expression
vd
TR
p
d
dd
TR
e
vv
TR
e
TR
p
vd
d
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Dalton’s Law of Partial Pressure
TR
e
TR
p
vd
d
epp d oror eppd
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Substitute eppd
TR
e
TR
p
vd
d TR
e
TR
ep
vd
oror
vd R
e
R
ep
T
1
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Remove Rd
vd R
e
R
)ep(
T
1
v
d
d R
Re)ep(
TR
1
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Define 622.
M
M
R
R
d
w
v
d
eepTR
1
d
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Remove p
eepTR
1
d
p
e
p
e1
TR
p
d
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Rearrange terms
p
e
p
e1
TR
p
d
)1(
p
e1
TR
p
d
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
By definition, virtual temperature is the temperature dry air must have in order to have the same density as moist air (mixture) at the same pressure
vdTRp
TRp ddd TRe vvInstead ofInstead of oror
UseUsep = total (mixture) pressurep = total (mixture) pressure
= mixture density= mixture density
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Substitution of
)1(
p
e1
TR
p
d
vdTRp Into
)1(
p
e1
TR
pRTp
ddv
Produces
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Rearrange
)1(
p
e1
TR
pRTp
ddv
)1(pe
1TRp
R
pT
dd
v
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Start Canceling!
)1(pe
1TRp
R
pT
dd
v
)1(
pe
1
TTv
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Still looks Ugly! Simplify!
)1(
pe
1
TTv
)622.1)(p/e(1
TTv
622.
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
)p/e378(.1
TTv
p = total (atmospheric) pressurep = total (atmospheric) pressure
e = water vapor pressuree = water vapor pressure
T = temperatureT = temperature
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Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Moist air (mixture) is less dense than dry air
Virtual temperature is greater than actual temperature
Small difference
)p/e378(.1
TTv
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
Ratio of the density of water vapor in the air to the (total) density of the air
vq
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
The mass of water vapor (mv) to the mass of dry air
Mass of Dry Air = mMass of Dry Air = mdd
Mass of Water Vapor = mMass of Water Vapor = mvv
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
The mass of water vapor (mv) to the mass of dry air
Mass of Dry Air = mMass of Dry Air = mdd
Mass of Water Vapor = mMass of Water Vapor = mvv
d
v
m
mw
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Expressed in g/kg– Dry Air
1 to 2 g/kg
– Tropical Air 20 g/kg
d
v
m
mw
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Can mixing ratio be expressed in terms of water vapor pressure?
Sure as it will rain on a meteorologist’s picnic!
d
v
m
mw
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
By definition
Divide top and bottom by volume (V)
d
v
m
mw
V/m
V/mw
d
v
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
But density is so.....
V/m
V/mw
d
v
V/m
d
vw
w = mixing ratiow = mixing ratio
vv = density of water vapor in air = density of water vapor in air
dd = density of dry air = density of dry air
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Ideal Gas Law
d
vw
TRp ddd
TRe vv
TR
p
d
dd
TR
e
vv
oror
oror
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Substitute
d
vw
TR
p
d
dd
TR
e
vv
TR
p/
TR
ew
d
d
v
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Simplify
Remember
TR
p/
TR
ew
d
d
v
dv
d
p
e
R
Rw
622.M
M
R
R
d
w
v
d
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Substitute into
But
v
d
R
R
dv
d
p
e
R
Rw
dp
ew
eppd p = total pressure of air (mixture)p = total pressure of air (mixture)
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Substitute into
Ta-Da!
