Chapter 3 Air Temperature Introduction Temperature –the measure of sensible heat of a substance,...
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Transcript of Chapter 3 Air Temperature Introduction Temperature –the measure of sensible heat of a substance,...
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Chapter 3
Air Temperature
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Introduction
• Temperature– the measure of sensible heat of a substance, or– Typically measured or observed at 4 feet above
the ground surface
• Many factors affect the temperature at a location, but there are five key factors...
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Instrument Shelter
• Thermometer at 1.2 m• Underlying surface –
grass or bare soil/dirt• Shelter is painted
white and has “vents” to allow air to flow through freely
• Set up so door opens away from Sun (on north side in NH) – why?
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Factors Influencing Temperature
1. Insolation– INcoming SOLar
radiATION
– affected by rotation and revolution of Earth
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Factors Influencing Temperature
2. Latitude- in general, temperatures decrease from equator to poles – why?
- temps also become more variable with increasing latitude (seasonal variation)
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Factors Influencing Temperature
3. Surface Type- smoothness (solar noon vs. early AM or late afternoon)- dark vs. light-colored surface– Urban Areas (Tucson and outside Tucson) – (Phoenix)
4. Continentality and the marine effect- “coastal vs. interior location” in text- water heats/cools more slowly than land (specific heat)– San Diego vs. Fargo
5. Elevation- lapse rate- greenhouse effect is less
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Continentality vs. Marine Effect
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Temperature Scales and Conversion
• Three scales: Celsius, Fahrenheit, Kelvin• Conversion formulas:
1. Celsius to Fahrenheit: 1.8 x (°C) + 322. Fahrenheit to Celsius: (°F – 32) ÷ 1.83. Celsius to Kelvin: 273.14 + °C
• 32°F/ 0°C=Freezing water• 212°F/100°C=Boiling water
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Surface Temperature• Controlled by balance of energy flow (net
radiation of substance)– If net radiation positive, substance heats– If net radiation negative, substance cools
• 3 Principal ways which energy moves to/from a surface:– 1. Latent heat transfer (storage or release of heat due to
change of state)• Ex: Evap. Cooling OR sweating
– 2. Conduction (flow of sensible heat via contact)– 3. Convection (heat is distributed by rising and mixing)
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Daily Cycle of Air Temperature
• _________is the main cause by the Earth which causes significant variability in incoming solar radiation in a 24-hour period?– Rotation!! (Day=Positive NR, Night=Negative NR)
• In general, lows temps occur in the morning and high temps occur in the afternoon.
• A sort of trickle-down effect from insolation to net radiation to daily temperature
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Daily Cycle of Air Temperature – Insolation (step 1)
• Insolation begins at sunrise, peaks at solar noon, and ends at sunset
• Daily maximum intensity and total daily insolation vary throughout year (day length, sun angle)
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Daily Cycle of Air Temperature – Net Radiation (step 2)
• Surplus beginning just after sunrise and ending just prior to sunset, deficit otherwise
• Magnitude and duration vary throughout year (day length, sun angle... again!)
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Daily Cycle of Air Temperature – The End Result
• Min temp occurs around sunrise (longest period of no insolation/negative net radiation); max occurs in mid-afternoon (convection causes mixing of warm/cool air)
• So... insolation and net radiation affect daily temp cycle (ignoring other conditions like cloudiness, fronts, precipitation, etc.)
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Human Activity and Temperature
• How do humans impact temperature?1. Removal of vegetation – less cooling via transpiration/evapotranspiration2. Pavement – conduct and hold heat3. Structures – more absorption; more reflection by vertical surfaces4. Fuel consumption/exhaust – a/c5. Greenhouse gases (mostly long-term)
• # 1 – 4 lead to development of urban heat island
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What’s an Urban Heat Island?
• Warmer area surrounding city due to less vegetation, building structure/components, pavement, and fuel consumption/exhaust
• Noticeable in both high and low temperatures• Does Tucson have one?
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Rural vs. Urban Climate Warming
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Vertical Temperature Structure of the Atmosphere
• With an increase in altitude, temperature can:
1. Lapse rate: temp decrease with height• MOST COMMON
2. Inversion: temp increase with height
3. Isothermal layer: no temp change
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Vertical Temperature Structure of the Atmosphere – Lapse Rate
• Lapse rate not always the same, but varies with humidity and temperature and moisture advection
• Measures the drop in temperature in degrees Celsius per 1,000m
• Just an average rate (6.5°C/1,000m)
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Vertical Temperature Structure of the Atmosphere
• Thermosphere– Upper layer, temp increases with height– Location of auroras (interaction of ions and radiation)
• Mesosphere– 3rd layer, temp decreases with height until mesopause– Lowest average temperatures in atmosphere (-90°C)
• Stratosphere– Next layer, strong ozone presence– Temp increases with altitude until stratopause
• Troposphere– Lowest layer, where most weather phenomena occur– Temp decreases with altitude until tropopause
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Vertical Temperature Structure of the Atmosphere
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Annual Cycle of Air Temperature• Revolution and tilt of axis variations in day length
insolation variation cycle of net radiation cycle of mean (average) monthly temperatures
• Also affected by:1. Elevation 3. Continentality vs. marine effect
2. Latitude 4. Albedo
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World Temperature Characteristics
• Common practice is to analyze January and July temperature – why?
• Study both spatial and temporal patterns• Isotherms-lines that are drawn on a map to
connect locations having the same temperature– World patterns of isotherms
• 1. Latitude
• 2. Coast/Interior
• 3. Elevation
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Spatial Temperature Patterns
• General decrease with increasing latitude (large annual insolation variation)
• Large land masses in high latitudes get VERY COLD (snow cover high albedo)
• Little change in equatorial regions (small annual insolation variation)
• Large north-south shift in isotherms over land, less over oceans (continentality, marine effect)
• High-elevations cold vs low elevations (lapse rate)• Perpetually ice- and snow-covered regions always much
colder than elsewhere (high elevation, high albedo)
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Spatial Temperature Patterns
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Temporal Temperature Patterns
• Annual range increases with latitude (insolation variations)
• Largest annual ranges over arctic/sub-arctic zones of Asia and North Am. (insolation)
• Moderately large ranges over tropical deserts (continentality)
• At same latitude, annual range over ocean less than over land (marine effect)
• Annual range very low over tropical oceans (little annual insolation variation, marine effect)
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Temporal Temperature Patterns
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Temporal Temperature Patterns
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Climate Change Studies• Ice cores and tree-ring growth• Climate modeling: “popular” technique is study of
increasing (usually doubling) CO2
• Intergovernmental Panel on Climate Change (IPCC)– 1995: “climate warming due to human activity”– 2001: global mean temp ↑, snow/ice cover ↓, global mean sea
level ↑, greenhouse gas concentrations ↑, cloud cover/precip ↑ in mid-latitudes of NH
• Kyoto Protocol- 1997: 38 industrial nations agree to ↓ greenhouse gas emissions to ~5% below 1990 levels- 1998: implementation of 1999-2000 reductions, emission trades, developing countries join- 2001: W rejects US participation, but 178 new nations