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ATM OCN 100 Summer 2002 1 ATM OCN 100 – Summer 2002 LECTURE 5 (con’t.) AIR TEMPERATURE: A Fundamental Weather Element u A. Background & Definitions u B. Thermometry u C. Near-surface air temperature climatology
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MADISON’S CURRENT WEATHER Madison Weather at 1000 AM CDT MON 24 JUN 2002 Updated twice an hour at :05 and :25 Sky/Weather: SUNNY Temperature: 81 F (27 C) Dew Point: 64 F (17 C) Relative Humidity: 56% Wind: SW6 MPH Barometer: 30.11F (1019.6 mb)
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ATM OCN 100 Summer 2002 3 Current Surface Winds with Streamlines & Isotachs (“iso” = equal & “tach” = speed) H L L H L H
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ATM OCN 100 Summer 2002 4 Current Surface Weather Map with Isobars (“iso” = equal & “bar” = weight), Fronts and Radar
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ATM OCN 100 Summer 2002 5 Current Temperatures ( ° F) & Isotherms (“iso” = equal +”therm” = temperature)
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ATM OCN 100 Summer 2002 6 This morning’s low temperatures ( o F)
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ATM OCN 100 Summer 2002 7 Yesterday’s high temperatures ( o F)
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ATM OCN 100 Summer 2002 8 Yesterday’s High Temperatures ( o F) – (1961-90) Average High Temperatures
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ATM OCN 100 Summer 2002 9 Current Dewpoints ( o F)
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ATM OCN 100 Summer 2002 10 Current Apparent Temperatures ( o F)
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ATM OCN 100 Summer 2002 11 Current Surface Weather Map with Isobars (“iso” = equal & “bar” = weight), Fronts and Radar
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ATM OCN 100 Summer 2002 12 CURRENT IR GABRIELLE
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ATM OCN 100 Summer 2002 13 Tomorrow AM Forecast Map
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ATM OCN 100 Summer 2002 14 Announcements u Homework 1 –Get from our webpage F http://www.aos.wisc.edu/~hopkins/aos100/homework/ –Due this Thursday 27 June 2002
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ATM OCN 100 Summer 2002 15 LATEST RADAR
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ATM OCN 100 Summer 2002 16
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17 Current Surface Weather Map with Isobars (“iso” = equal & “bar” = weight), Fronts and Radar
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ATM OCN 100 Summer 2002 18 Today is the Summer Solstice See Fig. 2.10 Moran & Morgan (1997)
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ATM OCN 100 Summer 2002 19 Earth’s Orbit of Sun – The Cause of the Seasons See Fig. 2.10 Moran & Morgan (1997)
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ATM OCN 100 Summer 2002 20 Today is the Autumnal Equinox See Fig. 2.10 Moran & Morgan (1997)
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ATM OCN 100 Summer 2002 21
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23 Track of Tropical Storm Helene
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ATM OCN 100 Summer 2002 24 Surface Weather Map from Today with Isobars & Fronts
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ATM OCN 100 Summer 2002 25 Forecast Weather Map for Tomorrow Morning
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ATM OCN 100 Summer 2002 26 Current Temperatures ( o F) & Isotherms
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ATM OCN 100 Summer 2002 27 Current Temperatures ( o F) – 24 Hrs Ago
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ATM OCN 100 Summer 2002 28 Last 24 hrs in Madison
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ATM OCN 100 Summer 2002 29 ATM OCN 100 - Summer 2002 LECTURE 5 AIR TEMPERATURE: A Fundamental Weather Element u A. BACKGROUND –Why do we want to know air temperature? – Meteorological Significance of Temperature F A measure of energy of atmosphere – Human Significance of Temperature F Humans are warm blooded; F Humans maintain a constant temperature.
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ATM OCN 100 Summer 2002 30 THE DEFINITIONS u TEMPERATURE – A measure of “heat intensity” of object. – Proportional to average energy of motion of individual molecules; or to average molecular speed. u HEAT – A form of energy; – Proportional to total amount of thermal energy found in object.
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ATM OCN 100 Summer 2002 31 B. THERMOMETRY u The Science of Thermometry – Measuring temperature. u Types of Thermometers – Liquid-in-glass thermometers – Deformation thermometers – Electrical thermometers – Radiation thermometers (radiometers) where... where...
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ATM OCN 100 Summer 2002 32 LIQUID-IN-GLASS THERMOMETERS u Concept: – Volume of fluid (Liquid mercury or alcohol) proportional to temperature; – Measure expansion of liquid in sealed tube.
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ATM OCN 100 Summer 2002 33 LIQUID-IN-GLASS THERMOMETERS (con’t.) u Special Recording Thermometers – Maximum recording thermometers (Mercury thermometers) – Minimum recording thermometers (Alcohol thermometers)
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ATM OCN 100 Summer 2002 34 Maximum-Minimum Thermometers
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ATM OCN 100 Summer 2002 35 DEFORMATION THERMOMETERS u Concept: – Length of material (e.g., metal) proportional to temperature; – Deflection of material monitored.