dp
ew eppd
ep
ew
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Expression for Mixing Ratio (w)– Water Vapor Pressure (e) in any units– Atmospheric Pressure (p) in any units
ep
e622.w
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Prof. Fred RemerUniversity of North Dakota
Mixing Ratio (w)Mixing Ratio (w)
Can be used to determine other water variables
Let’s look at– Specific Humidity – Water Vapor Pressure (e)
– Virtual Temperature (Tv)
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
By definition
But
vqq = specific humidityq = specific humidity
vv = density of water vapor in air = density of water vapor in air
= density of air = density of air
dv dd = density of dry air = density of dry air
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
Substitute into
Results in
But
vqdv
dv
vq
V
m
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
Substitute into
Results in
dv
vq
V
m
V/mV/m
V/mq
dv
v
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
Eliminate V
dv
v
mm
mq
V/mV/m
V/mq
dv
v
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
Divide top and bottom by md
dv
v
mm
mq
dddv
dv
m/mm/m
m/mq
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
But so
dddv
dv
m/mm/m
m/mq
d
v
m
mw
1w
wq
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Prof. Fred RemerUniversity of North Dakota
Specific Humidity (q)Specific Humidity (q)
Expression for specific humidity (q)– Mixing Ratio (w) in kg kg-1
1w
wq
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
Pressure exerted by water vapor is a fraction of total pressure of air
Fraction is proportional to # of moles in mixture
pfe e = water vapor pressuree = water vapor pressure
f = fractional amount of water vapor f = fractional amount of water vapor
p = total pressure of airp = total pressure of air
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
How many moles of water are in a sample of air?
Number of moles of water
w
vv M
mn
nnvv = # of moles = # of moles
mmvv = mass of water molecules = mass of water molecules
MMww = molecular weight of water = molecular weight of water
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
How many moles of dry air are in a sample of air?
Number of moles of dry air
d
dd M
mn
nndd = # of moles = # of moles
mmdd = mass of dry air = mass of dry air
MMdd = mean molecular weight of dry air = mean molecular weight of dry air
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
How many moles of air are in a sample of air?
Number of moles of air
d
d
w
v
M
m
M
mn
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
What is the molar fraction of water vapor in the air?
Substitute into
ddwv
wv
M/mM/m
M/mf
pfe
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
Yikes! Let’s make this more manageable!
ddwv
wv
M/mM/m
M/mf
pfe
pM/mM/m
M/me
ddwv
wv
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Prof. Fred RemerUniversity of North Dakota
pM/mM/m
M/me
ddwv
wv
Water Vapor Pressure (e)Water Vapor Pressure (e)
Multiply top and bottowm by Mw/md
pm/M
m/M
M/mM/m
M/me
dw
dw
ddwv
wv
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Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
Canceling out
pm/M
m/M
M/mM/m
M/me
dw
dw
ddwv
wv
pM/Mm/m
m/me
dwdv
dv
![Page 58: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/58.jpg)
Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
But
pM/Mm/m
m/me
dwdv
dv
d
v
m
mw
Mixing RatioMixing Ratio
andand 622.M
M
R
R
d
w
v
d
![Page 59: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/59.jpg)
Prof. Fred RemerUniversity of North Dakota
Water Vapor Pressure (e)Water Vapor Pressure (e)
pM/Mm/m
m/me
dwdv
dv
d
v
m
mw
d
w
M
M
pw
we
![Page 60: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/60.jpg)
Prof. Fred RemerUniversity of North Dakota
pw
we
Water Vapor Pressure (e)Water Vapor Pressure (e)
Expression for water vapor pressure (e)– Mixing Ratio (w) in kg kg-1
– Atmospheric Pressure (p)
![Page 61: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/61.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Derive an expression for virtual temperature (Tv) using mixing ratio (w)
)1(
pe
1
TTv
![Page 62: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/62.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Expression for water vapor pressure
pw
we
)1(
pe
1
TTv
oror
w
w
p
e
![Page 63: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/63.jpg)
Prof. Fred RemerUniversity of North Dakota
)1(
pe
1
TTv
w
w
p
e
Virtual Temperature (TVirtual Temperature (Tvv))
Substituting
)1(
ww
1
TTv
![Page 64: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/64.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Expand
)1(
ww
1
TTv
ww
ww
1
TTv
![Page 65: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/65.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Common denominator w+
ww
ww
1
TTv
ww
ww
ww
TTv
![Page 66: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/66.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Group
ww
ww
ww
TTv
wwww
TTv
![Page 67: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/67.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Simplify
wwww
TTv
ww
TTv
![Page 68: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/68.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Divide numerator by denominator (polynomial division) and eliminate w2 terms
)w1(
wTTv
w1
1TTv
![Page 69: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/69.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (TVirtual Temperature (Tvv))
Substitute = .622
w1
1TTv
w61.1TTv
![Page 70: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/70.jpg)
Prof. Fred RemerUniversity of North Dakota
Virtual Temperature (Tv)Virtual Temperature (Tv)
Expression for virtual temperature– Mixing Ratio (w) in kg kg-1
w61.1TTv
![Page 71: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/71.jpg)
