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ATMOSPHERIC TEMPERATURE SOUNDING

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ATMOSPHERIC TEMPERATURE SOUNDING. If radiation is selected in a sounding channel for which. and we define a function K(z) =. - PowerPoint PPT Presentation
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dz dz d z T B L 0 ) ( )) ( , ( ) ( ATMOSPHERIC TEMPERATURE SOUNDING iation is selected in a sounding channel for which we define a function K(z) = dz d When the primary absorber is a well mixed gas (e.g. oxygen or CO 2 ) with known concentration it can be seen that the measured radiance is essentially a weighted average of the atmospheric temperature profile, or dz z K z T B L 0 ) ( )) ( , ( ) ( unction K(z) that defines this vertical average is known as a TING FUNCTION
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Page 1: ATMOSPHERIC TEMPERATURE SOUNDING

dzdz

dzTBL

0

)())(,()(

ATMOSPHERIC TEMPERATURE SOUNDING

If radiation is selected in a sounding channel for which

and we define a function K(z) =

dz

d

When the primary absorber is a well mixed gas (e.g. oxygen or CO2) with known concentration it can be seen that the measured radiance is essentially a weighted average of the atmospheric temperature profile, or

dzzKzTBL

0

)())(,()(

The function K(z) that defines this vertical average is known as a

WEIGHTING FUNCTION

Page 2: ATMOSPHERIC TEMPERATURE SOUNDING

CO2slicing: weighting functions

Bands w/greater CO2 absorptionhave weighting functions more

sensitive to high clouds

S. Platnick, ISSAOS ‘02Example spectra (~ 12.65-14 µm)

MODIS CO2 band weighting functions

1000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

321000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

32

Page 3: ATMOSPHERIC TEMPERATURE SOUNDING

BT in and out of clouds for MODIS CO2 bands

S. Platnick, ISSAOS ‘02

1000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

321000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

32

Page 4: ATMOSPHERIC TEMPERATURE SOUNDING
Page 5: ATMOSPHERIC TEMPERATURE SOUNDING

CO2slicing: weighting functions

Bands w/greater CO2 absorptionhave weighting functions more

sensitive to high clouds

S. Platnick, ISSAOS ‘02Example spectra (~ 12.65-14 µm)

MODIS CO2 band weighting functions

1000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

321000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

32

Page 6: ATMOSPHERIC TEMPERATURE SOUNDING

ρ1,T1,P1

Cross section [m2]

ρ2,T2,P2

>

ρ3,T3,P3

>

ρ4,T4,P4

>ρ5,T5,P5

>

Page 7: ATMOSPHERIC TEMPERATURE SOUNDING
Page 8: ATMOSPHERIC TEMPERATURE SOUNDING

CO2slicing: weighting functions

Bands w/greater CO2 absorptionhave weighting functions more

sensitive to high clouds

S. Platnick, ISSAOS ‘02Example spectra (~ 12.65-14 µm)

MODIS CO2 band weighting functions

1000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

321000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

32

Page 9: ATMOSPHERIC TEMPERATURE SOUNDING
Page 10: ATMOSPHERIC TEMPERATURE SOUNDING

CO2slicing: weighting functions

Bands w/greater CO2 absorptionhave weighting functions more

sensitive to high clouds

S. Platnick, ISSAOS ‘02Example spectra (~ 12.65-14 µm)

MODIS CO2 band weighting functions

1000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

321000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

32

Page 11: ATMOSPHERIC TEMPERATURE SOUNDING
Page 12: ATMOSPHERIC TEMPERATURE SOUNDING

CO2slicing: weighting functions

Bands w/greater CO2 absorptionhave weighting functions more

sensitive to high clouds

S. Platnick, ISSAOS ‘02Example spectra (~ 12.65-14 µm)

MODIS CO2 band weighting functions

1000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

321000

100

10

0.0 0.2 0.4 0.6 0.8 1.0

Pre

ssu

re (

mb

)

Weighting Function dt(,p)/d ln p

Channel 32 33 34 35 36

Central Wavelength (µm)

12.020 13.335 13.635 13.935 14.235

36

1.2

35

34

33

32

Page 13: ATMOSPHERIC TEMPERATURE SOUNDING
Page 14: ATMOSPHERIC TEMPERATURE SOUNDING

INSTABILITY INDICES

Page 15: ATMOSPHERIC TEMPERATURE SOUNDING

MSG Lifted Index

Page 16: ATMOSPHERIC TEMPERATURE SOUNDING
Page 17: ATMOSPHERIC TEMPERATURE SOUNDING

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