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ATM OCN 100 Summer 2002 36 DEFORMATION THERMOMETERS u Example: – Bimetallic Thermometer; – Used in Thermostats & Thermographs.
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ATM OCN 100 Summer 2002 37 ELECTRICAL THERMOMETERS u Concept: – Electrical resistance of material proportional to temperature; – Measure electric current. u Example: – Thermistor; – Used in radiosondes & automatic weather stations.
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ATM OCN 100 Summer 2002 38 A Radiosonde
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ATM OCN 100 Summer 2002 39 Thermistor on Radiosonde
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ATM OCN 100 Summer 2002 40 Thermal Sensor at ASOS
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ATM OCN 100 Summer 2002 41 RADIATION THERMOMETERS u Concept: – “Heat Radiation” from material proportional to object’s temperature; – Measure emitted radiation. u Example: – Radiometer; – Used on-board satellites.
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ATM OCN 100 Summer 2002 42 Temperatures Retrieved from Infrared Satellite Imagery http://www.ametsoc.org/amsedu/WES/composite_ir.html
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ATM OCN 100 Summer 2002 43 Example of Satellite-Based Radiometers: Current Sea Surface Temperatures from SSEC http://www.ssec.wisc.edu/data/sst/latest_sst.gif
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ATM OCN 100 Summer 2002 44 THERMOMETRY [con’t.] u Measurement requirements – Standard instruments – Thermometer Exposure – Standardized observations
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ATM OCN 100 Summer 2002 45 Surface Weather Station
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ATM OCN 100 Summer 2002 46 Inside an Instrument Shelter
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ATM OCN 100 Summer 2002 47 Automated NWS-FAA Surface Weather Station
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ATM OCN 100 Summer 2002 48 Thermal Sensor at ASOS
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ATM OCN 100 Summer 2002 49 THERMOMETRY [con’t] u Temperature Scales – Historical Background – The Fahrenheit, Celsius and Kelvin Scales – Temperature Scale Conversions where...
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ATM OCN 100 Summer 2002 50 THERMOMETRY [con’t] u Temperature Scales – Historical Background F Need at least 2 reproducible points – The Fahrenheit, Celsius & Kelvin Scales
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ATM OCN 100 Summer 2002 51 Reproducible Reference Temperature Points See Fig 4.3 Moran & Morgan (1997)
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ATM OCN 100 Summer 2002 52 Temperature Scales Fig. 3.1 Moran & Morgan (1997)
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ATM OCN 100 Summer 2002 53 TEMPERATURE SCALES (con’t.) u Relationships:
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ATM OCN 100 Summer 2002 54 TEMPERATURE SCALES (con’t.) u Converting Fahrenheit to Celsius
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ATM OCN 100 Summer 2002 55 TEMPERATURE SCALES (con’t.) u Converting Celsius to Fahrenheit
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ATM OCN 100 Summer 2002 56 TEMPERATURE SCALES (con’t.) u Converting Celsius to Kelvin u Converting Kelvin to Celsius
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ATM OCN 100 Summer 2002 57 C. THE CLIMATOLOGY of NEAR- SURFACE AIR TEMPERATURE u Temporal Variation in Air Temperature – diurnal cycle (afternoon maximum vs. sunrise minimum) – annual cycle (summer maximum vs. winter minimum)
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ATM OCN 100 Summer 2002 58 January Temperatures - Madison, WI (1981-90)
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ATM OCN 100 Summer 2002 59 July Temperatures - Madison, WI (1981-90)
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ATM OCN 100 Summer 2002 60 Sample Meteorogram for Madison, WI
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ATM OCN 100 Summer 2002 61 Last 24 hours for Madison, WI
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ATM OCN 100 Summer 2002 62 Last 24 hours for Madison, WI
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ATM OCN 100 Summer 2002 63
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64 C. THE CLIMATOLOGY of NEAR- SURFACE AIR TEMPERATURE u Temporal Variation in Air Temperature – diurnal cycle (afternoon maximum vs. sunrise minimum) – annual cycle (summer maximum vs. winter minimum) u Spatial Variation in Air Temperature – north-south (polar vs. tropical) – land-ocean (continental vs. maritime)
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ATM OCN 100 Summer 2002 65
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68 This morning’s low temperatures ( o F)
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ATM OCN 100 Summer 2002 69 Yesterday’s high temperatures ( o F)
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ATM OCN 100 Summer 2002 70 Yesterday’s High Temperatures ( o F) – (1961-90) Average High Temperatures
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ATM OCN 100 Summer 2002 71 C. THE CLIMATOLOGY of NEAR- SURFACE AIR TEMPERATURE (con’t.) u Average Daily Temperatures & Degree-Day Units – Background – Types of Degree-Day Units F Heating Degree-Day Units F Cooling Degree-Day Units F Growing Degree-Day Units – Degree-Day Units Computations (where...)
