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Chapter 5 Global Temperature (Continued). Lecture 12 2 February, 2005. Land versus ocean differences. Clouds and Temperature Changes. Clouds trap net radiation in lower troposphere. Clouds reduce surface insolation. Little seasonal change in ocean surface temp. - PowerPoint PPT Presentation
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Chapter 5
Global Temperature (Continued)
Lecture 122 February, 2005
Land versus ocean differences
Clouds and Temperature Changes
Clouds reduce surface insolation
Clouds trap net radiation in
lower troposphere
Little seasonal change in
ocean surface temp
warmest ocean waters occur in
the western tropical Pacific
notice the changes in sea
ice in the northern and
southern hemispheres
focus on differences between the northern and southern hemispheres
why should northern Siberia
have the greatest seasonality?
why should the seasonality in N.
America be smaller than in Asia at similar
latitudes?
Difference between January & July
Seasonal Temperature Range in Siberiathe seasonality in northern
Siberia is extreme for several reasons:
continentalitysolar angles
clear, dry air with little cloud cover (think of albedo & greenhouse
cloud effects)Verkhoyansk, Russia has a 105 °C min-max range!
Marine and Continental Climates
WitchitaKS
San FranciscoCA
Marine and Continental Climates
VerkhoyanskRussia
TrondheimNorway
Gulf Stream & Temperature inWestern Europe
think of the Gulf Stream as a gigantic river of warm water in the Atlantic (moving about
6.4 kph/4 mph)the amount of water flow in this ‘river’ is
~100 sverdrups (100 million cubic meters per second)
Not exactly the whole story…
the Gulf Stream was named and partly discovered by Benjamin Franklin
The Gulf
Stream
The Gulf Stream and Temperatures in Western Europe
the Gulf Stream largely explains why Iceland is mostly green, even though it sits just below the
Arctic Circlevariations in the Gulf Stream have had huge implications for human societies, such as
allowing the Vikings to reach eastern Canada and the little Ice Age
water-to-land heat transfers are accomplished via latent heat transfers and
direct sensible heating of air overlying warm water
Movie: ‘The Day After Tomorrow’
California current & temperatures
in coastal Californiawater can directly warm or
cool nearby land masses - compare California’s cool
coastal Mediterranean climate with the warm coastal climate of Italy
Air temperature patterns
isotherm - a line connecting points of equal temperature - analogous to a line on a topo map connecting points of equal elevation
some definitions
thermal equator - a line connecting all points of highest average temperature
notice the thermal
equator over land
notice the influence of
large mountain
ranges
see how isotherms
shift poleward
over continental interiors?
where would the hottest places be?
why?
•Show energy budget animation
Air Temperature and the Human Body
•Wind chillCorrelates cold and wind speed
•Heat indexCorrelates heat and humidity
Wind Chill Table
Heat Index Table
Figure 2
Chapter 6Atmospheric and Oceanic Circulation
Concepts in this chapterair pressure
winds (global, regional, and local)global circulation systems
four driving forces in the atmosphereprimary high and low pressure areas in the atmosphere
upper air circulationocean currents & circulation
“We live submerged at the bottom of an ocean of the element air.”
-Evangelista Torricelli
Air Pressure
Air pressurerecall that air pressure is force per unit
area
Ideal Gas LawP V = n R T
where R is a constantPressure*Volume = Moles*constant*Temperature
With Moles of air constant, Pressure increases
• as Volume decreases (Temperature constant)• as Temperature increases (constant Volume)
Ideal Gas LawPV = nRT
I. pressure increases if # molecules increases (constant volume)
II. pressure increases if volume decreases (constant temperature)
III. pressure increases if temperature increases (constant volume)
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I. II.
Pressure*Volume = Moles*constant*Temperature
III.
a quick and dirty estimate of air pressure at the surface
1. define pressure: force per unit area
2. force = mass*acceleration due to gravity
(F = m g)3. mass of the atmosphere = 5x1018
kggravitational acceleration = 9.81 m s-2
4. surface area of Earth = 4R2
= 4(6,400km)2 = 5x1014 square meters5. plug it all in ….
Pressure = F / A = m g /A= 5x1018 kg * 9.81 m s-2 / 5x1014 m2
~ 100,000 kg /(m s2) Newtons per m2 (Pascal)
~ 1000 millebar (mb)
sea level pressure = 1013 mb = 101.3 kPa = 14.5 lbs/sq. in = 29.92” mercury = 760 mm mercury = 1
atmosphere
the weight of air literally pushes mercury up the
column
what would the column’s height be on
top of Mt. Everest?
elevation is ~8 km~ 75% of air is below
-> 0.25 * 29.92 in ~ 7.5 in
Barometer
Pressure in the Atmosphere and Ocean
to calculate atmospheric pressure (in mb) by height (Z):
P(Z) = 1014*[1-0.0226*Z]^5.26
to calculate water pressure (in mb) by depth (D, in m):
P(D) = 100*D
Total Pressure by Depth
0
2
4
6
8
10
12
14
1013
1023
13
2036
13
3049
13
4062
13
5075
13
6088
13
7101
13
8114
13
9127
131E
+061E
+061E
+06
Pressure (mb)
Dep
th (
km)
even though gravity is pulling on both air and water, air is compressible (water
is not)
Scuba Diving & Pressurerule of thumb in scuba diving:
Each 10 m (33 ft) increase in depth increases the pressure on every square
inch of your body by 1 atmosphere
Dive to 30 m, you have 4 atmospheres of pressure pushing on you (3 ocean + 1
atmos)