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MOPITT Averaging Kernels

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Page 1: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

MOPITT Averaging Kernels

Page 2: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

Eigenvectors of Averaging Kernel Matrix

Page 3: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

Smoothing Effects of the Averaging Kernel

Page 4: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

Error Analysis for TES CO Retrievals

Page 5: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

Error Analysis for TES O3 Retrievals

Page 6: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

Terrestrial Radiation Spectrum From Space!

Composite of blackbody radiation spectra for different T

Sahara

Mediterranean

Antarctica

surface!

troposphere stratosphere

Atmospheric T profile

Trop.

Strat.

Meso.

Page 7: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

10 km

30 km

15 µm CO2 Absorption Band

[Wallace and Hobbs, 2006]

Page 8: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance

Tropospheric Emission Spectrometer (TES) CO2Red arrow indicates the change in radiance at 710 cm-1 due to change in CO2 at 10 km

• The 2 band between 680-725 cm-1 is sensitive mainly to CO2 in the upper troposphere and lower stratosphere

• The radiance in the spectral regions 970-990 and 1070-1110 cm-1 is sensitive to changes in CO2 in the middle and lower troposphere

[Kulawik et al., ACP, 2010]

Page 9: MOPITT Averaging Kernels - atmosp.physics.utoronto.cadbj/PHY2506/lectures11-12_slide… · Tropospheric Emission Spectrometer (TES) CO2 Red arrow indicates the change in radiance