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Blackbody Radiation/ Planetary Energy Balance

Blackbody Radiation/ Planetary Energy Balance

Blackbody Radiation/ Planetary Energy Balance. *Electromagnetic Spectrum *Blackbody radiation – temperature *Sun’s heat at the earth *Earth’s blackbody radiation to space *Planetary radiation temperature of Earth *Surface temperature of Earth. 1000. 100. 10. 1. 0.1. 0.01.

By alina
(166 views)


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BASIC RADIATIVE TRANSFER

BASIC RADIATIVE TRANSFER

BASIC RADIATIVE TRANSFER. RADIATION & BLACKBODIES. Radiation Flux (F)  [W/m 2 ] Intensity (I)  [W/m 2 /sr] Monochromatic Intensity (I l )  [W/m 2 /sr/nm]. Objects that absorb 100% of incoming radiation are called blackbodies

By love (219 views)

Atmospheric Radiative Transfer

Atmospheric Radiative Transfer

PHYS 721. http://userpages.umbc.edu/~martins/PHYS721/. Atmospheric Radiative Transfer. Motivation, applications and issues Definitions and Radiation Quantities Thermal Emission/Absorption Basics Solar and Terrestrial Spectra From Single to Multiple Scattering

By mkenyon (0 views)

Radiative Transfer Simulations

Radiative Transfer Simulations

The Proximity Effect of LBGs:. Radiative Transfer Simulations. Antonella Maselli, OAArcetri, Firenze, Italy Collaborators: A.Ferrara, M. Bruscoli, S. Marri & R. Schneider. Marri et al 2003, in preparation Bruscoli et al, 2003,MNRAS,343,L45 Maselli et al, 2003,submitted to MNRAS.

By sakura (102 views)

RADIATIVE HEAT TRANSFER

RADIATIVE HEAT TRANSFER

RADIATIVE HEAT TRANSFER. Thermal radiation is the electromagnetic radiation emitted by a body as a result of its temperature. There are many types of electromagnetic radiation; thermal is only one of them. It propagated at the speed of light, 3×10 8 m/s.

By rian (206 views)

Introduction to radiative transfer

Introduction to radiative transfer

Introduction to radiative transfer. Robert Hudson. Electromagnetic spectrum. Schematic of a wave. WAVELENGTH. DISTANCE BETWEEN SUCCESSIVE PEAKS GIVEN THE SYMBOL λ MANY UNITS USED : (A) MICRON, 10 -6 METERS (B) NANOMETER, 10 -9 METERS (C) ANGSTROM, 10 -10 METERS. FREQUENCY.

By brandy (139 views)

Chapter  6 Radiative Transfer

Chapter 6 Radiative Transfer

Chapter 6 Radiative Transfer. Radiative Transfer.

By ekeifer (0 views)

Lecture 3 Radiative Transfer

Lecture 3 Radiative Transfer

Lecture 3 Radiative Transfer. Lower Solar Atmosphere has two layers: Photosphere - 100 km thick; opaque Chromosphere - 10,000 km thick; optically thin; cooler. (I) Local Thermodynamic Equilibrium Equation of Transfer: Optical Depth. Thermodynamic Equilibrium

By csilla (191 views)

Introduction to radiative transfer

Introduction to radiative transfer

By vesna (86 views)

Radiative Transfer – An Overview

Radiative Transfer – An Overview

Radiative Transfer – An Overview. Acknowledgements. http://cimss.ssec.wisc.edu/goes/comet/radiative_transfer.html www.weatherchaos.umd.edu/class-presentations/Hudson_Intro_rad_trans.ppt http://timeforchange.org/radiation-wavelength-and-greenhouse-effect. Outline. What is radiative transfer?

By buckminster-ward (161 views)

Radiative Transfer Model Vijay Natraj

Radiative Transfer Model Vijay Natraj

Radiative Transfer Model Vijay Natraj. Why RADIANT?. The optical depth sensitivity of doubling The necessity of re-computing the entire RT solution if using a code such as DISORT if only a portion of the atmosphere changes

By anastasia-hero (115 views)