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ATM OCN 100 Summer 2002 73 From NOAA: Climate Prediction Center
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ATM OCN 100 Summer 2002 74
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75 DEGREE-DAY CALCULATIONS u Calculate daily average temperature & then Heating Degree-Day Units:
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ATM OCN 100 Summer 2002 76 HEATING DEGREE-DAY CALCULATION u If T max = 40 o F and T min = 30 o F, then:
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ATM OCN 100 Summer 2002 77 Annual Heating Degree Day Units See Fig. 3.11A Moran & Morgan (1997) 7493 149 10269 Point Barrow: 19674
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ATM OCN 100 Summer 2002 78 DEGREE-DAY CALCULATIONS u Calculate daily average temperature & then Cooling Degree-Day Units:
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ATM OCN 100 Summer 2002 79 COOLING DEGREE-DAY CALCULATION u If T max = 80 o F and T min = 60 o F, then:
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ATM OCN 100 Summer 2002 80 D. VARIATION OF OBSERVED AIR TEMPERATURE WITH HEIGHT u Temperature lapse rates – Rate of temperature decrease with height – Units: Celsius degrees per 1000 meters or Fahrenheit degrees per 1000 feet u Layer nomenclature – lapse – inversion – isothermal where... where...
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ATM OCN 100 Summer 2002 81 LAPSE CONDITIONS Temperature decreases with height
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ATM OCN 100 Summer 2002 82 INVERSION CONDITIONS Temperature increases with height
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ATM OCN 100 Summer 2002 83 ISOTHERMAL CONDITIONS Temperature remains constant with height
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ATM OCN 100 Summer 2002 84 RADIOSONDE LOCATIONS
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ATM OCN 100 Summer 2002 85 GREEN BAY RADIOSONDE SOUNDING TUES AM
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ATM OCN 100 Summer 2002 86 TALAHASSEE RADIOSONDE SOUNDING TUES AM
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ATM OCN 100 Summer 2002 87 U.S. STANDARD ATMOSPHERE See Fig. 1.9 Moran & Morgan (1997)
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ATM OCN 100 Summer 2002 88 VERTICAL TEMPERATURE VARIATIONS (con’t.) The temperature spheres See Fig. 1.9 Moran & Morgan (1997) Troposphere Stratosphere Mesosphere Thermosphere Tropopause Stratopause Mesopause
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ATM OCN 100 Summer 2002 89 U.S. STANDARD ATMOSPHERE See Fig. 1.9 Moran & Morgan (1997) Troposphere Stratosphere Mesosphere Thermosphere
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ATM OCN 100 Summer 2002 90 VERTICAL TEMPERATURE VARIATIONS (con’t.) u The Standard Reference Atmosphere – The Temperature “Spheres” – The boundaries or “pauses” u Reasons for vertical temperature structure u Implications of vertical temperature structure
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ATM OCN 100 Summer 2002 91 8 ppmv = 0.0008%
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ATM OCN 100 Summer 2002 92 VERTICAL TEMPERATURE VARIATIONS (con’t.) u The Temperature Spheres – Troposphere – Stratosphere – Mesosphere – Thermosphere
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ATM OCN 100 Summer 2002 93 VERTICAL TEMPERATURE VARIATIONS (con’t.) u The Standard Reference Atmosphere – The Temperature “Spheres” – The boundaries or “pauses”
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ATM OCN 100 Summer 2002 94 U.S. STANDARD ATMOSPHERE See Fig. 1.9 Moran & Morgan (1997) Troposphere Stratosphere Mesosphere Thermosphere Tropopause Stratopause Mesopause
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ATM OCN 100 Summer 2002 95 VERTICAL TEMPERATURE VARIATIONS (con’t.) u The Standard Reference Atmosphere – The Temperature “Spheres” – The boundaries or “pauses” u Reasons for vertical temperature structure u Implications of vertical temperature structure
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ATM OCN 100 Summer 2002 96 U.S. STANDARD ATMOSPHERE See Fig. 1.9 Moran & Morgan (1997) Troposphere Stratosphere Mesosphere Thermosphere Tropopause Stratopause Mesopause
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ATM OCN 100 Summer 2002 97 RADIOSONDE LOCATIONS
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ATM OCN 100 Summer 2002 98 GREEN BAY RADIOSONDE SOUNDING TUES AM
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ATM OCN 100 Summer 2002 99 TALAHASSEE RADIOSONDE SOUNDING TUES AM
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ATM OCN 100 Summer 2002 100 GREEN BAY RADIOSONDE SOUNDING Monday PM
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ATM OCN 100 Summer 2002 101 GREEN BAY RADIOSONDE SOUNDING Tuesday AM
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ATM OCN 100 Summer 2002 102 ANCHORAGE RADIOSONDE SOUNDING Monday PM
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106 See Fig. 19.9 Moran & Morgan (1997)
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ATM OCN 100 Summer 2002 107 See Fig. 19.9 Moran & Morgan (1997)
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