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Physical Geographyby Alan Arbogast
Chapter 5
Global Temperature Patterns
Lawrence McGlinnDepartment of GeographyState University of New York - New Paltz
Absorbed Radiation
• Stored in Earth’s land and water surfaces as sensible heat which can be felt & measured
• Stored heat can be released from surface by:– Radiation to atmosphere or to space– Conduction to atmosphere– Evaporation/Latent heat to atmosphere
Evaporation/Latent Heat
• Liquid water → Water vapor (gas)
• Latent Heat – heat energy associated with the changing state of water– Heat absorbed in evaporation– Breaks molecular bonds of liquid– Cannot be felt or measured– Released when condensation occurs
Changing State of Water
GAS
LIQUIDSOLID
Depos
ition
Hea
t Rel
ease
dSu
blim
atio
nH
eat A
bsor
bed
Vaporization
Condensation
Heat R
eleased
Heat A
bsorbed
Heat Released
Heat Absorbed
Melting
Freezing
Reflected Radiation• Depends on surface albedo and angle of
incidence (link to animation)
• Albedo – % of insolation an object reflects– High – dark surfaces– Low – light surfaces
• Angle of incidence – Sun angle– High – little reflectance– Low – high reflectance, esp. water
Solar Radiation and Earth’s Surface
Solar Radiation and Earth’s Surface
Solar Radiation and Earth’s Surface
Local Factors Influencing Air Temperature
• Urban Effect– Urban Heat Island
• Darker surfaces – less reflection• Less forest cover• Less water on surface• Heat from human energy use
The Urban Environment
Urban Heat Island
Global NET R
• Non-vegetated surfaces lose heat in one of 3 ways:– Latent heat of evaporation – energy released
as water changes state– Sensible heat – heat you can feel and
measure; convection and conduction– Ground heating and cooling – energy stored
during warm periods and released during cool periods
Radiation Budgets: Types of Heating
Pasture: Shannon, GA
Desert: Big Bend National Park, TX
Riparian Environment: Rio Grande River, TX
Global Radiation Budget
• Major variations in net radiation by latitude• Surplus vs. Deficit
•Net Radiation – difference between incoming and outgoing radiation
(Balance between incoming and outgoing radiation on Earth)
Global Radiation Budget• Seasonal variation in net radiation
Daily Insolation•Yearly pattern Variation by latitude
Heat vs. Temperature
• Heat and Temperature are not the same thing
• Heat: a form of energy that flows from one system or object to another because the two are at different temperatures
• Temperature: a measure of the average kinetic energy (motion) of individual molecules in matter
Principal Temperature Controls
• Latitude
• Altitude
• Cloud Cover
• Land-Water Heating Differences
Latitude and Temperature
• Latitude – Affects insolation– Sun angles– Daylength
Altitude
• Altitude – High altitude has greater daily range– High altitude has lower annual average
Cloud Cover
Land–Water Heating Differences
• Evaporation (= latent heat)
• Transparency (= penetration of insolation)
• Specific heat (differs among objects)
• Movement (= vertical mixing)
• Ocean currents and sea surface temperatures(= spread of energy spatially)
All this leads to this important concept:Marine vs. continental effects
Land–Water Heating Differences Continental Marine
Land Is Opaque
The Gulf Stream
Marineand Continental Climates
Local Factors Influencing Air Temperature
• Maritime vs. Continental Location
Annual Range of Surface Temp• Temp range on land vs. temp range on water
Earth’s Temperature Patterns
• Isotherm and thermal equator• January Temperature Map
– Thermal equator movement southward– More pronounced over large continents
• July Temperature Map – Thermal equator movement northward– More pronounced over large continents
• Annual Temperature Range Map – Continentality
January Temperatures
July Temperatures
Global Temperature Ranges