Thermal IR February 23, 2005 Emissivity Kirchoff’s Law Thermal Inertia, Thermal Capacity, and Thermal Conductivity Review for Midterm Reminder: Midterm Exam on Monday! Review sheet is posted. Thermal IR (cont’d)

Emissivity No objects in the world are true blackbodies; rather, they are selectively radiating bodies. Emissivity (є) is the ratio between the radiant flux exiting a real world selective radiating body (M r ) and a blackbody at the same temperature (M b ) A graybody outputs a constant emissivity that is less than one at all wavelengths Emissivity

All selectively radiating bodies have emissivities ranging from 0 to <1 that fluctuate depending upon the wavelengths of energy being considered. A graybody outputs a constant emissivity that is less than one at all wavelengths.  Some materials like distilled water have emissivities close to one (0.99) over the wavelength interval from  m. Others such as polished aluminum (0.08) and stainless steel (0.16) have very low emissivities. All selectively radiating bodies have emissivities ranging from 0 to <1 that fluctuate depending upon the wavelengths of energy being considered. A graybody outputs a constant emissivity that is less than one at all wavelengths.  Some materials like distilled water have emissivities close to one (0.99) over the wavelength interval from  m. Others such as polished aluminum (0.08) and stainless steel (0.16) have very low emissivities. EmissivityEmissivity

Spectral emissivity of a blackbody, a graybody, and a hypothetical selective radiator 2x reduction Spectral radiant exitance distribution of the blackbody, graybody, and hypothetical selective radiator Spectral Emissivity, e Spectral Radiant Exitance W m -2 um -1

Two rocks lying next to one another on the ground could have the same true kinetic temperature but have different apparent temperatures when sensed by a thermal radiometer simply because their emissivities are different. The emissivity of an object may be influenced by a number factors, including: color surface roughness moisture content wavelength viewing angle Two rocks lying next to one another on the ground could have the same true kinetic temperature but have different apparent temperatures when sensed by a thermal radiometer simply because their emissivities are different. The emissivity of an object may be influenced by a number factors, including: color surface roughness moisture content wavelength viewing angle EmissivityEmissivity

Emissivity Water, distilled0.99 Asphalt0.95 Vegetation0.96 to 0.98 Snow0.83 to 0.85 Concrete0.71 to 0.90 Stainless Steel0.16 Aluminum0.05 to 0.08 * From Table 8-1 (p. 258) Emissivity of Selected Materials

The Russian physicist Kirchhoff found that in the infrared portion of the spectrum the spectral emissivity of an object generally equals its spectral absorptance, i.e.  ~ . This is often phrased as: The Russian physicist Kirchhoff found that in the infrared portion of the spectrum the spectral emissivity of an object generally equals its spectral absorptance, i.e.  ~ . This is often phrased as: “good absorbers are good emitters and “good absorbers are good emitters and good reflectors are poor emitters”. good reflectors are poor emitters”. The Russian physicist Kirchhoff found that in the infrared portion of the spectrum the spectral emissivity of an object generally equals its spectral absorptance, i.e.  ~ . This is often phrased as: The Russian physicist Kirchhoff found that in the infrared portion of the spectrum the spectral emissivity of an object generally equals its spectral absorptance, i.e.  ~ . This is often phrased as: “good absorbers are good emitters and “good absorbers are good emitters and good reflectors are poor emitters”. good reflectors are poor emitters”. Kirchoff’s Radiation Law

Thermal capacity (c) is the ability of a material to store heat. It is measured as the number of calories required to raise a gram of material (e.g. water) 1 ˚C (cal g -1 ˚C -1 ). Thermal capacity (c) is the ability of a material to store heat. It is measured as the number of calories required to raise a gram of material (e.g. water) 1 ˚C (cal g -1 ˚C -1 ). Thermal conductivity (K) is the rate that heat will pass through a material and is measured as the number of calories that will pass through a 1-cm cube of material in 1 second when two opposite faces are maintained at 1 ˚C difference in temperature (cal cm -1 sec -1 ˚C). Thermal conductivity (K) is the rate that heat will pass through a material and is measured as the number of calories that will pass through a 1-cm cube of material in 1 second when two opposite faces are maintained at 1 ˚C difference in temperature (cal cm -1 sec -1 ˚C). Thermal capacity (c) is the ability of a material to store heat. It is measured as the number of calories required to raise a gram of material (e.g. water) 1 ˚C (cal g -1 ˚C -1 ). Thermal capacity (c) is the ability of a material to store heat. It is measured as the number of calories required to raise a gram of material (e.g. water) 1 ˚C (cal g -1 ˚C -1 ). Thermal conductivity (K) is the rate that heat will pass through a material and is measured as the number of calories that will pass through a 1-cm cube of material in 1 second when two opposite faces are maintained at 1 ˚C difference in temperature (cal cm -1 sec -1 ˚C). Thermal conductivity (K) is the rate that heat will pass through a material and is measured as the number of calories that will pass through a 1-cm cube of material in 1 second when two opposite faces are maintained at 1 ˚C difference in temperature (cal cm -1 sec -1 ˚C). Thermal Properties of Terrain

Thermal inertia (P) is a measurement of the thermal response of a material to temperature changes and is measured in calories per square centimeter per second square root per degree Celsius (cal cm -2 sec -1/2 ˚C -1 ). Thermal inertia is computed using the equation: Thermal inertia (P) is a measurement of the thermal response of a material to temperature changes and is measured in calories per square centimeter per second square root per degree Celsius (cal cm -2 sec -1/2 ˚C -1 ). Thermal inertia is computed using the equation: P = (K x p x c) 1/2 where K is thermal conductivity, p is density (g cm -3 ), and c is thermal capacity. Density is the most important property in this equation because thermal inertia generally increases linearly with increasing material density. Thermal inertia (P) is a measurement of the thermal response of a material to temperature changes and is measured in calories per square centimeter per second square root per degree Celsius (cal cm -2 sec -1/2 ˚C -1 ). Thermal inertia is computed using the equation: Thermal inertia (P) is a measurement of the thermal response of a material to temperature changes and is measured in calories per square centimeter per second square root per degree Celsius (cal cm -2 sec -1/2 ˚C -1 ). Thermal inertia is computed using the equation: P = (K x p x c) 1/2 where K is thermal conductivity, p is density (g cm -3 ), and c is thermal capacity. Density is the most important property in this equation because thermal inertia generally increases linearly with increasing material density. Thermal Inertia

There is an inverse relationship between having high spatial resolution and high radiometric resolution when collecting thermal infrared data. Thermal Infrared Remote Sensing