Prof. Fred RemerUniversity of North Dakota
Review of Water VariablesReview of Water Variables
Water Vapor Pressure
TRe vv
pw
we
![Page 72: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/72.jpg)
Prof. Fred RemerUniversity of North Dakota
Review of Water VariablesReview of Water Variables
Virtual Temperature
w61.1TTv
)p/e378(.1
TTv
![Page 73: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/73.jpg)
Prof. Fred RemerUniversity of North Dakota
Review of Water VariablesReview of Water Variables
Mixing Ratio
d
v
m
mw
ep
e622.w
d
vw
![Page 74: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/74.jpg)
Prof. Fred RemerUniversity of North Dakota
Review of Water VariablesReview of Water Variables
Specific Humidity
vq1w
wq
![Page 75: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/75.jpg)
Prof. Fred RemerUniversity of North Dakota
Water in the AtmosphereWater in the Atmosphere
Moisture Variables– Water Vapor Pressure– Virtual Temperature– Mixing Ratio– Specific Humidity
Amount of Moisture in the Atmosphere
![Page 76: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/76.jpg)
Prof. Fred RemerUniversity of North Dakota
Water in the AtmosphereWater in the Atmosphere
Unanswered Questions– How much water vapor can the air hold?– When will condensation form?– Is the air saturated?
The Beer Analogy
![Page 77: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/77.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
You are thirsty! You would like a
beer. Obey your thirst!
![Page 78: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/78.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
Pour a glass but watch the foam
![Page 79: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/79.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
Wait! Some joker put
a hole in the bottom of your Styrofoam cup!
It is leaking!
![Page 80: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/80.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
Having had many beers already, you are intrigued by the phenomena!
![Page 81: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/81.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
Rate at beer flows from keg is constant
![Page 82: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/82.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
Rate at beer flows from keg is constant
Rate at beer flows from cup depends on height
![Page 83: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/83.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
The higher the level of beer in the cup, the faster it leaks!
![Page 84: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/84.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
The cup fills up Height
becomes constant
Equilibrium Reached
Inflow(Constant)
Leakage(Varies with
Height)
![Page 85: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/85.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
What do you do?
Inflow(Constant)
Leakage(Varies with
Height)
![Page 86: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/86.jpg)
Prof. Fred RemerUniversity of North Dakota
The Beer AnalogyThe Beer Analogy
Get a new cup!
![Page 87: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/87.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Similar to what happens to water in the atmosphere
![Page 88: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/88.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Molecules in liquid water attract each other
In motion
![Page 89: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/89.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Collisions Molecules near
surface gain velocity by collisions
![Page 90: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/90.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Fast moving molecules leave the surface
Evaporation
![Page 91: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/91.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Soon, there are many water molecules in the air
![Page 92: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/92.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Slower molecules return to water surface
Condensation
![Page 93: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/93.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Net Evaporation– Number leaving
water surface is greater than the number returning
– Evaporation greater than condensation
![Page 94: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/94.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Molecules leave the water surface at a constant rate
Depends on temperature of liquid
![Page 95: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/95.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Molecules return to the surface at a variable rate
Depends on mass of water molecules in air
![Page 96: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/96.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Rate at which molecule return increases with time– Evaporation
continues to pump moisture into air
– Water vapor increases with time
![Page 97: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/97.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Eventually, equal rates of condensation and evaporation
“Air is saturated” Equilibrium
![Page 98: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/98.jpg)
Prof. Fred RemerUniversity of North Dakota
OverviewOverview
Derive a relationship that describes this equilibrium
![Page 99: Prof. Fred Remer University of North Dakota Water in the Atmosphere](https://reader031.vdocuments.net/reader031/viewer/2022012916/5697bfa81a28abf838c9942c/html5/thumbnails/99.jpg)
Prof. Fred RemerUniversity of North Dakota
Clausius-Clapeyron Clausius-Clapeyron EquationEquation