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Measurement and simulation of mid‐ and far‐infrared spectra in the presence of cirrus
52
Citations
29
References
2010
Year
EngineeringAtmospheric SoundingClimate ModelingAbsorption SpectroscopyInfrared Window RegionOptical PropertiesAtmospheric ScienceInfrared OpticThermal Infrared Remote SensingAtmospheric SensingMeteorologyIce CloudPhysicsInfrared TechnologyInfrared SpectroscopyRadiation MeasurementCloud PhysicInput UncertaintiesNear-infrared SpectroscopyRadiometryClimate DynamicsAtmospheric RadiationInfrared SensorNatural SciencesSpectroscopyRemote SensingSatellite MeteorologyInfrared Systems
Abstract Observed far‐infrared and mid‐infrared radiance spectra measured in situ above cirrus with both the Tropospheric Airborne Fourier Transform Spectrometer (TAFTS) and the Airborne Research Interferometer Evaluation System (ARIES) are presented. Two sets of upwelling spectra between wavenumbers 100 and 1415cm −1 taken over ice cloud of visible optical thickness 0.1 and 0.3 are shown. These observations address the need for more measurements of radiance from cirrus, particularly in the far infrared, where experimental data are lacking. A test of consistency in modelling in both the far infrared and mid infrared is performed by fitting a model calculation of radiances in the infrared window region, and comparing with the measured radiances. In this consistency check, the sampling of the surrounding atmosphere and the cloud is given extensive consideration. The model was not able to consistently reproduce the observed radiance across the entire region, and was particularly poor in the 330–600cm −1 region of the far infrared. Possible causes are thought to be primarily model input uncertainties arising from inadequate sampling of cloud and atmosphere. Copyright © 2010 Royal Meteorological Society and Crown Copyright.
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