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OCN 5401 Chapter 3 Heat Transfer Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453
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Heat Flux (W·m -2 = J·s -1 ·m -2 ) Q s – radiation from the sun Q b – back radiation from Earth Q e – evaporative heat loss or gain Q h – sensible heat loss or gain Q v – advective heat loss or gain Q t = Q s – Q b – Q e – Q h – Q v James Prescott Joule, FRS
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Radiation Paths reflected refracted absorbed scattered transmitted V1V1 V2V2 Index of Refraction (η 2 /η 1 ) = V 1 /V 2 η water-air = 1.333 (at 20°C) irradiance Willebrord Snell
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Solar Spectrum Max Planck
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C SUN : What is the solar constant? where If T SUN = 5775K, C SUN = ? Distributed solar irradiance at top of atmosphere (MJ/m 2 /day) Solar irradiance
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The solar constant isn’t constant! SOHO UV images of 11 year solar cycle Note the sunspots
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Albedo
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Distribution of Water and Land Solar Heating Inflow = Outflow C SUN (1-A)πr 2 = 4πr 2 σT 4 If A=0.3 and C SUN =1367 W·m -2, what is T=?
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Earth’s mean temperature balance requires an extra term Q GHE : What is the greenhouse effect? T Earth : What is Earth’s temperature? A: Is Earth’s albedo fixed?
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How would Earth’s temperature change if the albedo changed from 30% to 29%? minus If T EARTH(A=30%) = 288K, T EARTH(A=29%) = ?
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Relative Humidity (RH) and Saturation Vapor Pressure (e s ) Example: RH = ? T air = 30°; T dew point = 10° e s = 39 mb; e air = 12 mb
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Evaporation from the Sea Surface Q e = ρ water E·L Evaporation (E) is in meters per second, and latent heat of evaporation (L) is L= 2495 x 10 3 J·kg -1 Evaporation minus precipitation in millimeters per day
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Seasonal Thermocline and Mixed-Layer Depth
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Earth Remote Sensing
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Passive Microwave Remote Sensing SSM/I – Special Sensor Microwave Imager microwave brightness temperatures at 19.35, 22.2, 37.0, and 85.5 GHz
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Sea Ice Variability
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Sea level from satellite altimetry (active microwave sensing)
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Infrared Satellite Imagery Infrared Image
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Upper few millimeters of the sea surface
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Sea Surface Temperature (SST) Skin Temperature and Bulk Temperature
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OCN 5401 Questions? Chapter 3
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